Q = (2/3)cbh [root](2gh)

where c = 0.62; or, better, the formula in § 42 may be used.

Gauging weirs are most commonly in the form of rectangular notches;

and care should be taken that the crest is accurately horizontal, and

that the weir is normal to the direction of flow of the stream. If the

planks are thick, they should be bevelled (fig. 67), and then the edge

may be protected by a metal plate about (1/10)th in. thick to secure

the requisite accuracy of form and sharpness of edge. In permanent

gauging weirs, a cast steel plate is sometimes used to form the edge

of the weir crest. The weir should be large enough to discharge the

maximum volume flowing in the stream, and at the same time it is

desirable that the minimum head should not be too small (say half a

foot) to decrease the effects of errors of measurement. The section of

the jet over the weir should not exceed one-fifth the section of the

stream behind the weir, or the velocity of approach will need to be

taken into account. A triangular notch is very suitable for

measurements of this kind.

[Illustration: FIG. 66.]

If the flow is variable, the head h must be recorded at equidistant

intervals of time, say twice daily, and then for each 12-hour period

the discharge must be calculated for the mean of the heads at the

beginning and end of the time. As this involves a good deal of

troublesome calculation, E. Sang proposed to use a scale so graduated

as to read off the discharge in cubic feet per second. The lengths of

the principal graduations of such a scale are easily calculated by

putting Q = 1, 2, 3 ... in the ordinary formulae for notches; the

intermediate graduations may be taken accurately enough by subdividing

equally the distances between the principal graduations.

[Illustration: FIG. 67.]

[Illustration: FIG. 68.]

The accurate measurement of the discharge of a stream by means of a

weir is, however, in practice, rather more difficult than might be

inferred from the simplicity of the principle of the operation. Apart

from the difficulty of selecting a suitable coefficient of discharge,

which need not be serious if the form of the weir and the nature of

its crest are properly attended to, other difficulties of measurement

arise. The length of the weir should be very accurately determined,

and if the weir is rectangular its deviations from exactness of level

should be tested. Then the agitation of the water, the ripple on its

surface, and the adhesion of the water to the scale on which the head

is measured, are liable to introduce errors. Upon a weir 10 ft. long,

with 1 ft. depth of water flowing over, an error of 1-1000th of a foot

in measuring the head, or an error of 1-100th of a foot in measuring

the length of the weir, would cause an error in computing the

discharge of 2 cub. ft. per minute.

_Hook Gauge._--For the determination of the surface level of water,

the most accurate instrument is the hook gauge used first by U. Boyden

of Boston, in 1840. It consists of a fixed frame with scale and

vernier. In the instrument in fig. 68 the vernier is fixed to the

frame, and the scale slides vertically. The scale carries at its lower

end a hook with a fine point, and the scale can be raised or lowered

by a fine pitched screw. If the hook is depressed below the water

surface and then raised by the screw, the moment of its reaching the

water surface will be very distinctly marked, by the reflection from a

small capillary elevation of the water surface over the point of the

hook. In ordinary light, differences of level of the water of .001 of

a foot are easily detected by the hook gauge. If such a gauge is used

to determine the heads at a weir, the hook should first be set

accurately level with the weir crest, and a reading taken. Then the

difference of the reading at the water surface and that for the weir

crest will be the head at the weir.

§ 56. _Modules used in Irrigation._--In distributing water for

irrigation, the charge for the water may be simply assessed on the

area of the land irrigated for each consumer, a method followed in

India; or a regulated quantity of water may be given to each consumer,

and the charge may be made proportional to the quantity of water

supplied, a method employed for a long time in Italy and other parts

of Europe. To deliver a regulated quantity of water from the

irrigation channel, arrangements termed modules are used. These are

constructions intended to maintain a constant or approximately

constant head above an orifice of fixed size, or to regulate the size

of the orifice so as to give a constant discharge, notwithstanding the

variation of level in the irrigating channel.

[Illustration: FIG. 69.]

§ 57. _Italian Module._--The Italian modules are masonry

constructions, consisting of a regulating chamber, to which water is

admitted by an adjustable sluice from the canal. At the other end of

the chamber is an orifice in a thin flagstone of fixed size. By means

of the adjustable sluice a tolerably constant head above the fixed

orifice is maintained, and therefore there is a nearly constant

discharge of ascertainable amount through the orifice, into the

channel leading to the fields which are to be irrigated.

[Illustration: FIG. 70.--Scale 1/100.]

In fig. 69, A is the adjustable sluice by which water is admitted to

the regulating chamber, B is the fixed orifice through which the water

is discharged. The sluice A is adjusted from time to time by the canal

officers, so as to bring the level of the water in the regulating

chamber to a fixed level marked on the wall of the chamber. When

adjusted it is locked. Let [omega]1 be the area of the orifice through

the sluice at A, and [omega]2 that of the fixed orifice at B; let h1

be the difference of level between the surface of the water in the

canal and regulating chamber; h2 the head above the centre of the

discharging orifice, when the sluice has been adjusted and the flow

has become steady; Q the normal discharge in cubic feet per second.

Then, since the flow through the orifices at A and B is the same,

Q = c1[omega]1 [root](2gh1) = c2[omega]2 [root](2gh2),

where c1 and c2 are the coefficients of discharge suitable for the two

orifices. Hence

c1[omega]1/c2[omega]2 = [root](h2/h1).

If the orifice at B opened directly into the canal without any

intermediate regulating chamber, the discharge would increase for a

given change of level in the canal in exactly the same ratio.

Consequently the Italian module in no way moderates the fluctuations

of discharge, except so far as it affords means of easy adjustment

from time to time. It has further the advantage that the cultivator,

by observing the level of the water in the chamber, can always see

whether or not he is receiving the proper quantity of water.

On each canal the orifices are of the same height, and intended to

work with the same normal head, the width of the orifices being varied

to suit the demand for water. The unit of discharge varies on

different canals, being fixed in each case by legal arrangements. Thus

on the Canal Lodi the unit of discharge or one module of water is the

discharge through an orifice 1.12 ft. high, 0.12416 ft. wide, with a

head of 0.32 ft. above the top edge of the orifice, or .88 ft. above

the centre. This corresponds to a discharge of about 0.6165 cub. ft.

per second.

[Illustration: FIG. 71.]

In the most elaborate Italian modules the regulating chamber is arched

over, and its dimensions are very exactly prescribed. Thus in the

modules of the Naviglio Grande of Milan, shown in fig. 70, the

measuring orifice is cut in a thin stone slab, and so placed that the

discharge is into the air with free contraction on all sides. The

adjusting sluice is placed with its sill flush with the bottom of the

canal, and is provided with a rack and lever and locking arrangement.

The covered regulating chamber is about 20 ft. long, with a breadth

1.64 ft. greater than that of the discharging orifice. At precisely

the normal level of the water in the regulating chamber, there is a

ceiling of planks intended to still the agitation of the water. A

block of stone serves to indicate the normal level of the water in the

chamber. The water is discharged into an open channel 0.655 ft. wider

than the orifice, splaying out till it is 1.637 ft. wider than the

orifice, and about 18 ft. in length.

§ 58. _Spanish Module._--On the canal of Isabella II., which supplies

water to Madrid, a module much more perfect in principle than the

Italian module is employed. Part of the water is supplied for

irrigation, and as it is very valuable its strict measurement is

essential. The module (fig. 72) consists of two chambers one above the

other, the upper chamber being in free communication with the

irrigation canal, and the lower chamber discharging by a culvert to

the fields. In the arched roof between the chambers there is a

circular sharp-edged orifice in a bronze plate. Hanging in this there

is a bronze plug of variable diameter suspended from a hollow brass

float. If the water level in the canal lowers, the plug descends and

gives an enlarged opening, and conversely. Thus a perfectly constant

discharge with a varying head can be obtained, provided no clogging or

silting of the chambers prevents the free discharge of the water or

the rise and fall of the float. The theory of the module is very

simple. Let R (fig. 71) be the radius of the fixed opening, r the

radius of the plug at a distance h from the plane of flotation of the

float, and Q the required discharge of the module. Then

Q = c[pi](R² - r²) [root](2gh).

Taking c = 0.63,

Q = 15.88(R² - r²) [root]h;

r = [root]{R² - Q/15.88 [root]h}.

Choosing a value for R, successive values of r can be found for

different values of h, and from these the curve of the plug can be

drawn. The module shown in fig. 72 will discharge 1 cubic metre per

second. The fixed opening is 0.2 metre diameter, and the greatest head

above the fixed orifice is 1 metre. The use of this module involves a

great sacrifice of level between the canal and the fields. The module

is described in Sir C. Scott-Moncrieff's _Irrigation in Southern

Europe_.

§ 59. _Reservoir Gauging Basins._--In obtaining the power to store the

water of streams in reservoirs, it is usual to concede to riparian

owners below the reservoirs a right to a regulated supply throughout

the year. This compensation water requires to be measured in such a

way that the millowners and others interested in the matter can assure

themselves that they are receiving a proper quantity, and they are

generally allowed a certain amount of control as to the times during

which the daily supply is discharged into the stream.

[Illustration: FIG. 72.]

Fig. 74 shows an arrangement designed for the Manchester water works.

The water enters from the reservoir at chamber A, the object of which

is to still the irregular motion of the water. The admission is

regulated by sluices at b, b, b. The water is discharged by orifices

or notches at a, a, over which a tolerably constant head is maintained

by adjusting the sluices at b, b, b. At any time the millowners can

see whether the discharge is given and whether the proper head is

maintained over the orifices. To test at any time the discharge of the

orifices, a gauging basin B is provided. The water ordinarily flows

over this, without entering it, on a floor of cast-iron plates. If the

discharge is to be tested, the water is turned for a definite time

into the gauging basin, by suddenly opening and closing a sluice at c.

The volume of flow can be ascertained from the depth in the gauging

chamber. A mechanical arrangement (fig. 73) was designed for securing

an absolutely constant head over the orifices at a, a. The orifices

were formed in a cast-iron plate capable of sliding up and down,

without sensible leakage, on the face of the wall of the chamber. The

orifice plate was attached by a link to a lever, one end of which

rested on the wall and the other on floats f in the chamber A. The

floats rose and fell with the changes of level in the chamber, and

raised and lowered the orifice plate at the same time. This mechanical

arrangement was not finally adopted, careful watching of the sluices

at b, b, b, being sufficient to secure a regular discharge. The

arrangement is then equivalent to an Italian module, but on a large

scale.

[Illustration: FIG. 73.--Scale 1/120.]

[Illustration: FIG. 74.--Scale 1/500.]

§ 60. _Professor Fleeming Jenkin's Constant Flow Valve._--In the

modules thus far described constant discharge is obtained by varying

the area of the orifice through which the water flows. Professor F.

Jenkin has contrived a valve in which a constant pressure head is

obtained, so that the orifice need not be varied (_Roy. Scot. Society_

_of Arts_, 1876). Fig. 75 shows a valve of this kind suitable for a

6-in. water main. The water arriving by the main C passes through an

equilibrium valve D into the chamber A, and thence through a sluice O,

which can be set for any required area of opening, into the

discharging main B. The object of the arrangement is to secure a

constant difference of pressure between the chambers A and B, so that

a constant discharge flows through the stop valve O. The equilibrium

valve D is rigidly connected with a plunger P loosely fitted in a

diaphragm, separating A from a chamber B2 connected by a pipe B1 with

the discharging main B. Any increase of the difference of pressure in

A and B will drive the plunger up and close the equilibrium valve, and

conversely a decrease of the difference of pressure will cause the

descent of the plunger and open the equilibrium valve wider. Thus a

constant difference of pressure is obtained in the chambers A and B.

Let [omega] be the area of the plunger in square feet, p the

difference of pressure in the chambers A and B in pounds per square

foot, w the weight of the plunger and valve. Then if at any moment

p[omega] exceeds w the plunger will rise, and if it is less than w the

plunger will descend. Apart from friction, and assuming the valve D to

be strictly an equilibrium valve, since [omega] and w are constant, p

must be constant also, and equal to w/[omega]. By making w small and

[omega] large, the difference of pressure required to ensure the

working of the apparatus may be made very small. Valves working with a

difference of pressure of ½ in. of water have been constructed.

[Illustration: FIG. 75.--Scale 1/24.]

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