CHAPTER VI.

GAUGING FLOW IN SEWERS.

A method frequently adopted to gauge the flow of the sewage is

to fix a weir board with a single rectangular notch across the

sewer in a convenient manhole, which will pond up the sewage;

and then to ascertain the depth of water passing over the notch

by measurements from the surface of the water to a peg fixed

level with the bottom of the notch and at a distance of two or

three feet away on the upstream side. The extreme variation in

the flow of the sewage is so great, however, that if the notch

is of a convenient width to take the maximum flow, the hourly

variation at the time of minimum flow will affect the depth of

the sewage on the notch to such a small extent that difficulty

may be experienced in taking the readings with sufficient

accuracy to show such variations in the flow, and there will be

great probability of incorrect results being obtained by reason

of solid sewage matter lodging on the notch. When the depth on

a l2 in notch is about 6 in, a variation of only 1-16th inch in

the vertical measurement will represent a difference in the

rate of the flow of approximately 405 gallons per hour, or

about 9,700 gallons per day. When the flow is about lin deep

the same variation of 1-16th in will represent about 162

gallons per hour, or 3,900 gallons per day. Greater accuracy

will be obtained if a properly-formed gauging pond is

constructed independently of the manhole and a double

rectangular notch, similar to Fig. 13, or a triangular or V-

shaped notch, as shown in Fig. 14, used in lieu of the simpler

form.

In calculating the discharge of weirs there are several formulæ

to choose from, all of which will give different results,

though comparative accuracy has been claimed for each. Taking

first a single rectangular notch and reducing the formulae to

the common form:

____

Discharge per foot in width of weir = C \/ H^3

where H = depth from the surface of still water above the weir to the level of

the bottom of the notch, the value of C will be as set out in the following

table:--

TABLE No. 5.

RECTANGULAR NOTCHES.

_____

Discharge per foot in width of notch = C \/ H^3

------------------------------------------------------------------

Values of C.

--------------------------------------+---------------------------

H Measured in | Feet. | Inches.

---------------+-----------+----------+-----------+---------------

| Gallons | C. ft | Gallons | C. ft

Discharge in | per hour. | per min | per hour. | per min

---------------+-----------+----------+-----------+---------------

Authority. | | | |

Box | 79,895 | 213.6 | 1,922 | 5.13

Cotterill | 74,296 | 198.6 | 1,787 | 4.78

Francis | 74,820 | 200.0 | 1,800 | 4.81

Mo'esworth | 80,057 | 214.0 | 1,926 | 5.15

Santo Crimp | 72,949 | 195.0 | 1,755 | 4.69

---------------+-----------+----------+-----------+---------------

In the foregoing table Francis' short formula is used, which

does not take into account the end contractions and therefore

gives a slightly higher result than would otherwise be the

case, and in Cotterill's formula the notch is taken as being

half the width of the weir, or of the stream above the weir. If

a cubic foot is taken as being equal to 6-1/4 gallons instead

of 6.235 gallons, then, cubic feet per minute multiplied by

9,000 equals gallons per day. This table can be applied to

ascertain the flow through the notch shown in Fig. 13 in the

following way. Suppose it is required to find the discharge in

cubic feet per minute when the depth of water measured in the

middle of the notch is 4 in Using Santo Crimp's formula the

result will be

C\/H^3 = 4.69 \/4^3 = 4.69 x 8 = 37.52

cubic feet per foot in width of weir, but as the weir is only 6

in wide, we must divide this figure by 2, then

37.52/2 = 18.76 cubic feet, which is the discharge per minute.

+------+ +------+

| | FIG. 13 | |

| | | |

| | | |

| +------+ +------+ |

| | | |

| | | |

| | | |

| +------+ |

| |

| |

| |

| |

+----------------------------------+

Fig. 13.-ELEVATION OF DOUBLE RECTANGULAR NOTCHED GAUGING WEIR.

+------+ +------+

| \ FIG. 13 / |

| \ / |

| \ / |

| \ / |

| \ / |

| \ / |

| \ / |

| \ / |

| \ / |

| \/ |

| |

| |

| |

| |

| |

+----------------------------------+

FIG. 14.-ELEVATION OF TRIANGULAR NOTCHED GAUGING WEIR.

FIG. 15.-LONGITUDINAL SECTION, SHOWING WEIR, GAUGE-PEG, AND HOOK-GAUGE

If it is required to find the discharge in similar terms with a

depth of water of 20 in, two sets of calculations are required.

First 20 in depth on the notch 6 in wide, and then 4 in depth

on the notch, 28 in minus 6 in, or 1 ft wide.

____ _____

(1) C\/ H^3 = 4.69/2 \/ 10^3 = 2.345 x 31.62 = 74.15

____ ____

(2) C\/ H^3 = 1.0 x 4.69 \/ 4^3 = 1.0 x 4.69 x 8 = 37.52

Total in c. ft per min = 111.67

The actual discharge would be slightly in excess of this.

In addition to the circumstances already enumerated which

affect the accuracy of gaugings taken by means of a weir fixed

in a sewer there is also the fact that the sewage approaches

the weir with a velocity which varies considerably from time to

time. In order to make allowance for this, the head calculated

to produce the velocity must be added to the actual head. This

can be embodied in the formula, as, for example, Santo Crimp's

formula for discharge in cubic feet per minute, with H measured

in feet, is written

__________________

195\/(11^3 + .035V - H^2

instead of the usual form of

____

195\/ H^3, which is used

when there is no velocity to take into account. The V

represents the velocity in feet per second.

Triangular or V notches are usually formed so that the angle

between the two sides is 90°, when the breadth at any point

will always be twice the vertical height measured at the

centre. The discharge in this case varies as the square root of

the fifth power of the height instead of the third power as

with the rectangular notch. The reason for the alteration of

the power is that _approximately_ the discharge over a notch

with any given head varies as the cross-sectional area of the

body of water passing over it. The area of the 90° notch is

half that of a circumscribing rectangular notch, so that the

discharge of a V notch is approximately equal to that of a

rectangular notch having a width equal to half the width of the

V notch at water level, and as the total width is equal to

double the depth of water passing over the notch the half width

is equal to the full depth and the discharge is equal to that

of a rectangular notch having a width equal to the depth of

water flowing over the V notch from time to time, both being

measured in the same unit, therefore

____ ____ ____

C \/ H^3 becomes C x H x \/ H^3 which equals C \/ H^5.

The constant C will, however, vary from that for the

rectangular notch to give an accurate result.

TABLE No. 6.

TRIANGULAR OR V NOTCHES.

____

Discharge = C x \/ H^5.

Values of C.

--------------+-----------------------+------------------------

H Measured in | Feet. | Inches.

--------------+----------+------------+-----------+------------

Discharge in | Gallons | C. ft per | Gallons | C. ft per

| per hour | min | per hour. | min

--------------+----------+------------+-----------+------------

Alexander | 59,856 | 160 | 120.0 | 0.321

Cotterill | 57,013 | 152.4 | 114.3 | 0.306

Molesworth | 59,201 | 158.2 | 118.7 | 0.317

Thomson | 57,166 | 152.8 | 114.6 | 0.306

--------------+----------+------------+-----------+------------

Cotterill's formula for the discharge in cubic feet per minute

is

_______

16 x C x B \/ 2g H^3

when B = breadth of notch in feet and H = height of water in

feet and can be applied to any proportion of notch. When B =

2H, that is, a 90° notch, C = .595 and the formula becomes

____

152.4 \/ H^5,

and when B = 4H, that is, a notch containing an angle of 126°

51' 36", C = .62 and the formula is then written

____

318 \/ H^5.

The measurements of the depth of the water above the notch

should be taken by a hook-gauge, as when a rule or gauge-slate

is used the velocity of the water causes the latter to rise as

it comes in contact with the edge of the measuring instrument

and an accurate reading is not easily obtainable, and, further,

capillary attraction causes the water to rise up the rule above

the actual surface, and thus to show a still greater depth.

When using a hook-gauge the top of the weir, as well as the

notch, should be fixed level and a peg or stake fixed as far

back as possible on the upstream side of the weir, so that the

top of the peg is level with the top of the weir, instead of

with the notch, as is the case when a rule or gauge-slate is

used. The hook-gauge consists of a square rod of, say, lin

side, with a metal hook at the bottom, as shown in Fig. 15, and

is so proportioned that the distance from the top of the hook

to the top of the rod is equal to the difference in level of

the top of the weir and the sill of the notch. In using it the

rod of the hook-gauge is held against the side of the gauge-peg

and lowered into the water until the point of the hook is

submerged. The gauge is then gently raised until the point of

the hook breaks the surface of the water, when the distance

from the top of the gauge-peg to the top of the rod of the

hook-gauge will correspond with the depth of the water flowing

over the weir.

The Sewerage of Sea Coast Towns · 第 6 / 15 章