an aggregate capacity equal to nine days’ supply, but the proportion
varies widely with the different companies. It is desired that the
water held in reserve shall be alone used while the river is in flood,
as, owing to its increased pollution, it is regarded as far more
dangerous than the water at other times; but as no record is kept of
the times when raw sewage is discharged, and no exact information is
available in regard to the times when the companies do not take in
raw water, it can safely be assumed that a considerable amount of raw
sewage does become mixed with the water which is drawn by the companies.
The water drawn from the river is filtered through 113 filters having
an area of 116 acres. None of the filters are covered, and with an
average January temperature of 39° but little trouble with ice is
experienced. A few new filters are provided with appliances for
regulating the rate on each filter separately and securing regular and
determined rates of filtration, but nearly all of the filters are of
the simple type described on page 48, and the rates of filtration are
subject to more or less violent fluctuation, the extent of which cannot
be determined.
The area of filters is being continually increased to meet increasing
consumption; the approximate areas of filters in use having been as
follows:
1839 First filters built
1855 37 acres
1866 47 acres
1876 77 acres
1886 104 acres
1894 116 acres
There has been a tendency to reduce somewhat the rate of filtration. In
1868, with 51 acres of filters, the average daily quantity of water
filtered was 111,000,000 gallons, or 2,180,000 gallons per acre. In
1884, with 97 acres of filter surface, the daily quantity filtered was
157,000,000 gallons, or 1,620,000 gallons per acre; and in 1893, with
116 acres of filter surface and 195,000,000 gallons daily, the yield
per acre was 1,680,000 gallons.
Owing to the area of filter surface out of use while being cleaned,
the variations in consumption of water, and the imperfections of the
regulating apparatus, the actual rates of filtration are often very
much higher and at times may easily be double the figures given.
Evidence regarding the healthfulness of the filtered river-water was
collected and examined in a most exhaustive manner in 1893 by a Royal
Commission appointed to consider the water-supply of the metropolis in
all its aspects with reference to future needs. This commission was
unable to obtain any evidence whatever that the water as then supplied
was unhealthy or likely to become so, and they report that the rivers
can safely be depended upon for many years to come.
The numbers of deaths from all causes and from typhoid fever annually
per million of inhabitants for the years 1885-1891 in the populations
receiving their waters from different sources in London were as follows:
Water used. Deaths from Deaths from
All Causes. Typhoid Fever.
Filtered Thames water only 19,501 125
Filtered Lea water only 21,334 167
Kent wells only 18,001 123
Thames and Lea jointly 18,945 138
Thames and Kent jointly 18,577 133
The population supplied exclusively from the Lea by the East London
Company is of a poorer class than that of the rest of London, and this
may account for the slightly higher death-rate in this section. Aside
from this the rate is remarkably uniform and shows no great difference
between the section drinking ground-water only and those drinking
filtered river-waters. The death-rate from typhoid fever is also very
uniform and, although higher than that of some Continental cities with
excellent water-supplies (Berlin, Vienna, Munich, Dresden), is very
low—lower than in any American city of which I have records.
In this connection, it was shown by the Registrar-General that there
is only a very small amount of typhoid fever on the watersheds of
the Thames and Lea, so that the danger of infection of the water as
distinct from pollution is less than would otherwise be the case. Thus
for the seven years above mentioned the numbers of deaths from typhoid
fever per million of population were only 105 and 120 on the watersheds
of the Thames and the Lea respectively, as against 176 for the whole of
England and Wales.
LONDON FILTERS, 1896.
Twenty-sixth Annual Report of the Local Government Board, pages 206-213.
--------------+-------+---------+-----------------+--------------------------
|Amount |Average | Average Rate | Bacterial Efficiency.
| of |Thickness| of Filtration. |
|Storage| of +--------+--------+--------+--------+--------
| Raw | Sand, |Imperial|Millions|Maximum.|Minimum.|Average.
Company. |Water, | Feet. |Gallons | U. S. | | |
| Days. | | per |Gallons | | |
| | | Square |per Acre| | |
| | |Foot per| Daily. | | |
| | | Hour. | | | |
--------------+-------+---------+--------+--------+--------+--------+--------
Chelsea | 12.0 | 4.0 | 1.75 | 2.19 | 99.92 | 99.62 | 99.86
West Middlesex| 5.6 | 2.75 | 1.25 | 1.56 | 99.94 | 91.48 | 99.79
Southwark & | | | | | | |
Vauxhall | 4.1 | 2.5 | 1.5 | 1.88 | 100.00 | 84.33 | 97.77
Grand Junction| 3.3 | 2.25 | 1.63 | 2.05 | 99.98 | 84.03 | 99.31
Lambeth | 6.0 | 2.8 | 2.08 | 2.60 | 99.97 | 96.45 | 99.81
New River | 2.2 | 4.4 | 1.89 | 2.37 | 100.00 | 77.14 | 99.07
East London | 15.0 | 2.0 | 1.33 | 1.67 | 99.93 | 97.03 | 99.56
--------------+-------+---------+--------+--------+--------+--------+--------
APPENDIX VI.
THE BERLIN WATER-WORKS.
The original works were built by an English company in 1856, and were
sold to the city in 1873 for $7,200,000.
The water was taken from the river Spree at the Stralau Gate, which
was then above, but is now surrounded by, the growing city. The water
was always filtered, and the original filters remained in use until
1893, when they were supplanted by the new works at Lake Müggel. Soon
after acquiring the works the city introduced water from wells by Lake
Tegel as a supplementary supply, but much trouble was experienced from
crenothrix, an organism growing in ground-waters containing iron, and
in 1883 this supply was replaced by filtered water from Lake Tegel.
With rapidly-increasing pollution of the Spree at Stralau the purity
of this source was questioned, and in 1893 it was abandoned (although
still held as a reserve in case of urgent necessity), the supply now
being taken from the river ten miles higher up, at Müggel.
The watershed of the Spree above Stralau, as I found by map
measurement, is about 3800 square miles; the average rainfall is about
25 inches yearly. At extreme low water the river discharges 457 cubic
feet per second, or 295 million gallons daily, and when in flood 5700
cubic feet per second may be discharged. The city is allowed by law to
take 46 million gallons daily for water-supply, and this quantity can
be drawn either at Stralau or at Müggel.
Above Stralau the river is polluted by numerous manufactories and
washing establishments, and by the effluent from a considerable part
of the city’s extensive sewage farms. The shipping on this part of the
river also is heavy, and sewage from the boats is discharged directly
into the river. The average number of bacteria in the Spree at this
point is something over ten thousand per cubic centimeter, and 99.6 per
cent of them were removed by the filters in 1893.
The watershed of the Spree above the new water-works at Müggel I found
by map measurement to be 2800 square miles, and the low water-discharge
is said to be 269 million gallons daily. The river at this point flows
through Lake Müggel, which forms a natural sedimentation-basin, and the
raw water is quite clear except in windy weather.
There were 16 towns on the watershed with populations above 2000 each
in 1890, and an aggregate population of 132,000, which does not include
the population of the smaller places or country districts. None of
these places purify their sewage so far as they have any. Fürstenwalde
with a population of 12,935, and 22 miles above Müggel, has surface
sewers discharging directly into the river. Above Fürstenwalde the
river runs through numerous lakes which probably remove the effect
of the pollution from the more distant cities. There is considerable
shipping on the river for some miles above Fürstenwalde (which forms a
section of the Friedrich Wilhelm Canal), but hardly any between Müggel
and Fürstenwalde. The raw water at Müggel contains two or three hundred
bacteria per cubic centimeter, and is thus a comparatively pure water
before filtration. It is slightly peaty and the filtered water has a
light straw color.
Lake Tegel, which supplies the other part of the city’s supply, is an
enlargement of the river Havel. The watershed above Tegel I find to be
about 1350 square miles, and the annual rainfall is about 22 inches.
The low water-discharge is said to be 182 million gallons daily, and
the city is allowed by law to take 23 million gallons for water-supply.
There were ten towns upon the watershed with populations above 2000
each in 1890, and with an aggregate population of 44,000. Of these
Tegel is directly upon the lake with a population of 3000, and
Oranienburg, 14 miles above, has a population of 6000 and is rapidly
increasing. The shipping on the lake and river is heavy. The lake water
ordinarily contains two or three hundred bacteria per cubic centimeter.
The lake is shallow and becomes turbid in windy weather.
There are 21 filter-beds at Tegel with a combined area of 12.40 acres
to furnish a maximum of 23 million gallons of water daily, and 22
filters at Müggel with a combined area of 12.7 acres to deliver the
same quantity. Twenty-two more filters will be built at Müggel within
a few years to purify the full quantity which can be taken from the
river. All of these filters are covered with brick arches supported by
pillars about 16 feet apart from centre to centre in each direction,
and the whole is covered by nearly 3 feet of earth, making them quite
frost-proof. The original filters at Stralau were open, but much
difficulty was experienced with them in winter.
The bottom of the filters at Tegel consists of 8 inches of concrete
above 20 inches of packed clay and with 2 inches of cement above, and
slopes slightly from each side to the centre. The central drain goes
the whole length of the filters and has a uniform cross-section of
about 1/7300 of the area of the whole bed. There are no lateral drains,
but the water is brought to the central drain by a twelve-inch layer
of stones as large as a man’s fist; above this there is another foot
of gravel of graded sizes supporting two feet of fine sand, which is
reduced by scraping to half its thickness before the sand is replaced.
The average depth of water above the sand is nearly 5 feet. The filters
are not allowed to filter at a rate above 2.57 million gallons per
acre daily, and at this rate with 70 per cent of the area in service
the whole legal quantity of water can be filtered. The filters work
at precisely the same rate day and night, and the filtered water
is continuously pumped as filtered to ample storage reservoirs at
Charlottenburg. The pumps which lift the water from the lake to the
filters work against a head of 14 feet. The apparatus for regulating
the rate of filtration was described on page 51.
As yet no full description of the Müggel works has been published, but
they resemble closely the Tegel works. Both were designed by or under
the direction of the late director of the water-works, Mr. Henry Gill.
The average daily quantity of water supplied for the fiscal year ending
March 31, 1893, was 29,000,000 gallons daily, which estimate allows
10 percent for the slip of the pumps. Of this quantity 9,650,000 was
furnished by Stralau and 19,350,000 by Tegel. The greatest consumption
in a single day was 43,300,000 gallons, or 26.6 gallons per head,
while the average quantity for the year was 18.4 gallons per head. All
water without exception is sold by meter, the prices ranging from 27.2
cents a thousand gallons for small consumers to 13.6 cents for large
consumers and manufacturers. The average receipts for all water pumped,
including that used for public purposes and not paid for, were 15.4
cents a thousand gallons, against the cost of production, 9.8 cents,
which covers operating expenses, interest on capital, and provision for
sinking fund. This leaves a handsome net profit to the city. On account
of the comparatively high price of the city water and the ease with
which well-water is obtained, the latter is almost exclusively used
for running engines, manufacturing purposes, etc., and this in part
explains the very low per-capita consumption.
The volume of sewage, however, for the same year, including rain-water,
except during heavy showers, was only 29 gallons per head, showing even
with the private water-supplies an extraordinarily low consumption.
The friction of the water in the 4.75 miles of 3-foot pipe between
Tegel and the reservoir at Charlottenburg presents an interesting
point. When well-water with crenothrix was pumped, the friction rose
to 34.5 feet, when the velocity was 2.46 feet per second. According to
Herr Anklamm, who had charge of the works at the time, the friction was
reduced to 19.7 feet when filtered water was used and after the pipe
had been flushed, and this has not increased with continued use. He
calculated the friction for the velocity according to Darcy 15.0 feet,
Lampe 17.8 feet, Weisbach 18.7 feet, and Prony 21.5 feet.
APPENDIX VII.
ALTONA WATER-WORKS.
The Altona water-works are specially interesting as an example of
a water drawn from a source polluted to a most unusual extent: the
sewage from cities with a population of 770,000, including its own, is
discharged into the river Elbe within ten miles above the intake and
upon the same side.
The area of the watershed of the Elbe above Altona is about 52,000
square miles, and the average rainfall is estimated to be about
28 inches, varying from 24 or less near its mouth to much higher
quantities in the mountains far to the south. On this watershed there
are 46 cities, which in 1890 had populations of over 20,000 each,
and in addition there is a permanent population upon the river-boats
estimated at 20,000, making in all 5,894,000 inhabitants, without
including either country districts or the numberless cities with less
than 20,000 inhabitants each. The sewage from about 1,700,000 of these
people is purified before being discharged; and assuming that as many
people living in cities smaller than 20,000 are connected with sewers
as live in larger places without being so connected, the sewage of
over four million people is discharged untreated into the Elbe and its
tributaries.
The more important of these sources of pollution are the following:
City Population On what Approximate
in 1890. River. Distance, Miles.
Shipping 20,000
Altona 143,353 Elbe 6
Hamburg 570,534 Elbe 7
Wandsbeck 20,586 Elbe 8
Harburg 35,101 Elbe 11
Magdeburg 202,325 Elbe 185
Dresden 276,085 Elbe 354
Berlin and suburbs 1,787,859 Havel 243
Halle 101,401 Saale 272
Leipzig 355,485 Elster 305
Chemnitz 138,955 Mulde 340
Prague 310,483 Moldau 500
The sewage of Berlin and of most of its suburbs is treated before being
discharged, and in addition the Havel flows through a series of lakes
below the city, allowing better opportunities for natural purification
than in the case of any of the other cities. Halle treats less than a
tenth of its sewage. Magdeburg will treat its sewage in the course of
a few years. Leipzig, Chemnitz, and other places are thinking more or
less seriously of purification.
The number of bacteria in the raw water at Altona fluctuates with the
tide and is extremely variable; numbers of 50,000 and 100,000 are not
infrequent, but 10,000 to 40,000 is perhaps about the usual range.
The works were originally built by an English company in 1860, and have
since been greatly extended. They were bought by the city some years
ago. The water is pumped directly from the river to a settling-basin
upon a hill 280 feet above the river. From this it flows by gravity
through the filters to the slightly lower pure-water reservoir and
to the city without further pumping. The filters are open, with
nearly vertical masonry walls, as described in Kirkwood’s report. The
cross-section of the main underdrain is 1/2800 of the area of the beds.
Considerable trouble has been experienced from frost. With continued
cold weather it is extremely difficult to satisfactorily scrape the
filters, and very irregular rates of filtration may result at such
times. In the last few years, with systematic bacterial investigation,
it has been found that greatly decreased efficiency frequently follows
continued cold weather, and the mild epidemics of typhoid fever
from which the city has long suffered have generally occurred after
these times. Thus a light epidemic of typhoid in 1886 came in March,
following a light epidemic in Hamburg. In 1887 a severe epidemic in
February followed a severe epidemic in Hamburg in December and January.
In 1888 a severe epidemic in March followed an epidemic in Hamburg
lasting from November to January. Hamburg’s epidemic of 1889, coming in
warm weather, September and October, was followed by only a very slight
increase in Altona. In 1891 Altona suffered again in February from a
severe epidemic, although very little typhoid had been in Hamburg. A
less severe outbreak also came in February, 1892, and a still slighter
one in February, 1893. In the ten years 1882-1892, of five well-marked
epidemics, three broke out in February and two in March, while two
smaller outbreaks came in December and January. No important outbreak
has ever occurred in summer or in the fall months, when typhoid
is usually most prevalent, thus showing clearly the bad effect of
frost upon open filters (see Appendix II). With steadily increasing
consumption the sedimentation-basin capacity of late years has become
insufficient as well as the filtering area, and it is not unlikely that
with better conditions a much better result could be obtained in winter
even with open filters.[63]
The brilliant achievement of the Altona filters was in the summer of
1892, when they protected the city from the cholera which
so ravaged Hamburg, although the raw water at Altona must have
contained a vastly greater quantity of infectious matter than that
which worked such havoc in Hamburg.
From these records it appears that for about nine months of the year
the Altona filters protect the city from the impurities of the Elbe
water, but that during cold weather, with continued mean temperatures
below the freezing-point, such protection is not completely afforded,
and bad effects have occasionally resulted. Notwithstanding the recent
construction of open filters in Hamburg it appears to me that there
must always be more or less danger from open filters in such a climate.
Hamburg’s danger, however, will be much less than Altona’s on account
of its better intake above the outlets of the sewers of Hamburg and
Altona, which are the most important points of pollution at Altona.
APPENDIX VIII.
HAMBURG WATER-WORKS.
The source and quality of the water previously supplied has been
sufficiently indicated in Appendix II. It was originally intended to
filter the water, but the construction of filters was postponed from
time to time until the fall of 1890, when the project was seriously
taken up, and work was commenced in the spring of 1891. Three years
were allowed for construction. In 1892, however, the epidemic of
cholera came, killing 8605 residents and doing incalculable damage to
the business interests of the city. The health authorities found that
the principal cause of this epidemic was the polluted water-supply.
To prevent a possible recurrence of cholera in 1893, the work of
construction of the filters was pressed forward much more rapidly than
had been intended. Electric lights were provided to allow the work to
proceed nights as well as days, and as a result the plant was put in
operation May 27, 1893, a full year before the intended time. Owing to
the forced construction the cost was materially increased.
The new works take the raw water from a point one and a half miles
farther up-stream, where it is believed the tide can never carry the
city’s own sewage, as it did frequently to the old intake. The water
is pumped from the river to settling-basins against heads varying with
tide and the water-level in the basins from 8 to 22 feet. Each of the
four settling-basins has an area of about 10 acres, and, with the water
6.56 feet deep, holds 20,500,000 gallons, or 82,000,000 gallons in
all. The works are intended to supply a maximum of 48,000,000 gallons
daily, but the present average consumption is only about 35,000,000
gallons (1892), or 59 gallons per head for 600,000 population.
This consumption is regarded as excessive, and it is hoped that it
will be reduced materially by the more general use of meters. The
sedimentation-basins are surrounded by earthen embankments with slopes
of 1:3, the inner sides being paved with brick above a clay layer. The
water flows by gravity from these basins to the filters, a distance
of 1-1/2 miles, through a conduit 8-1/2 feet in diameter. The flow of
the water out of the basins and from the lower end of the conduit is
regulated by automatic gates connected with floats, shown by Fig. 11,
page 60.
The filters are 18 in number, and each has an effective area of 1.89,
or 34 acres in all. They are planned to filter at a rate of 1.60
million gallons per acre daily, which with 16 filters in use gives a
daily quantity of 48,000,000 gallons as the present limit of the works.
The sides of the filters are embankments with 1:2 slopes. Both sides
and bottoms have 20 inches of packed clay, above which are 4 inches of
puddle, supporting a brick pavement laid in cement. The bricks are laid
flat on the bottom, but edge-wise on the sides where they will come in
contact with ice.
The main effluent-drain has a cross-section for the whole length of
the filter of 4.73 square feet, or 1/17000 of the area of the filter;
and even at the low rate of filtration proposed, the velocity in the
drain will reach 0.97 foot. The drain has brick sides, 1.80 feet
high, covered with granite slabs. The lateral drains are all of brick
with numerous large openings for admission of water. They are not
ventilated, and I am unable to learn that any bad results follow this
omission.
The filling of the filters consists of 2 feet of gravel, the top being
of course finer than the bottom layers, above which are 40 inches of
sand, which are to be reduced to 24 inches by scraping before being
refilled. The water over the sand, when the latter is of full depth,
is 43 inches deep, and will be increased to 59 inches with the minimum
sand-thickness. The apparatus for regulating the rate of filtration was
described page 52. The cost of the entire plant, including 34 acres
effective filter-surface, 40 acres of sedimentation-basins, over 2
miles of 8-1/2-foot conduit, pumping-machinery, sand-washing apparatus,
laboratory, etc., was about 9,500,000 marks, or $2,280,000. This all
reckoned on the effective filter area is $67,000 per acre, or $3.80 per
head for a population of 600,000.
The death-rate since the introduction of filtered water has been lower
than ever before in the history of the city, but as it is thought that
other conditions may help to this result, no conclusions are as yet
drawn.
DEATHS IN HAMBURG FROM ALL CAUSES, AND FROM TYPHOID FEVER, BEFORE AND
AFTER THE INTRODUCTION OF FILTERS.
--------------------+-----------+-----------+--------------
|Deaths from|Deaths from|
|all Causes | Typhoid |
Year. | per 1000 | Fever per |
| Living. | 100,000 |
| | Living. |
--------------------+-----------+-----------+--------------
1880 | 24.9 | 26 |
1881 | 24.1 | 30 |
1882 | 23.7 | 27 |
1883 | 25.2 | 25 |
1884 | 25.1 | 26 |
1885 | 25.3 | 42 |
1886 | 29.0 | 71 |
1887 | 26.6 | 88 |
1888 | 24.5 | 54 |
1889 | 23.5 | 43 |
1890 | 22.0 | 27 |
1891 | 23.4 | 24 |
1892 | 41.1 | 34 |Cholera year.
1893 | 20.2 | 18 |Filtered water
| | | from May 28.
1894 | 17.9 | 7 |
1895 | 19.0 | 11 |
1896 | 17.3 | 6 |
1897 | 17.0 | 7 |
1898 | 17.5 | 5 |
Average for 5 years,| | |
excluding cholera | | |
year, before | | |
filtration, | | |
1887 to 1891 | 24.0 | 47.2 |
Average for 5 years | | |
with filtration, | | |
1894 to 1898 | 17.7 | 7.2 |
--------------------+-----------+-----------+--------------
APPENDIX IX.
NOTES ON SOME OTHER EUROPEAN WATER-SUPPLIES.
=Amsterdam.=—The water is derived from open canals in the dunes. These
canals have an aggregate length of about 15 miles, and drain about 6200
acres. The water, as it enters the canals from the fine dune-sand,
contains iron, but this is oxidized and deposited in the canals. The
water after collection is filtered. It has been suggested that by using
covered drains instead of open canals for collecting the water, the
filtration would be unnecessary; but, on the other hand, the cost of
building and maintaining covered drains in the very fine sand would be
much greater than that of the canals, and it is believed, also, that
the water so collected would contain iron, the removal of which might
prove as expensive as the present filtration. In 1887 filters were
built to take water from the river Vecht, but the city has refused to
allow the English company which owns the water-works to sell this water
for domestic purposes, and it is only used for public and manufacturing
purposes, only a fraction of the available supply being required.
Leyden, the Hague, and some other Dutch cities have supplies like the
dune supply of Amsterdam, and they are invariably filtered.
=Antwerp= is also supplied by an English company. The raw water is
drawn from a small tidal river, which at times is polluted by the
sewage of Brussels. It is treated by metallic iron in Anderson revolver
purifiers, and is afterward filtered at a rather low average rate. The
hygienic results are closely watched by the city authorities, and are
said to be satisfactory.
=Rotterdam.=—The raw water is drawn from the Maas, as the Dutch
call the main stream of the Rhine after it crosses their border. The
population upon the river and its tributaries in Switzerland, Germany,
Holland, France, and Belgium is very great; but the flow is also great,
and the low water flow is exceptionally large in proportion to the
average flow, on account of the melting snow in summer in Switzerland,
where it has its origin.
The original filters had wooden under-drains, and there was constant
trouble with crenothrix until the filters were reconstructed without
wood, since which time there has been no farther trouble. The present
filters are large and well managed. There is ample preliminary
sedimentation.
=Schiedam.=—The filters at Schiedam are comparatively small, but are
of unusual interest on account of the way in which they are operated.
The intake is from the Maas just below Rotterdam. The city was unable
to raise the money to seek a more distant source of supply, and the
engineer, H. P. N. Halbertsma, was unwilling to recommend a supply
from so doubtful a source without more thorough treatment than simple
sand-filtration was then thought to be. The plan adopted is to filter
the supply after preliminary sedimentation through two filters of 0.265
acre each, and the resulting effluent is then passed through three
other filters of the same size. River sand is used for the first, and
the very fine dune sand for the second filtration. The cost both of
construction and operation was satisfactory to the city, and much below
that of any other available source; and the hygienic results have been
equally satisfactory, notwithstanding the unfavorable position of the
intake.
=Magdeburg.=—The supply is drawn from the Elbe, and is filtered through
vaulted filters after preliminary sedimentation. The pollution of
the river is considerable, although less than at Altona or even at
Hamburg. The city has been troubled at times by enormous discharges of
salt solution from salt-works farther up, which at extreme low water
have sometimes rendered the whole river brackish and unpleasant to the
taste; but arrangements have now been made which, it is hoped, will
prevent the recurrence of this trouble.
=Breslau= is supplied with filtered water from the river Oder,
which has a watershed of 8200 square miles above the intake, and is
polluted by the sewage from cities with an aggregate population of
about 200,000, some of which are in Galicia, where cholera is often
prevalent. In recent years the city has been free from cholera, and
from more than a very limited number of typhoid-fever cases; but the
pollution is so great as to cause some anxiety, notwithstanding the
favorable record of the filters, and there is talk of the desirability
of securing another supply. Until 1893 there were four filter-beds,
with areas of 1.03 acres each, and not covered. In 1893 a fifth bed was
added. This is covered by vaulting and is divided into four sections,
which are separately operated, so that it is really four beds of 0.25
acre each. The vaulting is concrete arches, supported by steel I beams
in one direction.
=Budapest.=—A great variety of temporary water-supplies have at
different times been used by this rapidly growing city. The filters
which for some years have supplied a portion of the supply have not
been altogether satisfactory; but perhaps this was due to lack of
preliminary sedimentation for the extremely turbid Danube water, and
also to inadequate filter-area. The city is rapidly building and
extending works for a supply of ground-water, and in 1894 the filters
were only used as was necessary to supplement this supply, and it was
hoped that enough well-water would be obtained to allow the filters to
be abandoned in the near future. The Danube above the intake receives
the sewage of Vienna and innumerable smaller cities, but the volume of
the river is very great compared to other European streams, so that the
relative pollution is not so great as in many other places.
=Zürich.=—The raw water is drawn by the city from the Lake of Zürich
near its outlet, and but a few hundred feet from the heart of the city.
Although no public sewers discharge into the lake, there is some
pollution from boats and bathers and other sources, and, judging by
the number of bacteria in the raw water, this pollution is increasing.
The raw water is extremely free from sediment, and the filters only
become clogged very slowly. The rate of filtration is high, habitually
reaching 7,000,000 gallons per acre daily; but, with the clear lake
water and long periods between scrapings, the results are excellent
even at this rate. The filters are all covered with concrete groined
arches.
Filtration was commenced in 1886, and was followed by a sharp decline
in the amount of typhoid fever, which, up to that time, had been rather
increasing; for the six years before the change there were sixty-nine
deaths from this cause annually per 100,000 living, and for the six
years after only ten, or one seventh as many; and this reduction is
attributed by the local authorities to the filtration.[64]
=St. Petersburg.=—The supply is drawn from the Neva River by an English
company, and is filtered through vaulted filters at a very high rate.
=Warsaw.=—The supply is drawn from the Weichsel River by the city, and
is filtered through vaulted filters after preliminary sedimentation at
a rate never exceeding 2,570,000 gallons per acre daily.
THE USE OF UNFILTERED SURFACE-WATERS.
The use of surface-water without filtration in Europe is comparatively
limited. In Germany this use is now prohibited by the Imperial Board
of Health. In Great Britain, Glasgow draws its supply unfiltered from
Loch Katrine; and Manchester and some other towns use unfiltered
waters from lakes or impounding reservoirs the watersheds of which are
entirely free from population. The best English practice, however, as
in Germany, requires the filtration of such waters even if they are not
known to receive sewage, and the
unpolluted supplies of Liverpool, Bradford, Dublin, and many other
cities are filtered before use.
THE USE OF GROUND-WATER.[65]
Ground-waters are extensively used in Europe, and apparently in
some localities the geological formations are unusually favorable
to this kind of supply. Paris derives all the water it now uses for
domestic purposes from springs, but has a supplementary supply from
the river for other purposes. Vienna and Munich also obtain their
entire supplies from springs, while Budapest, Cologne, Leipzig,
Dresden, Frankfurt, many of the great French cities, Brussels, a part
of London, and many other English cities derive their supplies from
wells or filter-galleries, and among the smaller cities all over Europe
ground-water supplies are more numerous than other kinds.
APPENDIX X.
LITERATURE OF FILTRATION.
The following is a list of a number of articles on filtration. The
list is not complete, but it is believed that it contains the greater
part of articles upon slow sand-filtration, and that it will prove
serviceable to those who wish to study the subject more in detail.
ANKLAMM. Glasers Annalen, 1886, p. 48.
A description of the Tegel filters at Berlin, with excellent plans.
BAKER. Engineering News.
Water purification in America: a series of descriptions of filters, as
follows: Aug. 3, 1893, Lawrence filter and description of apparatus of
screening sand and gravel; Apr. 26, 1894, filter at Nantucket, Mass.;
June 7, 1894, filters at Ilion, N. Y., plans; June 14, 1894, filters
at Hudson, N. Y.; July 12, 1894, filters at Zürich, Switzerland,
plans; Aug. 23, 1894, filters at Mt. Vernon, N. Y., plans.
BERTSCHINGER. Journal für Gas- und Wasserversorgung, 1889, p. 1126.
A record of experiments made at Zürich upon the effect of rate of
filtration, scraping, and the influence of vaulting. Rate and vaulting
were found to be without effect, but poorer results followed scraping.
The numbers of bacteria in the lake-water were too low to allow
conclusive results.
—— Journal für Gas- und Wasserversorgung, 1891, p. 684.
A farther account of the Zürich results, with full analyses and a
criticism of Fränkel and Piefke’s experiments.
BOLTON. Pamphlet, 1884.
Descriptions and statistics of London filters.
BÖTTCHER and OHNESORGE. Zeitschrift für Bauwesen, 1876, p. 343.
A description of the Bremen works, with full plans.
BURTON. Water-supply of Towns. London, 1894.
Pages 94-115 are upon filtration and mention a novel method of
regulating the rate.
CODD. Engineering News, Apr. 26, 1894.
A description of a filter at Nantucket, Mass.
CRAMER. Centralblatt für Bauwesen, 1886, p. 42.
A description of filters built at Brieg, Germany.
CROOK. London Water-supply. London, 1883.
DELBRUCK. Allgemeine Bauzeitung, 1853, p. 103.
A general article on filtration; particularly valuable for notices of
early attempts at filtration and of the use of alum.
Deutsche Verein von Gas- und Wasserfachmänner.
Stenographic reports of the proceedings of this society are printed
regularly in the _Journal für Gas- und Wasserversorgung_, and the
discussions of papers are often most interesting.
DROWN. Journal Association Eng. Societies, 1890, p. 356.
Filtration of natural waters.
FISCHER. Vierteljahresschrift für Gesundheitspflege, 1891, p. 82.
Discussion of papers on water-filtration.
FRÄNKEL. Vierteljahresschrift für Gesundheitspflege, 1891, p. 38.
On filters for city water-works.
FRÄNKEL and PIEFKE. Zeitschrift für Hygiene, 1891, p. 38, Leistungen
der Sandfiltern.
E. FRANKLAND. Report in regard to the London filters for 1893
in the Annual Summary of Births, Deaths, and Causes of Death in
London and Other Great Towns, 1893. Published by authority of the
Registrar-General.
P. FRANKLAND. Proc. Royal Society, 1885, p. 379.
The removal of micro-organisms from water.
—— Proceedings Inst. Civil Engineers, 1886, lxxxv. p. 197.
Water-purification; its biological and chemical basis.
—— Trans. of Sanitary Institute of Great Britain, 1886.
Filtration of water for town supply.
FRÜHLING. Handbuch der Ingenieurwissenschaften, vol. ii.
Chapter on water-filtration gives general account of filtration, with
details of Königsberg filters built by the author and not elsewhere
published.
FULLER. Report Mass. State Board of Health, 1892, p. 449.
Report Mass. State Board of Health, 1893, p. 453.
Accounts of the Lawrence experiments upon water-filtration for 1892
and 1893.
—— American Public Health Association, 1893, p. 152.
On the removal of pathogenic bacteria from water by sand filtration.
—— American Public Health Association, 1894, p. 64.
Sand filtration of water with special reference to results obtained at
Lawrence, Mass.
GILL. Deutsche Bauzeitung, 1881, p. 567.
On American rapid filters. The author shows that they are not to be
thought of for Berlin, as they would be more expensive as well as
probably less efficient than the usual procedure.
—— Journal für Gas- und Wasserversorgung, 1892, p. 596.
A general account of the extension of the Berlin filters at Müggel. No
drawings.
GRAHN. Journal für Gas- und Wasserversorgung, 1877, p. 543.
On the filtration of river-waters.
—— Journal für Gas- und Wasserversorgung, 1890, p. 511.
Filters for city water-works.
—— Vierteljahresschrift für Gesundsheitpflege, 1891, p. 76.
Discussion of papers presented on filtration.
—— Journal für Gas- und Wasserversorgung, 1894, p. 185.
A history of the “Rules for Water-filtration” (Appendix I), with some
discussion of them.
GRAHN and MEYER. Reiseberichte über künstliche central Sandfiltration.
Hamburg, 1876.
An account of the observations of the authors in numerous cities,
especially in England.
GRENZMER. Centralblatt der Bauverwaltung, 1888, p. 148.
A description of new filters at Amsterdam, with plans.
GRUBER. Centralblatt für Bakteriologie, 1893, p. 488.
Salient points in judging of the work of sand-filters.
HALBERTSMA. Journal für Gas- und Wasserversorgung, 1892, p. 43.
Filter-works in Holland. Gives sand, gravel, and water thickness, with
diagrams.
—— Journal für Gas- und Wasserversorgung, 1892, p. 686.
Description of filters built by the author at Leeuwarden, Holland,
with plans.
HART. Proceedings Inst. of Civil Engineers, 1890, c. p. 217.
Description of filters at Shanghai.
HAUSEN. Journal für Gas- und Wasserversorgung, 1892, p. 332.
An account of experiments made for one year with three 16-inch filters
at Helsingfors, Finland, with weekly analyses of effluents.
HAZEN. Report of Mass. State Board of Health, 1891, p. 601.
Experiments upon the filtration of water.
—— Report of Mass. State Board of Health, 1892, p. 539.
Physical properties of sands and gravels with reference to their use
in filtration. (Appendix III.)
HUNTER. Engineering, 1892, vol. 53, p. 621.
Description of author’s sand-washing apparatus.
KIRKWOOD. Filtration of River-waters. New York, 1869.
A report upon European filters for the St. Louis Water Board in 1866.
Contains a full account of thirteen filtration-works visited by the
author, and of a number of filter-galleries, with a project for
filters for St. Louis. This project was never executed, but the report
is a wonderful work which appeared a generation before the American
public was able to appreciate it. It was translated into German, and
the German edition was widely circulated and known.
KOCH. Zeitschrift für Hygiene, 1893.
Water-filtration and Cholera: a discussion of the Hamburg epidemic of
1892 in reference to the effect of filtration.
KRÖHNKE. Journal für Gas- und Wasserversorgung, 1893, p. 513.
An account of experiments made at Hamburg, as a result of which the
author recommends the addition of cuprous chloride to the water before
filtration to secure greater bacterial efficiency.
KÜMMEL. Journal für Gas- und Wasserversorgung, 1877, p. 452.
Operation of the Altona filters, with analyses.
—— Vierteljahresschrift für Gesundheitspflege, 1881, p. 92.
The water-works of the city of Altona.
—— Journal für Gas- und Wasserversorgung, 1887, p. 522.
An article opposing the use of rapid filters (David’s process).
—— Journal für Gas- und Wasserversorgung, 1890, p. 531.
A criticism of Fränkel and Piefke’s results, with some statistics of
German and English filters. (The English results are taken without
credit from Kirkwood.)
—— Vierteljahresschrift für Gesundheitspflege, 1891, p. 87.
Discussion of papers on filtration, with some statistics.
—— Vierteljahresschrift für Gesundheitspflege, 1892, p. 385.
The epidemic of typhoid-fever in Altona in 1891.
—— Journal für Gas- und Wasserversorgung, 1893, p. 161.
Results of experiments upon filtration made at Altona, and bacterial
results of the Altona filters in connection with typhoid death-rates.
—— Trans. Am. Society of Civil Engineers, 1893, xxx. p. 330.
Questions of water-filtration.
LESLIE. Trans. Inst. Civil Engineers, 1883, lxxiv. p. 110.
A short description of filters at Edinburgh.
LINDLEY. A report for the commissioners of the Paris Exposition of
1889 upon the purification of river-waters, and published in French
or German in a number of journals, among them _Journal für Gas- und
Wasserversorgung_, 1890, p. 501.
This is a most satisfactory discussion of the conditions which modern
experience has shown to be essential to successful filtration.
MASON. Engineering News, Dec. 7, 1893.
Filters at Stuttgart, Germany, with plans.
MEYER and SAMUELSON. Deutsche Bauzeitung, 1881, p. 340.
Project for filters for Hamburg, with diagrams. Except in detail, this
project is the same as that executed twelve years later.
MEYER. Deutsche Bauzeitung, 1892, p. 519.
Description of the proposed Hamburg filters, with diagrams.
—— The Water-works of Hamburg.
A paper presented to the International Health Congress at Rome, March
1894, and published as a monograph. It contains a full description of
the filters as built, with drawings and views in greater detail than
the preceding paper.
MILLS. Special Report Mass. State Board of Health on the Purification
of Sewage and Water, 1890, p. 601.
An account of the Lawrence experiments, 1888-1890.
—— Report Mass. State Board of Health, 1893, p. 543.
The Filter of the Water-supply of the City of Lawrence and its Results.
—— Trans. Am. Society of Civil Engineers, 1893, xxx. p. 350.
Purification of Sewage and Water by Filtration.
NEVILLE. Engineering, 1878, xxvi. p. 324.
A description of the Dublin filters, with plans.
NICHOLS. Report Mass. State Board of Health, 1878, p. 137.
The filtration of potable water.
OESTER. Gesundheits-Ingenieur, 1893, p. 505.
What is the Rate of Filtration? A purely theoretical discussion.
ORANGE. Trans. Inst. Civil Engineers, 1890, c. p. 268.
Filters at Hong Kong.
PFEFFER. Deutsche Bauzeitung, 1880, p. 399.
A description of filters at Liegnitz, Germany.
PIEFKE. Results of Natural and Artificial Filtration. Berlin, 1881.
Pamphlet.
—— Journal für Gas- und Wasserversorgung, 1887, p. 595. Die Principien
der Reinwassergewinnung vermittelst Filtration.
A sketch of the theory and practical application of filtration.
—— Zeitschrift für Hygiene, 1889, p. 128. Aphorismen über
Wasserversorgung.
A discussion of the theory of filtration, with a number of experiments
on the thickness of sand-layers, etc.
PIEFKE. Vierteljahresschrift für Gesundheitspflege, 1891, p. 59.
On filters for city water-works.
FRÄNKEL and PIEFKE. Zeitschrift für Hygiene, 1891, p. 38.
Leistungen der Sandfiltern. An account of the partial obstruction of
the Stralau filters by ice, and a typhoid epidemic which followed.
Experiments were then made upon the passage of cholera and typhoid
germs through small filters.
PIEFKE. Journal für Gas- und Wasserversorgung, 1891, p. 208. Neue
Ermittelungen über Sandfiltration.
The above mentioned experiments being objected to on certain
grounds, they were repeated by Piefke alone, confirming the previous
observations on the passage of bacteria through filters, but under
other conditions.
—— Zeitschrift für Hygiene, 1894, p. 151, Über Betriebsführung von
Sandfiltern.
A full account of the operation of the Stralau filters in 1893, with
discussion of the efficiency of filtration, etc.
PLAGGE AND PROSKAUER. Zeitschrift für Hygiene, 11. p. 403.
Examination of water before and after filtration at Berlin, with
theory of filtration.
REINCKE. Bericht über die Medicinische Statistik des Hamburgischen
Staates für 1892.
Contains a most valuable discussion of the relations of filtration to
cholera, typhoid fever, and diarrhœa, with numerous tables and charts.
(Abstract in Appendix II.)
REINSCH. Centralblatt für Bakteriologie, 1895, p. 881.
An account of the operation of the Altona filters. High numbers of
bacteria in the effluents have often resulted from the discharge of
sludge from the sedimentation-basins onto the filters, due to the
interference of ice on the action of the floating outlet for the
basins, and this, rather than the direct effect of cold, is believed
to be the direct cause of the low winter efficiency. The author urges
the necessity of a deeper sand-layers in no case less than 18 inches
thick.
RENK. Gesundheits-Ingenieur, 1886, p. 54.
—— Über die Ziele der künstliche Wasserfiltration.
RUHLMANN. Wochenblatt für Baukunde, 1887, p. 409.
A description of filters at Zürich.
SALBACH. Glaser’s Annalen, 1882.
Filters at Groningen, Holland, built in 1880. Alum used.
SAMUELSON. Translation of Kirkwood’s “Filtration of River-waters” into
German, with additional notes especially on the theory of filtration
and the sand to be employed. Hamburg, 1876.
SAMUELSON. Filtration and constant water-supply. Pamphlet. Hamburg,
1882.
—— Journal f. Gas- und Wasserversorgung, 1892, p. 660.
A discussion of the best materials and arrangement for sand-filters.
SCHMETZEN. Deutsche Bauzeitung, 1878, p. 314.
Notice and extended criticism of Samuelson’s translation of Kirkwood.
SEDDEN. Jour. Asso. Eng. Soc., 1889, p. 477.
In regard to the sedimentation of river-waters.
SEDGWICK. New England Water-works Association, 1892, p. 103.
European methods of Filtration with Reference to American Needs.
SOKAL. Wochenschrift der östreichen Ingenieur-Verein, 1890, p. 386.
A short description of the filters at St. Petersburg, and a comparison
with those at Warsaw.
STURMHÖFEL. Zeitschrift f. Bauwesen, 1880, p. 34.
A description of the Magdeburg filters, with plans.
TOMLINSON. American Water-works Association, 1888.
A paper on filters at Bombay and elsewhere.
TURNER. Proc. Inst. Civil Engineers, 1890, c. p. 285.
Filters at Yokohama.
VAN DER TAK. Tijdschrift van de Maatschapping van Bouwkunde, 1875(?).
A description (in Dutch) of the Rotterdam water-works, including the
wooden drains which caused the trouble with crenothrix, and which have
since been removed. Diagrams.
VAN IJSSELSTEYN. Tijdschrift van het Koninklijk Instituut van
Ingenieurs, 1892-5, p. 173.
A description of the new Rotterdam filters, with full drawings.
VEITMEYER. Verhandlungen d. polyt. Gesell. zu Berlin, April, 1880.
Filtration and purification of water.
WOLFFHÜGEL. Arbeiten aus dem Kaiserliche Gesundheitsamt, 1886, p. 1.
Examinations of Berlin water for 1884-5, with remarks showing superior
bacterial efficiency with open filters.
—— Journal für Gas- u. Wasserversorgung, 1890, p. 516.
On the bacterial efficiency of the Berlin filters, with diagrams.
ZOBEL. Zeitschrift des Vereins deutsche Ingenieure, 1884, p. 537.
Description of filters at Stuttgart.
OTHER LITERATURE.
Many scientific and engineering journals publish from time to time
short articles or notices on filtration which are not included in the
above list. Among such journals none gives more attention to filtration
than the _Journal für Gasbeleuchtung und Wasserversorgung_, which
publishes regularly reports upon the operation of many German filters,
and gives short notices of new construction. The first articles upon
filtration in this journal were a series of descriptions of German
water-works in 1870-73, including descriptions of filters at Altona,
Brunswick, Lübeck, etc. Stenographic reports of many scientific
meetings have been published, particularly since 1890, and since 1892
there has been much discussion in regard to the “Rules for Filtration”
given in Appendix I.
A Report of a Royal Commission to inquire into the water-supply of the
metropolis, with minutes of evidence, appendices, and maps (London,
1893-4), contains much valuable material in regard to filtration.
The monthly reports of the water examiner, and other papers published
by the Local Government Board, London, are often of interest.
The German “Verein von Gas- u. Wasserfachmänner” prints without
publishing a most useful annual summary of German water-works
statistics for distribution to members. Many of the statistics given in
this volume are from this source.
Description of the filters at Worms was given in the _Deutsche
Bauzeitung_, 1892, p. 508; of the filters at Liverpool in
_Engineering_, 1889, p. 152, and 1892, p. 739. The latter journal also
has given a number of descriptions of filters built in various parts of
the world by English engineers, but, excepting the articles mentioned
in the above list, the descriptions are not given in detail.
MORE RECENT ARTICLES.
The following are a few of the more important articles which have
appeared since the first edition of this book. In addition many
articles of current interest have appeared in the technical journals,
particularly in the journals mentioned above.
CLARK. Reports of Mass. State Board of Health, 1894 to 1897, inclusive.
Articles on the filtration of water, giving accounts of experiments at
the Lawrence Experiment Station, and records of the operation of the
Lawrence city filter. These experiments are directed principally to
the removal of bacteria from sewage-polluted waters.
—— Jour. New England Water Works Assoc., XI., p. 277.
Removal of Iron from Ground Waters. A description of certain
experiments.
FOWLER. Jour. New England Water Works Assoc., XII., p. 209.
The Operation of a Slow Sand Filter. A most helpful and thorough
description of the operation of sand filters at Poughkeepsie for a
long period of years.
FULLER. Water Purification at Louisville. D. Van Nostrand Co., 1898.
A report upon a series of most exhaustive experiments carried out at
Louisville, directed principally to the clarification of excessively
muddy waters. Contains a full account of methods of coagulation, and
of experiments with the electrical treatment of water.
—— Report on Water Filtration at Cincinnati. City document, 1899.
Account of experiments with sand filters, with and without coagulants,
and with other processes applied to the Ohio River water at Cincinnati.
GILL. Filters at Muggel. Proc. Institute of Civil Engineers, 1894-5;
vol. 119, p. 236.
A description of the new vaulted filter plant designed by the author
for Berlin, Germany. Plans and views.
GOETZE. Journal für Gasbeleuchtung und Wasserversorgung, 1897, p. 169.
Selbstthätige Wasseraustrittsregler besonders für Filter. A
description of the automatic regulating device for filters used at
Bremen.
—— Zeitschrift des Vereines deutscher Ingenieure, XXX.
Reinigung des Trinkwassers in Bremen durch mehrmalige Sandfiltration.
A description of the method of double filtration used at Bremen,
giving results obtained in full. No drawings.
GRAHN. Journal für Gasbeleuchtung und Wasserversorgung, 1895.
Water purification plant at the city of Magdeburg. A description of
the old plant, and the changes which have been made in it to increase
its capacity, and make it conform to the requirements of the German
official instructions regarding filtration. Many illustrations and
plans.
HALBERTSMA. Journal für Gasbeleuchtung und Wasserversorgung, 1896.
Die Resultate der doppelten Filtration zu Schiedam. A description of
double filtration at Schiedam, with the bacterial results for the two
years, 1894 and 1895, showing an average bacterial efficiency of 99.76
per cent.
HAZEN. Report to Filtration Commission, Pittsburgh. City document, 1899.
A description of experiments upon the treatment of the Allegheny River
water by sand and mechanical filters.
—— Ohio State Board of Health Report, 1897, p. 154.
Report on the Mechanical Filtration of the Public Water Supply
of Lorain. Gives the results of a five-weeks test of the Jewell
mechanical filters at Lorain, treating Lake Erie water.
KEMNA. The Biology of Sand Filtration. Read before the annual
convention of the British Association of Water Works Engineers.
Abstract in Engineering News, XLI., p. 419.
Describing organisms which develop in open sand filters, both animal
and vegetable, and their effects upon the process. A quite full
account of the author’s extended experience, and the only paper
treating this subject.
MAGAR. Journal für Gasbeleuchtung und Wasserversorgung, 1897, p. 4.
Reinigungsbetrieb der offener Sandfilter des Hamburger Filterwerkes in
Frostzeiten. A new method of cleaning open filters in winter without
the removal of the ice.
PANWITZ. Arbeiten aus dem Kaiserlichen Gesundheitsamte, XIV., p. 153.
Die Filtration von Oberflächenwasser in den deutschen Wasserwerken
während der Jahre 1894 bis 1896.
A description of the filtration works in Germany, and the results
obtained from them, particularly from the point of view of bacterial
efficiency. Results are graphically shown by a series of charts.
REYNARD. Le Génie Civil, 1896, XXVIII., p. 321.
Purification of water with the aid of metallic iron. Describing the
works of the Compagnie Général des Eaux for supplying the suburbs
of Paris with filtered water, the capacity of the works being over
23,000,000 gallons daily.
WESTON. Rhode Island State Board of Health, 1894.
Report of the Results Obtained with Experimental Filters at the
Pattaconset Pumping Station of the Providence Water Works. Relates
particularly to the bacterial purification obtained with rapid
filtration aided by sulphate of alumina. These were the first
systematic experiments made with mechanical filters.
WHEELER. Journal of the New England Water Works Assoc., XI., p. 301.
Covered Sand Filter at Ashland, Wis.
A description of the covered filters built by the author at Ashland
Wis. for the purification of the bay water. Views and drawings.
APPENDIX XI.
THE ALBANY WATER-FILTRATION PLANT.
(Abridged from Proceedings American Society of Civil Engineers, Nov.
1899.)
Albany, N. Y., was originally supplied with water by gravity from
certain reservoirs on small streams west and north of the city. In
time, with increasing consumption, the supply obtained from these
sources became inadequate, and an additional supply from the Hudson
River was introduced. The water was obtained from the river through
a tunnel under the Erie Basin, and a pumping-station was erected in
Quackenbush Street to pump it to reservoirs, one of which served also
as the distributing point for one of the gravity supplies. The intake,
which was used first in 1873, drew water from the river opposite the
heart of the city. In recent years, the amount of water drawn from this
source has greatly exceeded that obtained from the gravity sources.
The Hudson River, at the point of intake, has a drainage area of 8240
square miles. Of this, 4541 square miles are tributary to the Hudson
above Troy, 3493 are tributary to the Mohawk, and 168 are tributary to
the Hudson below the Mohawk.
The minimum flow may be estimated at 1657 cubic feet per second, or
1,060,000,000 gallons per 24 hours, or at least fifty times the maximum
consumption.
The cities and larger towns upon the river above the intake, with
estimated populations and distances, are as follows:
MOST IMPORTANT CITIES, TOWNS, AND VILLAGES ON THE WATERSHED OF THE
HUDSON ABOVE ALBANY.
------------+-----------+-----------+-----------------------------
| |Approximate| Population in
Place. | County. | Distance +--------+-------+------------
| | above | 1880. | 1890. | 1900.
| | Intake, | | |
| | Miles. | | |(Estimated.)
------------+-----------+-----------+--------+-------+------------
Troy |Rensselaer | 4 | 56,747 | 60,956| 65,470
Watervliet |Albany | 4 | 8,820 | 12,967| 19,040
Green Island|Rensselaer | 5 | 4,160 | 4,463| 4,788
Cohoes |Albany | 8 | 19,416 | 22,509| 26,450
Lansingburg |Rensselaer | 8 | 7,432 | 10,550| 14,980
Waterford |Saratoga | 9 | (1,822)| 1,822| (1,822)
Schenectady |Schenectady| 28 | 13,655 | 19,002| 26,450
Hoosic Falls|Rensselaer | 44 | 4,530 | 7,014| 10,860
Amsterdam |Montgomery | 44 | 9,466 | 17,336| 31,730
Glens Falls |Warren | 49 | 4,900 | 9,509| 18,450
Saratoga |Saratoga | 51 | 8,421 | 11,975| 17,010
Springs | | | | |
Johnstown |Fulton | 56 | 5,013 | 7,768| 12,040
Gloversville|Fulton | 58 | 7,133 | 13,864| 26,930
North Adams,| | | | |
Mass. |Berkshire | 68 | 10,191 | 16,074| 25,340
Adams, Mass.|Berkshire | 75 | 5,591 | 9,213| 15,181
Little Falls|Herkimer | 82 | 6,910 | 8,783| 11,160
Utica |Oneida | 107 | 33,914 | 44,007| 57,090
Rome |Oneida | 127 | 12,194 | 14,991| 18,430
32 villages | | | 52,523 | 61,869| 76,194
------------+-----------+-----------+--------+-------+------------
Total, not including rural | | |
population |272,838 |354,672| 479,415
Per square mile | 33 | 43| 59
------------------------------------+--------+-------+------------
Without entering into a detailed discussion, it may be said that the
amount of sewage, with reference to the size of the river and the
volume of flow, is a fraction less than that at Lawrence, Mass.,
where a filter-plant has also been constructed, but the pollution is
much greater than that of most American rivers from which municipal
water-supplies are taken.
The filtration-plant completed in 1899 takes the water from a point
about two miles above the old intake. Pumps lift the water to the
sedimentation-basin, from which it flows to the filters and thence
through a conduit to the pumping-station previously used.
DESCRIPTION OF PLANT.
=Intake.=—The intake consists of a simple concrete structure in the
form of a box, having an open top covered with rails 6 inches apart,
and connected below, through a 36-inch pipe, with a well in the
pumping-station. Before going to the pumps the water passes through a
screen with bars 2 inches apart, so arranged as to be raked readily.
The rails over the intake and this screen are intended to stop matters
which might obstruct the passageways of the pumps, but no attempt is
made to stop fish, leaves, or other floating matters which may be
in the water. The arrangement, in this respect, is like that of the
filter at Lawrence, Mass., where the raw water is not subjected to
close screening. There is room, however, to place finer screens in the
pump-well, should they be found desirable.
[Illustration: HUDSON RIVER
NEAR INTAKE
FIG. 1.]
[Illustration: SEDIMENTATION-BASIN, PUMPING-STATION, AND OUTLETS.]
[Illustration: SEDIMENTATION-BASIN, AN OUTLET, AND LABORATORY.
[_To face page 290._]
]
=Pumping-station.=—The centrifugal pumps have a guaranteed capacity
of 16,000,000 gallons per 24 hours against a lift of 18 feet, or
12,000,000 gallons per 24 hours against a lift of 24 feet. The ordinary
pumping at low water is against the higher lift, and under these
conditions either pump can supply the ordinary consumption, the other
pump being held in reserve.
The pumping-station building, to a point above the highest flood-level,
is of massive concrete construction, without openings. Nearly all
the machinery is necessarily below this level, and in high water
the sluice-gates are closed, and the machinery is thus protected
from flooding. The superstructure is of pressed brick, with granite
trimmings.
=Meter for Raw Water.=—Upon leaving the pumping-station the water
passes through a 36-inch Venturi meter having a throat diameter of 17
inches, the throat area being two ninths of the area of the pipe. The
meter records the quantity of water pumped, and is also arranged to
show on gauges in the pumping-station the rate of pumping.
=Aeration.=—After leaving the meter, the water passes to the
sedimentation-basin through eleven outlets. These outlets consist of
12-inch pipes on end, the tops of which are 4 feet above the nominal
flow-line of the sedimentation-basin. Each of these outlet-pipes is
pierced with 296 3/8-inch holes extending from 0.5 to 3.5 feet below
the top of the pipe. These holes are computed so that when 11,000,000
gallons of water per day are pumped all the water will pass through the
holes, the water in the pipes standing flush with the tops. The water
is thus thrown out in 3256 small streams, and becomes aerated. When
more than the above amount is pumped, the excess flows over the tops of
the outlet-pipes in thin sheets, which are broken by the jets.
[Illustration:
GENERAL PLAN
FIG. 2.]
Regarding the necessity for aeration, no observations have been taken
upon the Hudson River, but, judging from experience with the Merrimac
at Lawrence, where the conditions are in many respects similar, the
water is at all times more or less aerated, and, for the greater
part of the year, it is nearly saturated with oxygen, and aeration
is not necessary. During low water in summer, however, there is much
less oxygen in the water, and at these times aeration is a distinct
advantage. Further, the river-water will often have a slight odor, and
aeration will tend to remove it. The outlets are arranged so that they
can be removed readily in winter if they are not found necessary at
that season.
=Sedimentation-basin.=—The sedimentation-basin has an area of 5 acres
and is 9 feet deep. To the overflow it has a capacity of 14,600,000
gallons, and to the flow-line of the filters 8,900,000 gallons.
There is thus a reserve capacity of 5,700,000 gallons between these
limits, and this amount can be drawn upon, without inconvenience, for
maintaining the filters in service while the pumps are shut down. This
allows a freedom in the operation of the pumps which would not exist
with the water supplied direct to the filters.
The water enters the sedimentation-basin from eleven inlets along
one side, and is withdrawn from eleven outlets directly opposite.
The inlets and aerating devices described previously bring the water
into the basin without current and evenly distributed along one
side. Both inlets and outlets are controlled by gates, so that any
irregularities in distribution can be avoided. The concrete floor of
the sedimentation-basin is built with even slopes from the toe of each
embankment to a sump, the heights of these slopes being 1 foot,
whatever their lengths. The sump is connected with a 24-inch pipe
leading to a large manhole in which there is a gate through which water
can be drawn to empty the basin. There is an overflow from the basin
to this manhole which makes it impossible to fill the basin above the
intended level.
[Illustration: LONGITUDINAL SECTION ON _a-b-c-d-e-f-g-h_
FILTER BEDS
PLAN AND SECTION OF FILTER NO. 2
FIG. 3.]
[Illustration: OUTSIDE WALL, READY FOR CONCRETE BACKING.]
[Illustration: SEDIMENTATION-BASIN: SHOWING CONSTRUCTION OF FLOOR.
[_To face page 294._]
]
=Filters.=—The filters are of masonry, and are covered to protect them
against the winters, which are quite severe in Albany. The piers,
cross-walls, and linings of the outside walls, entrances, etc., are of
vitrified brick. All other masonry is concrete. The average depth of
excavation for the filters was 4 feet, and the material at the bottom
was usually blue or yellow clay. In some places shale was encountered.
In one place soft clay was found, and there the foundations were made
deeper. The floors consisted of inverted, groined, concrete arches,
arranged to distribute the weight of the walls and vaulting over the
whole area of the bottom.
The groined arch-vaulting is of concrete with a clear span of 11 feet
11 inches, a rise of 2-1/2 feet, and a thickness of 6 inches at the
crown. It was put in in squares, the joints being on the crowns of the
arches parallel with the lines of the piers, and each pier being the
centre of one square. The manholes are in alternate sections, and are
of concrete, built in steel forms with castings at the tops, securely
jointed to the concrete.
Above the vaulting there are 2 feet of earth and soil, grassed on
top. The tops of the manholes are 6 inches above the soil to prevent
rain-water from entering them. The drainage of the soil is effected
by a depression of the vaulting over each pier, partially filled with
gravel and sand, from which water is removed by a 2-inch tile-drain
going down the centre of the pier and discharging through its side just
above the top of the sand in the filter.
In order to provide ready access to each filter, a part of the vaulting
near one side is elevated and made cylindrical in shape, making an
inclined runway from the sand-level to a door the threshold of which is
6 inches above the level of the overflow.
[Illustration:
FILTER BEDS
SECTION OF FILTERS
FIG. 4.]
This sand-run is provided with permanent timber runways and with secure
doors.
[Illustration: Section.
Elevation.
FIG. 5.—ENTRANCE TO A FILTER.]
The manholes of the filters are provided with double covers of steel
plates to exclude the cold. The covers also exclude light. When
cleaning the filters, light can be admitted by removing the covers.
Supports for electric lights are placed in the vaulting, so that the
filters can be lighted by electricity and the work of cleaning can be
done at night, and in winter under heavy snow, without removing the
covers. The electric lights have not yet been installed.
The regulator-houses, the entrances to the sand-runs, and all exposed
work are of pressed brick with Milford granite trimmings and slate
roofs. The regulator-houses have double walls and double windows and
a tight ceiling in the roof, to make them as warm as possible and to
avoid the necessity of artificial heat to prevent freezing.
[Illustration: COMPUTED FRICTIONAL RESISTANCE OF DRAINAGE SYSTEM OF
ONE FILTER WHEN OPERATING AT A RATE OF 100 M.M. PER HOUR, EQUAL TO
2,570,000 GALS. PER ACRE DAILY.
STANDARD GRAVEL SECTIONS.
FIG. 6.]
[Illustration: PLACING THE FLOOR OF A FILTER.]
[Illustration: BUILDING THE BRICK PIERS.
[_To face page 298._]
]
The main underdrains for removing the filtered water are of
vitrified pipe surrounded by concrete and are entirely below the floors
of the filters.
Connections with the main drain are made through thirty-eight 6-inch
outlets in each filter, passing through the floor and connected with
6-inch lateral drains running through the whole width of the filter.
These drains were made with pipes having one side of the bell cut off
so that they would lie flat on the floor and make concentric joints,
without support and without having to be wedged. They were laid with a
space of about 1 inch between the barrels, leaving a large opening for
the admission of water from the gravel.
The underdrainage system is so designed that, when starting a filter
after cleaning, the friction of the sand is about 50 mm. at a rate of
3,000,000 gallons per acre daily, and the friction of the underdrainage
system is estimated at 10 mm. This very low friction, which is
necessary, is obtained by the use of ample sizes for the underdrains
and low velocities in them. In the outlet and measuring devices
moderate losses of head are not objectionable, and the sizes of the
pipes and connections are, therefore, smaller than the main underdrains.
The gravel surrounding the underdrains is of three grades. The material
was obtained from the river-bed by dredging, and was of the same stock
as that used for preparing ballast for the concrete. It was separated
and cleaned by a special, cylindrical, revolving screen. The coarsest
grade of gravel was that which would not pass round holes 1 inch in
diameter, and free from stones more than about 2 inches in diameter. At
first it was required to pass a screen with holes 2 inches in diameter,
but this screen removed many stones which it was desired to retain, and
the screen was afterward changed to have holes 3 inches in diameter.
The intermediate grades of gravel passed the 1-inch holes, and were
retained by a screen with round holes 3/8 inch in diameter. The finest
gravel passed the above screens and was retained by a screen with
round holes 3/16 inch in diameter. The gravel was washed, until free
from sand and dirt, by water played upon it during the process of
screening, and it was afterward taken over screens in the chutes, where
it was separated from the dirty water, and, when necessary, further
quantities of water were played upon it at these points.
[Illustration:
INLET TO FILTER BED. SECTION ON M-N-O
REGULATOR CHAMBER
LONGITUDINAL SECTION ON A-B-C-D
REGULATOR CHAMBER
SECTION ON K-L
FILTER BEDS
INLET VALVES AND REGULATOR CHAMBER
INLET TO FILTER BED
SECTIONAL PLAN ON P-Q
ORIFICE INDICATOR MARKER
DETAILS OF APPARATUS IN REGULATOR HOUSE
REGULATOR CHAMBER
SECTIONAL PLAN ON E-F-G-H-J
FIG. 7.]
The average mechanical analyses of the three grades of gravel are shown
by Fig. 8. Their effective sizes were 23, 8, and 3 mm. respectively,
and for convenience they are designated by these numbers. The average
uniformity coefficient for each grade was about 1.8.
The 23-mm. gravel entirely surrounded the 6-inch pipe-drains, and was
carried slightly above their tops. In some cases it was used to cover
nearly the whole of the floor, but this was not insisted upon.
The 8-mm. gravel was obtained in larger quantity than the other sizes,
and was used to fill all spaces up to a plane 2-1/2 inches below the
finished surface of the gravel, this layer being about 2 inches thick
over the tops of the drains, and somewhat thicker elsewhere.
The 3-mm. gravel was then applied in a layer 2-1/2 inches deep, and the
surface levelled.
The preliminary estimates of cost were based upon the use of
filter-sand from a bank near the filter-site. Further examination
showed that this sand contained a considerable quantity of lime, and
it was found by experiment with a small filter constructed for that
purpose that the use of this sand would harden the water by about 2
parts in 100,000, and the amount of lime contained in the sand, namely,
about 7 per cent, was sufficient to continue this hardening action
for a considerable number of years. This was regarded as a serious
objection to its use, and the specifications were drawn limiting the
amount of lime in the sand. This excluded all of the local bank sands.
The river-sands which were used were nearly free from lime, and in the
end the sand as secured was probably not only free from lime, but more
satisfactory in other ways, and also cheaper than the bank-sand would
have been.
[Illustration: MECHANICAL COMPOSITION OF FILTER SAND AND GRAVELS.
(ARROWS SHOW REQUIREMENT OF SPECIFICATION)
_Diameters in Millimeters_
FIG. 8.]
The specifications of the filter-sand require that “The filter-sand
shall be clean river-, beach-, or bank-sand, with either sharp or
rounded grains. It shall be entirely free from clay, dust, or organic
impurities, and shall, if necessary, be washed to remove such materials
from it. The grains shall, all of them, be of hard material which will
not disintegrate, and shall be of the following diameters: Not more
than 1 per cent, by weight, less than 0.13 mm., nor more than 10 per
cent less than 0.27 mm.; at least 10 per cent, by weight, shall be
less than 0.36 mm., and at least 70 per cent, by weight, shall be less
than 1 mm., and no particles shall be more than 5 mm. in diameter.
The diameters of the sand-grains will be computed as the diameters of
spheres of equal volume. The sand shall not contain more than 2 per
cent, by weight, of lime and magnesia taken together and calculated as
carbonates.”
[Illustration: PLACING THE CONCRETE VAULTING.]
[Illustration: GENERAL VIEW OF VAULTING, UNDER CONSTRUCTION.
[_To face page 302._]
]
[Illustration: FIG. 9.]
The sand was obtained from the river at various places by dredging.
It was first taken up by dipper-dredges, and brought in scows to a
point in the back channel a little north of the filter-plant. It was
there dumped in a specially prepared place in the bottom of the river,
from which it was lifted by a hydraulic dredge and pumped through a
15-inch pipe an average distance of 525 feet to points selected, and
varied from time to time, on the flats north of the filters. The water
containing the sand was then put through screens having meshes which
excluded all stones 5 mm. in diameter and over, and was then taken into
basins where the sand was deposited and afterward carted to the filters.
Two ejector sand-washing machines, shown in Fig. 9, are provided at
convenient places between the filters. In them the dirty sand is mixed
with water, and is thrown up by an ejector, after which it runs through
a chute into a receptacle, from which it is again lifted by another
ejector. It passes in all through five ejectors, part of the dirty
water being wasted each time. The sand is finally collected from the
last ejector, where it is allowed to deposit from the water.
Water is admitted to each filter through a 20-inch pipe from a pipe
system connecting with the sedimentation-basin. Just inside of the
filter-wall is placed a standard gate, and beyond that a balanced
valve connected with an adjustable float to shut off the water when
it reaches the desired height on the filter. These valves and floats
were constructed from special designs, and are similar in principle to
valves used for the same purpose in the Berlin water-filters.
Each filter is provided with an overflow, so arranged that it cannot be
closed, which prevents the water-level from exceeding a fixed limit in
case the balanced valve fails to act. An outlet is also provided near
the sand-run, so that unfiltered water can be removed quickly from the
surface of the filter, should it be necessary, to facilitate cleaning.
The outlet of each filter is through a 20-inch gate controlled by a
standard graduated to show the exact distance the gate is open. The
water rises in a chamber and flows through an orifice in a brass plate
4 by 24 inches, the centre of which is 1 foot below the level of the
sand-line. At the nominal rate of filtration, 3,000,000 gallons per
acre daily, 1 foot of head is required to force the water through the
orifice. With other rates the head increases or decreases approximately
as the square of the rate and forms a measure of it. With water
standing in the lower chamber, so that the orifice is submerged, it is
assumed that the same rates will be obtained with a given difference
in level between the water on the two sides of the orifice as from an
equal head above the centre of the orifice when discharging into air.
=Measurement of Effluent.=—In order to show the rate of filtration two
floats are connected with the water on the two sides of the orifice.
These floats are counterbalanced; one carries a graduated scale, and
the other a marker which moves in front of the scale and shows the rate
of filtration corresponding to the difference in level of the water
on the two sides. When the water in the lower chamber falls below the
centre of the orifice, the water in the float-chamber is nevertheless
maintained at this level. This is accomplished by making the lower part
of the tube water-tight, with openings just at the desired level, so
that when the water falls below this point in the outer chamber it does
not fall in the float-chamber.
To prevent the loss of water in the float-chamber by evaporation or
from other causes, a lead pipe is brought from the other chamber and
supplies a driblet of water to it constantly; this overflows through
the openings, and maintains the water-level at precisely the desired
point. The floats thus indicate the difference in water-level on the
two sides of the orifice whenever the water in the lower chamber is
above the centre of the orifice; otherwise they indicate the height of
water in the upper chamber above the centre of the orifice, regardless
of the water-level in the lower chamber. The scale is graduated to show
the rates of filtration in millions of gallons per acre of filtering
area. In computing this scale the area of the filters is taken as 0.7
acre, and the coefficient of discharge as 0.61.
At the ordinary rates of filtration the errors introduced by the
different conditions under which the orifice operates will rarely
amount to as much as 100,000 gallons per acre daily, or one thirtieth
of the ordinary rate of filtration. Usually they are much less than
this. The apparatus thus shows directly, and with substantial accuracy,
the rate of filtration under all conditions.
=Measurement of Loss of Head.=—Two other floats with similar
connections show the difference in level between the water standing on
the filter and the water in the main drain-pipe back of the gate, or,
in other words, the frictional resistance of the filter, including the
drains. This is commonly called the loss of head, and increases from
0.2 foot or less, with a perfectly clean filter, to 4 feet with the
filter ready for cleaning. When the loss of head exceeds 4 feet the
rate of filtration cannot be maintained at 3,000,000 gallons per acre
daily with the outlet devices provided, and, in order to maintain the
rate, the filter must be cleaned.
=Adjustment of Gauges.=—The adjustment of the gauges showing the rate
of filtration and loss of head is extremely simple. When a filter is
put in service the gates from the lower chamber to the pure-water
reservoir and to the drain are closed, the outlet of the filter opened,
and both chambers allowed to fill to the level of the water on the
filter. The length of the wire carrying the gauge is then adjusted so
that the gauge will make the desired run without hitting at either end,
and then the marker is adjusted. As both the rate of filtration and
loss of head are zero under these conditions, it is only necessary to
set the markers to read zero on the gauges to adjust them. The gates
can then be opened for regular operation, and the readings on the
gauges will be correct.
[Illustration: INTERIOR OF A FILTER: DRAIN, GRAVEL AND SAND LAYERS.]
[Illustration: INTERIOR OF A FILTER, READY FOR USE.
[_To face page 306._]
]
It is necessary to use wires which are light, flexible, and which will
not stretch. At first piano-wire, No. 27 B. & S. gauge, was used, and
was well adapted to the purpose, except that it rusted rapidly. Because
of the rusting it was found necessary to substitute another wire,
and cold-drawn copper wire, No. 24 B. & S. gauge, was used with fair
results. Stretching is less serious than it would otherwise be, as the
correctness of the adjustment can be observed and corrected readily
every time a filter is out of service.
From the lower chambers in the regulator-houses the water flows
through gates to the pipe system leading to the pure-water reservoir.
Drain-pipes are also provided which allow the water to be entirely
drawn out of each filter, should that be necessary for any reason,
and without interfering with the other filters or with the pure-water
reservoir.
The outlets of the filters are connected in pairs, so that filtered
water can be used for filling the underdrains and sand of the filters
from below prior to starting, thus avoiding the disturbance which
results from bringing dirty water upon the sand of a filter not filled
with water.
=Laboratory Building.=—The scientific control of filters is regarded
as one of the essentials to the best results, and to provide for this
there is a laboratory building at one end of the central court between
the filters and close to the sedimentation-basin, supplied with the
necessary equipment for full bacterial examinations, and also with
facilities for observing the colors and turbidities of raw and filtered
waters, and for making such chemical examinations as may be necessary.
This building also provides a comfortable office, dark room, and
storage room for tools, etc., used in the work.
=Pure-water Reservoir.=—A small pure-water reservoir, 94 feet square
and holding about 600,000 gallons, is provided at the filter-plant. The
construction is similar to that of the filters, but the shapes of the
piers and vaulting were changed slightly, as there was no necessity for
the ledges about the bottoms of the piers and walls; while provision
is made for taking the rain-water, falling upon the vaulting above, to
the nearest filters instead of allowing it to enter the reservoir. The
floor and roof of the reservoir are at the same levels as those of the
filters.
CAPACITY OF PLANT AND MEANS OF REGULATION.
The various filters have effective filtering areas of from 0.702 to
0.704 acre, depending upon slight differences in the thickness of the
walls in different places. For the purpose of computation, the area of
each filter is taken at 0.7 acre. The nominal rate of filtration is
taken as 3,000,000 gallons per acre daily, at which rate each filter
will yield 2,100,000 gallons daily, and, with one filter out of use
for the purpose of being cleaned, seven filters normally in use will
yield 14,700,000 gallons. The entrances and outlets are all made of
sufficient size, so that rates 50 per cent greater than the foregoing
are possible. The capacities of the intake, pumping-station, and piping
are such as to supply any quantity of water which the filters can
take, up to an extreme maximum of 25,000,000 gallons in 24 hours. The
pure-water conduit from the filters to Quackenbush Street is nominally
rated at 25,000,000 gallons per 24 hours, after it has become old and
somewhat tuberculated. In its present excellent condition it will carry
a larger quantity,
At the pumping-station at Quackenbush Street there are three Allis
pumps, each capable of pumping 5,000,000 gallons per 24 hours. In
addition to the above there are the old reserve pumps with a nominal
capacity of 10,000,000 gallons per 24 hours, which can be used if
necessary, but which require so much coal that they are seldom used.
For practical purposes the 15,000,000 gallons represents the pumping
capacity of this station and also the capacity of the filters, but
the arrangements are such that in case of emergency the supply can be
increased to 20,000,000 or even 25,000,000 gallons for a short time.
The water is pumped through rising mains to reservoirs holding
37,000,000 gallons, not including the Tivoli low-service reservoir,
which is usually supplied from gravity sources. The reservoir capacity
is such that the pumping can be suspended at Quackenbush Street
for considerable periods if necessary, and in practice it has been
suspended at certain times, especially on Sundays. The amount of water
required is also somewhat irregular. The drainage areas supplying the
gravity reservoirs are much larger, relatively, than the reservoirs,
and at flood periods the volume of the gravity supply is much greater
than that which can be drawn in dry weather. Thus it happens that, at
certain seasons of the year, the amount of water to be pumped is but a
fraction of the nominal capacity of the pumps, and at these times it is
possible to shut the pumps down for greater lengths of time.
=Capacity of Pure-water Reservoir.=—The storage capacity provided
between the filters and the Quackenbush Street pumps is comparatively
small, namely, 600,000 gallons, or one hour’s supply at the full
nominal rate. A larger basin, holding as much as one third or one
half of a day’s supply, would be in many respects desirable in this
position, but the conditions were such as to make it practically
impossible. The bottom of the reservoir could not be put lower without
deepening and increasing greatly the expense of the conduit-line. On
the other hand, the flow-line of the reservoir could not be raised
without raising the level of the filters, which was hardly possible
upon the site selected. The available depth of the reservoir was thus
limited between very narrow bounds, and to secure a large capacity
would have necessitated a very large area, and consequently a great
expense. Under these circumstances, and especially in view of the
abundant storage capacity for filtered water in the distributing
reservoirs, it was not deemed necessary to provide a large storage, and
only so much was provided as would allow the pumps to be started at
the convenience of the engineer, and give a reasonable length of time
for the filters to be brought into operation. For this the pure-water
reservoir is ample, but it is not enough to balance any continued
fluctuations in the rate of pumping.
=Method of Regulating and Changing the Rate of Filtration.=—With
all the Allis pumps running at their nominal capacity, the quantity
of water required will just about equal the nominal capacity of the
filters. When only one or two pumps are running, the rate of filtration
can be reduced. With the plant operating up to its full capacity, the
water-level in the pure-water reservoir will be below the level of
the standard orifices in the filter outlets. When the rate of pumping
is reduced, if no change is made in the gates controlling the filter
outlets, the water will gradually rise in the pure-water reservoir and
in the various regulator chambers, and will submerge the orifices and
gradually reduce the head on the filters, and consequently the rates
of filtration, until those rates equal the quantity pumped. In case
the pumping is stopped altogether, the filters will keep on delivering
at gradually reduced rates until the water-level in the pure-water
reservoir reaches that of the water on the filters.
When the pumps are started up, after such stoppage or reduced rate
of pumping, the water-levels in the pure-water reservoir and in the
gate-chambers will be lowered gradually, and the filters will start
to operate it first with extremely low rates, which will increase
gradually until the water is depressed below the orifices, when they
will again reach the rates at which they were last set. The regulators
during all this time will show the rate of filtration on each filter,
and, if any inequalities occur which demand correction, the gates on
the various outlets can be adjusted accordingly.
[Illustration: CENTRAL COURT, SHOWING SAND-WASHER, DIRTY SAND, ETC.]
[Illustration: SEDIMENTATION BASIN, FILTERS, ETC.
[_To face page 310._]
]
The arrangement, in this respect, combines some of the features of
the English and German plants. In the English plants the filters are
usually connected directly with the clear-water basin, and that in turn
with the pumps, and the speed of filtration is required to respond
to the speed of the pumps, increasing and decreasing with it, being
regulated at all times by the height of water in the pure-water
reservoir. This arrangement has been subject to severe criticism,
because the rate of filtration fluctuates with the consumption, and
especially because the rates of filtration obtained simultaneously in
different filters may be different. There was no way to determine at
what rate any individual filter was working, and there was always a
tendency for a freshly scraped filter to operate much more rapidly than
those which had not been scraped for some time.
This led to the procedure, first formulated by the Commission of German
Water-works Engineers in 1894, and provided for in most of the German
works built or remodelled since that time, of providing pure-water
storage sufficient in amount to make the rate of filtration entirely
independent of the operation of the pumps. Each filter was to be
controlled by itself, be independent of the others, and deliver its
water into a pure-water reservoir lower than itself, so that it could
never be affected by back-water, and so large that there would never be
a demand for sudden changes in the rate of filtration.
This procedure has given excellent results in the German works; but
it leads oftentimes to expensive construction. It involves, in the
first place, a much greater loss of head in passing through the works,
because the pure-water reservoir must be lower than the filters, and
the cost of the pure-water reservoir is increased greatly because
of its large size. The regulation of the filters is put upon the
attendants entirely, or upon automatic devices, and regulation by what
is known as “responding to the pumps” is eliminated.
More recently, the German authorities have shown less disposition to
insist rigidly upon the principles advanced in 1894. In a compilation
of the results of several years’ experience with German water-filters,
Dr. Pannwiz[66] makes a statement of particular interest, of which a
free translation is as follows:
“Most of the German works have sufficient pure-water reservoir capacity
to balance the normal fluctuations in consumption,
so that the rate of filtration is at least independent of the hourly
fluctuations in consumption. Of especial importance is the superficial
area of the pure-water reservoir. If it is sufficiently large, there is
no objection to allowing the water-level in it to rise to that of the
water upon the filters. With very low rates of consumption during the
night the filters may work slowly and even stop, without damage to the
sediment layers when the stopping and starting take place slowly and
regularly, because of the ample reservoir area.”
“The very considerable fluctuations from day to day, especially those
arising from unusual and unforeseen occurrences, are not provided for
entirely by even very large and well-arranged reservoirs. To provide
for these without causing shock, the rate of filtration must be changed
carefully and gradually, and the first essential to success is a good
regulation apparatus.”
“Responding to the pumps” has a great deal to recommend it. It allows
the pure-water reservoir to be put at the highest possible level, it
reduces to a minimum the loss of head in the plant, and yet provides
automatically, and without the slightest trouble on the part of the
attendants, for the delivery of the required quantity of water by the
filters at all times. If the filters are connected directly to the
pumps there is a tendency for the pulsations of the pumps to disturb
their operation, which is highly objectionable, even if the pumps are
far removed; and this exists where filters are connected directly to
the pumps, and a pure-water reservoir is attached to them indirectly.
By taking all the water through the pure-water reservoir and having no
connection except through it, this condition is absolutely avoided, and
the pull on the filters is at all times perfectly steady.
Much has been said as to the effect of variation in the rate of
filtration upon the efficiency of filters. Experiments have been made
at Lawrence and elsewhere which have shown that, as long as the maximum
rate does not exceed a proper one, and under reasonable regulations,
and with the filter in all respects in good order, no marked decrease
in efficiency results from moderate fluctuations in rate. There is
probably a greater decrease in efficiency by stopping the filter
altogether, especially if it is done suddenly, than by simply reducing
the rate. The former sometimes results in loosening air-bubbles in the
sand, which rise to the surface and cause disturbances, but this is not
often caused by simple change in rate.
On the whole, there is little evidence to show that, within reasonable
limits, fluctuations in rate are objectionable, or should be excluded
entirely, especially in such cases as at Albany, where arrangements to
prevent them would have resulted in very greatly increased first cost.
The inferior results sometimes obtained with the system of “responding
to the pumps” as it existed in earlier works, and still exists in many
important places, undoubtedly arises from the fact that there is no
means of knowing and controlling the simultaneous rate of filtration in
different filters, and that one filter may be filtering two or three
times as fast as another, with nothing to indicate it.