CHAPTER VI.

ABOUT WATER—HYDROSTATICS AND HYDRAULICS—LAW OF ARCHIMEDES—THE BRAMAH

PRESS—THE SYPHON.

At present we will pass from Air to Water, from Pneumatics to

Hydrostatics and Hydraulics. We must remember that Hydrostatics and

Hydraulics are very different. The former treats of the weight and

pressure of liquids when they are at rest, the latter treats of them in

motion. We will now speak of the properties of Liquids, of which Water

may be taken as the most familiar example.

We have already seen that Matter exists in the form of Solids, Liquids,

and Gases, and of course Water is one form of Matter. It occupies a

certain space, is slightly compressible; it possesses weight, and

exercises force when in motion. It is a fluid, but also a liquid. There

are fluids not liquid, such as air or steam, to take equally familiar

examples. These are elastic fluids and compressible, while water is

inelastic, and termed incompressible.

The chemical composition of water will be considered hereafter, but at

present we may state that water is composed of oxygen and hydrogen, and

proportions of eight of the former to one of the latter by weight; in

volume the hydrogen is as two to one.

From these facts, as regards water, we learn that volume and weight

are very different things,—that equal volumes of various things may

have different weights, and that volume (or bulk) by no means indicates

weight Equal volumes of feathers and sand will weigh very differently.

[The old “catch” question of the “difference in weight between a pound

of lead and a pound of feathers” here comes to the mind. The answer

generally given is that “feathers make the heavier ‘pound’ because

they are weighed by avoirdupois, and lead by troy weight.” This is an

error. They are both weighed in the same way, and pound for pound are

the same _weight_, though different in _volume_.]

Fluids in equilibrium have all their particles at the same distance

from the centre of the earth, and although within small distances

liquids appear perfectly level (in a direct line), they must, as the

sea does, conform to the shape of the earth, though in small levels the

space is too limited to admit of any deviation from the plane at right

angle to the direction of gravity.

Liquids always fall to a perfectly level surface, and water will seek

to find its original level, whether it be in one side of a bent tube,

in a watering pot and its spout, or as a fountain. The surface of the

water will be on the same level in the arms of a bent tube, and the

fountain will rise to a height corresponding with the elevation of the

parent spring whence it issues. The waterworks companies first pump

the water to a high reservoir, and then it rises equally high in our

high-level cisterns.

As an example of the force of water, a pretty little experiment may be

easily tried, and, as many of our readers have seen in a shop in the

Strand in London, it always is attractive. A good-sized glass shade

should be procured and placed over a water tap and basin, as per the

illustration herewith. Within the glass put a number of balls of cork

or other light material. Let a stop-cock, with a small aperture, be

fixed upon the tube leading into the glass. Another tube to carry away

the water should, of course, be provided, but it may be used over

again. When the tap is properly fixed, if the pressure of the water be

sufficient, it will rush out with some force, and catching the balls as

they fall to the bottom of the glass shade bear them up as a juggler

would throw oranges from hand to hand. If coloured balls be used the

effect may be enhanced, and much variety imparted to the experiment,

which is very easy to make.

[Illustration: Fig. 57.—Water jet and balls.]

Water exercises an enormous pressure, but the pressure does not depend

upon the amount of water in the vessel. It depends upon the vessel’s

height, and the dimensions of the base. This has been proved by filling

vessels whose bases and heights are equal, but whose shapes are

different, each holding a different quantity of water. The pressure at

the bottom of each vessel is the same, and depends upon the depth of

the water. If we subject a portion of the liquid surface to certain

force, this pressure will be dispersed equally in all directions, and

from an acquaintance with this fact the Hydraulic Press was brought

into notice. If a vessel with a horizontal bottom be filled with water

to a depth of one foot, every square foot will sustain a pressure of

62·37 lbs., and each square inch of 0·433 lbs.

[Illustration: Figs. 58, 59, 60, 61.—Pressure of Water.]

We will now explain the principle of this WATER PRESS. In the small

diagram, the letters A B represent the bottom of a cylinder which has a

piston fitted in it (P). Into the opposite side a pipe is let in, which

leads from a force-pump D, which is fitted with a valve E, opening

upwards. When the piston in D is pulled up water enters through the

valve; when the piston is forced down the valve shuts, and the water

rushes into the chamber A B. The pressure pushes up the large piston

with a force multiplied as many times as the area of the small piston

is contained in the large one. So if the large one be ten times as

great as the small one, and the latter be forced down with a 10 lb.

pressure, the pressure on the large one will be 100 lbs., and so on.

[Illustration: Fig. 62.—Water Press.]

The accompanying illustration shows the form of the Hydraulic or Bramah

Press. A B C D is a strong frame, F the force-pump worked by means of

a lever fixed at G, and H is the counterprise. E is the stop-cock to

admit the water (fig. 63).

[Illustration: Fig. 63.—Bramah Press.]

The principles of hydrostatics will be easily explained. The Lectures

of M. Aimé Schuster, Professor and Librarian at Metz, have taught us in

a very simple manner the principle of Archimedes, in which it is laid

down that “a body immersed in a liquid loses a portion of its weight

equal to the weight of the liquid displaced by it.” We take a body

of as irregular form as we please; a stone, for example. A thread is

attached to the stone, and it is then placed in a glass of water full

up to the brim. The water overflows; a volume of the liquid equal to

that of the stone runs over. The glass thus partially emptied is then

dried, and placed on the scale of a balance, beneath which we suspend

the stone; equilibrium is established by placing some pieces of lead

in the other scale. We then take a vase full of water, into which we

plunge the stone suspended from the scale, supporting the vase by means

of bricks. The equilibrium is now broken; to re-establish it, it is

necessary to fill up with water the glass placed on the scale; that

is to say, we put back in the glass the weight of a volume of water

precisely equal to that of the stone.

[Illustration: Fig. 64.—Demonstration of the upward pressure of

liquids.]

If it is desired to investigate the principles relating to connected

vessels, springs of water, artesian wells, etc., two funnels, connected

by means of an india-rubber tube of certain length, will serve for the

demonstration; and by placing the first funnel at a higher level, and

pouring in water abundantly, we shall see that it overflows from the

second.

A disc of cardboard and a lamp-glass will be all that is required to

show the upward pressure of liquids. I apply to the opening of the

lamp-glass a round piece of cardboard, which I hold in place by means

of a string; the tube thus closed I plunge into a vessel filled with

water. The piece of cardboard is held by the pressure of the water

upwards. To separate it from the opening it suffices to pour some

water into the tube up to the level of the water outside (fig. 64). The

outer pressure exercised on the disc, as well as the pressure beneath,

is now equal to the weight of a body of water having for its base the

surface of the opening of the tube, its depth being the distance from

the cardboard to the level of the water.

Syringes, pumps, etc., are the effects of atmospheric pressure.

Balloons rise in the air by means of the pressure of gas; a balloon

being a body plunged in gas, is consequently submitted to the same laws

as a body plunged in water.

Boats float because of the pressure of liquid, and water spurts from

a fountain for the same reason. I recollect having read a very useful

application of the principles of fluid pressure.

[Illustration: Fig 65.—Experiment on the convexity of a meniscus.]

A horse was laden with two tubs for carrying a supply of water, and

in the bottom of the tubs a valve was fixed. When the horse entered

the stream the tubs were partly immersed; the water then exercised its

upward pressure, the valve opened, and the tubs slowly filled. When

they were nearly full the horse turned round and came out of the water;

the pressure had ceased.

Thus the action of the water first opened the valve, and then closed it.

The particular phenomena observable in the water level in narrow

spaces, as of a fine glass tube, or the level of two adjoining waves,

capillary phenomena, etc., do not need any special appliance for

demonstration, and it is the same with the convexity or concavity of

meniscuses.

Fig. 65 represents a pretty experiment in connection with these

phenomena. I take a glass, which I fill up to the brim, taking care

that the meniscus be concave, and near it I place a pile of pennies.

I then ask my young friends how many pennies can be thrown into the

glass without the water overflowing. Everyone who is not familiar with

the experiment will answer that it will only be possible to put in one

or two, whereas it is possible to put in a considerable number, even

ten or twelve. As the pennies are carefully and slowly dropped in, the

surface of the liquid will be seen to become more and more convex, and

one is surprised to what an extent this convexity increases before the

water overflows.

The common _syphon_ may be mentioned here. It consists of a bent tube

with limbs of unequal length. We give an illustration of the syphon

(fig. 66). The shorter leg being put into the mixture, the air is

exhausted from the tube at _o_, the aperture at _g_ being closed with

the finger. When the finger is removed the liquid will run out. If the

water were equally high in both legs the pressure of the atmosphere

would hold the fluid in equilibrium, but one leg being longer, the

column of water in it preponderates, and as it falls, the pressure on

the water in the vessel keeps up the supply.

[Illustration: Fig. 66.—The Syphon.]

Apropos of the syphon, we may mention a very simple application of the

principle. Cut off a strip of cloth, and arrange it so that one end

shall remain in a glass of water while the other hangs down, as in the

illustration. In a short time the water from the upper glass will have

passed through the cloth-fibres to the lower one (fig. 67).

This attribute of porous substances is called _capillarity_, and shows

itself by _capillary attraction_ in very fine pores or tubes. The same

phenomenon is exhibited in blotting paper, sugar, wood, sand, and

lamp-wicks, all of which give familiar instances of capillarity. The

cook makes use of this property by using thin paper to absorb grease

from the surface of soups.

Capillarity (referred to on page 25) is the term used to define

capillary force, and is derived from the word _capillus_, a hair; and

so very small bore tubes are called capillary tubes. We know that when

we plunge a glass tube into water the liquid will rise up in it, and

the narrower the tube the higher the water will go; moreover, the water

inside will be higher than at the outside. This is in accordance with a

well-known law of adhesion, which induces concave or convex surfaces[9]

in the liquids in the tubes, according as the tube is wetted with the

liquid or not. For instance, water, as we have said, will be higher in

the tube, and concave in form; but mercury will be depressed below the

outside level, and convex, because mercury will not adhere to glass.

When the force of cohesion to the sides of the tube is more than twice

as great as the adhesion of the particles of the liquid, it will rise

up the sides, and if the forces be reversed, the rounded appearance

will follow. This accounts for the convex appearance, or “meniscus,” in

the column of mercury in a barometer.

Amongst the complicated experiments to demonstrate molecular

attraction, the following is very simple and very pretty:—Take two

small balls of cork, and having placed them in a basin half-filled with

water, let them come close to each other. When they have approached

within a certain distance they will rush together. If you fix one of

them on the blade of your penknife, it will attract the other as a

magnet, so that you can lead it round the basin (fig. 68). But if the

balls of cork are covered with grease they will _repel_ each other,

which fact is accounted for by the form of the _menisques_, which are

convex or concave, according as they are moistened, or preserved from

action of the water by the grease.

[Illustration: Fig. 67.—An improvised syphon.]

This attribute is of great use in the animal and vegetable kingdoms.

The rising of the sap is one instance of the latter.

Experience in hydrostatics can be easily applied to amusing little

experiments. For instance, as regards the syphon, we may make an image

of _Tantalus_ as per illustration (fig. 69). A wooden figure may be cut

in a stooping posture, and placed in the centre of a wide vase, as if

about to drink. If water be poured slowly into the vase it will never

rise to the mouth of the figure, and the unhappy _Tantalus_ will remain

in expectancy. This result is obtained by the aid of a syphon hidden in

the figure, the shorter limb of which is in the chest. The longer limb

descends through a hole in the table, and carries off the water. These

vases are called _vases of Tantalus_.

The principle of the syphon may also be adapted to our domestic

filters. Charcoal, as we know, makes an excellent filter, and if we

have a block of charcoal in one of those filters,—now so common,—we can

fix a tube into it, and clear any water we may require. It sometimes

(in the country) happens that drinking-water may become turgid, and in

such a case the syphon filter will be found useful.

[Illustration: Fig. 68.—Molecular attraction.]

The old “deception” jugs have often puzzled people. We give an

illustration of one, and also a sketch of the “deceptive” portion

(figs. 70 and 71). This deception is very well managed, and will create

much amusement if a jug can be procured; they were fashionable in the

eighteenth century, and previously. A cursory inspection of these

curious utensils will lead one to vote them utterly useless. They are,

however, very quaint, and if not exactly useful are ornamental. They

are so constructed, that if an inexperienced person wish to pour out

the wine or water contained in them, the liquid will run out through

the holes cut in the jug.

To use them with safety it is necessary to put the spout A in

one’s mouth, and close the opening B with the finger, and then

by drawing in the breath, cause the water to mount to the lips by the

tube which runs around the jug. The specimens herein delineated have

been copied from some now existent in the museum of the Sèvres china

manufactory.

The _Buoyancy of Water_ is a very interesting subject, and a great

deal may be written respecting it. The swimmer will tell us that it is

easier to float in salt water than in fresh. He knows by experience

_how difficult it is to sink_ in the sea; and yet hundreds of people

are drowned in the water, which, if they permitted it to exercise its

power of buoyancy, would help to save life.

[Illustration: Fig. 69.—Vase of Tantalus.]

The sea-water holds a considerable quantity of salt in solution, and

this adds to its resistance, or floating power. It is heavier than

fresh water, and the Dead Sea is so salt that a man cannot possibly

sink in it. This means that the man’s body, bulk for bulk, is much

lighter than the water of the Dead Sea. A man will sink in fresh, or

ordinary salt water if the air in his lungs be exhausted, because

without the air he is much heavier than water, bulk for bulk. So if

anything is weighed in water, it apparently loses in weight exactly

equal to its own bulk of water.

Water is the means by which the _Specific Gravity_ of liquids or solids

is found, and by it we can determine the relative densities of matter

in proportion. Air is the standard for gases and vapours. Let us

examine this, and see what is meant by SPECIFIC GRAVITY.

We have already mentioned the difference existing between two equal

volumes of different substances, and their weight, which proves that

they may contain a different number of atoms in the same space. We also

know, from the principle of Archimedes, that _if a body be immersed in

a fluid, a portion of its weight will be sustained by the fluid equal

to the weight of the fluid displaced_.

[Illustration: Fig. 70.—Deception jugs of old pattern.]

[This theorem is easily proved by filling a bucket with water, and

moving it about in water, when it will be easy to lift; and likewise

the human body may be easily sustained in water by a finger under the

chin.]

The manner in which Archimedes discovered the displacement of liquids

is well known, but is always interesting. King Hiero, of Syracuse,

ordered a crown of gold to be made, and when it had been completed

and delivered to His Majesty, he had his doubts about the honesty of

the goldsmith, and called to Archimedes to tell him whether or not

the crown was of gold, pure and simple. Archimedes was puzzled, and

went home deep in thought. Still considering the problem he went to

the bath, and in his abstraction filled it to the brim. Stepping in he

spilt a considerable quantity of water, and at once the idea struck

him that any body put into water would displace its own weight of the

liquid. He did not wait to dress, but ran half-naked to the palace,

crying out, “Eureka, Eureka! I have found it, I have found it! “What

had he found?—He had solved the problem.

[Illustration: Fig. 71.—Section of jug.]

He got a lump of gold the same weight as the crown, and immersed it

in water. He found it weighed nineteen times as much as its own bulk

of water. But when he weighed the kings crown he found it displaced

more water than the pure gold had done, and consequently it had been

adulterated by a lighter metal. He assumed that the alloy was silver,

and by immersing lumps of silver and gold of equal weight with the

crown, and weighing the water that overflowed from each dip, he was

able to tell the king how far he had been cheated by the goldsmith.

It is by this method now that we can ascertain the specific gravity of

bodies. One cubic inch of water weighs about half an ounce (or to be

exact, 252½ grains). Take a piece of lead and weigh it in air; it

weighs, say, eleven ounces. Then weigh it in a vase of water, and it

will be only ten ounces in weight. So lead is eleven times heavier than

water, or eleven ounces of lead occupy the same space as one ounce of

water.

[Illustration: Fig. 72.—Weighing metal in water.]

[The heavier a fluid is, or the greater its density, the greater will

be the weight it will support. Therefore we can ascertain the purity

or otherwise of certain liquids by using hydrometers, etc., which will

float higher or lower in different liquids, and being gauged at the

standard of purity, we can ascertain (for instance) how much water is

in the milk when supplied from the dairy.]

[Illustration: Fig. 73.—Hydrometer.]

But to return to SPECIFIC GRAVITY, which means the

“Comparative density of any substance relatively to water,” or as

Professor Huxley says, “The weight of a volume of any liquid or solid

in proportion to the weight of the same volume of water, at a known

temperature and pressure.”

Water, therefore, is taken as the unit; so anything whose equal

volume under the same circumstances is twice as heavy as the water,

is declared to have its specific gravity 2; if three-and-a-half times

it is 3·5, and so on. We append a few examples; so we see that things

which possess a higher specific gravity than water sink, which comes to

the same thing as saying they are heavier than water, and _vice versâ_.

To find the specific gravity of any solid body proceed as above, in the

experiment of the lead. By weighing the substance in and out of water

we find the weight of the water displaced; that is, the first weight

less the second. Divide the weight in air by the remainder, and we

shall find the specific gravity of the substance.

[Illustration: Fig. 74.—Over-shot wheel of mill.]

The following is a table of specific gravities of some very different

substances, taking water as the unit.

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

|Substance.| Specific ||Substance.| Specific ||Substance. | Specific |

| | Gravity. || | Gravity. || | Gravity. |

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

| Platinum | 21·5 || Iron | 7·79 || Water | 1·000 |

| Gold | 19·5 || Tin | 7·29 || Sea Water | 1·026 |

| Mercury | 13·59 || Granite | 2·62 || Rain Water | 1·001 |

| Lead | 11·45 || Oak Wood | 0·77 || Ice | ·916 |

| Silver | 10·50 || Cork | 0·24 || Ether | 0·723 |

| Copper | 8·96 || Milk | 1·032 || Alcohol | 0·793 |

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

But we have by no means exhausted the uses of water. Hydrodynamics,

which is the alternative term for hydraulics, includes the

consideration of many forms of water-wheels, most of which, as

mill-wheels, are under-shot, or over-shot accordingly as the water

passes horizontally over the floats, or acts beneath them. These wheels

are used in relation to the fall of water. If there is plenty of water

and a slight fall, the under-shot wheel is used. If there is a good

fall less water will suffice, as the weight and momentum of the falling

liquid upon the paddles will turn the wheel. Here is the Persian

water-wheel, used for irrigation (fig. 75). The Archimedian Screw,

called after its inventor, was one of the earliest modes of raising

water. It consists of a cylinder somewhat inclined, and a tube bent

like a screw within it. By turning the handle of the screw the water is

drawn up and flows out from the top.

[Illustration: Fig. 75.—Irrigation wheel in Egypt.]

The Water Ram is a machine used for raising water to a great height by

means of the momentum of falling water.

The Hydraulic Lift is familiar to us all, as it acts in our hotels, and

we need only mention these appliances here; full descriptions will be

found in Cyclopædias.

We have by no means exhausted the subject of Water in this chapter. Far

from it. But when we come to Chemistry and Physical Geography we shall

have more to tell, and our remarks as to the application of science to

Domestic Economy, in accordance with our plan, will also lead us up to

some of the uses of water. So for the present we will take our leave

of water in a liquid form, and meet it again under the application of

Heat, which subject will take us to Ice and Steam,—two very different

conditions of water.

FOOTNOTES:

[9] The curved surface of a column of liquid is termed a “meniscus,”

from the Greek word _meniskos_, meaning “a little lens.”

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