HYDRAULIC DATA.

_Water is practically non-elastic._ A pressure of 30,000 lbs. to the

square inch has been applied and its contraction has been found to

be less than one-twelfth. Experiment appears to show that for each

atmosphere of pressure it is condensed 47-1/2 millionth of its bulk.

The mechanical properties of liquids are determined on the hypothesis

that liquids are incompressible; according to known general principles

this is found to be for all practical purposes true, yet liquids are

more compressible than solids. If water be confined in a perfectly

rigid cylindrical vessel, its compression would equal 1/300000 of its

length for every pound per unit of area of the end pressure.

Water is nearly 100 times as compressible as steel, yet for almost all

practical purposes, liquids may be considered as non-elastic bodies

without involving sensible error.

_The pressure upon the horizontal base of any vessel containing a

fluid, is equal to the weight of a column of the fluid, found by

multiplying the area of the base into the perpendicular height of the

column, whatever be the shape of the vessel._

This follows, since here the distance of the center of gravity of the

base from the surface of the fluid, is the same as the perpendicular

height of the column. With a given base and height, therefore, the

pressure is the same whether the vessel is larger or smaller above,

whether its figure is regular or irregular, whether it rises to the

given height in a broad open funnel, or is carried up in a slender tube.

Hence, _any quantity of water, however small, may be made to balance

any quantity, however great_. This is called the _hydrostatic paradox_.

The experiment is usually performed by means of a water-bellows,

as represented in Fig. 84. When the pipe AD is filled with water,

the pressure upon the surface of the bellows, and consequently the

force with which it raises the weights laid on it, will be equal to

the weight of a cylinder of water, whose base is the surface of the

bellows, and height that of the column AD. Therefore, by making the

tube small, and the bellows large, the power of a given quantity of

water, however small, may be increased indefinitely. The pressure of

the column of water in this case corresponds to the force applied by

the piston in the hydrostatic press.

[Illustration: FIG. 84.]

We have already seen that the pressure on the bottom of a vessel

depends neither on the form of the vessel nor on the quantity of the

liquid, but simply on the height of the liquid above the bottom. But

the pressure thus exerted must not be confounded with the pressure

which the vessel itself exerts on the body which supports it. The

latter is always equal to the combined weight of the liquid and the

vessel in which it is contained, while the former may be either smaller

or greater than this weight, according to the form of the vessel. This

fact is often termed the _hydrostatic paradox_, because at first sight

it appears paradoxical.

CD (Fig. 85) is a vessel composed of two cylindrical parts of unequal

diameters, and filled with water to _a_. From what has been said

before, the bottom of the vessel CD supports the same pressure as if

its diameter were everywhere the same as that of its lower part; and it

would at first sight seem that the scale MN of the balance, in which

the vessel CD is placed, ought to show the same weight as if there

had been placed in it a cylindrical vessel having the same weight of

water, and having the diameter of the part D. But the pressure exerted

on the bottom of the vessel is not all transmitted to the scale MN;

for the _upward_ pressure upon the surface _n o_ of the vessel is

precisely equal to the weight of the _extra_ quantity of water which a

cylindrical vessel would contain, and balances an equal portion of the

_downward_ pressure on _m_. Consequently the pressure on the plate MN

is simply equal to the weight of the vessel CD and of the water which

it contains.

[Illustration: FIG. 85.]

_Pressure exerted anywhere upon a mass of liquid is transmitted

undiminished in all directions, and acts with the same force on all

equal surfaces, and in a direction at right angles to those surfaces._

To get a clearer idea of the truth of this principle, let us conceive

a vessel of any given form in the sides of which are placed various

cylindrical apertures, all of equal size, and closed by movable

pistons. Let us, further, imagine this vessel to be filled with liquid

and unaffected by the action of gravity; the pistons will, obviously,

have no tendency to move. If now a weight of P pounds be placed upon

the piston A (Fig. 86), which has a surface A, it will be pressed

inwards, and the pressure will be transmitted to the internal faces of

each of the pistons B, C, D, and E, which will each be forced outwards

by a pressure P, their surfaces being equal to that of the first

piston. Since each of the pistons undergoes a pressure, P, equal to

that on A, let us suppose two of the pistons united so as to constitute

a surface 2_a_; it will have to support a pressure 2P. Similarly, if

the piston were equal to 3_a_, it would experience a pressure of 3P;

and if its area were 100 or 1,000 times that of _a_, it would sustain a

pressure of 100 or 1,000 times P. In other words, the pressure on any

part of the internal walls of the vessel would be proportional to the

surface.

The principle of the equality of pressure is assumed as a consequence

of the constitution of fluids.

By the following experiment it can be shown that pressure is

transmitted in all directions; a cylinder provided with a piston is

fitted into a hollow sphere (Fig. 87). in which small cylindrical jets

are placed perpendicular to the sides. The sphere and the cylinder

being both filled with water, when the piston is moved the liquid

spouts forth from all the orifices, and not merely from that which is

opposite to the piston.

[Illustration: FIG. 86.]

[Illustration: FIG. 87.]

The reason why a satisfactory quantitative experimental demonstration

of the principle of the equality of pressure cannot be given is that

the influence of the weight of the liquid and of the friction of the

pistons cannot be altogether eliminated.

NOTE.—_The influence of the weight (or gravity) of water and its

fractional resistance in practical use_ is so great upon all the

processes of numbers and of the application of the natural laws

governing the operation of fluids, as stated under the heading of

Hydraulic Data, that separate pages will hereafter be found devoted

to a more extended explanation of this subject of gravity and

friction of water.

Yet an approximate verification may be effected by the experiment

represented in Fig. 88. Two cylinders of different diameters are

joined by a tube and filled with water. On the surface of the liquid

are two pistons, P and p, which hermetically close the cylinders, but

move without friction. Let the area of the large piston, P, be, for

instance, thirty times that of the smaller one, p. That being assumed,

let a weight, say of two pounds, be placed upon the small piston; this

pressure will be transmitted to the water and to the large piston, and

as this pressure amounts to two pounds on each portion of its surface

equal to that of the small piston, the large piston must be exposed

to an upward pressure thirty times as much, or of sixty pounds. If

now, this weight be placed upon the large piston, both will remain in

equilibrium; but if the weight is greater or less, this is no longer

the case.

[Illustration: FIG. 88.]

It is important to observe that in speaking of the transmission of

pressure to the sides of the containing vessel, these pressures must

always be supposed to be perpendicular to the sides.

_Equilibrium or state of rest of superposed liquids._ In order that

there should be equilibrium when several heterogeneous liquids are

superposed in the same vessel, each of them must satisfy the conditions

necessary for a single liquid, and further there will be a stable

state of rest only when the liquids are arranged in the order of their

decreasing densities from the bottom upwards.

The last condition is experimentally demonstrated by means of the

_phial of four elements_. This consists of a long narrow bottle

containing mercury, water, colored red, saturated with carbonate of

potash, alcohol, and petroleum. When the phial is shaken the liquids

mix, but when it is allowed to rest they separate; the mercury sinks

to the bottom, then comes the water, then the alcohol, and then the

petroleum. This is the order of the decreasing densities of the bodies.

The water is saturated with carbonate of potash to prevent its mixing

with the alcohol.

This separation of the liquids is due to the same cause as that which

enables solid bodies to float on the surface of a liquid of greater

density than their own. It is also on this account that fresh water, at

the mouths of rivers, floats for a long time on the denser salt water

of the sea; and it is for the same reason that cream, which is lighter

than milk, rises to the surface.

_The pressure upon any particle of a fluid of uniform density is

proportioned to its depth below the surface._

[Illustration: FIG. 89.]

_Example 1._ Let the column of fluid ABCD Fig. (1) be perpendicular

to the horizon. Take any points, _x_ and _y_, at different depths,

and conceive the column to be divided into a number of equal spaces

by horizontal planes. Then, since the density of the fluid is uniform

throughout, the pressure upon _x_ and _y_, respectively, must be in

proportion to the number of equal spaces above them, and consequently

in proportion to their depths.

_Example 2._ Let the column be of the same perpendicular height as

before, but inclined as is Fig. (2); then its quantity, and of course

its weight, is _increased_ in the same ratio as its length exceeds its

height; but since the column is partly supported by the plane, like any

other heavy body, the force of gravity acting upon it is _diminished_

on this account in the same ratio as its length exceeds its height;

therefore as much as the pressure on the base would be augmented by

the increased length of the column, just so much it is lessened by the

action of the inclined plane; and the pressure on any part of C_c_

will be, as before, proportioned to its perpendicular depth; and the

pressure of the inclined column AC_ac_ will be the same as that of the

perpendicular column ABCD.

_Fluids rise to the same level in the opposite arms of a recurved

tube._

[Illustration: FIG. 90.]

Let ABC, (Fig. 90) be a recurved tube: if water be poured into one arm

of the tube, it will rise to the same height in the other arm. For, the

pressure acting upon the lowest part at B, in opposite directions, is

proportioned to its depth below the surface of the fluid. Therefore,

these depths must be equal, that is, the height of the two columns

must be equal, in order that the fluid at B may be at rest; and unless

this part is at rest, the other parts of the column cannot be at rest.

Moreover, since the equilibrium depends on nothing else than the

_heights of_ the respective columns, therefore, the opposite columns

may differ to any degree in quantity, shape, or inclination to the

horizon. Thus, if vessels and tubes very diverse in shape and capacity,

as in Fig. p. 84 be connected with a reservoir, and water be poured

into any one of them, it will rise to the same level in them all.

The reason of this fact will be further understood from the application

of the principle of _equal momenta_, for it will be seen that the

velocity of the columns, when in motion, will be as much greater in the

smaller than in the larger columns, as the quantity of matter is less;

and hence the opposite momenta will be constantly equal.

Hence, water conveyed in aqueducts or running in natural channels, will

rise just as high as its source. Between the place where the water

of an aqueduct is delivered and the spring, the ground may rise into

hills and descend into valleys, and the pipes which convey the water

may follow all the undulations of the country, and the water will run

freely, provided no pipe is laid higher than the spring.

_Pressure of water due to its weight._ The pressure on any particle of

water is proportioned to its depth below the surface. The pressure of

still water in pounds per square inch against the sides of any pipe,

channel, or vessel of any shape whatever, is due solely to the “head”

or height of the level surface of the water above the point at which

the pressure is considered and is equal to ·43302 lbs. per square foot,

every foot of head or 62·355 lbs. per square foot for every foot of

head at 62° F.

The pressure per square inch is equal in all directions downwards,

upwards or sideways and is independent of the shape or size of the

containing vessel; for example, the pressure on a plug forced inward on

a square inch of the surface of water is suddenly communicated to every

square inch of the vessel’s surface, however great and to every inch of

the surface of any body immersed in it.

[Illustration: Various shapes of vessel.]

It is this principle which operates with such astonishing effect in

hydrostatic presses, of which familiar examples are found in the

hydraulic pumps, by the use of which boilers are tested. By the mere

weight of a man’s body when leaning on the extremity of a lever, a

pressure may be produced of upwards of 20 tons; it is the simplest and

most easily applicable of all contrivances for increasing human power,

and it is only limited by want of materials of sufficient strength to

utilize it.

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