CHAPTER XXI

AUTOMATIC DOSING DEVICES

283. Types. 284. Operation. 285. Three Alternating Siphons.

286. Four or More Alternating Siphons. 287. Timed Siphons.

288. Multiple Alternating and Timed Siphons. 506–512

SEWERAGE AND SEWAGE TREATMENT

CHAPTER I

INTRODUCTION

=1. Sewerage and the Sanitary Engineer.=—Present day conceptions of

sanitation are based on the scientific discoveries which have resulted

so much in the increased comfort and safety of human life during the

past century, in the increase of our material possessions, and the

extent of our knowledge. The danger to health in the accumulation of

filth, the spreading of disease by various agents, the germ theory of

disease, and other important principles of sanitation can be counted

among the more recent scientific discoveries and pronouncements.

Experience has shown, and continues to show, that the increase of

population may be inhibited by accumulations of human waste in populous

districts. The removal of these wastes is therefore essential to the

existence of our modern cities.

The greatest need of a modern city is its water supply. Without it city

life would be impossible. The next most important need is the removal of

waste matters, particularly wastes containing human excreta or the germs

of disease. To exist without street lights, pavements, street cars,

telephones, and the many other attributes of modern city life might be

possible, although uncomfortable. To exist in a large city without

either water or sewerage would be impossible. The service rendered by

the sanitary engineer to the large municipality is indispensable. In

addition to the service necessary to the maintenance of life in large

cities, the sanitary engineer serves the smaller city, the rural

community, the isolated institution, and the private estate with

sanitary conveniences which make possible comfortable existence in them,

and which are frequently considered as of paramount necessity. Training

for service in municipal sanitation is training for a service which has

a more direct beneficial effect on humanity than any other engineering

work, or any other profession. W. P. Gerhard states:

_A Sanitary Engineer_ is an engineer who carries out those works

of civil engineering which have for their object:

(_a_) The promotion of the public and individual health;

(_b_) The remedying of insanitary conditions;

(_c_) The prevention of epidemic diseases.

A well-educated sanitary engineer should have a thorough knowledge

of general civil engineering, of architecture, and of sanitary

science. The practice of the sanitary engineer embraces water

supply, sewerage, and sewage and garbage disposal for cities and

for single buildings; the prevention of river pollution, the

improvement of polluted water supplies; street paving and street

cleaning, municipal sanitation, city improvement plans, the laying

out of cities, the preparation of sanitary surveys, the regulation

of noxious trades, disinfection, cremation, and the sanitation of

buildings.

The need of the work of the sanitary engineer in the provision of sewers

and drains is thrust upon us in our daily experience by the clogging of

sewers, the flooding of streets by heavy rains, filthy conditions in

unsewered districts, increased values of property and improved

conditions of living in sewered districts, and in many other ways. The

increasing demand for sewerage and the amount of money expended on sewer

construction is indicated by the information given in Table I.

=2. Historical.=—An ordinance passed by the Roman Senate in the name of

the Emperor about A.D. 80, states:

I desire that nobody shall conduct away any excess water without

having received my permission or that of my representatives; for

it is necessary that a part of the supply flowing from the

delivery tanks shall be utilized not only for cleaning our city,

but also for flushing the sewers.[1]

Neither the sewers mentioned nor the distributing pipes of the public

water supply were connected to individual residences. The contributions

to the sewers came from the ground and the street surface. The streets

were the receptacles of liquid and solid wastes and were often little

more than open sewers. A promenade after dark in an ancient, medieval,

or early modern city was accompanied not only by the underfoot dangers

of an uneven pavement or an encounter with a footpad, but with the

overhead danger from the emptying of slops into the streets from the

upper windows. Sewers were used for the collection of surface water; the

discharge of fecal matter into them was prohibited. The problem of the

collection of sewage remained unsolved until the Nineteenth Century.

TABLE 1

POPULATION TRIBUTARY TO SEWERAGE SYSTEMS

──────────────────────────────────────┬──────────┬──────────┬──────────

│ 1905[2] │ 1915[3] │ 1920[4]

──────────────────────────────────────┼──────────┼──────────┼──────────

Population discharging raw sewage into│ │ │

the sea or tidal estuaries │ 6,500,000│ 8,500,000│

Population discharging raw sewage into│ │ │

inland streams or lakes │20,400,000│26,400,000│

Population connected to systems where │ │ │

sewage is treated in some way │ 1,100,000│ 6,900,000│

Population connected with sewerage │ │ │

systems │28,000,000│41,800,000│46,300,000

──────────────────────────────────────┴──────────┴──────────┴──────────

The development of the London sewers was commenced early in the

Nineteenth Century. The sewerage system of Hamburg, Germany, was laid

out in 1842 by Lindley, an English engineer who with other English

engineers performed similar work in other German cities because of their

earlier experience in English communities. Berlin’s present system dates

from 1860. The construction of storm-water drains in Paris dates from

1663.[5] They were intended only as street drains but are now included

in the comprehensive system of the city. The first comprehensive

sewerage system in the United States was designed by E. S. Chesbrough

for the City of Chicago in 1855. Previous to this time sewers had been

installed in an indifferent manner and without definite plan. The

installation of a comprehensive sewerage system in Baltimore in 1915

marks the completion of installation of sewerage systems in all large

American cities.

In the early days of sewerage design it was considered unsafe to

discharge domestic wastes into the sewers as the concentration of so

much sewage was expected to create great nuisances and dangers to

health. That the fear that the concentration of large quantities of

sewage would create a nuisance was not ill founded is proven by the

conditions on the Thames at London in 1858–59. Dr. Budd states:[6]

For the first time in the history of man, the sewage of nearly

three millions of people had been brought to seethe and ferment

under a burning sun in one vast open _cloaca_ lying in their

midst.

The result we all know. Stench so foul we may well believe had

never before ascended to pollute this lower air. Never before at

least had a stink risen to the height of an historic event.... For

months together the topic almost monopolized the public prints....

‘India is in revolt and the Thames stinks’ were the two great

facts coupled together by a distinguished foreign writer, to mark

the climax of a national humiliation.[7]

The problem of sewage disposal followed the more or less successful

solutions of the problem of sewage collection. In England the British

Royal Commission on Sewage Disposal was appointed in 1857 and issued its

first report in 1865. The first studies in the United States were

started in 1887 by the establishment of an experiment station at

Lawrence, Massachusetts, where valuable work has been done. The station

is under the State Board of Health, which issued its first report

containing the results of the work at the station, in 1890.

Various methods of sewage treatment preparatory to disposal have been

devised from time to time. Some have fallen into disuse, such as the A.

B. C. (alum, blood and clay) process, and others have taken a permanent

place, such as the septic tank. The unsolved problems of sewage

collection, and the number of persons still unserved by sewerage and

sewage disposal opens a wide field to the study and construction of

sewerage works.

=3. Methods of Collection.=—The method of collection which involves the

removal of night soil from a privy vault, the pail system which involves

the collection of buckets of human excreta from closets and homes,

indoor chemical closets, and other makeshift methods of collection are

of extreme importance where no sewers exist, but they are not properly

considered as sewerage systems or sewerage works. These methods of

collection are generally confined to rural districts and to outlying

parts of urban communities. They require constant attention for their

proper conduct and little skill for their installation, the principal

requirements being to make the receptacles fly-proof.

The pneumatic system was introduced by Liernur, a Dutch engineer.[8] It

is used in parts of a few cities in Europe, but it is not capable of use

on a large scale. It consists of a system of air-tight pipes, connecting

water closets, kitchen sinks, etc., with a central pumping station at

which an air-tight tank is provided from which the air is partly

exhausted. As little water as possible is allowed to mix with the fecal

matter and other wastes in order not to overtax the system. Solid and

liquid wastes are drawn to the central station when the waste valve on

the plumbing fixture is opened.

The collection of sewage in a system of pipes through which it is

conducted by the buoyant effect and scouring velocity of water is known

as the water-carriage system. This is the only method of sewage

collection in general use in urban communities. In this system solid and

liquid wastes are so highly diluted with water as either to float or to

be suspended therein. The mixture resulting from this high dilution

follows the laws of hydraulics as applied to pure water, or water

containing suspended matter. It will flow freely through properly

designed conduits and will concentrate the sewage wastes at the point of

ultimate disposal.

=4. Methods of Disposal.=—Sewage is disposed of by dilution in water, by

treatment on land, or occasionally by discharging it into channels that

contain no diluting water. Some form of treatment to prepare sewage for

ultimate disposal is frequently necessary and will undoubtedly be

required in a comparatively short time for all sewage discharged into

watercourses. The solid matters removed by treatment may be buried,

burned, dumped into water, or used as a fertilizer.

If the volume of diluting water, or the area and character of land used

for disposal are not as they should be, a nuisance will be created. The

aim of all methods of sewage treatment has so far been to produce an

effluent which could be disposed of without nuisance and in certain

exceptional cases to protect public water supplies from pollution.

Financial returns have been sought only as a secondary consideration. A

few sewage farms and irrigation projects might be considered as

exceptions to this as the value of the water in the sewage as an

irrigant has been the primary incentive to the promotion of the farm.

It is to be remembered that since the aim of all sewage treatment is to

produce an effluent that can be disposed of without causing a nuisance,

the simplest process by which this result can be attained under the

conditions presented is the process to be adopted. No attempt is made to

_purify_ sewage completely, or on a practical scale to make drinking

water.

=5. Methods of Treatment.=—Screening and sedimentation are the primary

methods for the treatment of sewage. By these methods a portion of the

floating and settleable solids are removed, preventing the formation of

unsightly scum and putrefying sludge banks. Chemicals are sometimes

added to the sewage to form a heavy flocculent precipitate which hastens

sedimentation of the solid matters in the sewage. The process in these

methods is mechanical and the solid matters removed from the sewage must

be disposed of by other methods than dilution with the sewage effluent.

More complete methods of treatment are dependent on biologic action.

Under these methods of treatment complete stabilization of the effluent

is approached, and in the most complete treatment an effluent is

produced which is clear, sparkling, non-odorous, non-putrescible, and

sterile. Sterilization of sewage, usually with chlorine or some of its

compounds, has been used, not to reduce the amount of diluting water

necessary, but to reduce the number of pathogenic germs and to minimize

the danger of the transmission of disease.

=6. Definitions.=—Sewage and sewerage are not synonymous terms although

frequently confused. Sewage is the spent water supply of a community

containing the waste from domestic, industrial or commercial use, and

such surface and ground water as may enter the sewer.[9] Sewerage is the

name of the system of conduits and appurtenances designed to carry off

the sewage. It is also used to indicate anything pertaining to sewers.

A difference is made between sanitary sewage, storm sewage, and

industrial wastes. Sanitary sewage, sometimes called domestic sewage, is

the liquid wastes discharged from residences or institutions, and

contains water closet, laundry and kitchen wastes. Storm sewage is the

surface run-off which reaches the sewers during and immediately after a

storm. Industrial wastes are the liquid waste products discharged from

industrial plants.

A sewer is a conduit used for conveying sewage.

The names of the conduits through which sewage may flow are:

_Soil Stack._—A vertical pipe in a building through which waste water

containing fecal matter or urine is allowed to flow.

_Waste Pipe._—A vertical pipe in a building through which waste water

containing no fecal matter is allowed to flow.

_House Drain._—The approximately horizontal portion of a house drainage

system which conveys the drainage from the soil stack or waste pipe to

the point of discharge from the building.

_House Sewer._—The pipe which leads from the outside wall of the

building to the sewer in the street.

_Lateral Sewer._—The smallest branch in a sewerage system, exclusive of

the house sewers.

_Sub-main or Branch Sewer._—A sewer from which the sewage from two or

more laterals is discharged.[10]

_Main or Trunk Sewer._—A sewer into which the sewage from two or more

sub-main or branch sewers is discharged.[11]

_Intercepting Sewer._—A sewer generally laid transversely to a sewerage

system to intercept some portion or all of the sewage collected by the

system.

_Relief Sewer._—A sewer intended to carry a portion of the flow from a

district already provided with sewers of insufficient capacity and thus

preventing overtaxing the latter.[12]

_Outfall Sewer._—That portion of a main or trunk sewer below all

branches.

_Flushing Sewer._—A conduit through which water is conveyed for flushing

portions of a sewerage system.

_Force Main._—A conduit through which sewage is pumped under pressure.

CHAPTER II

WORK PRELIMINARY TO DESIGN

=7. Division of Work.=—Engineering work on sewerage can be divided into

four parts, namely: preliminary, design, construction and maintenance.

An engineer may be engaged during any one or all of these periods on the

same sewerage system, and should therefore be acquainted with his duties

during each period.

=8. Preliminary.=—The demand for sewerage normally follows the

installation or extension of the public water supply. It may be caused

by: a lack of drainage on some otherwise desirable tract of real estate;

from a public realization of unpleasant or unhealthful conditions in a

built-up district; or through the realization by the municipal

administration of the necessity for caring for the future. In whatever

way the demand may be created the engineer should take an active part in

the promotion of the work.

The engineer’s duties during the preliminary period are: to make a study

of the possible methods by which the demand for sewerage can be

satisfied; to present the results of this study in the form of a report

to the committee or organization responsible for the promotion of the

work; and so to familiarize himself with the conditions affecting the

installation of the proposed plans as to be able to answer all inquiries

concerning them. This work will require the general qualities of

character, judgment, efficiency and the understanding of men in

addressing interested persons individually and collectively on the

features of the proposed plans, and the exercise of engineering

technique in the survey and the drawing of the plans. The engineer

should assure himself that all legal requirements in the drawing of

petitions, advertising, permits, etc., have been complied with. This

requires some knowledge of national, state, and local laws. Although

none the less essential their description is not within the scope of

this book.

The engineer’s preliminary report should contain a section devoted to

the feasibility of one or more plans which may be explained in more or

less detail with a statement of the cost and advantages of each. A

conclusion should be reached as to the most desirable plan and a

recommendation made that this plan be installed. Other sections of the

report may be devoted to a history of the growing demand, a description

of the conditions necessitating sewerage, possible methods of financing,

and such other subjects as may be pertinent. The making of the

preliminary plan and the design of sewerage works are described in

subsequent chapters.

=9. Estimate of Cost.=—In making an estimate of cost the information

should be presented in a readable and easily comprehended manner. It is

necessary that the items be clearly defined and that all items be

included. The method of determining the costs of doubtful items such as

depreciation, interest charges, labor, etc., and the probability of the

fluctuation of the costs of certain items should be explained.

The engineer’s estimate may be divided somewhat as follows:

Labor.

Material.

Overhead. This may include construction plant, office expense,

supervision, bond, interest on borrowed capital, insurance,

transportation, etc. The amount of the item is seldom less than 15

per cent and is usually over 20 per cent of the contract price.

Contingencies. This allowance is usually 10 to 15 per cent of the

contract price.

Profit. This should be from 5 to 10 per cent of the sum of the

four preceding items.

The contract price is the sum of these items. To this may be added:

Engineering. 2 to 5 per cent of the contract price.

Extra Work. Zero to 15 per cent of the contract price; dependent

on the character of the work, the completeness of the preliminary

information, the completeness of the plans, etc.

Legal expense.

Purchase of land, rights of way, etc., etc.

The cost of the sewer may be stated as so much per linear foot for

different sizes of pipe, including all appurtenances such as manholes,

catch-basins, etc., or the items may be separated in great detail

somewhat as follows:

Earth excavation, per cu. yd.

Rock excavation, per cu. yd.

Backfill, per cu. yd.

Brick manholes, 3 feet by 4 feet, per foot of depth.

Vitrified sewer pipe with cement joints, in place,

... inches in diameter, 0 to 6 feet deep

6 to 8 feet deep

8 to 10 feet deep

Repaving, macadam per sq. yd.

asphalt per sq. yd.

Flush-tanks, ... gal. capacity, per tank.

Service pipes to flush-tanks, per linear foot., etc., etc.

These methods represent the two extremes of presenting cost estimates.

Each method, or modification thereof, may have its use, dependent on

circumstances.

Reliable cost data are difficult to obtain. Lists of prices of materials

and labor are published in certain engineering and trade periodicals.

The Handbook of Cost Data by H. P. Gillette contains lists of the amount

of material and labor used on certain specific jobs and types of

construction. The price of labor and materials on the local market can

be obtained from the local Chamber of Commerce, contractors and other

employers of labor, and dealers in the desired commodities. Contract

prices for sewerage work published in the construction news sections of

engineering periodicals may be a guide to the judgment of the probable

cost of proposed work, but are generally dangerous to rely upon as full

details are lacking in the description of the work. A wide experience in

the collection and use of cost data is the desirable qualification for

making estimates of cost. It is possessed by few and is not an

infallible aid to the judgment.

Having completed the design and summary of the bills of material and

labor necessary for each structure or portion of the sewerage system,

the product of the unit cost and the amount of each item plus an

allowance for overhead will equal the cost of the item. The total cost

will be the sum of the costs of each item. The items should be so

grouped that the cost of the different portions of the system are

separated in order that the effect on the total cost resulting from

different combinations of items or the omission of any one item may be

readily computed.

A method for estimating the approximate cost of sewers, devised by W. G.

Kirchoffer[13] depends upon the use of the diagram shown in Fig. 2. The

factors for local conditions are shown in Table 2. For example, let it

be required to find the cost of a 15–inch vitrified pipe sewer at a

depth of 9 feet, if the unit costs of labor and material and the

conditions are the same as shown in Table 3.

[Illustration:

FIG. 2.—Diagram for Estimating the Cost of Sewers.

Eng. News, Vol. 76, p. 781.

]

_Solution_

First: To find the factor depending on local conditions, enter the

diagram at the 10–inch diameter and continue down until the

intersection with the depth of trench at 8.2 feet is found. Now go

diagonally parallel to lines running from left to right upwards to

the intersection with the vertical line through a cost of 45 cents

per foot. The diagonal line running from left to right downwards

through this intersection corresponds to a factor of about 11.

TABLE 2

FACTORS FOR COSTS OF SEWERS TO BE USED WITH FIGURE 2

────────────────────────────────────────────────────────────────┬──────

Character of Material │Factor

────────────────────────────────────────────────────────────────┼──────

Clay, gravel and boulders, Medford │22–26

Mostly sand, deep trenches sheeted. Wages medium. Richland │

Center. │21–22

Sandy clay. Wages medium. Labor conditions good at Kiel. │15–20

Sand. _Sandy_ clay, some water. Labor conditions good. Pipe │

prices medium at Manston. │14–20

Gravelly clay, ⅒th laid in concrete at Burlington. │13–22

Sandy clay, some water, sheeting at La Farge. │17–23

Sand with water. │ 20

Gravel and boulders. High wages. │ 26

Clay soil. Good digging. │ 17

Sandy clay. Some water. │ 23

Clay 2 miles inland. Laborers boarded at sanitarium, Wales │ 35

Clay, gravel and boulders at Plymouth. │20–27

Sand, clay and good digging at Lake Mills. │16–19

Red clay. Machine work at North Milwaukee. │20–24

Good digging. Wages medium at West Salem. │17–19

Sandy soil, bracing only required. No water. Wages and pipe │

medium. │ 14

Red sticky clay. │ 24

Good digging in any soil. Work scarce. │ 15

Red clay. No bracing. │ 20

Work inland from railroad. Boarding laborers _and_ other │

expenses. │ 35

────────────────────────────────────────────────────────────────┴──────

Second: To find the cost of 15–inch pipe at a depth of 9.0 feet,

enter the diagram at a diameter of 15 inches and continue down

until the intersection with a depth of trench at 9 feet is found.

Now go diagonally parallel to lines running from left to right

upwards to the intersection with the diagonal line running from

left to right downwards corresponding to the factor of 11 found

above. The vertical line passing through this point shows the cost

to be 67 cents per foot.

TABLE 3

COST OF SEWER CONSTRUCTION AT ATLANTIC, IOWA

(From Gillette’s Handbook of Cost Data)

Material: Clay, not difficult to spade and requiring little or no

bracing and practically no pumping. All hand work except backfill which

was done by team and scraper. Depth of trench averaged 8.2 feet; width

30 inches. Diameter of pipe 10 inches.

───────────────────────────────────────────────────────────┬─────┬─────

Item │Wage,│Cost,

│Cents│Cents

│ per │ per

│Hour │Foot.

───────────────────────────────────────────────────────────┼─────┼─────

Pipe. │ │0.20

Hauling team and driver. │ 30│ .003

Hauling. Man helping. │ 17│ .001

Cement and sand. │ │ .006

Pipe layers. │ 22│ .014

Pipe layer’s helper. │ 17│ .014

Trenching. Top men. │ 17│ .027

Trenching. Bottom men. │ 17│ .130

Trenching. Scaffold men. │ 17│ .002

Trenching. Bracing men. │ 17│ .002

Backfilling. Shovel. │ 17│ .010

Backfilling. Team and scraper. │ 30│ .008

Backfilling. Man and scraper. │ 17│ .005

Water boy. │ 10│ .006

Foreman. │ 30│ .022

───────────────────────────────────────────────────────────┼─────┼─────

Total. │ │ .450

───────────────────────────────────────────────────────────┴─────┴─────

METHODS OF FINANCING

The construction of sewerage works may be paid for by the issue of

municipal bonds, by special assessment, by funds available from the

general taxes, or by private enterprise.

=10. Bond Issues.=—A municipal bond is a promise by the municipality to

pay the face value of the bond to the holder at a certain specified

time, with interest at a stipulated rate during the interim. The

security on the bond is the taxable property in the municipality. The

legal restrictions thrown around municipal bond issues, the value of the

taxable property in the municipality, all of which may be used as

security for municipal bonds, and the fact that a municipality can be

sued in case of default, make municipal bonds desirable and provide a

good market for their sale. The funds available from a municipal bond

issue are limited by the amount that the legal limit is in excess of the

outstanding issues. The legal limit varies in different states from

about 5 to 15 per cent of the assessed value of the property in the

municipality. In some cases the amount available from municipal bonds

has been increased by forming a municipality within a municipality such

as a sanitary district, a park district, a drainage district, etc.,

which comprises a large portion or all of an existing municipal

corporation. This case is well illustrated in some parts of the City of

Chicago where the municipal taxing powers are shared by the City

government, the Sanitary District, and Park Commissioners. The right to

create a new municipal corporation must be granted by the state

legislature. Knowledge of fixed bonds, serial bonds, life of bonds,

sinking funds, etc. is an important part of an engineer’s education.[14]

Bond issues must usually be presented to the voters for approval at an

election. If approved, and other legal procedure has been followed, the

bonds may be bought by some of the many bonding houses, or by private

individuals, and the money is immediately available for construction.

The bonds are redeemed by general taxation spread over the period of the

issue.

=11. Special Assessment.=—A special assessment is levied against

property benefited directly by the structure being paid for. Special

assessments are used for the payment for the construction of lateral

sewers which are a direct benefit to separate districts but are without

general benefit to the city. In case the construction of an outfall

sewer or the erection of a treatment plant, which may be of some general

benefit, is necessary to care for a separate district, a part of the

expense may be borne by funds available from general taxation. The legal

procedure for the raising of funds by special assessment and the purpose

to which the funds so raised may be applied are stipulated in great

detail in different states and their directions must be followed

implicitly. Illinois procedure, which is similar to that in some other

states, is as follows: a meeting of the interested property owners is

called by a committee or board of the municipal government, as the

result of a petition by interested persons or through the independent

action of the Board. At this preliminary meeting or public hearing

arguments for and against the proposed improvement are heard. The

engineer is present at this meeting to answer questions and to advise

concerning the engineering features of the plan. If approval is given by

the Board the plan and specifications are prepared complete in every

detail and incorporated in an ordinance which is presented to the

legislative branch of the city government for passage. If the project is

adopted it is taken to the county court. An assessment roll is prepared

by a commissioner appointed by the court. This roll shows the amount to

be assessed against each piece of property benefited. A hearing is then

held in the county court at which the owner of any assessed property may

voice objections to the continuation of the project. The project may be

thrown out of court for many different reasons, such as the misspelling

of a street name, an error in an elevation, an error in the description

of a pavement, but most important of all is definite proof that the

benefit is not equal to the assessment. The many minor irregularities

which may nullify the procedure in a special assessment differ in

different states and in different courts in the same state, but in

general no court can approve an assessment greater than the benefits

given. After the project has passed through the county court and the

assessment roll has been approved, bonds may be issued for the payment

of the contractor. Special assessment bonds are liens against the

property assessed and have not the same security as a general municipal

bond. For this reason a city which has reached its legal limit of

municipal bond issues can still pay for work by special assessment.

The funds available from special assessments are limited only by the

benefit to the property assessed. The amount of the benefit is difficult

to fix and may lead to much controversy. It should not exceed the amount

demanded for similar work in other localities, unless unusual and

well-understood reasons can be given.

=12. General Taxation.=—In paying for public improvements by general

taxation the money is taken from the general municipal funds which have

been apportioned for that purpose by the legislative department of the

municipal government. This method of raising funds for sewerage

construction is seldom used unless the political situation is

unfavorable to the success of a bond issue or special assessment and the

need for the improvement is great. It is usually difficult to

appropriate sufficient funds for new construction as the general tax is

apportioned to support only the operating expenses of the city, and

statutory provisions limit the amount of tax which can be levied.

=13. Private Capital.=—Private capital has been used for financing

sewerage works in some cases because of the aversion of the public in

some cities to the payment of a tax for the negative service performed

by a sewer. Sewers are buried, unseen, and frequently forgotten, but

knowledge of their necessity has spread and the number of privately

owned sewerage works is diminishing because of the better service which

can be provided by the municipality.

Franchises are granted to private companies for the construction of

sewers only after the city has exhausted other methods for the raising

of capital. The return on the private capital invested is received from

a rental paid by the city, or paid directly by the users of the system,

an initial payment usually being demanded for connection to the system.

To be successful the enterprise must be popular and must fill a great

need. This method of financing sewerage works is seldom employed as

favorable conditions are not common.

PRELIMINARY WORK

=14. Preparing for Design.=—Methods for the design of sewerage systems

are given in Chapter V. Before the design is made certain information is

essential. A survey must be made from which the preliminary map can be

prepared as described in Art. 42. Other necessary information which is

the basis of subsequent estimates of the quantity of sewage to be cared

for must be obtained by a study of rates of water consumption and the

density and growth of population, the measurement of the discharge from

existing sewers, and the compilation of rainfall and run-off data. If no

rainfall data are available estimates must be made from the nearest

available data. Observations of rainfall or run-off for periods of less

than 10 to 20 years are likely to be misleading. Methods for gathering

and using this information are explained in subsequent chapters.

Underground surveys are desirable along the lines of the proposed sewers

to learn of obstructions, difficult excavation and other conditions

which may be met. All such data are seldom gathered except for sewerage

systems involving the expenditure of a large amount of money. For

construction in small towns or small extensions to an existing system

the funds are usually insufficient for extensive preliminary

investigation. The saving in this respect is paid unknowingly to the

contractor as compensation for the risk in bidding without complete

information.

=15. Underground Surveys.=—These may be more or less extensive dependent

on the character of the district in which construction is to take place.

In built-up districts the survey should be more thorough than in

sparsely settled districts where only the character of the excavated

material is of interest and no obstructions are to be met.

Underground surveys furnish to the engineer and to prospective bidders

on contract work information on which the design and estimate of cost

and the contractor’s bid may be based and without which no intelligent

work can be done. By removing much of the uncertainty of the conditions

to be met in the construction of the sewer, the design can be made more

economical and the contractor’s bid should be markedly lower,

sufficiently so to repay more than the expense of the survey. The

information to be obtained consists of the location of the ground-water

level, and the location and sizes of water, gas, and sewer pipes,

telephone and electric conduits, street-car tracks, steam pipes, and all

other structures which may in any way interfere with subsurface

construction. These structures should be located by reference to some

permanent point on the surface. The elevation of the top of the pipes,

except sewers, rather than the depth of cover should be recorded, as the

depth of cover is subject to change. The elevation of sewers should be

given to the invert rather than to the top of the pipe.

A portion of the map of the subsurface conditions at Washington, D. C.,

is shown in Fig. 3. Many of the dimensions and notations are not shown

to avoid confusion on this small reproduction.[15] Colors are generally

used instead of different forms of cross hatching to show the different

classes of pipe and structures. In addition to a record of the

underground structures the character of the ground and the pavement

should be recorded. A comprehensive underground survey is seldom

available nor does time usually permit its being made preliminary to the

design of a sewerage system. The character of the material through which

the sewer is to pass should be determined in all cases.

[Illustration:

FIG. 3.—Record Map of Underground Structures, Washington, D. C.

Eng. Record, Vol. 74, p. 263.

The various subsurface lines are differentiated by colors as follows:

_A_—Sewers, vermilion. _B_—Water mains, blue. _C_—Potomac Electric

Power Co., carmine. _D_—Washington Railway and Electric Co.,

carmine. _E_—Capital Traction Co., violet. _F_—Chesapeake and

Potomac Telephone Co., green. _G_—Washington Gas Light Co., green.

_H_—Western Union Telegraph Co., orange. _I_—Postal Telegraph Co.,

orange. _K_—Private vaults, black. _L_—City Electric Co., yellow.

]

[Illustration:

FIG. 4.

Punch Drill.

]

Underground pipes and structures are located by excavations, which may

be quite extensive in some cases. Their position is fixed by

measurements referred to manholes and other underground structures which

are somewhat permanent in position. A city engineer should grasp every

opportunity to record underground structures when excavations are made

in the streets. The character of the material through which the sewer is

to pass is determined by borings.

=16. Borings.=—Methods used for the investigation of subsurface

conditions preliminary to sewer construction are: punch drilling, boring

with earth auger, jet boring, wash boring, percussion drilling, abrasive

drilling, and hydraulic drilling. The last three methods named are used

only for unusually deep borings or in rock.

Punch drills are of two sorts. The simplest punch drill consists of an

iron rod ⅞ of an inch to 1 inch in diameter, in sections about 4 feet

long. One section is sharpened at one end and threaded at the other so

that the next section can be screwed into it without increasing the

diameter of the rod, as shown in Fig. 4. The drill is driven by a sledge

striking upon a piece of wood held at the top of the drill to prevent

injury to the threads. The drill should be turned as it is driven to

prevent sticking. It is pulled out by a hook and lever as shown in Fig.

5. It is useful in soft ground for soundings up to 8 to 12 feet in

depth. Another form of punch drill described by A. C. Veatch[16]

consists of a cylinder of steel or iron, one to two feet long split

along one side and slightly spread. The lower portion is very slightly

expanded and tempered into a cutting edge. In use it is attached to a

rope or wooden poles and lifted and dropped in the hole by means of a

rope given a few turns about a windlass or drum. By this process the

material is forced up into the bit, slightly springs it, and so is held.

When the bit is filled it is raised to the surface and emptied. Much

deeper holes can be made with this than with the sharpened solid rod.

[Illustration:

FIG. 5.—Lever for Pulling Punch Drill.

]

[Illustration:

FIG. 6.—Earth Augers.

]

Types of earth augers about 1½-inches in diameter are shown in Fig. 6.

They are screwed on to the end of a section of the pipe or rod and as

the hole is deepened successive lengths of pipe or rod are added. The

device is operated by two men. It is pulled by straight lifting or with

the assistance of a link and lever similar to that shown in Fig. 5. The

device is suitable for soft earth or sand free from stones, and can be

used for holes 15 to 25 feet in depth. For deeper holes a block and

tackle should be used for lifting the auger from the hole. It is not

suitable for holes deeper than about 35 feet.

In the jetting method water is led into the hole through a ¾-inch or

1–inch pipe, and forced downward through the drill bit or nozzle against

the bottom of the hole. The complete equipment is shown in Fig. 7.[17]

It is not always necessary to case the hole as shown in the figure as

the muddy water and the vibration of the pipe puddle the sides so that

they will stand alone. The jet pipe may be churned in the hole by a rope

passing over a block and a revolving drum. In suitable soft materials

such as clay, sand, or gravel, holes can be bored to a depth of 100 feet

and samples collected of the material removed. An objection to the

method is the difficulty of obtaining sufficient water.

[Illustration:

FIG. 7.—Jetting Outfit.

U. S. Geological Survey, Water Supply Paper, No. 257

1. Simple Jetting Outfit. 2. Jetting Process. 3. Common Jetting Drill.

4_a_ and 4_b_. Expansion Bit or Paddy. 5. Drive Shoe.

]

Methods of drilling in rock up to depths of 20 feet are described in

Chapter XI under Rock Drilling. For deeper holes percussion, abrasive,

or hydraulic methods as used for deep well drilling must be employed.

CHAPTER III

QUANTITY OF SEWAGE

=17. Dry weather Flow.=—Estimates of the quantity of sewage flow to be

expected are ordinarily based on the population, the character of the

district, the rate of water consumption, and the probable ground-water

flow. Future conditions are estimated and provided for, as the sewers

should have sufficient capacity to care for the sewage delivered to them

during their period of usefulness.

=18. Methods for Predicting Population.=—Methods for the prediction of

future population are given in the following paragraphs.

The method of _graphical extension_. This is the quickest and most

simple of all. In this method a curve is plotted on rectangular

coordinates to any convenient scale, with population as ordinates and

years as abscissas. The curve is extended into the future by judgment of

its general tendency. An example is given of the determination of the

population of Urbana, Illinois, in 1950. Table 4 contains the population

statistics which have been plotted on line A in Fig. 8 and extended to

1950. The probable population in 1950 is shown by this line to be about

21,000.

The method of _geometrical progression_. In this method the rate of

increase during the past few years or decades is assumed to be constant

and this rate is applied to the present population to forecast the

population in the future. For example the rate of increase of population

in Urbana for the past 7 decades has varied widely, but indications are

that for the next few decades it will be about 20 per cent. Applying

this rate from 1920 to 1950 the population in 1950 is shown to be about

17,800. It is evident that this method may lead to serious error as

insufficient information is given in the table to make possible the

selection of the proper rate of increase.

TABLE 4

POPULATION STUDIES

────┬────────────────────────────

│ Urbana, Illinois

────┼──────────┬────────┬────────

Year│Population│Absolute│Per Cent

│ │Increase│Increase

│ │for Each│for Each

│ │ Decade │ Decade

────┼──────────┼────────┼────────

1850│ 210│ │

1860│ 2,038│ 1828│ 85.6

1870│ 2,277│ 239│ 10.5

1880│ 2,942│ 665│ 22.6

1890│ 3,511│ 569│ 16.2

1900│ 5,728│ 2217│ 38.7

1910│ 8,245│ 2517│ 30.5

1920│ 10,230│ 1985│ 19.4

────┴──────────┴────────┴────────

────┬───────────────────────────────────────────────────────────────

│ Population of

────┼───────┬────────┬─────────┬────────┬──────┬───────────┬────────

Year│Decatur│Danville│Champaign│Kankakee│Peoria│Bloomington│ Ann,

│ │ │ │ │ │ │ Arbor

│ │ │ │ │ │ │Michigan

│ │ │ │ │ │ │

────┼───────┼────────┼─────────┼────────┼──────┼───────────┼────────

1850│ │ 736│ │ │ 5,095│ 1,594│

1860│ 3,839│ 1,632│ 1,727│ 2,984│14,045│ 7,075│ 5,097

1870│ 7,161│ 4,751│ 4,625│ 5,189│22,849│ 14,590│ 7,368

1880│ 9,547│ 7,733│ 5,103│ 5,651│29,259│ 17,180│ 8,061

1890│ 16,841│ 11,491│ 5,839│ 9,025│41,024│ 20,484│ 9,431

1900│ 20,754│ 16,354│ 9,098│ 13,595│56,100│ 23,286│ 14,509

1910│ 31,140│ 27,871│ 12,421│ 13,986│66,950│ 25,786│ 14,817

1920│ 43,818│ 33,750│ 15,873│ 16,721│76,121│ 28,638│ 19,516

────┴───────┴────────┴─────────┴────────┴──────┴───────────┴────────

[Illustration:

FIG. 8.—Diagram Showing Methods for Estimating Future Population.

]

The method of utilizing a _decreasing rate of increase_. This method

attempts to correct the error in the assumption of a constant rate of

increase. After a certain period of growth, as the age of a city

increases its rate of increase diminishes. In applying this knowledge to

a prediction of the future population of a city the population curve is

plotted, as in the graphical method and a straight line representing a

constant rate or increase is drawn tangent to the curve at its end. The

curve is then extended at a flatter rate in accordance with the rate of

change of a similar nearby larger city. This method has not been applied

to any of the cities included in Table 4, as none has reached that

limiting period where the rate of increase has begun to diminish.

The method of utilizing an _arithmetical rate of increase_. This method

allows for the error of the geometrical progression which tends to give

too large results for old and slow-growing cities. This method generally

gives results that are too low. The absolute increase in the population

during the past decade or other period is assumed to continue throughout

the period of prediction. Applying this method to the same case, the

increase in the population during the past decade was 2,000. Adding

three times this amount to the population in 1920, the population of

Urbana in 1950 will be about 16,000.

The method involving the _graphical comparison with other cities_ with

similar characteristics. In this method population curves of a number of

cities larger than Urbana but having similar characteristics, are

plotted with years as abscissas and population as ordinates, with the

present population of Urbana as the origin of coordinates. The

population curve for Urbana is first plotted. It will lie entirely in

the third quadrant as shown by the heavy full line in Fig. 8. The

population curves of some larger cities are then plotted in such a

manner that each curve passes through the origin at the time their

population was the same as that of the present population of Urbana.

These curves lie in the first and third quadrants. The population curve

of the city in question is then extended to conform with the curves of

older cities in the most probable manner as dictated by judgment. Such a

series of plots has been made in Fig. 8. The results indicate that the

population of Urbana in 1950 will be about 25,500.

The last method described will give the most probable result as it is

the most rational. For quick approximations the geometrical progression

is used. The arithmetical progression is useful only as an approximate

estimate for old cities.

=19. Extent of Prediction.=—The period for which a sewerage system

should be designed is such that each generation bears its share of the

cost of the system. It is unfair to the present generation to build and

pay for an extensive system that will not be utilized for 25 years. It

is likewise unfair to the next generation to construct a system

sufficient to comply with present needs only, and to postpone the

payment for it by a long term bond issue. An ideal solution would be to

plan a system which would satisfy present and future needs and to

construct only those portions which would be useful during the period of

the bond issue. Unfortunately this solution is not practical, because,

1st, it is less expensive to construct portions of the system such as

the outfall, the treatment plant, etc., to care for conditions in

advance of present needs, and 2nd, the life of practically all portions

of a sewerage system is greater than the legal or customary time limit

on bond issues.

A compromise between the practical and the ideal is reached by the

design of a complete system to fulfill all probable demands, and the

construction of such portions as are needed now in accordance with this

plan. The payment should be made by bond issues with as long life as is

financially or legally practical, but which should not exceed the life

of the improvement.

The prediction of the population should therefore be made such that a

comprehensive system can be designed with intelligence. Practice has

seldom called for predictions more than 50 years in the future.

=20. Sources of Information on Population.=—The United States decennial

census furnishes the most complete information on population.

Unfortunately it becomes somewhat old towards the end of a decade. More

recent information can be obtained from local sources. Practically every

community takes an annual school census the accuracy of which is fairly

reliable. The general tendencies of the population to change can be

learned by a study of the post office records showing the amount of mail

matter handled at various periods. Local chambers of commerce and

newspapers attempt to keep records of population, but they are often

inaccurate. Another source of information is the gross receipts of

public service companies, such as street railways, water, gas,

electricity, telephone, etc. The population can be assumed to have

increased almost directly as their receipts, with proper allowance for

change in rates, character of management, and other factors.

=21. Density of Population.=—So far the study of population has been

confined to the entire city. It is frequently necessary to predict the

population of a district or small section of a city. A direct census may

be taken, or more frequently its population is determined by estimating

its density based on a comparison with similar districts of known

density, and multiplying this density by the area of the district. In

determining the density, statistics of the population of the entire city

will be helpful but are insufficient for such a problem. A special

census of the area involved would be conclusive but is generally

considered too expensive. A count of the number of buildings in the

district can be made quickly, and the density determined by

approximating the number of persons per building. Statistics of the

population of various districts together with a description of the

character of the district are given in Table 5.

[Illustration:

FIG. 9.—Density, Area, and Population, Cincinnati, Ohio. 1850 to 1950.

]

TABLE 5

DENSITIES OF POPULATION

────────────┬────────────────────────────────────────┬────────┬────────

City │ Character of District │ Area, │Density

│ │ Acres │per Acre

────────────┼────────────────────────────────────────┼────────┼────────

Philadelphia│Thomas Run. Residential. Mostly pairs of│ │

│ two and three-story houses. 1204 acres│ │

│ settled. │ 1,840│ 59

│Pine Street. Residential. Mostly solid │ │

│ four to six-story houses. 156 acres │ │

│ settled. │ 160│ 97

│Shunk Street. Residential. Mostly pairs │ │

│ of two and three-story houses. 539 │ │

│ acres settled. │ 539│ 119

│Lombard Street. Tenements and hotels, │ │

│ 145 acres settled. │ 147│ 113

│York Street. Residential and │ │

│ manufacturing. 354 acres settled. │ 358│ 94

│ │ │

New York │Residential. Three-story dwellings with │ │

City │ 18–foot frontage, and four-story flats│ │

│ with 20–foot frontage. │ │ 100

│Residential. Five-story flats. │ │520–670

│Residential. Six-story flats. │ │800–1000

│Residential. Six-story apartments. High │ │

│ class. │ │ 300

│ │ │

Chicago │1st Ward. Retail and commercial. The │ │

│ “Loop”. │ 1,440│ 20.5

│2d Ward. Commercial and low-class │ │

│ residential solidly built up. │ 800│ 53.5

│3d Ward. Low-class residential. │ 960│ 48.1

│5th Ward. Industrial. Some low-class │ │

│ residences. Not solidly built up. │ 2,240│ 25.51

│6th Ward. Residential. Four and │ │

│ five-story apartments. A few detached │ │

│ residences. │ 1,600│ 47.0

│7th Ward. Same as Ward 6. Not solidly │ │

│ built up. Contains a large park. │ 4,160│ 21.7

│8th Ward. Industrial. Sparsely settled. │ 13,624│ 4.8

│9th Ward. Industrial and low-class │ │

│ residential. Solidly built up. │ 640│ 70.0

│10th Ward. Same as Ward 9. │ 640│ 80.8

│13th Ward. Low-class residential. │ │

│ Solidly built with three and │ │

│ four-story flats. │ 6,100│ 36.7

│16th Ward. Middle-class residential. │ │

│ Some industries. Well built up. │ 800│ 81.5

│19th Ward. Industrial and commercial. │ │

│ Some low-class residences. │ 640│ 90.7

│20th Ward. Low-class residential. Some │ │

│ industries. Entirely built up. │ 800│ 77.1

│21st Ward. Industrial. Entirely built │ │

│ up. │ 960│ 49.9

│23d Ward. Industrial and residential. │ 800│ 55.4

│24th Ward. Residential apartment houses │ │

│ and middle-class residences. │ 1,120│ 46.8

│25th Ward. Residential. High-class │ │

│ apartments. Wealthy homes. Contains a │ │

│ large park. │ 4,160│ 24.0

│26th Ward. Residential. Middle-class │ │

│ homes and apartments. Fairly well │ │

│ built up. │ 4,640│ 16.1

│27th Ward. Residential. Sparsely │ │

│ settled. │ 20,480│ 5.5

│29th Ward. Low-class residential. │ │

│ Two-story frame houses. “Back of the │ │

│ Yards”. │ 6,400│ 12.8

│30th Ward. The Stock Yards. │ 1,280│ 40.1

│32d Ward. Scattered residences. │ 8,480│ 8.3

│33d Ward. Scattered residences. │ 12,944│ 5.5

│35th Ward. Scattered residences. │ 4,960│ 12.0

│ │ │

General │The most crowded conditions with │ │

average │ five-story and higher, contiguous │ │

│ buildings in poor class districts. │ │750–1000

│Five and six-story contiguous flat │ │

│ buildings. │ │500–750

│Six-story high-class apartments. │ │300–500

│Three and four-story dwellings, business│ │

│ blocks and industrial establishments. │ │

│ Closely built up. │ │100–300

│Separate residences, 50 to 75–foot │ │

│ fronts, commercial districts, │ │

│ moderately well built up. │ │ 50–100

│Sparsely settled districts and scattered│ │

│ frame dwellings for individual │ │

│ families. │ │ 0–50

────────────┴────────────────────────────────────────┴────────┴────────

The density of population in Cincinnati from 1850 to 1913 with

predictions to 1950 is given in Fig. 9.[18] This shows the densities for

the entire city and is illustrative of the manner in which future

conditions were predicted for the design of an intercepting sewer. The

data given in Table 5 are of value in estimating the densities of

population in various districts. The Committee on City Plan of the Board

of Estimate and Apportionment of New York City obtained some valuable

information on this point, especially in Manhattan. Three-story

dwellings with 18–foot frontage, or four-story flats with 20–foot

frontage, presumably contiguous, were found to hold 100 persons to the

acre. Five-story flats held 520 to 670 persons per acre. Six-story flats

held 800 to 1,000 persons per acre, and high-class six-story apartments

held less than 300 per acre.

=22. Changes in Area.=—In order to determine the probable extent of a

proposed sewerage system it is important to estimate the changes in the

area of a city as well as the changes in the population. With the same

population and an increased area the quantity of sewage will be

increased because of the larger amount of ground water which will enter

the sewers. Predictions of the area of a city are less accurate than

predictions of population because the factors affecting changes cannot

be so easily predicted. An area curve plotted against time would be

helpful in guiding the judgment, but its extension into the future based

on past occurrences would be futile. A knowledge of the city, its

political tendencies, possibilities of extension, and other factors must

be weighed and judged. The engineer, if he is ignorant of the city for

which he is making provision, is dependent upon the testimony of real

estate men, business men and others acquainted with the local situation.

=23. Relation between Population and Sewage Flow.=—The amount of sewage

discharged into a sewerage system is generally equal to the amount of

water supplied to a community, exclusive of ground water. The entire

public water supply does not reach the sewers, but the losses due to

leakage, lawn sprinkling, manufacturing processes, etc., are made up by

additions from private water supplies, surface drainage, etc. The

estimated quantity of water used but which did not reach the sewers in

Cincinnati is shown in Table 6. The amount shown represents 38 per cent

of the total consumption. Unless direct observations have been made on

existing sewers or other factors are known which will affect the

relation between water supply and sewage, the average sewage flow

exclusive of ground water, should be taken as the average rate of water

consumption. Experience has shown that water consumption increases after

the installation of sewers.

TABLE 6

ESTIMATED QUANTITY OF WATER USED BUT NOT DISCHARGED INTO THE SEWERS IN

CINCINNATI

Expressed in gallons per capita per day, and based on a total

consumption of 125 to 150 gallons per capita per day.

──────────────────────────────────────────────────────────────┬────────

Steam railroads. │6 to 7

Street sprinklers. │6 to 7

Consumers not sewered. │9 to 10½

Manufacturing and mechanical. │6 to 7

Lawn sprinklers. │3 to 3½

Leakage. │18 to 21

──────────────────────────────────────────────────────────────┴────────

The public water supply is generally installed before the sewerage

system. By collecting statistics on the rate of supply of water a fair

prediction can be made of the quantity of sewage which must be cared

for. The rate of water supply varies widely in different cities. It is

controlled by many factors such as meters, cost and availability of

water, quality of water, climate, population, etc. In American cities a

rough average of consumption is 100 gallons per capita per day. Other

factors being equal the rate of consumption after meters have been

installed will be about one-half the rate before the meters were

installed. Low cost, good quantity and good quality will increase the

rate of consumption, and the rate will increase slowly with increasing

population. Statistics of rates of water consumption are given in Table

7.

=24. Character of District.=—The various sections of a city are

classified as commercial, industrial, or residential. The residential

districts can be subdivided into sparsely populated, moderately

populated, crowded, wealthy, poor, etc. Commercial districts may be

either retail stores, office buildings, or wholesale houses. Industrial

districts may be either large factories, foundries, etc., or they may be

made up of small industries housed in loft buildings.

In cities of less than 30,000 population the refinement of such

subdivisions is generally unnecessary in the study of sewage flow, all

districts being considered the same. The data given in Tables 8 and 9

indicate the difference to be found in different districts of large

cities. The Milwaukee data are presented in a form available for

estimates on different bases. These data are shown in Table 10.

TABLE 7

RATES OF WATER CONSUMPTION

From Journals of American and New England Water Works Associations

───────────────────────────────────┬───────────┬───────────┬───────────

City │Population │ Per Cent │Consumption,

│ in │ Metered │ Gal. per

│ Thousands │ │Capita per

│ │ │ Day

───────────────────────────────────┼───────────┼───────────┼───────────

Tacoma, Wash. │ 100 │ 11.6│ 460

Buffalo, N. Y. │ 450 │ 4.9│ 310

Cheyenne, Wyo. │ 13 │ │ 270

Erie, Pa. │ 72 │ 3.0│ 198

Philadelphia, Pa. │ 1611 │ 4.6│ 180

St. Catherines, Ont. │ 17 │ 3.2│ 160

Port Arthur, Ont. │ 18 │ 14.7│ 145

Ogdensburg, N. Y. │ 18 │ 0.2│ 140

Los Angeles, Cal. │ 516 │ 77.9│ 140

Wilmington, Del. │ 92 │ 43.7│ 125

Lancaster Pa. │ 60 │ 34.6│ 120

Richmond, Va. │ 120 │ 75.2│ 115

St. Louis, Mo. │ 730 │ 6.7│ 110

Springfield, Mass. │ 100 │ 94.4│ 110

Keokuk, Ia. │ 14 │ 64.5│ 105

Jefferson City, Mo. │ 13.5│ 34.4│ 100

Muncie, Ind. │ 30 │ 23.8│ 95

Burlington, Ia. │ 24 │ 4.5│ 90

Council Bluffs, Ia. │ 32 │ 75.5│ 80

San Diego, Cal. │ 85 │ 100 │ 80

Monroe, Wis. │ 3 │ 100 │ 80

Yazoo City, Miss. │ 7 │ 84.1│ 75

Oak Park, Illinois. │ 26 │ 100 │ 70

Portsmouth, Va. │ 75 │ 8.1│ 65

New Orleans, La. │ 360 │ 99.7│ 60

Rockford, Ill. │ 53 │ 93.0│ 55

Fort Dodge, Ia. │ 20 │ 96.0│ 50

Manchester, Vt. │ 1.5│ 69.0│ 45

Woonsocket, R. I. │ 47.5│ 95.6│ 35

───────────────────────────────────┴───────────┴───────────┴───────────

Attempts have been made to express the rate of sewage flow in different

units other than in gallons per capita per day. A unit in terms of

gallons per square foot of floor area tributary has been suggested for

commercial and industrial districts. It has not been generally adopted.

The rates of flow in New York City as reported in this unit by W. S.

McGrane are given in Table 11.

The most successful way to predict the flow from commercial or

industrial districts is to study the character of the district’s

activities and to base the prediction on the quantity of water demanded

by the commerce and industry of the district affected.

=25. Fluctuations in Rate of Sewage Flow.=—The rate of flow of sewage

from any district varies with the season of the year, the day of the

week, and the hour of the day. The maximum and minimum rates of sewage

flow are the controlling factors in the design of sewers. The sewers

must be of sufficient capacity to carry the maximum load which may be

put upon them, and they must be on such a grade that deposits will not

occur during periods of minimum flow. The maximum and minimum rates of

flow are usually expressed as percentages of the average rate of flow.

TABLE 8

SEWAGE FLOW FROM DIFFERENT CLASSES OF DISTRICTS

Arranged from data by Kenneth Allen in Municipal Engineer’s Journal,

Feb., 1918.

──────────────────────────────────────────────────────┬───────┬───────

District │Gallons│Gallons

│ per │ per

│Capita │ Acre

│per Day│per Day

──────────────────────────────────────────────────────┼───────┼───────

Buffalo, N. Y. From Report of International Joint │ │

Commission on the Pollution of Boundary Waters: │ │

Industrial: Metal and automobile plants. Maximum. │ │ 13,000

Industrial: Meat packing, chemical and soap. │ │ 16,000

Commercial: Hotels, stores and office buildings. │ │ 60,000

Domestic: Average. │ 80 │

Domestic: Apartment houses. │ 147 │

Domestic: First-class dwellings. │ 129 │

Domestic: Middle-class dwellings. │ 81 │

Domestic: Lowest-class dwellings. │ 35.5│

│ │

Cincinnati, Ohio. 1913 Report on Sewerage Plan: │ │

Industrial, in addition to residential and ground │ │

water. │ │ 9,000

Commercial, in addition to residential and ground │ │

water. │ │ 40,000

Domestic. │ 135 │

│ │

Detroit, Mich.: │ │

Domestic. │ 228 │

Industrial, in addition to residential and ground │ │

water. │ │ 12,000

Commercial, in addition to residential and ground │ │

water. │ │ 50,000

│ │

Milwaukee, Wis. 1915 Report of Sewerage Commission: │ │

Industrial, maximum. │ 81 │ 16,600

Industrial, average. │ 31 │ 8,300

Commercial, maximum. │ │ 60,500

Commercial, average. │ │ 37,400

Wholesale commercial, maximum. │ │ 20,000

Wholesale commercial, average. │ │ 9,650

──────────────────────────────────────────────────────┴───────┴───────

TABLE 9

OBSERVED WATER CONSUMPTION IN DIFFERENT CLASSES OF DISTRICTS IN NEW YORK CITY

From data by Kenneth Allen in Municipal Engineers Journal, for 1918

─────────────┬─────────────┬──────────┬─────────────┬───────────┬─────────────

Hotels │ Daily Cons. │Tenements │ Daily Cons. │Office and │ Daily Cons.

│ Gals. per │ │ Gals. per │ Loft │ Gals. per

│1000 Sq. Ft. │ │1000 Sq. Ft. │ Buildings │1000 Sq. Ft.

│ Floor Area │ │ Floor Area │ │ Floor Area

─────────────┼────────┬────┼──────────┼────────┬────┼───────────┼────────┬────

Building │Max.[19]│Avg.│ Location │Max.[19]│Avg.│ Building │Max.[19]│Avg.

─────────────┼────────┼────┼──────────┼────────┼────┼───────────┼────────┼────

Hotel │ │ │78th–79th │ │ │McGraw │ │

Biltmore. │ │ │ St. and │ │ │ Bldg. │ │

│ 470 │368 │ B’way. │ 256 │192 │ │ 309 │206

Hotel │ │ │410 E. │ │ │N. Y. │ │

McAlpin. │ │ │ 65th St.│ │ │ Telephone│ │

│ 753 │694 │ │ 350 │295 │ Bldg. │ │194

Hotel Plaza. │ │ │30th St. │ │ │Met. Life │ │

│ │ │ and │ │ │ Bldg. │ │

│ │ │ Madison │ │ │ │ │

│ 630 │578 │ Ave │ 306 │188 │ │ │256

Hotel Waldorf│ │ │27 Lewis │ │ │42d St. │ │

Astoria. │ 618 │482 │ St. │ 307 │250 │ Bldg │ │271

Hotel Astor. │ │ │258 │ │ │Municipal │ │

│ │ │ Delancey│ │ │ Bldg. │ │

│ 732 │492 │ St. │ 267 │226 │ │ │118

Hotel │ │ │ │ │ │Equitable │ │

Vanderbilt.│ 604 │545 │ │ │ │ Bldg. │ 366 │268

─────────────┼────────┼────┼──────────┼────────┼────┼───────────┼────────┼────

Average │ 634 │526 │ Average │ 297 │230 │ Average │ 338 │219

─────────────┴────────┴────┴──────────┴────────┴────┴───────────┴────────┴────

TABLE 10

SEWAGE FLOW FROM DIFFERENT CLASSES OF DISTRICTS BASED ON 1915 REPORT OF

MILWAUKEE SEWERAGE COMMISSION

────────────────────────────────────────────────────────────────┬──────

Ratio of maximum to average rate for department store district. │ 1.755

Ratio of maximum to average rate for hotel district. │ 1.65

Ratio of maximum to average rate for office building district. │ 1.51

Ratio of maximum to average rate for wholesale commercial │

district. │ 2.1

│

│——————│——————

Average and maximum gallons per thousand square feet of │ │

floor area: │ Avg. │ Max.

│——————│——————

For department store district. │ 232│ 407

For office building district. │ 541│ 891

For wholesale commercial district. │ 164│ 344

For all districts except wholesale commercial. │ 381│ 618

│ │

Average and maximum gallons per day: │ │

For all districts except wholesale commercial. │17,700│29,800

For wholesale commercial district. │ 9,650│20,000

─────────────────────────────────────────────────────────┴──────┴──────

TABLE 11

RATES OF CONSUMPTION PREDICTED FOR DIFFERENT DISTRICTS IN NEW YORK CITY

────────────┬───────────┬──────┬────────┬────────┬─────────

│ Net Bldg. │ │Observed│Observed│

│Area in Sq.│ Avg. │Cons. in│Cons. in│Predicted

District │ Ft. per │Number│ g.p.d. │ g.p.d. │ Mean

│ Acre for │ of │per 1000│per 1000│ Cons.

│ Ultimate │Floors│Sq. Ft. │Sq. Ft. │

│Consumption│ │ Max. │ Avg. │

────────────┼───────────┼──────┼────────┼────────┼─────────

Hotel and │ 24,800│ 15│ 634│ 526│ 500

midtown. │ │ │ │ │

Midtown and │ 24,800│ 15│ 338│ 219│ 300

financial.│ │ │ │ │

East and │ │ │ │ │

West of │ 24,800│ 10│ 297│ 230│ 300

midtown. │ │ │ │ │

Apartment, │ │ │ │ │

59th to │ 20,400│ 7│ │ 230│ 300

155th Sts.│ │ │ │ │

Manhattan │ │ │ │ │

north of │ 20,400│ 5│ │ 230│ 300

155th St. │ │ │ │ │

────────────┴───────────┴──────┴────────┴────────┴─────────

────────────┬─────────┬─────────┬─────────┬────────┬────────

│Predicted│Predicted│Predicted│Measured│Measured

│ Mean in │ Dry │Max. Dry │Avg. Dry│Max. Dry

District │ Million │ Weather │ Weather │Weather │Weather

│Gals. per│ Flow, │ Flow, │ Flow, │ Flow,

│Acre per │ c.f.s. │ c.f.s. │ c.f.s. │ c.f.s.

│ Day │per Acre │per Acre │per Acre│per Acre

────────────┼─────────┼─────────┼─────────┼────────┼────────

Hotel and │ .20 │ .29│ .34│ 1.04 │ .146

midtown. │ │ │ │ │

Midtown and │ .12 │ .18│ .23│ .078│ .110

financial.│ │ │ │ │

East and │ │ │ │ │

West of │ .074│ .12│ .15│ .057│ .097

midtown. │ │ │ │ │

Apartment, │ │ │ │ │

59th to │ .043│ .06│ .09│ │

155th Sts.│ │ │ │ │

Manhattan │ │ │ │ │

north of │ .031│ .05│ .08│ │

155th St. │ │ │ │ │

────────────┴─────────┴─────────┴─────────┴────────┴────────

Midtown district consists of department stores, large railroad

terminals, industrial and loft buildings, and sky-scraper office

buildings.

It is difficult to set any definite figure for the percentage which the

maximum rate of flow is of the average. Fluctuations above and below the

average are greater the smaller the tributary population. This relation

can be expressed empirically as

_M_ = 500⁄_P_^⅕,

in which _M_ represents the per cent which the maximum flow is of the

average, and _P_ represents the tributary population in thousands. The

expression should not be used for populations below 1,000 nor above

1,000,000. Having determined the expected average flow of sewage by a

study of the population, water consumption, etc., the maximum quantity

of sewage is determined by multiplying the average flow by the per cent

which the maximum is of the average. In this connection W. G. Harmon[20]

offers the relation

_M_ = 1 + 14⁄(4 + √(_P_)),

which was used in the design of the Ten Mile Creek intercepting sewer at

Toledo, Ohio. For rough estimates and for comparative purposes the ratio

of the average to the minimum flow can be taken the same as the ratio of

the maximum to the average flow, unless direct gaugings or other

information show it to be otherwise.

[Illustration:

Fig. 10.—Daily and Hourly Variations of Sewage Flow.

]

1. Toledo, O.; Manufacturing average.

2. Toledo, O.; Manufacturing, Monday.

3. Toledo, O.; Manufacturing, Sunday.

4. Toledo, O.; Residential, average.

5. Toledo, O.; Residential, Monday.

6. Toledo, O.; Residential, Sunday.

7. Cincinnati, O., Industrial, average.

8. Cincinnati, O.; Residential, average.

9. Cincinnati, O.; Commercial, average.

10. Average of 7 cities.

The fluctuations of flow in commercial and industrial districts are so

different from those in residential districts that the formulas given

should not be used in the design of sewers other than those draining

residential areas. It is reasonable to suppose that fluctuations in

rates of flow from industrial districts are dependent upon the character

of the tributary industries. A study of these industries will give

valuable light on the maximum and minimum rates at which sewage will be

delivered to the sewers.

Hourly, daily, and seasonal fluctuations in rates of sewage flow are of

interest in the design of pumping stations to give knowledge of the

rates at which the pumps must operate at various periods. The

fluctuations in rates of sewage flow during various hours and days in

different cities and districts are shown in Fig. 10. Fluctuations in

rate of flow of sewage lag behind fluctuations in rate of water

consumption, the time being dependent on the distance through which the

wave of change must travel in the sewer.

=26. Effect of Ground Water.=—Sewers are seldom laid with water-tight

joints. Since they usually lie below the ground water level it is

inevitable that a certain amount of ground water will enter. Various

units have been suggested for the expression of the inflow of ground

water in an attempt to include all of the many factors. Some of these

units are: gallons per acre drained by the sewer per day, gallons per

mile of pipe per day, gallons per inch diameter per mile of pipe per

day, etc. Since the ground water enters pipe sewers at the joints, the

longer the joints the greater the probability of the entrance of ground

water. The last unit is therefore the most logical but the accuracy of

the result is scarcely worthy of such refinement and the unit usually

adopted is gallons per mile of pipe per day.

No definite figure can be given for the amount of ground water to be

expected in sewers since the character of the soil and the ground water

pressure must be considered. Relatively normal infiltration may be found

from 5,000 to 80,000 gallons per mile of pipe per day. The minimum is

seldom reached in wet ground and the maximum is frequently exceeded.

Table 12 shows the amount of ground water measured in various sewers as

given by Brooks.[21]

=27. Résumé of Method for Determination of Quantity of Dry weather

Sewage.=—The steps in the determination of the quantity of sewage are:

determine the period in the future for which the sewers are to be

designed; estimate the population and tributary area at the end of this

period; estimate the rate of water consumption and assume the sewage

flow to equal the water consumption; determine the maximum and minimum

rates of sewage flow; and finally, estimate the maximum rate of ground

water seepage and add it to the maximum rate of sewage flow to give the

total quantity of sewage to be carried by the proposed sewers.

TABLE 12

DATA ON THE INFILTRATION OF GROUND WATER INTO SEWERS

Abstracted from paper by J. N. Brooks in Transactions Am. Society of Civil

Engineers, Vol. 76, p. 1909.

───────────┬─────┬──────┬─────┬───────┬──────┬─────┬──────────────────────

Place │ │Diam- │ │ │ │ │

│ │ eter │ │ Wet │ Avg. │ │

│ │ or │ │Trench,│ Head │Char-│

│ │Dimen-│ │ Per │ of │acter│

│ │sions │ │Cent of│Ground│ of │

│ │ in │Mate-│ Total │Water,│Sub- │

│Shape│Inches│rial │Length │ Fee │grade│ Gallons per 24 Hours

───────────┼─────┼──────┼─────┼───────┼──────┼─────┼─────┬──────┬─────────

│ │ │ │ │ │ │ │ Per │

│ │ │ │ │ │ │ │ Inch │

│ │ │ │ │ │ │ │Diam- │

│ │ │ │ │ │ │ │ eter │

│ │ │ │ │ │ │ Per │ Per │

│ │ │ │ │ │ │Foot │ Mile │

│ │ │ │ │ │ │ of │ of │Per Mile

│ │ │ │ │ │ │Joint│ Pipe │ of Pipe

───────────┼─────┼──────┼─────┼───────┼──────┼─────┼─────┼──────┼─────────

Boston, │ │ 8 to │ │ │ │ │ │ │

Mass. │Circ.│ 36 │V.P. │ │ │ │ 2.6│ 1,818│ 40,000

East │ │ │ │ │ │ │ │ │

Orange, │ │ │ │ │ │ │ │ │

N. J. │ │ │ │ │ 10│ Q. │ │ │ 22,400

East │ │ │ │ │ │ │ │ │

Orange, │ │ 8 to │ │ │ │ │ │ │

N. J. │ │ 24 │V.P. │ │ │ │ 0.8│ 540│ 8,650

Joint trunk│ │ │ │ │ │ │ │ │

sewer, │ │ │ │ │ │ │ │ │

New │ │ │ │ │ │G. & │ │ │

Jersey │ │ │ │ │ │ Q. │ │ │ 25,000

Rogers │ │ │ │ │ │ │ │ │

Park, │ │ │ │ │ │ │ │ │

Ill. │ │ 6 │ │ │ │ │ 0.3│ 207│ 1,240

Altoona, │ │ │ │ │ │ │ │ │

Pa. │ │ 30 │ │ │ │ │ 5.0│ 2,890│ 86,592

Concord, │ │ │ │ │ │ │ │ │

Mass. │ │ │ │ 18│ 8│ │ │ │ 43,000

Malden, │ │ │ │ │ │ │ │ │

Mass. │Circ.│ │V.P. │ 60│ │ │ │ │ 50,000

Westboro, │ │ │ │ │ │ │ │ │

Mass. │ │ 15 │V.P. │ 100│ │ │ │88,100│1,320,300

Fond du │ │ │ │ │ │ │ │ │

Lac, Wis.│Circ.│ 24 │V.P. │ 100│ 5│ C. │ 1.5│ 1,010│ 24,370

East │ │ │ │ │ │ │ │ │

Orange, │ │10 to │ │ │ │ │ │ │

N. J. │Circ.│ 24 │V.P. │ 100│ │ │ 4.7│ 2,540│ 43,250

Ocean │ │ │ │ │ │ │ │ │

Grove, N.│ │ 4 to │ │ │ │ │ │ │

J. │Circ.│ 12 │V.P. │ 100│ 3│S.C. │ 2.7│ 1,890│ 15,126

Ocean │ │ │ │ │ │ │ │ │

Grove, N.│ │ 4 to │ │ │ │ │ │ │

J. │Circ.│ 12 │V.P. │ 100│ 4│S.C. │ 7.9│ 5,480│ 43,764

East │ │ │ │ │ │ │ │ │

Orange, │ │ 24 × │ │ │ │ │ │ │

N. J. │Rect.│ 36 │Brick│ 100│ │ │ │ │ 570,000

Westboro, │ │ │ │ │ │ │ │ │

Mass. │ │ │Brick│ │ │ │ │ │ 415,850

Altoona, │ │ 33 × │B. & │ │ │ │ │ │

Pa. │Rect.│ 44 │ C. │ │ │ │ │ 5,390│ 264,000

Columbus, │ │ 42 × │Con- │ │ │ │ │ │

Ohio. │H.S. │ 42 │crete│ │ │ │ │ 120│ 6,340

Bronx │ │ │ │ │ │ │ │ │

Valley, │ │44 to │Con- │ │ │ │ │ │

N. Y. │Circ.│ 72 │crete│ │ │ G. │ │ 123│ 7,266

Cincinnati,│ Estimated in design. Data not │ │ │ │

Ohio. │ from Brooks │ │ │ │ 67,500

Milwaukee, │ Residential districts, gals. per acre per │ │ 1460 to

Wis. │ day. Not taken from Brooks │ │ 2200

───────────┴─────────────────────────────────────────────┴──────┴─────────

Abbreviations: H.S. = horseshoe shaped; B. & C = Brick and concrete; V.P.

= vitrified pipe; G. = gravel; Q. = quicksand; S. C. = sand clay; C. =

clay.

QUANTITY OF STORM WATER

=28. The Rational Method.=—The water which falls during a storm must be

removed rapidly in order to prevent the flooding of streets and

basements, and other damages. The quantity of water to be cared for is

dependent upon: the rate of rainfall, the character and slope of the

surface, and the area to be drained. All methods for the determination

of storm-water run-off, whether rational or empirical, depend upon these

factors.

The so-called Rational Method can be expressed algebraically, as,

_Q_ = _AIR_,

in which _Q_ = rate of run-off in cubic feet per second;

_A_ = area to be drained expressed in acres;

_I_ = percentage imperviousness of the area;

_R_ = maximum average rate of rainfall over the entire

drainage area, expressed in inches per hour, which

may occur during the time of concentration.

The area to be drained is determined by a survey. A discussion of _R_

and _I_ follows in the next two sections. An example of the use of the

Rational Method is given on page 95.

=29. Rate of Rainfall.=—Rainfall observations have been made over a long

period of time by United States Weather Bureau observers and others.

Continuous records are available in a few places in this country showing

rainfall observations covering more than a century. Such records have

been the bases for a number of empirical formulas for expressing the

probable maximum rate of rainfall in inches per hour, having given the

duration of the storm. Table 13 is a collection of these formulas with a

statement as to the conditions under which each formula is applicable.

The formula most suitable to the problem in hand should be selected for

its solution.[22]

TABLE 13

RAINFALL FORMULAS

────────────┬─────────────────────────┬────────────────────────────────

Name of │ Conditions for which │ Formula

Originator │ Formula is Suitable │

────────────┼─────────────────────────┼────────────────────────────────

E. S. Dorr │ │_i_ = 150⁄(_t_ + 30)

A. N. Talbot│Maximum storms in Eastern│_i_ = 360⁄(_t_ + 30)

│ United States │

A. N. Talbot│Ordinary storms in │_i_ = 105⁄(_t_ + 15)

│ Eastern United States │

Emil │Heavy rainfall near New │_i_ = 120⁄(_t_ + 20), etc.

Kuichling │ York City │

L. J. Le │For San Francisco. See T.│

Conte │ A. S. C. E. v. 54, p. │_i_ = 7⁄_t_^½

│ 198 │

Sherman │Maximum for Boston, Mass.│_i_ = 25.12⁄_t_^{.687}

Sherman │Extraordinary for Boston,│_i_ = 18⁄_t_ ^½

│ Mass. │

Webster │Ordinary for │_i_ = 12⁄_t_^{0.6}

│ Philadelphia, Pa. │

│Ordinary storms for │

Hendrick │ Baltimore. Eng. & │_i_ = 105⁄(_t_ + 10)

│ Cont., Aug. 9. 1911 │

J. de │Ordinary storms for │_i_ = 163⁄(_t_ + 27)

Bruyn-Kops│ Savannah, Ga. │

C. D. Hill │For Chicago, Ill. │_i_ = 120⁄(_t_ + 15)

Metcalf and │Louisville, Ky. Am. Sew. │_i_ = 14⁄_t_^½

Eddy │ Prac., Vol I. │

W. W. Horner│St. Louis, Mo. Eng. News,│_i_ = 56⁄(_t_ + 5)^{.85}

│ Sept. 29, 1910 │

R. A. │For Spokane, Wash. Eng. │_i_ = 23.92⁄(_t_ + 2.15) + 0.154

Brackenbuy│ Record, Aug. 10, 1912 │

Metcalf and │New Orleans │_i_ = 19⁄_t_^½

Eddy │ │

Metcalf and │For Denver, Colo. │_i_ = 84⁄(_t_ + 4)

Eddy │ │

│Central Park, N. Y. │

Kenneth │ 51–Year Record. Eng. │_i_ = 400⁄(2_t_ + 40)[23]

Allen │ News-Record, April 7, │

│ 1921, p. 588 │

────────────┴─────────────────────────┴────────────────────────────────

=30. Time of Concentration.=—By the time of concentration is meant the

longest time without unreasonable delay that will be required for a drop

of water[24] to flow from the upper limit of a drainage area to the

outlet. Assuming a rainfall to start suddenly and to continue at a

constant rate and to be evenly distributed over a drainage area of 100

per cent imperviousness and even slope towards one point, the rate of

run-off would increase constantly until the drop of water from the upper

limit of the area reached the outlet, after which the rate of run-off

would remain constant. In nature the rate of rainfall is not constant.

The shorter the duration of a storm the greater the intensity of

rainfall. Therefore the maximum run-off during a storm will occur at the

moment when the upper limit of the area has commenced to contribute.

From that time on the rate of run-off will decrease.

The time of concentration can be measured fairly well by observing the

moment of the commencement of a rainfall, and the time of maximum

run-off from an area on which the rain is falling. A prediction of the

time of concentration is more or less guess work. As the result of

measurements some engineers assume the time of concentration on a city

block built up with impervious roofs and walks, and on a moderate slope,

is about 5 to 10 minutes. This is used as a basis for the judgment of

the time of concentration on other areas. For relatively large drainage

areas such a method cannot be used. The procedure is to measure the

length of flow through the drainage channels of the area, to assume the

velocity of the flood crest through these channels and thus to determine

the time of concentration. Table 14 shows the flood crest velocities in

various streams of the Ohio River Basin under flood conditions. The

velocity over the surface of the ground may be approximated by the use

of the formula[25]

_V_ = 2,000_I_√(_S_),

in which _V_ = the velocity of flow over the surface of the ground in

feet per minute;

_I_ = the percentage imperviousness of the ground;

_S_ = the slope of the ground.

For areas up to 100 acres where natural drainage channels are not

existent this formula will give more satisfactory results than guesses

based on the time of concentration of certain known areas.

Having determined the time of concentration, the rate of rainfall _R_ to

be used in the Rational Method is found by substitution in some one of

the rainfall formulas given in Table 13.

TABLE 14

FLOOD CREST VELOCITIES IN OHIO RIVER BASIN IN MARCH, 1913

From Table 12. U. S. G. S., Water Supply Paper. No. 334

───────────┬───────────────┬────────┬────────┬───────────────┬─────────┬───────────┬────────

River │ Stations │ │Distance│ Distance of │Velocity │ Velocity │

│ │Distance│to Mouth│ Lower Station │ between │ from │ Time

│ │between │ of │ below │Stations,│Pittsburgh,│between

│ │Stations│ River, │Starting-point,│Miles per│ Miles per │Stations

│ │in Miles│ Miles │ Miles │ Hour │ Hour │in Hours

───────────┼───────────────┼────────┼────────┼───────────────┼─────────┼───────────┼────────

Ohio │Pittsburgh, │ │ │ │ │ │

│ Pa., to │ │ │ │ │ │

│ Wheeling, W. │ │ │ │ │ │

│ Va. │ 90│ 967│ 90│ 9.0│ 9.0│ 10.0

Ohio │Wheeling, W. │ │ │ │ │ │

│ Va., to │ │ │ │ │ │

│ Marietta, │ │ │ │ │ │

│ Ohio │ 82│ 877│ 172│ 5.9│ 7.2│ 14

Ohio │Marietta, Ohio,│ │ │ │ │ │

│ to │ │ │ │ │ │

│ Parkersburg, │ │ │ │ │ │

│ W. Va. │ 12│ 795│ 184│ 0.9│ 4.8│ 14

Ohio │Parkersburg to │ │ │ │ │ │

│ Point │ │ │ │ │ │

│ Pleasant, W. │ │ │ │ │ │

│ Va. │ 80│ 783│ 264│ 6.7│ 5.3│ 12

Ohio │Point Pleasant │ │ │ │ │ │

│ to │ │ │ │ │ │

│ Huntington, │ │ │ │ │ │

│ W. Va. │ 44│ 703│ 308│ 11.0│ 5.7│ 4

Ohio │Huntington to │ │ │ │ │ │

│ Catlettsburg,│ │ │ │ │ │

│ W. Va. │ 9│ 659│ 317│ 0.8│ 4.1│ 11

Ohio │Catlettsburg, │ │ │ │ │ │

│ W. Va., to │ │ │ │ │ │

│ Portsmouth, │ │ │ │ │ │

│ Ohio │ 38│ 650│ 355│ │ 5.0│

Ohio │Portsmouth │ │ │ │ │ │

│ Ohio, to │ │ │ │ │ │

│ Maysville, │ │ │ │ │ │

│ Ky. │ 52│ 612│ 407│ 5.2│ 5.0│ 10

Ohio │Maysville, Ky.,│ │ │ │ │ │

│ to │ │ │ │ │ │

│ Cincinnati, │ │ │ │ │ │

│ Ohio │ 61│ 560│ 468│ 6.8│ 5.2│ 9

Ohio │Cincinnati, │ │ │ │ │ │

│ Ohio, to │ │ │ │ │ │

│ Louisville, │ │ │ │ │ │

│ Ky. │ 136│ 499│ 604│ 11.4│ 5.9│ 12

Ohio │Louisville, │ │ │ │ │ │

│ Ky., to │ │ │ │ │ │

│ Evansville, │ │ │ │ │ │

│ Ind. │ 183│ 363│ 787│ 1.9│ 5.3│ 96

Ohio │Evansville, │ │ │ │ │ │

│ Ind., to Mt. │ │ │ │ │ │

│ Vernon Ind. │ 36│ 180│ 823│ 9.0│ 5.3│ 4

Ohio │Mt. Vernon, │ │ │ │ │ │

│ Ind., to │ │ │ │ │ │

│ Paducah, Ky.│ 101│ 144│ 924│ 2.1│ 4.6│ 48

Ohio │Paducah, Ky. to│ │ │ │ │ │

│ Cairo, Ill. │ 43│ 43│ 967│ 2.9│ 4.2│ 15

Monongahela│Fairmont, W. │ │ │ │ │ │

│ Va., to Lock │ │ │ │ │ │

│ No. 2 Pa. │ │ │ │ │ │

│ (Upper) │ 107│ 119│ 107│ 6.7│ │ 16

Little │Creston, W. │ │ │ │ │ │

Kanawha │ Va., to Dam. │ │ │ │ │ │

│ No. 4 W. Va. │ │ │ │ │ │

│ (Upper) │ 16│ 48│ 16│ 16.0│ │ 1

New │Radford, W. │ │ │ │ │ │

│ Va., to │ │ │ │ │ │

│ Hinton, W. │ │ │ │ │ │

│ Va. │ 78│ 139│ 78│ 3.0│ │ 26

Kanawha │Kanawha Falls, │ │ │ │ │ │

│ W. Va. to │ │ │ │ │ │

│ Charleston, │ │ │ │ │ │

│ W. Va. │ 37│ 95│ 37│ 2.6│ │ 14

Scioto │Columbus, Ohio,│ │ │ │ │ │

│ to │ │ │ │ │ │

│ Chillicothe, │ │ │ │ │ │

│ Ohio │ 52│ 110│ 52│ 4.7│ │ 11

Miami │Dayton, Ohio, │ │ │ │ │ │

│ to Hamilton, │ │ │ │ │ │

│ Ohio │ 44│ 77│ 44│ 14.7│ │ 3

Kentucky │Highbridge, │ │ │ │ │ │

│ Ky., to │ │ │ │ │ │

│ Frankfort, │ │ │ │ │ │

│ Ky. │ 52│ 117│ 52│ 5.2│ │ 10

Cumberland │Celina, Tenn. │ │ │ │ │ │

│ to Nashville,│ │ │ │ │ │

│ Tenn. │ 190│ 383│ 190│ 2.9│ │ 64.5

Tennessee │Knoxville to │ │ │ │ │ │

│ Chattanooga, │ │ │ │ │ │

│ Tenn. │ 183│ 635│ 183│ 3.2│ │ 57

───────────┴───────────────┴────────┴────────┴───────────────┴─────────┴───────────┴────────

NOTE.—The velocities shown are the velocities of the crest of the flood wave and are not the

average velocity of the flow of the river. The velocity of the crest of the flood wave

should be used in determining the time of concentration. The flood crest velocity is slower

then that of the river because of the storage in the river basin.

=31. Character of Surface.=—The proportion of total rainfall which will

reach the sewers depends on the relative porosity, or imperviousness,

and the slope of the surface. Absolutely impervious surfaces such as

asphalt pavements or roofs of buildings will give nearly 100 per cent

run-off regardless of the slope, after the surfaces have become

thoroughly wet. For unpaved streets, lawns, and gardens the steeper the

slope the greater the per cent of run-off. When the ground is already

water soaked or is frozen the per cent of run-off is high, and in the

event of a warm rain on snow covered or frozen ground, the run-off may

be greater than the rainfall. The run-off during the flood of March,

1913, at Columbus, Ohio, was over 100 per cent of the rainfall. Table

15[26] shows the relative imperviousness of various types of surfaces

when dry and on low slopes. The estimates for relative imperviousness

used in the design of the Cincinnati intercepter are given in Table 16.

TABLE 15

VALUES OF RELATIVE IMPERVIOUSNESS

Roof surfaces assumed to be water-tight 0.70– 0.95

Asphalt pavements in good order .85– .90

Stone, brick, and wood-block pavements with tightly cemented

joints .75– .85

The same with open or uncemented joints .50– .70

Inferior block pavements with open joints .40– .50

Macadamized roadways .25– .60

Gravel roadways and walks .15– .30

Unpaved surfaces, railroad yards, and vacant lots .10– .30

Parks, gardens, lawns, and meadows, depending on surface

slope and character of subsoil .05– .25

Wooded areas or forest land, depending on surface slope and

character of subsoil .01– .20

Most densely populated or built up portion of a city .70– .90

TABLE 16

COEFFICIENTS OF IMPERVIOUSNESS USED IN THE DESIGN OF THE CINCINNATI SEWERS

──────────────┬─────────────────────────────┬──────────────────┬───────────

Character of │ │ │Residential,

Improvement │ │ │291.1 A. 20

│ │ │ per Acre,

│ │ │ Middle

│ │ │ Class,

│ │ │ Detached

│ │ │Dwellings,

│ │ │Yellow and

│ │Combined Tenement │ Blue Clay

│ │ and Industrial. │ Overlying

│Typical Commercial Area, 30.4│ 35.6 A., 55 per │ Beds of

│A. None Undeveloped. Sand and│ Acre. Clay, Sand │ Shale and

│ Gravel │ and Gravel │ Sandstone

──────────────┼──────┬─────┬─────┬──────────┼──────┬─────┬─────┼─────┬─────

│ Area │ │ │Equivalent│ Area │ │ │ Per │

│ in │ Per │ │Imp. Area,│ in │ Per │ │Cent │

│1000’s│Cent │ I, │ 1000’s │1000’s│Cent │ I, │ of │ I,

│Square│Total│Esti-│ Square │Square│Total│Esti-│Total│Esti-

│ Feet │Area │mated│ Feet │ Feet │Area │mated│Area │mated

──────────────┼──────┼─────┼─────┼──────────┼──────┼─────┼─────┼─────┼─────

Roofs: │ │ │ │ │ │ │ │ │

Public and │ │ │ │ │ │ │ │ │

commercial│ 881.2│ 66.5│ 0.90│ 793.0│ 66.8│ 4.3│ 0.40│ 4.8│ 0.40

Residences │ │ │ │ │ 289.2│ 18.6│ .90│ 13.1│ .90

Barns and │ │ │ │ │ │ │ │ │

sheds │ │ │ │ │ 79.2│ 5.1│ .75│ 1.4│ .75

│ │ │ │ │ │ │ │ │

Interior │ │ │ │ │ │ │ │ │

Walks: │ │ │ │ │ │ │ │ │

Brick │ 7.5│ 0.6│ .40│ 3.0│ 35.6│ 2.3│ .40│ 0.6│ .40

Cement │ 10.0│ 0.7│ .75│ 7.5│ 22.6│ 1.5│ .75│ 2.6│ .75

│ │ │ │ │ │ │ │ │

Street Walks: │ │ │ │ │ │ │ │ │

Brick │ 6.1│ 0.5│ .40│ 2.4│ 48.2│ 3.1│ .40│ 1.0│ .40

Cement │ 139.3│ 10.5│ .75│ 104.5│ 78.1│ 5.0│ .75│ 3.4│ .75

│ │ │ │ │ │ │ │ │

Street │ │ │ │ │ │ │ │ │

Pavements: │ │ │ │ │ │ │ │ │

Asphalt, │ │ │ │ │ │ │ │ │

brick, │ │ │ │ │ │ │ │ │

wood block│ 145.5│ 11.0│ .85│ 123.7│ │ │ │ 5.0│ .85

Granite │ │ │ │ │ │ │ │ │

block │ 111.4│ 8.4│ .75│ 83.6│ │ │ │ 1.0│ .75

Macadam and │ │ │ │ │ │ │ │ │

cobble │ 23.2│ 1.8│ .40│ 9.3│ 238.6│ 15.4│ .40│ 4.8│ .40

Granite and │ │ │ │ │ │ │ │ │

poor │ │ │ │ │ │ │ │ │

macadam │ │ │ │ │ │ │ │ 0.4│ .20

│ │ │ │ │ │ │ │ │

Unimproved │ │ │ │ │ │ │ │ │

yards and │ │ │ │ │ │ │ │ │

lawns: │ │ │ │ │ 692.4│ 44.7│ .15│ │

Tributary to│ │ │ │ │ │ │ │ │

paved │ │ │ │ │ │ │ │ │

gutters │ │ │ │ │ │ │ │ 57.1│ .15

Not │ │ │ │ │ │ │ │ │

tributary │ │ │ │ │ │ │ │ │

to paved │ │ │ │ │ │ │ │ │

gutters │ │ │ │ │ │ │ │ 7.9│ .10

──────────────┼──────┼─────┼─────┼──────────┼──────┼─────┼─────┼─────┼─────

Total │1324.2│100.0│ │ 1127.0│1550.7│100.0│ │100.0│

──────────────┼──────┴─────┴─────┴──────────┼──────┴─────┴─────┼─────┴─────

Impervious │ │ │

coefficient │ │ │

for the │ │ │

district │ 85.1 │ 44.4 │ 35.9

──────────────┴─────────────────────────────┴──────────────────┴───────────

C. E. Gregory[27] states that _I_, in the expression _Q_ = _AIR_ is a

function of the time of concentration or the duration of the storm. If

_t_ represents the time of concentration and _T_ represents the duration

of the storm, then when _T_ is less than _t_

_I_ = 0.175_t_^⅓,

but when _T_ is greater than _t_,

_I_ = 0.175⁄_t_(_T_^{4/3} − (_T_ − _t_)^{4/3}).

Gregory condenses Kuichling’s rules with regard to the per cent run-off,

as follows:

1. The per cent of rainfall discharged from any given drainage

area is nearly constant for heavy rains lasting equal periods of

time.

2. This per cent varies directly with the area of impervious

surface.

3. This per cent increases rapidly and directly or uniformly with

the duration of the maximum intensity of the rainfall until a

period is reached which is equal to the time required for the

concentration of the drainage waters from the entire area at the

point of observation, but if the rainfall continues at the same

intensity for a longer period this per cent will continue to

increase at a much smaller rate.

4. This per cent becomes larger when a moderate rain has

immediately preceded a heavy shower on a partially permeable

territory.

Gregory’s formulas have not been generally accepted and are not widely

used in practice. Marston stated:[28]

All that engineers are at present, warranted in doing is to make

some deduction from 100 per cent run-off ... the deduction ...

being at present left to the engineer in view of his general

knowledge and his familiarity with local conditions.

Burger states[29] in the same connection:

In its application there will usually be as many results

(differing widely from each other) as the number of men using it.

In spite of these objections the Rational Method is in more favor with

engineers than any other method.

=32. Empirical Formulas.=—The difficulty of determining run-off with

accuracy has led to the production by engineers of many empirical

formulas for their own use. Some of these formulas have attracted wide

attention and have been used extensively, in some cases under conditions

to which they are not applicable. In general these formulas are

expressions for the run-off in terms of the area drained, the relative

imperviousness, the slope of the land, and the rate of rainfall.

The Burkli-Ziegler formula, devised by a Swiss engineer for Swiss

conditions and introduced into the United States by Rudolph Hering, was

one of the earliest of the empirical formulas to attract attention in

this country. It has been used extensively in the form

_Q_ = _CiA_∜(_S_⁄_A_),

in which_Q_ = the run-off in cubic feet per second;

_i_ = the maximum rate of rainfall in inches per hour over

the entire area. This is determined only by

experience in the particular locality, and is usually

taken at from 1 to 3 inches per hour;

_S_ = the slope of the ground surface in feet per thousand,

_A_ = the area in acres;

_C_ = an expression for the character of the ground surface,

or relative imperviousness. In this form of the

expression _C_ is recommended as 0.7.

The McMath formula was developed for St. Louis conditions and was first

published in Transactions of the American Society of Civil Engineers,

Vol. 16, 1887, p. 183. Using the same notation as above, the formula is,

_Q_ = _CiA_⁵√(_S_⁄_A_),

McMath recommended the use of _C_ equal to 0.75, _i_ as 2.75 inches per

hour, and _S_ equal to 15. The formula has been extended for use with

all values of _C_, _i_, _S_, and _A_ ordinarily met in sewerage

practice. Fig. 11 is presented as an aid to the rapid solution of the

formula.

[Illustration:

FIG. 11.—Diagram for the Solution of McMath’s Formula,

_Q_ = _Aci_⁵√_S_⁄_A_.

]

Other formulas have been devised which are more applicable to drainage

areas of more than 1,000 acres.[30] Such areas are met in the design of

sewers to enclose existing stream channels draining large areas.

Kuichling’s formulas, published in 1901 in the report of the New York

State Barge Canal, were devised for areas greater than 100 square miles.

The following modification of these formulas for ordinary storms on

smaller areas was published for the first time in American Sewerage

Practice, Volume I, by Metcalf and Eddy:

_Q_ = 25,000⁄(_A_ + 125) + 15.

[Illustration:

FIG. 12.—Comparison of Empirical Run-off Formulas.

]

It is to be noted that the only factor taken into consideration is the

area of the watershed. It is obvious that other factors such as the rate

of rainfall, slope, imperviousness, etc., will have a marked effect on

the run-off.

There are other run-off formulas devised for particular conditions, some

of which are of as general applicability as those quoted. Two formulas

which are frequently quoted are: Fanning’s, _Q_ = 200_M_^⅝ and Talbot’s

_Q_ = 500_M_^¼, in which _M_ is the area of the watershed in square

miles. A comprehensive treatment of the subject is given in American

Sewerage Practice, Vol. I, by Metcalf and Eddy.

A comparison of the results obtained by the application of a few

formulas to the same conditions is shown graphically in Fig. 12. It is

to be noted that the divergence between the smallest and largest results

is over 100 per cent. As these formulas are not all applicable to the

same conditions, the differences shown are due partially to an extension

of some of them beyond the limits for which they were prepared.

=33. Extent and Intensity of Storms.=—In the design of storm sewers it

is necessary to decide how heavy a storm must be provided for. The very

heaviest storms occur infrequently. To build a sewer capable of caring

for all storms would involve a prohibitive expense over the investment

necessary to care for the ordinary heavy storms encountered annually or

once in a decade. This extra investment would lie idle for a long period

entailing a considerable interest charge for which no return is easily

seen. The alternative is to construct only for such heavy storms as are

of ordinary occurrence and to allow the sewers to overflow on

exceptional occasions. The result will be a more frequent use of the

sewerage system to its capacity, a saving in the cost of the system, and

an occasional flooding of the district in excessive storms. The amount

of damage caused by inundations must be balanced against the extra cost

of a sewerage system to avoid the damage. A municipality which does not

provide adequate storm drainage is liable, under certain circumstances,

for damages occasioned by this neglect. It is not liable if no drainage

exists, nor is it liable if the storm is of such unusual character as to

be classed legally as an act of God.

Kuichling’s studies of the probabilities of the occurrence of heavy

storms are published in Transactions of the American Society of Civil

Engineers, Vol. 54, 1905, p. 192. Information on the extent of rain

storms is given by Francis in Vol. 7, 1878, p. 224, of the same

publication. Kuichling expresses the intensity of storms which will

occur,

once in 10 years as _i_ = 105⁄(_t_ + 20),

once in 15 years as _i_ = 120⁄(_t_ + 20),

in which _i_ is the intensity of rainfall in inches per hour and _t_ is

the duration of the storm in minutes.

CHAPTER IV

THE HYDRAULICS OF SEWERS

=34. Principles.=—The hydraulics of sewers deals with the application of

the laws of hydraulics to the flow of water through conduits and open

channels. In so far as its hydraulic properties are concerned the

characteristics of sewage are so similar to those of water that the same

physical laws are applicable to both. In general it is assumed that the

energy lost due to friction between the liquid and the sides of the

channel varies as some function of the velocity, usually the square, and

that the total energy passing any section of the stream differs from the

energy passing any other section only by the loss of energy due to

friction.

The general expression for the flow of sewage would then be,

_h_ = (_f_)_V_^n,

in which _h_ is the head or energy lost between any two sections, and

_V_ is the average velocity of flow between these sections. It is to be

noted in this general expression that the quantity and rate of flow past

all sections is assumed to be constant. This condition is known as

_steady flow_. Problems are encountered in sewerage design which involve

conditions of unsteady flow, and methods of solution of them have been

developed based on modifications of this general expression. The average

velocity of flow is computed by dividing the rate (quantity) of flow

past any section by the cross-sectional area of the stream at that

section. This does not represent the true velocity at any particular

point in the stream, as the velocity near the center is faster than that

near the sides of the channel. The distribution of velocities in a

closed circular channel is somewhat in the form of a paraboloid

superimposed on a cylinder.

The laws of flow are expressed as formulas the constants of which have

been determined by experiment. It has been found that these constants

depend on the character of the material forming the channel and the

hydraulic radius. The _hydraulic radius_ is defined as the ratio of the

cross-sectional area of the stream to the length of the wetted

perimeter, or line of contact between the liquid and the channel,

exclusive of the horizontal line between the air and the liquid.

=35. Formulas.=—The loss of head due to friction caused by flow through

circular pipes flowing full as expressed by Darcy is,

_h_ = _f_(_l_⁄_d_) (_V_^2⁄2_g_),

in which _h_ is the head lost due to friction in the distance _l_, _V_

is the velocity of flow, _g_ is the acceleration due to gravity, and _f_

is a factor dependent on _d_ and the material of which the pipe is made.

A formula for _f_ expressed by Darcy as the result of experiments on

cast-iron pipe is,

_f_ = 0.0199 + 0.00166⁄_d_,

in which _d_ is the diameter in feet. In using the formula with this

factor the units used must be feet and seconds.

Another form of the same expression is known as the Chezy formula. It is

an algebraic transformation of the Darcy formula, but in the form shown

here, by the use of the hydraulic radius, it is made applicable to any

shape of conduit either full or partly full. The Chezy formula is,

_V_ = _C_√(_RS_),

in which _R_ is the hydraulic radius, _S_ the slope ratio of the

hydraulic gradient, and _C_ a factor similar to _f_ in the Darcy

formula.

Kutter’s formula was derived by the Swiss engineers, Ganguillet and

Kutter, as the result of a series of experimental observations. It was

introduced into the United States by Rudolph Hering and its derivation

is given in Hering and Trautwine’s translation of “The Flow of Water in

Open Channels by Ganguillet and Kutter.” In English units it is,

_V_ = {(1.81/_n_ + 41.67 + .0028/_S_)/(1 + (_n_/√_R_)(41.67 +

(.0028/_S_)))}√(_RS_),

in which _n_ is a factor expressing the character of the surface of the

conduit and the other notation is as in the Chezy formula. _V_ is the

velocity in feet per second, _S_ is the slope ratio, and _R_ the

hydraulic radius in feet. The values of _n_ to be used in all cases are

not agreed upon, but in general the values shown below are used in

practice.

VALUES OF _n_ IN KUTTER’S FORMULA

_n_ CHARACTER OF THE MATERIALS

0.009 Well-planed timber.

0.010 Neat cement or very smooth pipe.

0.012 Unplaned timber. Best concrete.

Smooth masonry or brickwork, or concrete sewers under ordinary

0.013 conditions.

0.015 Vitrified pipe or ordinary brickwork.

0.017 Rubble masonry or rough brickwork.

0.020 } Smooth earth.

0.035

0.030 } Rough channels overgrown with grass.

0.050

Kutter’s formula is of general application to all classes of material

and to all shapes of conduits. It is the most generally used formula in

sewerage design.

The cumbersomeness of Kutter’s formula is caused somewhat by the attempt

to allow for the effect of the low slopes of the Mississippi River

experiments on the coefficients. The correctness of these experiments

has not been well established and the slopes are so flat that the

omission of the term 0.0028⁄_S_ will have no appreciable effect on the

value of _V_ ordinarily used in sewer design. The difference between the

value of _V_ determined by the omission of this term and the value of

_V_ found by including it is less than 1 per cent for all slopes greater

than 1 in 1,000 for 8 inch pipe (_R_ = 0.167 feet). As the diameter of

the pipe or the hydraulic radius of the channel increases up to a

diameter of 13.02 feet (_R_ = 3.28 feet), the difference becomes less

and at this value of _R_ there is no difference whether the slope is

included or not. For larger pipes the difference increases slowly. For a

16 foot pipe (_R_ = 4 feet) on a slope of 1 in 1,000 the difference is

less than 0.2 per cent, and on a slope of 1 in 10,000 the difference is

approximately 1 per cent. Flatter slopes than these are seldom used in

sewer design, except for very large sewers where careful determinations

of the hydraulic slope are necessary. It is therefore safe in sewer

design to use Kutter’s formula in the modified form shown below in which

the term (.0028)⁄_S_ has been omitted.

_V_ = (1.81 + 41.67_n_)_R_√_S_/_n_(√_R_ + 41.67_n_).

Bazin’s formula is

_V_ = √(_RS_)/√(α + β/_d_)

in which α and β are constants for different classes of material. For

cast-iron pipe α is 0.00007726 and β is 0.00000647. This formula is

seldom used in sewerage design.

Exponential formulas have been developed as the result of experiments

which have demonstrated that _V_ does not vary as the one-half power of

_R_ and _S_ but that the relation should be expressed as,

_V_ = _CR_^{_p_}_S_^{_q_},

in which _p_ and _q_ are constants and _C_ is a factor dependent on the

character of the material. The various formulas coming under this

classification have been given the names of the experimenters proposing

them. Examples of these formulas are: Flamant’s, in English units, for

new cast-iron pipe, which is,

_V_ = 232_R_^{.715}_S_^{.572},

and Lampé’s for the same material which is,

_V_ = 203.3_R_^{.694}_S_^{.555}.

These formulas are useful only for the material to which they apply, but

they can be used for conduits of any shape. A. V. Saph and E. W. Schoder

have shown[31] that the general formula for all materials lies between

the limits,

_V_ = (93 to 142)_S_^{.50 to .55}_R_^{.63 to .69}.

Hazen and Williams’ formula is in the form,

_V_ = 1.31_CR_^{.63}_S_^{.54},

in which _C_ is a factor dependent on the character of the material of

the conduit. The values of _C_ as given by Hazen and Williams are,

_C_ CHARACTER OF MATERIAL

95 Steel pipe under future conditions. (Riveted steel.)

Cast iron under ordinary future conditions and brick

100 sewers in good condition.

110 New riveted steel, and cement pipe.

120 Smooth wood or masonry conduits under ordinary conditions.

Masonry conduits after some time and for very smooth pipes

such as glass, brass, lead, etc., when old, and for new

130 cast-iron pipe under ordinary conditions.

This formula is of as general application as Kutter’s formula and is

easier of solution, but being more recently in the field and because of

the ease of the solution of Kutter’s formula by diagrams it is not in

such general use. Exponential formulas are used more in waterworks than

in sewerage practice.

Manning’s formula is in the form,

_V_ = 1.486⁄_n__R_^⅔_S_^½

in which _n_ is the same as for Kutter’s formula. Charts for the

solution of Manning’s formula are given in Eng. News-Record, Vol. 85,

1920, p. 837.

=36. Solution of Formulas.=—The solution of even the simplest of these

formulas, such as Flamant’s, is laborious because of the exponents

involved. Darcy’s and Kutter’s formulas are even more cumbersome because

of the character of the coefficient. The labor involved in the solution

of these formulas has resulted in the development of a number of

diagrams and other short cuts. Since each formula involves three or more

variables it cannot be represented by a single straight line on

rectangular coordinate paper. The simplest form of diagram for the

solution of three or more variables is the nomograph, an example of

which is shown in Fig. 13 for the solution of Flamant’s formula. A

straight-edge placed on any two points of the scales of two different

vertical lines will cross the other line at a point on the scale

corresponding to its correct value in the formula. Such a diagram is in

common use for the solution of problems for the flow of water in

cast-iron pipe.

[Illustration:

FIG. 13.—Diagram for the Solution of Flamant’s Formula for the Flow of

Water in Cast-iron Pipe.

]

Fig. 14 has been prepared to simplify the solution of Hazen and

Williams’ formula. The scales of slope for different classes of material

are shown on vertical lines to the left of the slope line. For use these

scales must be projected horizontally on the slope line. The scales for

other factors are shown on independent reference lines.

For example let it be required to find the loss of head in a 12

inch pipe carrying 1 cubic foot per second when the coefficient of

roughness is 100. A straight-edge placed at 1.0 cubic feet per

second on the quantity scale, and 12 inches on the diameter scale

crosses the slope line at .00092 opposite the slope scale for _c_

= 100. It crosses the velocity line at 1.31 feet per second.

Kutter’s formula is the most commonly used for sewer design and has been

generally accepted as a standard in spite of its cumbersomeness. Fig. 15

is a graphical solution of Kutter’s formula for small pipes, and Fig. 16

for larger pipes. The diagrams are drawn on the nomographic principle

and give solutions for a wide range of materials, but they are specially

prepared for the solution of problems in which _n_ = .015. In their

preparation the effect of the slope on the coefficient has been

neglected. Fig. 17 is drawn on ordinary rectangular coordinate paper and

can be used only for the solution of problems in which _n_ = .015. Both

diagrams are given for practice in the use of the different types.

[Illustration:

FIG. 14.—Diagram for the Solution of Hazen and Williams’ Formula.

]

[Illustration:

FIG. 15.—Diagram for the Solution of Kutter’s Formula.

For values of _n_ between 0.010 and 0.020. Specially arranged for _n_

= 0.015. Values of Q from 0.1 to 10 second-feet.

]

[Illustration:

FIG. 16.—Diagram for the Solution of Kutter’s Formula.

For values of _n_ between 0.010 and 0.020. Specially arranged for _n_

= 0.015. Values of Q from 10 to 1,000 second-feet.

]

[Illustration:

FIG. 17.—Diagram for the Solution of Kutter’s Formula.

]

[Illustration:

FIG. 18.—Conversion Factors for Kutter’s Formula.

]

In Figs. 15 and 16 the diameter scales are varied for different values

of the roughness coefficient _n_. The velocity scale is shown _only for

a value of n = .015_. The velocity for other values of _n_ can be

determined by the method given in the following paragraphs.

37. =Use of Diagrams.=—There are five factors in Kutter’s formula: _n_,

_Q_, _V_, _d_ (or _R_), and _S_. If any three of these are given the

other two can be determined, except when the three given are _Q_, _V_,

and _d_. These three are related in the form _Q_ = _AV_, which is

independent of slope or the character of the material. There are only

nine different combinations possible with these five factors, which will

be met in the solution of Kutter’s formula. The solution of the problems

by means of the diagrams is simple when the data given include _n_

= .015. For other given values of _n_ the solution is more complicated.

Results of the solution of types of each of the nine problems are given

in Table 17 and the explanatory text below.

_If n is given and is equal to .015_, the solution is simple.

For example in Table 17 _case 1, example 1_; to be solved on Fig.

15. Place a straight-edge at 1.0 on the _Q_ line and at 6 inches

on the diameter line for _n_ = .015. The slope and the velocity

will be found at the intersection of the straight-edge with these

respective scales.

All problems in which _n_ is given as .015 and the solution for which

falls within the limits of Fig. 15 or 16 should be solved by placing a

straight-edge on the two known scales and reading the two unknown

results at the intersection of the straight-edge and the remaining

scales.

For example in _case 1_, _example 2_ find the intersection of the

horizontal line representing _Q_ = 100 with the sloping diameter

line representing _d_ = 48 inches. The vertical slope line passing

through this point represents _S_ = .0065 and the sloping velocity

line passing through this point represents 8.5 feet per second.

In general problems in which _n_ = .015, can be solved on Fig. 17 by

finding the intersection of the two lines representing the given data,

and reading the values of the remaining variables represented by the

other two lines passing through this point.

TABLE 17

SOLUTIONS OF PROBLEMS BY KUTTER’S FORMULA

─────┬───────┬────────────────────────────┬────────────────────────────

Case │Example│ Given │ Found

─────┼───────┼─────┬─────┬────┬────┬──────┼─────┬─────┬────┬────┬──────

│ │ _n_ │ _Q_ │_V_ │_d_ │ _S_ │ _n_ │ _Q_ │_V_ │_d_ │ _S_

─────┼───────┼─────┼─────┼────┼────┼──────┼─────┼─────┼────┼────┼──────

1 │ 1 │0.015│ 1.0│ 2.5│ 6│ │ │ │5.0 │ │0.0575

1 │ 2 │ .015│100.0│ │ │ │ │ │8.5 │ │.0065

1 │ 3 │ .020│ 1.0│ │ 6│ │ │ │5.0 │ │.13

1 │ 4 │ .020│100.0│ │ 48│ │ │ │8.5 │ │.0125

2 │ 1 │ .015│ 5.0│ │ │0.0003│ │ │1.2 │28 │

2 │ 2 │ .010│ 5.0│ │ │.0003 │ │ │1.7 │23.5│

3 │ 1 │ .015│ │ │ 18│.002 │ │ 4.0│2.25│ │

3 │ 2 │ .018│ │ │ 18│.0008 │ │ 2.0│1.1 │ │

4 │ 1 │ .015│ 2.0│ 2.5│ │ │ │ │ │12 │.00475

4 │ 2 │ .011│ 2.0│ 2.5│ │ │ │ │ │12 │.0022

5 │ 1 │ .015│ │ 5.0│ 36│ │ │ 35.0│ │ │.0038

6 │ 1 │ .018│ │ 5.0│ │.001 │ │185.0│ │80 │

7 │ 1 │ │ 3.0│ │ 18│.002 │0.019│ │1.7 │ │

7 │ 2 │ │ 50.0│ │ 36│.005 │ .012│ │7.0 │ │

8 │ 1 │ │ 6.0│ 2.5│ │.003 │ .018│ │ │21 │

9 │ 1 │ │ │ 4.2│ 66│.00059│ .011│100.0│ │ │

─────┴───────┴─────┴─────┴────┴────┴──────┴─────┴─────┴────┴────┴──────

_If n is given and is not equal to .015_ the solution is not so simple.

In Fig. 15 and 16 the diagram is so drawn that the _position_ of the

diameter scales for all values of _n_ is fixed on the vertical

“diameter” line. The _scales_ of diameter change for each value of _n_.

These scales of diameter are shown for each value of _n_ from .010

to .020 on vertical lines to the left of the “diameter” line. For use,

the proper diameter scale for any given value of _n_ must be projected

horizontally upon the vertical “diameter” line. The velocity can be

determined on Fig. 15 and 16, _only when the diameter has been

determined_ and then _only when the diameter scale for n equal .015 is

used, since the only scale shown for velocity is for n = .015._

For example, in _Case 1_, _Example 3_ there are given _n_ = .020,

_Q_, and _d_. Find the intersection of the vertical line for _n_ =

.020 with the sloping diameter line for _d_ = 6 inches. Project

the intersection horizontally to the right to the vertical

“diameter” line. Place a straight-edge at this point and at _Q_ =

1.0 on the quantity scale. The required value of _S_ is read at

the intersection of the straight-edge and the slope scale and is

equal to 0.13. The intersection of the straight-edge in this

position with the velocity scale is not the required value of the

velocity since the velocity scale is made out for _n_ = .015 and

not .020. It is necessary to change the position of the

straight-edge so that it may lie on _Q_ equal 1.0 and on _d_ equal

6 inches for _n_ equal .015. The value of _V_ is shown in this

position as 5 feet per second.

The reverse process for Fig. 15 and 16 is illustrated _by Case 4_,

_Example 2_ in which _n_ = .011 and _Q_ and _V_ are also given.

When _Q_ and _V_ are given the value of _d_ is fixed independent

of all other factors. Therefore the value of _d_ can be read from

the scale with _n_ = .015 and is found to be 12 inches. Now find

the value of _d_ = 12 inches on the scale for _n_ = .011 and

project on to the “diameter” line. Place the straight-edge at this

point and at _Q_ = 2. The required slope is read as .0022.

Fig. 17 is prepared for the solution of problems in which _n_ = .015

only. For problems in which _n_ has some other value it is necessary to

transform the data to equivalent conditions in which _n_ = .015. This is

done by means of the conversion factors shown in Fig. 18. The given

slope or velocity is multiplied by the proper factor to convert from or

to the value of _n_ = .015.

For example in _Case 1_, _Example 4_ there are given _n_ = .020,

_Q_, and _d_. With _Q_ and _d_ given the value of _V_ can be read

from Fig. 17 without conversion. The corresponding value of _S_

for _n_ = .015 is .0065. It is now necessary to use the

transformation diagram Fig. 18. The hydraulic radius of the given

pipe is one foot. On Fig. 18 at the intersection of the slope line

for _R_ = 1.0 foot and _n_ = .020 the value of the factor is read

as 1.92. Since the given _n_ is for rougher material than that

represented by _n_ = .015 the required slope must be greater than

for _n_ = .015 to give the same velocity. It is therefore

necessary to multiply .0065 × 1.92 and the required slope is

.0125.

In _Case 6_, _Example 1_ there are given _n_ = .018, _d_, and _S_.

The remaining factors are to be solved by Fig. 17. Solve first as

though _n_ = .015 in order to find an approximate value of _d_ or

_R_. In this case it is evident that _d_ is greater than 57

inches. The value of _R_ is therefore about 1.25. Referring to

Fig. 18 the conversion factor for the slope for _n_ = .018 is

about 1.52. Since the given slope for _n_ = .018 is .001, for an

equal velocity and for _n_ = .015 the slope should be less.

Therefore in reading Fig. 17 it is necessary to use a slope of

.001⁄1.52 = .00066. The diameter is found to be about 80 inches.

Since this is nearer to the correct diameter the value of the

conversion factor must be corrected for this approximation. The

hydraulic radius for an 80 inch pipe is 1.67 feet, and the

conversion factor from Fig. 18 is about 1.48. The slope for _n_ =

.015 should be therefore .001⁄1.48 = .000675 and from Fig. 17 the

required diameter and quantity are read as 80 inches and 185

second-feet, respectively.

_If n is not given_ but must be solved for, the solution on Fig. 15 and

16 is relatively simple. The desired value of _n_ is read at the

intersection of the sloping diameter line representing the known

diameter and the horizontal projection of the intersection of the

straight-edge with the vertical “diameter” line.

For example in _Case 7_, _Example 1_ there are given _Q_, _d_, and

_S_. Lay the straight-edge on the given values of _Q_ = 3 and _S_

= .002. At the point where the straight-edge crosses the vertical

“diameter” line project a horizontal line to the sloping diameter

line for _d_ = 18 inches. The vertical line passing through this

point represents a value of _n_ = .019. In order to find the value

of _V_ lay the straight-edge on _Q_ = 3 and _d_ = 18 inches for

_n_ = .015. The value of _V_ is read as 1.7.

A slightly different condition is illustrated in the solution of

_Case 8_, _Example 1_ in which _Q_, _V_ and _S_ are given.

Determine first the value of _d_ as though _n_ = .015. Then

proceed to determine _n_ as in the preceding examples.

The solution for an unknown value of _n_ on Fig. 17 is not so simple. It

must be determined by working backwards from the conversion factor.

For example in _Case 7_, _Example 2_ there are given _Q_, _d_, and

_S_. The value of _V_ is read directly as though _n_ = .015 as 7

feet per second. The value of _S_ read for _n_ = .015 is .0075.

But the given slope is .005. Since the given slope is flatter than

that for _n_ = .015 the conversion factor is less than unity and

is therefore .005⁄.0075 = 0.67. With this value of the conversion

factor and the value of _R_ given as 0.75 the value of _n_ is read

from Fig. 18 as slightly greater than .012.

=38. Flow in Circular Pipes Partly Full.=—The preceding examples have

involved the flow in circular pipes completely filled. The same methods

of solution can be used for pipes flowing partly full except that the

hydraulic radius of the wetted section is used instead of the diameter

of the pipe. Diagrams are used to save labor in finding the hydraulic

radius and the other hydraulic elements of conduits flowing partly full.

The hydraulic elements of a conduit for any depth of flow are: (_a_) The

hydraulic radius, (_b_) the area, (_c_) the velocity of flow, and (_d_)

the quantity or rate of discharge. The velocity and quantity when partly

full as expressed in terms of the velocity and quantity when full as

calculated by Kutter’s formula will vary slightly with different

diameters, slopes and coefficients of roughness. The other elements are

constant for all conditions for the same type of cross-section. The

hydraulic elements for all depths of a circular section for two

different diameters and slopes are shown in Fig. 19. The differences

between the velocity and quantity under the different conditions are

shown to be slight, and in practice allowance is seldom made for this

discrepancy.

In the solution of a problem involving part full flow in a circular

conduit the method followed is to solve the problem as though it were

for full flow conditions and then to convert to partial flow conditions

by means of Fig. 19, or to convert from partial flow conditions to full

flow conditions and solve as in the preceding section.

For example let it be required to determine the quantity of flow

in a 12–inch diameter pipe with _n_ = .015 when on a slope of .005

and the depth of flow is 3 inches. First find the quantity for

full flow. From Fig. 15 this is 2.0 cubic feet per second. The

depth of flow of 3 inches is one-fourth or 0.25 of the full depth

of 12 inches. From Fig. 19, running horizontally on the 0.25 depth

line to meet the quantity curve, the proportionate quantity at

this depth is found to be on the 0.13 vertical line, and the

quantity of flow is therefore 2 × 0.13 = 0.26 cubic feet per

second.

[Illustration:

FIG. 19.—Hydraulic Elements of Circular Sections.

]

_d_ = 12′ 0″ _s_ = .0004 _n_ = .015

_d_ = 1′ 0″ _s_ = .01 _n_ = .013

Another problem, involving the reversal of this process is illustrated

by the following example:

Let it be required to determine the diameter and full capacity of

a vitrified pipe sewer on a grade of 0.002 if the velocity of flow

is 3.0 feet per second when the sewer is discharging at 30 per

cent of its full capacity, the depth of flow being 12 inches. From

Fig. 19 the depth of flow when the sewer is carrying 30 per cent

of its full capacity is 0.38 of its full depth. Since the partial

depth is 12 inches the full diameter is 12⁄.038 = 31.6 inches. The

velocity of flow at 38 per cent depth is 86 per cent of the full

velocity. Since the velocity given is 3.0 feet per second, the

full velocity is 3.0⁄.86 = 3.5 feet per second. With a full

velocity of 3.5 feet per second and a diameter of 31.6 inches from

Fig. 16 the full capacity of the sewer is 18 cubic feet per

second.

=39. Sections Other than Circular.=—The ordinary shape used for small

sewers is circular. The difficulty of constructing large sewers in a

circular shape, special conditions of construction such as small head

room, soft foundations, etc., or widely fluctuating conditions of flow

have led to the development of other shapes. For conduits flowing full

at all times a circular section will carry more water with the same loss

of head than any other section under the same conditions. In any section

the smaller the flow the slower the velocity, an undesirable condition.

The ideal section for fluctuating flows would be one that would give the

same velocity of flow for all quantities. Such a section is yet to be

developed. Sections have been developed that will give relatively higher

velocities for small quantities of flow than are given by a circular

section. The best known of these sections is the egg shape, the

proportions and hydraulic elements of which are shown in Fig. 20. Other

shapes that have the same property, but which were not developed for the

same purpose are the rectangular, the U-shape, and the section with a

cunette. The egg-shaped section has been more widely used than any other

special section. It is, however, more difficult and expensive to build

under certain conditions, and has a smaller capacity when full than a

circular sewer of the same area of cross-section. Various sections are

illustrated in Fig. 22 and 23.

The U-shaped section is suitable where the cover is small, or close

under obstructions where a flat top is desirable and the fluctuations of

flow are so great as to make advantageous a special shape to increase

the velocity of low flows. The proportions of a U-shaped section are

shown in Fig. 23 (6). Other sections used for the same purpose are the

semicircular and special forms of the rectangular section.

The proportions and the hydraulic elements of the square-shaped section

are shown in Fig. 21. This is useful under low heads where a flat roof

is required to carry heavy loads, and the fluctuations of flow are not

large.

Sections with cunettes have not been standardized. A cunette is a small

channel in the bottom of a sewer to concentrate the low flows, as shown

in Fig. 22 (7). A cunette can be used in any shape of sewer.

[Illustration:

FIG. 20.—Hydraulic Elements of an Egg-shaped Section.

_d_ = 6′ 0″ _s_ = .00065 _n_ = .015

]

[Illustration:

FIG. 21.—Hydraulic Elements of a Square Section.

_d_ = 10′ 0″ _s_ = .0004 _n_ = .015

]

Sections developed mainly because of the greater ease of construction

under certain conditions are the basket handle, the gothic, the

catenary, and the horse shoe. Some of these shapes are shown in Fig. 22

and 23. They are suitable for large sewers on soft foundations, where it

is desirable to build the sewer in three portions, such as invert, side

walls, and arch. They are also suitable for construction in tunnels

where the shape of the sewer conforms to the shape of the timbering, or

in open cut work where the shape of the forms are easier to support.

Problems of flow in all sections can be solved by determining the

hydraulic radius involved, and substituting directly in the desired

formula, or by the use of one of the diagrams after converting to the

equivalent circular diameter. The determination of the hydraulic radius

of these special sections is laborious, and hence other less difficult

methods are followed. Problems are more commonly solved by converting

the given data into an equivalent circular sewer, solving for the

elements of this circular sewer and then reconverting into the original

terms, or by working in the other direction. The hydraulic elements of

various sections when full are given in Table 18.

TABLE 18

HYDRAULIC ELEMENTS OF SEWER SECTIONS. SEWERS FLOWING FULL.

───────────────┬─────────────┬─────────────┬─────────────┬──────────────

Section │Area in Terms│ Hydraulic │ Vert. Dia. │ Source

│ Vertical │ Radius in │_D_ in Terms │

│ Diameter │ terms of │ of Dia. _d_ │

│Squared _D_^2│Vertical Dia.│of Equivalent│

│ │ _D_ │ Circular │

│ │ │ Section │

───────────────┼─────────────┼─────────────┼─────────────┼──────────────

Circular │ 0.7854│ 0.250 │1.000 │

Egg │ 0.5150│ .1931│1.295 │Eng. Record,

│ │ │ │ Vol. 72: 608

Ovoid │ 0.5650│ .2070│1.208 │Eng. Record,

│ │ │ │ Vol. 72: 608

Semi-elliptical│ 0.8176│ .2487│1.041 │Eng. News,

│ │ │ │ Vol. 71: 552

Catenary │ 0.6625│ .2237│1.1175 │Eng. Record,

│ │ │ │ Vol. 72: 608

Horseshoe │ 0.8472│ .2536│0.985 │Eng. Record,

│ │ │ │ Vol. 72: 608

Basket handle │ 0.8313│ .2553│0.979 │Eng. Record,

│ │ │ │ Vol. 72: 608

Rectangular │ 1.3125│ .2865│0.7968 │Hydraulic

│ │ │ │ Dgms. and

│ │ │ │ Tbls.

│ │ │ │ Garrett

Square (3 sides│ 1.0000│ .333 │0.7500 │Eng. Record,

wet) │ │ │ │ Vol. 72: 608

Square (4 sides│ 1.0000│ .250 │1.0000 │Eng. Record,

wet) │ │ │ │ Vol. 72: 608

───────────────┴─────────────┴─────────────┴─────────────┴──────────────

[Illustration:

1. Standard Egg-shaped Section, North Shore Intercepter, Chicago,

Illinois.

]

[Illustration:

Sewerage and Sewage Treatment · 第 21 / 29 章