CHAPTER III

_The Nature of Liquids_

THE difference between a gas and a liquid is that in the former the

atoms and molecules move to and fro in an independent existence,

whereas in the latter they are always in touch with one another though

they are changing partners continually. In the rivalry between motion

and attractive forces the motion is no longer in complete control: the

attractive forces have now sufficient power to keep the general body

of molecules in touch with one another, or at least so many of them

so that they form a definite volume of liquid, having a surface that

we can see. Yet the control of the attractive forces is not absolute:

there is a continual process which we call evaporation. Suppose a bowl

of water to be placed in an empty room. The molecules of the water are

all in movement--vibrating, turning, shifting, and changing partners

all the time. But their motion is not enough to make them break away

from one another, except at the surface, where the conditions are of a

special nature. In consequence the molecules hold together as a body

having a definite volume, and there are boundaries to that volume.

Only at the surface there are breakaways: in the constant interchange

of motion it will happen that some of the outlying molecules have

impulses given to them which are big enough to break their connection

with the molecules below, and they leave the surface for good. If this

had happened to molecules within the liquid, they would have been

recaptured. Thus the room in which the bowl of water has been placed

will contain a gradually increasing number of water molecules flying

about independently as a gas. If the room is closed, the increase will

not go on forever, because there will come a time when the number of

free water molecules in the room is so great that molecules strike the

surface of the water and re-enter it as fast as others leave it. The

room has become saturated with water vapor. That may happen before the

bowl is empty; but if the air in the room is continuously removed,

carrying the water vapor with it, the water in the bowl will all

evaporate in time.

The molecules that leave the surface will always be those that possess

more than the average amount of energy, part of which they spend in

tearing themselves away from their fellows; the average energy of the

main body will fall steadily as evaporation proceeds. In other words,

the water becomes colder and colder. We all know this effect well. If

we wave our hands when they are wet we feel the chill: we are, in fact,

using somewhat excessively a process which nature employs to cool our

bodies to the proper temperature. Our bodies are called on to make

good the excess of energy which the evaporating molecules have carried

away with them. The rate of chilling may be increased by the use of a

liquid which evaporates more rapidly than water; so, for example, the

surgeon at one time used an ether spray to cause local freezing. In

hot, dry countries drinking-water is cooled by putting it into a bag

made of porous canvas, which is hung so as to be shaded from the sun

but exposed to the wind, and the hotter and drier the wind the better.

[Illustration: Fig. 13.--The cryophorus.

The lower bulb, which is empty, is immersed in liquid air. The upper

bulb contains water which quickly freezes.]

In the hot Australian summer it is usual to see the bag hanging under

the veranda of the house or the roof of the railway station of a

country township. The water leaks through the canvas and is quickly

evaporated by the passing air, so that the water which is left grows

cool.

We can carry out the experiment in a very striking manner on the

lecture-room table. The two bulbs shown in the figure contain water

only, no air. The water is first brought to the upper bulb, and the

lower is then immersed in liquid air; in two or three minutes the water

is frozen, although the upper bulb has been nowhere near the liquid

air. The explanation is that the water molecules which fling themselves

from the surface of the water make their way down the tube and so to

the lower bulb. This would happen whether or no there were any liquid

air round the lower vessel; but then they would come back again, most

of them at least, and return to the water carrying their superabundant

energy with them. Thus the water would be very little cooled. If,

however, the lower bulb is reduced in temperature by the liquid air,

the molecules do not return. Their motion is taken away from them and

they collect first as water and then as ice in the lower bulb. The

water in the upper bulb is rapidly cooled, and soon frozen. The reason

for removing the air from the bulbs is that it is necessary to give the

water molecules a clear road, so that the evaporation may take place

quickly. If the operation were too slow, heat would leak in from the

outside air at such a rate that the freezing would not take place. The

presence of the air does not stop the energetic molecules from leaving

the surface, but it hampers their subsequent movements, reducing the

action to the process of diffusion which we have already considered.

When a liquid boils, the temperature has been raised to such a pitch

that the evaporating molecules are sufficient in number and speed to

lift off the air from the surface of the liquid and push it back _en

masse_. It is no longer the case that the individual molecules have

to thread their way through a crowd. The whole process is so strikingly

different in appearance from that of evaporation that the essential

similarity is apt to be overlooked. The temperature at which a liquid

boils depends on the pressure which the evaporating molecules have to

overcome: at the top of Mount Blanc boiling water is 27° F. cooler than

it is at the base.

The heat that is wanted if a liquid is to be evaporated is a measure

of the energy required to tear the molecules away from one another.

Perhaps that does not impress the mind with a sense of the importance

of these forces, which, though individually minute, are so powerful in

the gross. We may, however, remind ourselves of the heat required to

convert water into steam and of the amount of work that the steam can

do. The forces are manifested to us more directly in every hanging

drop of water or other liquid. The molecules are clinging to one

another like bees in a swarm. The links with which the molecules of the

last layer are attached to the surface from which the drop is hanging

are carrying the whole weight of the drop.

[Illustration: Fig. 14.]

Again the impression of the magnitude and importance of the forces is

not fairly conveyed by this simple effect; but the experiment can be

developed into a more impressive form.

Here is a bent glass tube containing water and no air. The water is

made to fill one limb entirely; if a little bubble of air is to be

found in it, it must be made to pass over into the other by holding

the tube in a suitable position and gently tapping it on the table.

When this has been done, the tube can be held so that the level of

the free end of the water column is far below the level of the other,

where it is clinging to the end of the glass tube. The weight of

the excess column on one side is all borne by the attachment of the

water molecules to the glass tube at the other side, and of other

water molecules to them. In fact, we have a drop of water about a foot

long. We cannot make a drop of this length hang from a finger, for the

reason that the water can break away by changing its shape. If that is

prevented, as it is in the glass tube, the magnitude of these molecular

forces is more obvious. When we try to stretch a bar of iron, the great

difficulty makes us realize the magnitude of the forces that keep the

molecules of solid iron together; we are apt to think that it is easy

to stretch a mass of water, but it is not so. It is easy to make the

water change its shape, but not to pull a layer of molecules directly

away from another with which it is in contact. Water is, in reality,

just as hard to stretch as to compress.

We may here make a little digression from our main line of argument,

because we come across a curious effect while we handle this bent tube.

If the tube is tilted so that the water runs along the tube and is

brought up sharply at one end, the sound of a blow is heard, as of two

hard substances striking each other; the blow is felt by the hand that

holds the tribe. The effect is sometimes described as an example of

water hammer; the explanation is simple enough. There is no air in the

tube, and the water strikes the end of the tube as if it were a rigid

body; and indeed it behaves as such because it is as incompressible. It

is necessary to be very careful in the handling of the tubes, because

it is so easy to knock out an end: it is just as if we struck a glass

vessel with a hammer. A very curious, and as it happens very serious,

example of this effect has manifested itself of recent years in the

wearing away of the propellers of ships that are driven by rapidly

turning screws. The illustration shows the erosion in a propeller blade

of the Mauretania (Plate IX a). The effect first appeared

when the adoption of the Parsons steam turbine increased the rate of

revolution of the screw and boats began to move faster, and it was at

first the cause of great loss, financial and otherwise. The explanation

was found in the fact that the steamship was advancing so fast and the

screws revolving so rapidly that the water could not fill up entirely

the holes that the blades left behind them.

[Illustration: PLATE IX.

A.

The right-hand figure shows erosion in a portion of an early propeller

blade of the “Mauretania.” Notice the small bite in the edge of the

blade shown in full in the left-hand figure.

B. Photograph of the cavitations formed by a propeller in the

experimental tank of the Parsons Marine Steam Turbine Co. The propeller

is the disc-shaped object at the left centre of the photograph. There

are three blades on it, and each is leaving a corkscrew line of bubbles

in the water which goes past the blade. We can see where the spirals

begin at the screw. (_Reproduced by courtesy of the Manganese Bronze

and Brass Co., Ltd._)]

The illustration shows the cavities as they are formed in a model tank

in the Turbinia Works at Newcastle (Plate IX b). They are

arranged in spirals; we can trace in the figure the spiral belonging to

each of the propeller blades.

[Illustration: Fig. 15.--Parsons’ water hammer.]

Now these cavities close up under the pressure of the surrounding

water, and since there is no air in them, the sides of the cavity

strike one another as hard and smartly, when they come together, as the

water in our tube could be made to strike the glass. If part of the

propeller blade forms part of a cavity wall, the blow may be so great

as to tear away pieces of the metal. It has cost much labor to arrive

at the full explanation and to provide a cure; propeller blades are now

made of an alloy specially designed to withstand erosion, and at the

same time the design of the blade has been improved. A very striking

experiment made in the course of these researches is illustrated in

Fig. 15. The strong metal vessel shown in the center of the figure is

filled with water and allowed to fall to the bottom of a tank, also

full of water, where its motion is suddenly stopped. The momentum of

the water in the cone aided by that of the heavy weight _W_ is

sufficient to make the water carry on its motion and leave a cavity

at the top of the cone at _V_. This fills up again immediately

afterward, on account of the pressure of the surrounding water, and as

it does so the water in the cone, increasing its velocity as it rushes

up into the narrowing space, strikes the top of the cavity so hard that

it punches a hole in the brass plate inserted at _P_.

The collapsing of the cavities formed by the screw makes quite a noise

in the water, so that a ship can be heard at great distances by the use

of an underwater receiver of sound.

Many of my readers will be familiar with a less serious example of the

blow that a mass of water can give because of its inelasticity: it

hurts considerably if one dives from any height and does not make a

proper entry into the water!

Since the molecules of a liquid all try to draw together under their

united attractions, they will bunch themselves together into a sphere

if they are allowed to do so, and this happens obviously when mercury

is dropped upon the table and breaks up into round drops which run

about as if they were round and hard.

[Illustration: DROPS OF MERCURY ON A TABLE

Fig. 16.

The small drops are almost perfect spheres. The large drops are

flattened out.]

Water will do the same thing if it does not wet the table: generally it

does wet the solid on which it rests, but we see many exceptions, as,

for example, when it is spilt on a dusty surface. What wetting means

and implies we have yet to consider: it is a very important part of

our subject. Gravitation also interferes with the tendency of a liquid

to gather into spheres. When the drops of mercury are very small they

look perfectly round, but larger masses are more like thick disks with

rounded edges. If we seek for good examples of the formation of spheres

by the general attraction of the molecules for one another, we must

contrive to avoid the influences both of wetting and of gravitation.

The small drops of mercury are a successful illustration. Another is to

be found in the manufacture of lead shot. The molten lead is allowed to

fall in a shower from the top of the shot tower, and gathers into round

drops as it falls, just as the rain does.

Perhaps it seems as if this were inconsistent with what has gone

before: gravitation has not been avoided and is indeed in full action,

yet the drops are formed. But the evil effect of gravitation is

indirect: it is the resistance to gravity which spoils the formation

of spheres. In the case of the large drops of mercury, the flattening

is due, not to gravitation directly, but to the upward pressure of the

table, which is resisting gravitation. When the drops of lead arrive at

the bottom of the tower they fall into water, which freezes them in the

shape they have acquired.

Here is an experiment to illustrate our point. The dark-looking liquid,

ortho-toluidine, does not mix with water, or, in other words, water

does not “wet” it, and its density is such that it floats conveniently

in a layer of pure water riding on a layer of salt water (Plate X

a). It is, even when spherical, supported at all points

by the surrounding water: it is not held up at one point only, as

a mercury drop would have to be were it a sphere resting on a hard

surface. In the circumstances of our experiment neither wetting nor

gravitation has any influence, and a large drop is formed, as we see:

it is perhaps a couple of inches in diameter. If it is pulled about by

a glass rod it sluggishly recovers itself; or, after wabbling heavily

through a variety of strange shapes, may break into smaller spheres.

When the rod is pressed gently against the sphere it makes a depression

or dimple on the surface; the toluidine’s effort to form a spherical

drop is for the moment interfered with, but it adapts itself as well as

possible to the circumstances. So also if we float some solid body--an

iron ball let us say--on the surface of mercury, a dimple is formed;

the surface of the mercury near the ball has the form shown in the

figure. If we look at the form of the mercury surface close to the wall

of the containing vessel, we see the same outline.

It is different when the liquid wets the wall of the vessel which holds

it or of the body which floats in it. If we put clean water into a

clean glass vessel, we see the water heaping itself against the side.

[Illustration: Fig. 17.--Iron ball floating on mercury (sectional

drawing)]

This is a more complicated effect than the other; evidently there are

attractive forces between the glass and the water. If a glass plate is

forced down into a dish full of mercury and made to touch the bottom

so that the mercury is squeezed out and none remains between the plate

and the bottom of the dish, it will stay where it is put, and indeed

great force is required to remove it. The explanation is simple and in

accordance with the principles which we have been considering.

[Illustration: Fig. 18.--Water heaped up against glass wall which it

wets.]

If the plate is to rise, the mercury must be made to get under it

again, otherwise the plate cannot rise far, because if there is not a

vacuum under the plate there is at most only a little air, which would

fall rapidly in pressure if the plate were raised.

[Illustration: PLATE X.

A. A large drop of liquid ortho-toluidine floating in water on a layer

of brine.

B. One bubble rests inside another, but as in Fig. 21 and for the same

reason the two do not coalesce.]

As the pressure on the top of the plate is more than that of the

atmosphere, the downward forces on the plate are greater than those

which try to lift it. At the edge of the plate the form of the mercury

surface is as shown in the figure: the mercury refuses to allow itself

to be drawn out into a thin sheet between the plate and the bottom of

the vessel.

[Illustration: Fig. 19.--Glass plate at bottom of dish containing

mercury. The plate is shown slightly lifted from the bottom, in order

to illustrate the refusal of the mercury to enter the vacuum so made.]

A drop of fluid which tries to draw itself together into a sphere

looks as if it were being held in an elastic bag. The atoms of mercury

in the surface are not quite in the same circumstances as those in

the interior, because they are exposed on one side, but it is only in

this sense that there is a surface film. We use the idea of a surface

film, nevertheless, finding it a convenient term; and we speak of its

tendency to contract and of its tension. Sometimes, however, there is

a real film on the surface which is different in composition from the

liquid of the interior, and then we find many strange and beautiful

consequences. The example most familiar to us is, no doubt, that of

the soap bubble. We put into the water a little soap, and at once we

find it easy to churn the soapy water into a pile of froth or blow it

out into bubbles. What has the soap to do with this effect? The answer

is to be found in the properties of the soap molecule. It is of very

curious shape, many times as long as it is broad; and it is made up

of a chain of carbon atoms fringed along its length with hydrogens,

and ending, at one end, in a little bunch of three hydrogen atoms,

at the other in a little group consisting of oxygen and sodium. The

former of these bunches is very self-contained: its attractions for

other atoms and molecules are small. But the latter is by no means so

unsociable: it is an active group tending to enter into association

with others, and especially it has a strong desire to join up with

molecules of water, for which reason the soap dissolves in the water.

Because, however, it is only one end of the chain which is very active

in this respect--the other end and the sides of the chain behave

differently--the soap molecules are apt to stay on the outer fringe

of the water if they come there in the course of their wanderings.

In this way a real film forms on the surface of the water, consisting

of soap molecules standing on end, so to speak, one end rooted in the

water, and the other exposed to the air. They are packed together side

by side like the corn in a field, or the pile on a piece of velvet.

They are not as free, however, as the hairs of the pile: they are

tied together side by side, because there is some force of attraction

between them when so laid alongside. We find that effect displayed

under other circumstances, as we shall see later. Thus they form a sort

of chain mail over the surface of the water--a real envelope. The sheet

can be stretched in the sense that if it has to be extended other long

molecules will come out of the body of the liquid and take their place

with the rest.

The soap bubble is a thin-walled sphere of solution bounded within

and without by the soap films; it holds together so well because the

films are there. It shrinks if the air within it is allowed to escape:

evidently the long molecules would gather together with the water

molecules as closely as possible. But there must be an outside, of

course, and where both kinds of molecules are present it is the long

chain molecules that form the outside layer. A very simple experiment

will illustrate still further the tendency to shrink. A wire ring is

dipped into some soap solution, and when lifted out carries a soap film

stretched across it.

[Illustration: Fig. 20.--A loop of very fine cotton is floated on the

soap film, and the part of the film inside the loop is touched with

a hot needle. Instantly the loop flies into a perfect circle. (By

courtesy of Prof. C. V. Boys.)]

In the film floats a ring of fine cotton shows. It is clear that which

was attached to the wire ring before the latter was put into the

solution. If the film inside the cotton loop is burst by touching it

with a hot needle, the loop flies instantly into the form of a perfect

circle, as the figure shows. It is clear that the whole film is under

tension and is trying to contract.

A very curious feature of the soap bubble is its reluctance to join up

with another bubble. If we blow a bubble on a ring (see Fig. 21), we

may take a second bubble and knock it against the first with force,

one would think, enough to break them. But the bubbles bounce from

one another like india-rubber balloons. Perhaps the explanation lies

in the fact that in both cases the outer layer consists of those ends

of the molecules which, as we saw before, have very little tendency to

associate with other molecules or parts of molecules.

[Illustration: Fig. 21.--Two bubbles in collision.

The two bubbles are pressing each other, and may be rubbed on each

other, but do not coalesce, because their liquids do not mix; it is

only the inactive ends of chain molecules that come into contact. (By

courtesy of Prof. C. V. Boys.)]

There is no tendency for the one bubble to coalesce with the other when

the two are pressed together, because the parts that come first into

contact do not attract each other.

[Illustration: Fig. 21A.]

This is very clearly seen in another of the wonderful experiments

of C. V. Boys.[4] A bubble is blown on a ring held in a stand (Fig.

21a).

A small ring carrying a tiny weight is attached to the under part of

the bubble as shown. A glass pipe is charged with solution and pushed

through the top of the bubble; when blown, a second bubble appears

within the first, and when it has attained a suitable size is released

by a skillful twist of the pipe. The inner bubble falls gently to rest

on the lower part of the outer, which it touches along a ring, not at

the bottom point. This is intentional, and was the purpose for which

the weight was attached to the outer bubble. The two do not tend to

coalesce, although in contact all along a line, no doubt because they

are presenting to each other surfaces composed of the inactive or

unsociable ends of the chains. If the outer bubble had not been pulled

out of shape, the inner and outer would have touched each other at

their lowest points. Now there is generally a drop of solution at the

lowest point of the inner bubble. When this comes into contact with the

outer, the bubbles generally coalesce. The drop of solution in some way

forms a bridge between the two. If the glass pipe be pushed through the

outer and made to touch the bottom point of the inner, and so drain it,

the weight hanging from the outer may be peeled off, and now the two

can touch each other at this lowest point without disaster (Plate X

b.)

The frothing of liquids is often caused by the presence of molecules

which have the same property of forming a skin over the surface. When

the foam gathers on a brook it is due to the presence of such molecules

as those of the various saponines, chain-like formations which are

found in many plants and trees. So also the foam that gathers on the

shore is believed to be due to the presence of similar molecules formed

in the seaweeds.

We have learned much about the form of these long-chain molecules

within recent years. In particular we are indebted to the late Lord

Rayleigh, to Devaux in France, to Langmuir in America, to Hardy and

to Adam in England for the examination of what happens when oils are

allowed to spread on water surfaces. We can repeat one or two of the

experiments in order to get an idea of the magnitude of the effects of

which we are speaking. We take a clean water surface, that is to say, a

surface free from any contamination by oil or grease. It is convenient

to attach a rubber tube to the tap and let the free end of the tube

lie at the bottom of a basin so that the water wells up and overflows

the edges, carrying away any dirt that has settled on its surface. We

now spread on the water a thin dusting of talc powder or anything else

that is convenient. Next we take a fine-drawn glass point or needle

and dip it into oil--olive oil will do--and then, after wiping nearly

all the oil off, dip the point of the slightly greasy needle into the

water surface. Instantly a circle is cleared round the needle (Plate

XI a). It appears that the long molecules range themselves

side by side on the surface as before; to the soap bubble they came

from within, now we apply them from without. Each molecule hastens to

root itself in the water by its active end, and stands upright, as if

it were a water plant rooted and growing in the water. In the end all

the molecules are successful, and a thin sheet, one molecule thick,

covers the surface of the water; its thickness is of the order of a

ten-millionth of an inch. By measuring the weight of the oil that has

been placed on the water—a difficult task, since it is so small—and the

area covered, it is possible to find a measure of the thickness of the

film.

[Illustration: PLATE XI.

A. Circles cleared by minute drops of oil.

B. The camphor boat.

A small piece of camphor is fastened at the stern of a very light

boat, and as it dissolves in the water the solution forms a him on the

surface. It is so eager to do so that it drives the boat away so as to

make room for itself If a little oil is put on the water and makes a

film all over it, the boat stops. If the oil partly covers the water,

the boat stops as soon as the ruler which is held by the operator in

the picture is pushed so far forward that the oil covers the surface

left to it.]

This is, in fact, the method that has been followed by the workers

mentioned. More recently it has been possible to apply a new method,

based on the use of X-rays, to the exact measurement of the same

quantity, and I hope to show you presently how this is done. On

the results of the earlier work it was possible to assert that the

thickness of the layer was such as would be expected if it were one

molecule thick; and the argument was greatly strengthened by the fact

that when different substances, known by chemists to be chain molecules

of different length, were placed upon the water, the thickness varied

with the length, as it ought to do.

If the drop of oil is small enough, and the dust is finely scattered,

the cleared spot is exactly circular. If we prick the water surface

somewhere else, another circle is formed. Each circle is totally

unaffected by the presence of others. This was relied on by Devaux to

show that the action of each drop was concerned only with the surface

round it over which the oil was spread: it was not a general effect on

the body of the liquid. It was just what one would expect if the drop

of oil had spread out until it was drawn down to a certain thickness

and could then spread no farther. By putting on a larger drop, we can

see that larger spaces are cleared. We may, for example, pour a few

drops into a large bath, and clear the whole surface. When the dust

layer on the surface of the water is broken up into little patches by

several applications of minute drops, in different places, and when

the surface is not covered all over with the oil film, we can observe

the quickness of the spreading by touching the surface with the oiled

needle at some little distance from a floating patch, and watching

how suddenly the patch is hurried away from the spot. The impulses

that are given in this way are the cause of the lively movements of

camphor fragments when they are dropped on the surface of the water,

an old experiment. As the camphor dissolves, the solution shoots

over the surface in a film, and the camphor itself recoils like a

gun when it is fired, or a rocket when the heated gases stream from

its tail. Sometimes the fragments dart to and fro and sometimes spin

round merrily. A tiny boat can be made to sail about on the water by

fastening a little piece of camphor on its stern in such a way as to

touch the water (Plate XI b). When a number of camphor boats

and pieces of camphor are all on the move, it is quaint to see how

suddenly it all goes dead when a little oil is poured on the water. The

oil film has covered the water in an instant, and the dissolved camphor

no longer spreads over the surface.

We have all heard of the stilling of the waves by pouring oil upon the

sea. We can watch the effect by making a series of waves run along the

long tank which Lord Rayleigh once used here for the same purpose; a

vacuum cleaner serves to provide the wind, and you see there is quite a

heavy storm on the water (Plate XII a, b). It is magically stilled if a

few drops of oil are allowed to fall in the center of the storm; after

a few moments the oil sheet is blown to the end of the tank and the

waves rise once more. We can repeat the experiment again and again. We

must suppose in this case that the wind has no “bite” on the water. The

latter is covered, as we know, with a film of oil, the top surface of

which is formed of the inactive ends of the long-chain molecules; and

it may well be that the molecules of the air when they strike it recoil

as from a smooth surface. A rough surface would be driven forward by

the impacts of the air molecules--rough, that is to say, in the sense

that the spaces between the exposed molecules are of the same size as

the molecules that strike. But if the surface of the oil film is very

smooth and has little tendency to hold on to any molecules that strike

it, the air cannot push it and make it rise in little waves which

afterward grow to great ones. So the oil stills the waves by stopping

the action of the wind, and the motion of the waves dies out in their

own friction.

We now come to the problem of the “wetting” of a surface. We know, for

example, that a clean glass surface is wetted by water, but not when it

is smeared with grease, even if the film is almost invisible. The water

molecules clearly refuse to associate with the molecules of the grease.

That is not surprising, perhaps, because we have seen that in some

cases at least the long molecules that make the fats and oils present

to the outside their inactive ends, which have very little attraction

for the water molecules. So water spilled on a greasy surface gathers

into drops, just as mercury when it is spilled on the table; the form

of the water is due to the general attraction of its molecules for one

another. An oiled needle can be gently laid on water without sinking

more than to make a depression in the surface, just as if there were

a skin on the water which gave slightly under the weight. Still more

striking, perhaps, is the floating of a greased wire sieve. (Fig. 22).

[Illustration: Fig. 22.--Greased sieve. (By courtesy of Prof. C. V.

Boys.)]

The sieve is dipped in melted paraffin wax, shaken so as to clear the

pores, and allowed to dry; it is well not to touch it with the fingers.

It will float readily and carry quite a lot of cargo, as Boys showed at

the Christmas lectures many years ago. Or it may be filled with water;

but the water must not be poured in roughly; it must be allowed to

flow in gently on to a piece of paper which can afterward be removed.

To show that the pores are quite open we can give the sieve a sharp

movement, when the water film gives way and the water falls in a heavy

shower on the floor.

When soda water is poured out into a clean, smooth tumbler, very few

bubbles come to the surface; but if the surface of the tumbler is at

all dirty or rough we may see streams of bubbles rising. There is a

beautiful old experiment which illustrates this effect, that of “the

grape and champagne.” We must use soda water instead of champagne. A

grape is not wetted by water, and so when it is put into the tumbler it

sinks to the bottom of the soda water, where it collects bubbles at a

great rate (Plate XII c). Soon it is covered over with a sheet

of bubbles that look like seed pearls, and these bring it by their

buoyancy to the surface. The grape is not much heavier than the water,

and does not require much to lift it. At the surface the grape parts

with some of its bubbles, which burst into the open air, and this goes

on until it sinks again, only to collect a few more bubbles and once

more be made buoyant. The process will repeat itself continually for

many minutes until the soda water is “dead.”

It is interesting to put in two glass beads instead of the grape. They

have been cleaned: washing with soap and water is efficient. No bubbles

form on them and they stay at the bottom.

[Illustration: PLATE XII.

A. Stormy water.

B. Oil stilling the storm.

C. Grape in soda water.

A and B. The blower raises a storm and the waves run along the tank.

A drop of oil stills the waves at once, and the water surface becomes

level. Notice the blank space in B. After a while, the oil is blown to

the end of the tank, and then the waves rise again. The photographs

have been retouched so as to bring out the reflection of the light by

the waves.

C. The grape and the greasy glass sinker are carried to the top by

bubbles; the clean glass sinker has no bubbles and stays at the

bottom.]

We take one of them out, rub it over with a greasy finger, and now it

behaves like the grape, collecting bubbles, rising, parting with some

of them, falling, and so on.

We must realize that when a bubble of carbonic-acid gas forms in the

soda water the particles of the gas have to collect and push back the

water all round. Now the water molecules are holding on to one another

tightly, and resist being torn asunder. For this reason we do not see

the bubbles forming in the middle of the water. At the edge, when the

glass is clean, the water wets the glass, or, in other words, the water

molecules are clinging to the glass even harder than they cling to one

another. Bubbles cannot under those circumstances form here, either,

for they would have to tear away the molecules from the glass. But it

is different if the surface is greasy and the molecules are not really

holding on to the glass--merely pressed against it by the pressure

of the rest of the water which is behind them. In that case the gas

bubbles find somewhere to grow, and quickly increase in size. It is

easier to push back the surrounding water when the bubbles have grown

somewhat. One of the most beautiful ways of showing that is by another

of Boys’ soap-bubble experiments. Two bubbles of different sizes are

blown on the two ends of the same tube; when they are allowed, through

the opening of a tap, to communicate with one another, the little bulb

blows out the big one and disappears. Of the mass of bubbles in the

soda water which lie side by side on the wall or the grape, the larger

ones tend to take up the smaller, and all of them to amalgamate.

The little streams of bubbles that we sometimes see rising from

definite points on the surface of the tumbler are due to some

irregularity in the glass--a tiny protuberance, perhaps--on which, if a

bubble tends to form, it already is past the earliest stages of small

diameters.

This tendency of bodies under water to collect bubbles and rise to the

surface has of recent years become the basis of a great metallurgical

industry. Various metal ores when crushed into powder form a mixture of

particles of rock material, such as quartz and various silicates, and

of metallic sulphides. It is found possible to treat the mixture so

as to cover the particles containing metal with a thin oil film, which

is not wetted by water, while at the same time the particles of rock

are still clean and the water wets them. The mass is then churned up

into a froth. All the metal-bearing particles are made buoyant by the

adherence of bubbles and rise to the top in a thick frothy scum; the

rest of the ore stays at the bottom of the vat, and the two parts are

easily separated.

There is one other experiment which will help to illustrate these

principles. We know that water heaps itself up against the side of a

clean glass vessel which contains it. The molecules cling to the glass,

and as it were climb up the wall on one another’s shoulders in their

eagerness to affix themselves thereto. If we dip two glass plates side

by side in the water, the water rises higher to the space between them

than it does outside. Those that are climbing one wall now help those

that are climbing the other. The effect is spoken of as being due to

“capillary action,” the name being given to it because it is so marked

in the case of a fine or “capillary” tube. The water in the fine bore

is lifted up to a great height, one inch in the case of a tube of

one-twentieth-inch diameter. If we float a small hollow glass ball on

the surface of the water, the water rises up the sides of the ball. If

two floating balls are made to approach each other, they will, when

within a short distance--perhaps half an inch--of each other, move

together, at the end quite violently.

[Illustration: Fig. 23.--Two hollow glass balls floating in mercury.

The pressure at _Q_ is less than the pressure at _R_ because it is at a

higher level in the water. The pressure at _R_ is the same as at _S_,

because _R_ and _S_ are on the same level. The pressure at _S_ is that

of the atmosphere, which is the same as the pressure at _P_. Hence the

pressure at _P_ is greater than the pressure at _Q_, and the one glass

ball is forced toward the other.]

We shall understand that if we consider the diagram in Fig. 23. Two

glass balls are floating in the water. The pressure at _Q_ is less

than the pressure at the level of the dotted line, because _Q_ is

at a higher level in the water. The pressure at the level of the dotted

line is the pressure of the atmosphere, because the line continues the

level of the water without. So the two pressures marked _P_, both

sensibly equal to the pressure of the atmosphere, overcome the two

pressures marked _Q_ and drive the balls together.

If we float on the water two balls made of paraffin, or two glass balls

coated with paraffin, the two attract each other as the clean glass

balls did, though the action is somewhat different.

[Illustration: Fig. 24.--Two greased glass balls floating on water.

The pressure at _P_ is greater than that of the atmosphere and

therefore than that of _Q_, and the balls are forced together.]

As the figure shows, the balls combine in making a dimple in the

water, and again if we study the forces acting on the balls we find

that the pressures are such as to force the balls together. But the

clean glass balls avoid the paraffin balls. This action is a little

more complicated, but it can be followed from the figure, which shows

the forces that are in action. When the vessel containing the water is

clean, and the water is heaped up against the side, the clean glass

balls are attracted to the side, just as they are attracted by each

other. On the other hand, the paraffin balls avoid the side of the

vessel. If now we carefully fill up the vessel with water until it

tends to brim over, so that the edge of the water no longer curls up

against the side, but curls down toward the edge of the vessel, the

clean balls leave for the middle and the paraffin balls come to the

side and stay there.

[Illustration: Fig. 25.

The left-hand ball is wetted by the water; the right hand ball is

greased and is not wetted. The pressure at _P_ is greater than

that at _Q_, and at _P_' greater than at _Q_'. Thus the

balls are forced apart.]

All these facts which we have been considering are illustrations of

the one principle on which the formation of a liquid depends, namely,

the strength of the attractions between the atoms and the molecules

which are strong enough to keep them in constant association with one

another, though they are not so strong as to bind them together into

a rigid, solid body. And it is important to remember that molecule

attaches itself to molecule at special points; one part of a molecule

may be able to exert a strong hold on a special part of another.

Presented differently to each other, there may be little or no tendency

for the two to join together.

Concerning the nature of things · 第 3 / 6 章