HOW TUNNELS ARE BUILT.

These notes describe very generally the way in which tunnels are built

through mud and gravel under parts of the sea or large rivers in such

a way that the men who build them are protected and as safe as the

carpenter who is building a house.

The way these tunnels are built is called the “shield” way because

the machine used is called a shield. It is given this name because it

shields the tunnel builders from the water and the mud which are ready

at every moment to overwhelm them and kill them.

The shield was invented in 1818 by a great Engineer, Marc Isambard

Brunel, who was a Frenchman living in England. The idea of the shield

came to him as he saw how the sea worm which attacks the wooden piles

of docks along the shore bores the holes it makes in the wood. The head

of this worm is very hard and can bite its way through the hardest

woods. As it goes through the wood its body makes a hard shelly coating

which lines the holes which its head has made and prevents the hole

from getting filled up. This is the general idea of a tunnel built by a

shield.

The first shield was used by Mr. Brunel to make a tunnel across the

Thames River at London, England. This is still the biggest tunnel

ever built by a shield, although not the longest, and is still

used by railroad trains. This tunnel was begun in 1825 and was

finished in 1843, and provides a history of almost unexampled and

not-to-be-excelled courage in attacking difficulties and skill in

defeating them.

Since the days of Brunel many great improvements have been made in the

shield and in the way of working it but the same idea is still there.

[Illustration: HOW THE SHIELD IS PUSHED FORWARD

This shows the rear end or tail end of one of the smaller shields, used

on the Hudson and Manhattan Railroad tunnels under the North or Hudson

River at New York. It shows the skin, the hydraulic jacks within the

skin and the piping and valves for working them. It also shows the

doors leading to the front or “face.” The erector is not shown, but the

circular hole in the middle shows where it would be attached.]

[Illustration: This shows one side of an air lock bulkhead wall with

the air lock in place. The boiler-like appearance of the lock is

clearly visible, as well as the door and the pressure gauge to tell the

air pressure inside the lock.]

[Illustration: This is a rear view of one of the Pennsylvania Tunnel

shields, taken after a length of tunnel had been completed. All the

details of construction are shown, but in this case the erector is

clearly seen also. The valves which control the erector and the rams

which push the shield forward are seen near the top of the shield. The

rods across the tunnel are turn-buckles used to keep the iron lining

from getting out of shape in the soft mud. These are removed later. The

floor and tracks in the bottom are temporary and are used for bringing

materials to and from the shield.]

After the days of Brunel’s shield another great help was given to

tunnel builders by the invention of the use of compressed air to hold

back the water which saturates the ground in which the tunnel is being

built.

~WHO INVENTED THE COMPRESSED AIR METHOD~

The first real invention of compressed air for this purpose was made

by Admiral Sir Thomas Cochrane who, in 1830, took out a patent for the

use of compressed air to expel the water from the ground in shafts and

tunnels and, by this means, to convert the ground from a condition of

quicksand to one of firmness. This patent covers all the essential

features of compressed air working.

As suggested above, the thing which compressed air does in a tunnel

is to push the water out from all the spaces which it fills in the

ground, so that the men who are digging away the ground for the tunnel

are working in firm dry ground instead of a mixture of earth and water

which will run into and fill the hole they dig as soon as it is dug.

Whenever a tunnel is being built below a body of water through ground

which is porous, or in other words through any ground except solid

rock or dense clay, the water fills every crevice and space in the

ground and is exerting a pressure of about half a pound per square inch

above the ordinary pressure of the air, (which is 15 pounds to the

square inch) for every foot of depth below the surface of the water;

so that supposing the tunnel is 40 feet below the water the water has

a pressure of nearly 20 pounds per square inch on every square inch

of the surface of the tunnel. This pressure causes the water to flow

violently into any hole or opening that is made in the ground, and,

unless the water is prevented from moving by some means or other, the

opening made would be very quickly filled with water and also with

ground as the rush of water will carry the sand, gravel or mud with it.

By Cochrane’s invention the whole tunnel is filled with air under

a pressure equal to the pressure of the water. This compressed air

therefore balances the pressure of the water and holds it back from

moving, and if the pressure of the air is made slightly greater than

that of the water the water is driven back from the tunnels for a short

distance so that when the tunnel is being dug the ground instead of

being wet is quite dry.

This explains the principles of the shield and compressed air way of

making a tunnel.

The following describes very shortly how these principles are put to

actual use.

Most tunnels which are built by shield and compressed air under rivers

or arms of the sea are lined with cast iron plates to protect the

railway or roadway which is in the tunnel.

The tunnel is a circular tube, or shell, and the plates have flanges

on all sides which are bolted together. This shell is put into place,

plate by plate, by means of the shield which not only protects the

workmen and the work under construction, but which helps to build the

iron shell. In fact it corresponds to the sea worm which bores through

the wood and lines the hole with a shell. In the case of the tunnel

the shell is made of iron. The shield itself consists of a steel tube

or cylinder slightly bigger in diameter than the tube or tunnel it

is intended to build. The front edge of this shield is made up of a

ring of sharp edged castings which form what is called the “cutting

edge.” Just behind the cutting edge is a bulkhead or wall of steel, in

which are openings which may be opened or closed at will. Behind this

bulkhead are placed a number of hydraulic jacks or presses arranged

around the shield and within it, so that by thrusting against the last

erected ring of iron lining the whole shield is pushed forward. The

rear end of the shield is a continuation of the cylinder which forms

the front end, and this part, called the “tail,” always overlaps the

last few feet of the built up iron shell.

[Illustration: This is a photograph of a model of the Pennsylvania

Tunnels to New York City, made for the Jamestown Tercentenary

Exposition of 1907. It is given because it illustrates, as no

photograph of actual work could do, the relationship between the

shield, the tunnel itself and the air lock. This view shows the rear

part of the shield on the extreme left, with the erector picking up an

iron plate. It shows a man bringing a car with two of the iron plates

up to the shield. Behind this man comes the bulkhead wall with the

emergency air lock in the top and the ordinary air lock for passing

in and out at the bottom. It also shows the upper platform to the

emergency lock along which the men can get to the emergency lock in

case of an accident.]

[Illustration: This is another view of the same model, but showing the

front view of the shield. The doors on the air locks are clearly shown.]

[Illustration: This is a photograph taken in one of the Pennsylvania

tunnels under the Hudson River. It shows the soft mud, through which

the tunnel is being built, flowing in a thick stream through one of

the doors of the shield. The mud under the Hudson, where these tunnels

are, is so soft that often the shield was pushed through the mud with

all the doors shut, so that no mud came into the tunnel and no digging

had to be done, but the shield pushed its way bodily through the mud,

the rings of iron lining being built up behind as usual. Generally,

however, a certain amount of mud was brought in and had to be removed.

This photograph shows how it looked.]

~HOW THE SHIELD CUTS THROUGH THE GROUND~

The diagram, Fig. 1, shows more clearly what is meant. From an

inspection of Figure 1 it is clear that, when the openings in the

shield bulkhead are closed, the tunnel is protected from an inrush

of either water or earth; the openings in the bulkhead may be so

regulated that control is maintained over the material passed through.

After a ring of iron lining has been erected within the tail of the

shield, the shield doors are opened and men go through them and dig

out enough earth for the shield to go ahead. The rams are then thrust

out thus pushing the shield ahead. Another ring of iron is built up

within the tail for which purpose an hydraulic swinging arm, called the

“erector,” is mounted on the shield face. This erector picks up the

plates and puts them into position, one by one, while the men bolt them

together. Excavation is then carried on again and the whole round of

work repeated, gaining every time the jacks are rammed or thrust out

a length equal to the length of one ring of iron lining. In carrying

out this work in ground charged with water the shield is assisted by

introducing compressed air as described before. To use the compressed

air thick bulkhead walls of masonry are built across the tunnel behind

the shield and into the space between the shield and the bulkhead wall

air is pumped, compressed to the same pressure as that of the water in

the ground, or in other words the pressure of the air in pounds per

square inch is about half the number of feet the tunnel is below the

water surface. This dries the ground and simplifies enormously the

difficulty of working in it. The diagram, (Fig. 1) shows a bulkhead

wall across the tunnel. In order to pass from the ordinary air outside

the bulkhead into the compressed air inside it, all the men and the

materials have to pass through the “air locks” which are built into

the wall. They are called air locks because they are like the locks on

a canal which raise the water from a lower to a higher level or lower

it from a higher to a lower level as the case may be. The difference

is that an air lock enables one to pass from air at a low pressure to

one of a higher, or vice versa. An air lock is made like a large boiler

with a door at each end. If we wish to enter the compressed air we

enter the lock from the outside. The door at the end has been tightly

closed to prevent the compressed air from rushing out. We close the

door behind us and are now tightly shut in the boiler-like lock. We now

open a valve and compressed air begins to flow quickly into the air

lock and the air gets hotter and hotter, due to the compression of the

air. Very likely an intense pain begins to make itself felt in the ears

but by swallowing hard and blowing the nose it may be relieved. It is

caused by the air pressure being greater on the outside of the ear drum

than on the inside. If the delicate ear passages are choked, because

of a cold or some such reason, it is unsafe to go further or the ear

drum may burst. When the pressure in the air lock has reached that in

the working chamber, the door leading to the shield may be opened and

we can pass to the working space and note the work going on. There is

no especial bodily sensation to be felt except a slight exhilaration

and it is curious to find that one cannot whistle. On leaving the

compressed air we enter the air lock by the door we left; a valve is

turned and the air begins to escape and the pressure in the air lock

begins to go down. As it does so the air becomes colder and colder

and the whole lock is filled with a wet fog due to the chilling by

expansion of the air. The air has to be allowed to escape very slowly,

as bubbles of air and gas otherwise form in the blood vessels and

tissues of the body giving rise to the very painful complaint known to

tunnel builders as “the bends,” and in very serious cases to paralysis

and even death. The higher the air pressure the more slowly must one

come out into the ordinary air.

[Illustration: MAKING THE JOINTS WATER TIGHT

This shows the erector building up the iron lining in one of the

Pennsylvania tunnels at New York. It shows clearly how the iron plates

are bolted together to make the rings of iron lining.]

[Illustration: The last, or closing, plate of each iron ring is called

the “key,” and is much shorter than the others. This photograph shows

the shield erector on one of the Pennsylvania tunnels picking up and

putting into place a key plate. This picture gives an idea of the mud

and dirt and wet in which the men who work in tunnels have to do their

work.]

[Illustration: Wherever possible, every space and crevice outside the

iron lining is filled with cement forced, in a liquid state, through

the iron lining by compressed air. This photograph shows the operation

of “grouting,” as it is called. The man at the left is in control of

the grouting. He has the hose, through which the grout is forced,

screwed to a pipe which passes through a hole made for the purpose in

the iron lining plates and called a “grout hole.” The two men in the

middle of the picture are attending to the “grouting machine” by which

the work is done. Water and cement are fed into the small boiler-like

tank, the tank closed and compressed air admitted thus blowing the

liquid cement through the hose and behind the iron lining. When no

more grout can be forced behind the iron lining all the space has been

filled. The man on the right is the engineers’ inspector taking note of

how much grouting is done, and seeing that the work is properly carried

out.]

[Illustration: This shows the process by which the iron lining is made

perfectly water-tight, so that, when the compressed air is taken off,

no water at all can get into the tunnel. Two operations are shown here.

One is called “grommetting the bolts,” the other is called “caulking

the joints.” The two men on the left, hanging on to the wrench, are

tightening up the bolts as tight as they can after having put on,

underneath the washers at the head and nut of each bolt, a ring of

spun yarn dipped in red lead and oil or tar or some such water-proof

material. A few of these “grommets” may be seen at the feet of the

third man from the left. The other four men are caulking the joints

between the iron plates by driving into the joints a mixture of sal

ammoniac and iron borings. This sets as hard as iron and if properly

done makes a perfectly water-tight joint.]

[Illustration: THE REMARKABLE ACCURACY OF ENGINEERING

Usually when crossing, with a tunnel, a wide river or estuary the

tunnel is started from each shore and the shields are pushed through

the ground until they meet somewhere about the middle of the river.

This shows two of the Pennsylvania tunnel shields which have met far

below the Hudson River. The white arrow shows where each shield ends.

The platform of one shield on which the man stands corresponds exactly

with the platform of the other shield. As may be imagined, it takes

very careful and skillful engineering and surveying work, both before

the work is begun and while it is being carried out, to enable tunnel

shields to meet like this. This part of the art of tunnelling would

take an article to itself.]

When the shield has been pushed across the entire length of the water

way which has to be tunnelled, and the whole of the iron tube or shell

is in place, a thick lining of concrete is placed inside the iron shell

to protect it and make the tunnel stronger. As an added safeguard

wherever the tunnel is in rock, gravel, strong clay or other ground

which is not so soft that it does not close tightly in on the outside

of the tube, liquid cement is forced by compressed air through holes

made in the iron plates for this purpose. This liquid cement enters

every pore or crevice in the surrounding ground and when it has set

hard it still further protects the iron with a coating of cement.

Pieces have been cut out of the iron lining of a tunnel built under the

river Thames at London, England, in 1869, which showed that the iron

at all places was as good as the day it was first put in forty years

before, and iron put in the lining of the Hudson River Tunnel about

1878 when removed after thirty years was in perfect condition.

[Illustration: SHIELD AT END OF JOURNEY

Sometimes, however, shields are not driven to meet one another, but end

their journey at some shaft or in some other tunnel previously built,

after having gone through thousands of feet of all kinds of ground,

from the hardest rock, which had to be blasted out foot by foot before

the shield could advance, through hard pan, gravel, boulders, piles,

rip-rap, made ground and mud so soft that it flows like melted butter.

Naturally, after an experience like this a shield does not look as

spick and span as when it started in life. This photograph shows one

of the shields of the Hudson and Manhattan Railroad in New York just

reaching the end of its journey, battered and bent but still in the

ring.]

[Illustration: This shows a piece of curved tunnel near Morton Street,

on the Hudson and Manhattan Railroad, and is given because of the clear

showing it gives of the iron lining. The track and floor are only the

temporary roads for use during construction.]

[Illustration: Sometimes it is necessary to make borings of the ground

below the tunnels. In some of these bore holes vast quantities of water

are found at a much higher pressure than the tunnel compressed air.

This picture shows a spouting bore hole in one of the Pennsylvania

tunnels during construction.]

[Illustration: The last thing to do before laying the track is to put

the concrete inside the iron lining. This picture shows this work going

on and the wooden forms or ribs for holding up the concrete while it is

setting.]

[Illustration: THE LAND END OF A GREAT TUNNEL UNDER THE HUDSON

This view is given to show how complicated an underground structure

may have to be made to take care of the requirements of traffic. This

view shows the three great reinforced concrete caissons sunk through

the earth at Jersey City in order to contain the switches and crossings

required to form the New Jersey connections of the uptown and downtown

tunnels of the Hudson and Manhattan Railroad.

These caissons were sunk under air pressure by excavating below them

just as though they were tunnels turned up on end. In sinking these

caissons the material passed through was water-logged made ground, and

the hulls of two sunken canal boats were encountered and had to be cut

into pieces small enough to be taken out through the locks.

The usual passenger rushing at high speed in the trains between Jersey

City and Newark and New York has little idea of the very complicated

structure necessary to allow of his doing so.

The information in this article was supplied by Jacobs & Davies, Inc.,

Consulting Engineers, 30 Church Street, New York, the Engineers for the

Pennsylvania Railroad, Hudson River Tunnels, the Hudson and Manhattan

Railroad, and many other tunnels in various parts of the world.

The illustrations were kindly supplied by the Pennsylvania Railroad and

the Hudson and Manhattan Railroad.]

~DANGERS OF TUNNEL BUILDING~

This account of tunnelling by shield and compressed air is very

short and gives no more than a bare statement of the principles and

chief methods of such work. Nothing has been said of the engineering

difficulties involved in the design of such work, nor of the delicate

surveying work necessary if one should hope to start two shields a

mile or two apart and have them meet as shown in Fig. 13 like two

great glass tumblers placed rim to rim after having travelled through

thousands of feet of every kind of ground. Nothing has been said of the

men who work on this most arduous form of subterranean navigation, how

they cheerfully face the dark and the water ever threatening above them

and the unseen but not less deadly ally, and yet foe, the compressed

air, with its dreaded result, the bends, or the men on the surface

who keep the air compressors running without pause or stop day in and

day out until the work is done so that their comrades below may work

in safety. Nothing has been said of the curious accidents that are

liable to occur as when the air pressure in the tunnel gets too high,

overbalances the water pressure and blows a hole through the river-bed

and forms a geyser in the river above. It gives no account of the

special difficulties which arise when special conditions are found;

for example, when the lower part of the tunnel is in rock and the

upper part is in soft material. In fact it is nothing more than a bare

outline but it hoped that some, who may not be clear in their minds as

to how tunnels are built, may learn some of the first principles of

this most romantic kind of work from this bald narrative.

Why Do My Teeth Chatter?

Your teeth chatter because when you are cold in a way that makes your

teeth chatter the little muscles which close the jaw act in a series of

quick little contractions which pull the jaw up, and then let it fall

by its own weight. This is repeated many times and, as the action is

quick, the chattering occurs. It is a peculiar thing that this occurs

in spite of the will or brain, when, as a matter of fact, these muscles

which operate the jaws are especially under the control of the brain.

The chattering is really a spasm caused by the cold, and all spasms act

independent of the will. Cold seems to act on the jaw muscles a good

deal like some poisons which cause spasms.

Where Did All the Water in the Oceans Come From?

No, it did not come from the rivers which empty themselves into the

oceans, because the oceans were there before the rivers existed. Part

of it comes from the rivers now, but only a little in comparison to all

the water there is in the ocean. I will try to tell you simply how all

the water got into the ocean.

There was a time when there was no water on the earth at all. That was

when the earth was red hot, just as it is to-day on the inside, and at

that time all the water we have to-day was up in the air in the form of

gases. Strange as it may seem to you, if you take two gases, one called

hydrogen and the other oxygen, and mix them the right way, they will

turn into water, and if you had the right kind of chemical apparatus

you could take water and turn it into these gases again. When, then,

the earth was still all red hot, all of our water was up in the air in

the form of these two gases. Then, later on, when the amount of heat on

the earth was just right to make these gases mix together, the water

came down out of the air in great quantities, and there was so much of

it that it completely covered the whole earth and no land was visible.

Later on, for various reasons, mountains were thrown up on the earth’s

surface by great earthquakes, and every time a mountain or a high place

was formed there had to be a hole or low place some place else, and the

water ran into these low places and stayed there, and that uncovered

more of the land, because there wasn’t enough water to fill all the

holes and cover the land too, and that is what makes our continents

and islands and all of the land we see. There is now about three times

as much earth covered with water as there is land. Of course, the sun

is always picking up water through what is called evaporation, which

means that it is taken into the air in the form of gases. Later it

comes down again in the form of rain and falls into the oceans or on

the land, where it sinks in, finally finding a stream or river, and

sooner or later gets back into the ocean again.

Why Don’t the Water in the Ocean Sink In?

This is due to the fact that there is a kind of substance at the

bottom of the ocean which the water cannot penetrate, in spite of the

tremendous pressure which the great body of deep water exerts. In all

places where the bottom of the ocean has a covering which water can

sink into it does so, but there are such a few places where this is

possible, by comparison, that the amount that gets out that way is not

noticeable. This water, if it can keep on going, will eventually reach

the inside of the earth, where it is red hot, and is turned into steam.

Where Does the Water in the Ocean Go at Low Tide?

To get to the answer of this you must know something about the tides.

The tide is caused by the pull of the moon on the waters in the ocean.

The moon revolves about the earth once each day and has the ability to

draw up the waters in the ocean toward it, as we have seen in our study

of the tides.

Now, when it is high tide in one place it is low tide in another. The

moon does not make more water, but only pulls it toward it from side to

side. When it is low tide where we are the water has simply moved as a

body toward the place where it is high tide.

The tides act a good deal like a see-saw, except that they move from

side to side instead of up and down. When one end of the see-saw goes

up the other end goes down, and when the “down” end comes up the other

end goes down. So the answer to your question really is that at low

tide the water which made it high tide a few hours before has gone to

some place where it is at that moment high tide.

Why Does the Ocean Look Blue at Times and at Other Times Green?

Sometimes when we look at the ocean from the pavilion or while on the

sand of our favorite bathing beach the water in the ocean looks very

beautifully blue, and on other days will look dark green from the same

point. Why is it? If you will stop to think that at night when there is

no moon or other light the water in the ocean looks black, I think you

will soon be on the right track to answer the question yourself.

When the sky is blue--the kind of blue we like to see in the sky when

we are at the beach--the water in the ocean is blue, because the sea

reflects the color of the sky, and when the sky is overcast and gray

the color reflected by the sea will be gray also.

But, say you, sometimes the water in the ocean is dark green, and yet

the sky is never green. Quite true, and I will try to tell you what

produces the green color. This happens sometimes where the water is

shallow, either near the shore or out further where there is a sandbar

or other shallow place. Sometimes at such points the sunlight strikes

the water at such an angle that the rays go clear to the bottom and are

reflected from that point--the bottom--to our eyes. In such a case the

light will be changed through a combination of the color of the bottom

at that point and the color of the sky itself at the time to make the

color green as it is reflected to our eyes from the bottom.

Why Does Water Run?

Water runs because it has not enough of anything in it to make it stick

together.

In school language we call this sticking-together-thing “cohesion.”

The principle of cohesion makes all the difference there is, so to

speak, between solids, liquids and gases. A brick, a stone, a stick

of wood, or a piece of iron and all other solid substances have a

certain amount of this property of cohesion, and the particles stick

together, enabling us to build buildings and other things which become

permanent structures. These solid substances are either naturally

cohesive or else man, as in the case of the brick, has brought together

certain things with little or no cohesion and made them stick together

permanently. In the case of the brick, he takes a quantity of clay,

which is cohesive only to a certain degree, bakes it in an oven and

it becomes hard enough--more cohesive--so that he can pile one on top

of the other and make a building. Then he puts sand, mixed with other

things--lime and water--between the bricks to hold the bricks together,

and makes a structure that will last. Two bricks have no natural

cohesion for each other and, therefore, they can only be held together

by something that has cohesion within itself and also for the bricks.

The lime, sand and water make mortar which is cohesive when properly

mixed, while in themselves neither lime nor sand have much cohesive

property, and water has none at all.

Liquids have little or no cohesion. Water has none, or very little.

Syrup has a good deal more, but will run over the edge of a piece of

bread and butter if you are not careful.

Gases have no cohesive properties at all and, therefore, fly all over

the place, through any opening they can find, either at the top of the

room or under the crack of the door. They are always trying to get to

some place else and will keep moving as long as not confined. Gases can

move in any direction.

Liquids, however, while they are inclined to be constantly on the move,

can only go in one direction--down hill, and they go down fast or slow

if there is a chance, in proportion to the amount of stick-together

properties they have. Liquids can never go up of their own accord,

excepting in the process of evaporation, and then only when changed

into gases. A lake of water will dry up completely by evaporation

unless fed by streams of water constantly flowing in, because

evaporation is constantly taking place wherever water is exposed to the

air.

What Makes the Water Boil?

What we call boiling in the water we see when water is put over a hot

fire long enough to make it boil, is the changing of the water from

what we generally regard it--a liquid--into gases. Water consists of

two gases--hydrogen and oxygen--in fact, two parts of hydrogen gas and

one part of oxygen gas when mixed will always make pure water. Now,

then, if liquid water is heated to a certain point or temperature it

turns into the two gases, oxygen and hydrogen, and comes to the top of

the water, which still remains in liquid form, in the form of a bubble

and explodes into the air--not a very loud explosion, but still an

explosion. The process of turning liquid water into gases is a gradual

one, and that is why the water does not all turn into one large bubble

at once and explode away. If you keep the fire going long enough, all

the water in the vessel will explode away into the air, a few bubbles

at a time. If you hold a cold plate over the vessel as the bubble

explodes you can catch some of these gases in the form of bubbles on

the under side of the plate, which are again liquid water. When the

water becomes hot enough it turns into bubbles and as bubbles rise

that is what makes the boiling you see. When the same gases then come

together again in a certain proportion under proper temperature they

turn into liquid water.

At What Point of Heat Does Water Boil?

The boiling point of water is the temperature at which it begins to

pass into the form of gases. This varies in different altitudes. At

the sea level the boiling point is at 212° Fahrenheit. On the top of

mountains, for instance, water would boil at a much lower temperature.

It would be possible to go high enough in a balloon so that the water

would fly from the pan in the form of gas without making the water hot.

Also, a mile below the level of the sea it would take many more degrees

of heat to make the water boil. It is said that high up in a balloon

you could not boil an egg hard in a pan of boiling water if you kept it

in the boiling water for an hour or more, whereas we know that an egg

will be hard-boiled if we keep it in boiling water down where we live

for more than five minutes.

The degree of heat at which water passes away into the form of gases

is regulated by the pressure of the air on the water and other things

about us. At the average level in the United States where people

live the pressure of the air on everything is fifteen pounds to the

square inch, and at this pressure water boils only after it reaches a

temperature of 212° Fahrenheit. As we go up the mountains the pressure

becomes less and less as we go up. At the top of Mount Blanc, which is

15,781 feet high, water boils at 185° Fahrenheit. If we took a balloon

from the top of the mountain we would come to a height where there was

no air pressure at all.

What Do We Mean by Fahrenheit?

The name Fahrenheit is used to distinguish the kind of scale most

commonly used on thermometers in Great Britain and the United States.

Gabriel Daniel Fahrenheit, a native of Dantzic, made the first

thermometer on which this scale was used, and it is named after him. In

this scale for thermometers the space between the freezing point and

the boiling point is divided into 180 degrees--the point for freezing

being marked 32 degrees and the boiling point 212 degrees.

Why Can’t We Swim as Easily in Fresh Water as in Salt Water?

Our bodies are heavier than fresh water, i. e., a bulk of fresh water

equal to the size of our body would weigh less than our body, so that

the first tendency is to sink to the bottom if we find ourselves in

fresh water. If man had not learned to swim that is what he would

always do, sink to the bottom; but having learned how to keep from

sinking, he is able to swim in fresh water. However, we find that an

amount of salt water equal to the bulk of a man in size is heavier than

an equal amount of fresh water, although such a bulk of ordinary salt

sea water will still weigh less than the man. A man will sink in salt

water also if he has not learned to swim or float, but he can keep up

with less effort in salt water, and also swim in it more easily. In

a nutshell, then, the answer to this question is that salt water is

heavier than fresh water. You can make salt water so full of salt that

it becomes heavier than a man. Great Salt Lake in Utah is so salty that

one cannot sink in it for this reason. You could drown yourself in it,

of course, by keeping your head under water, but whether in shallow

water or deep water you would not sink in Great Salt Lake.

Why Do We Say Some Water Is Hard and Other Water Soft?

What we call hard water contains certain salts which soft water does

not contain. This salt in hard water is lime or some other salts which

the water has picked up out of the ground as it passed through either

coming up or going down. On the other hand, we can guess after having

been told this much that if we can find any water that has not passed

through the ground, and, therefore, not had a chance to pick up any

salts, we will have soft water. From that point it is easy to guess,

then, that rain water must be soft water, and so it is. The water in

the cisterns, which is rain water, is soft water, and the kind we get

out of the wells is hard water.

We do not like to wash either our faces or our clothes in hard water,

especially when it is necessary to use soap, because when we use soap

with hard water the soap undergoes chemical change which prevents its

dissolving in the water. Therefore, you cannot easily do a good job

of washing in hard water. On the other hand it is easy to dissolve

the soap in pure rain water or soft water and that is the kind we,

therefore, prefer for washing.

How Does Water Put a Fire Out?

This is at first a puzzling question, because back in your mind is the

thought that since hydrogen and oxygen are necessary to make a fire

burn, it seems strange that water, which is composed of oxygen and

hydrogen, will also put it out.

A burning fire throws off heat, but if too much of the heat is taken

from the fire suddenly the temperature of the fire is sent down so far

below the point at which the oxygen of the air will combine with it

that the fire cannot burn. We speak commonly as though water thrown on

a fire drowns it. That is practically what happens. Scientifically what

happens is that the water thrown upon the fire absorbs so much of the

heat to itself that the temperature of the fire is reduced below the

point where oxygen will combine with the carbon in the burning material

and the fire goes out.

To answer the unasked part of your question at the same time I will

say that hydrogen and oxygen when combined as water will put the fire

out rather than make it burn, more because when these gases take the

form of water they are already once burned, and you know that anything,

substance or gas, which has already been burned cannot be burned again.

It required great heat to make oxygen and hydrogen combine and form

water, and it also takes great heat to separate them again. So they are

really burned once before they become water.

Where Does the Rain Go?

Eventually almost all of the rain that falls runs into the rivers

and lakes and later finds its way into the ocean, where it is again

taken up into the air by the sun’s rays. But many other things happen

to parts of the rain which do not find their way into the ocean. In

the paved street, of course, where the water cannot sink in, it flows

into the gutter and thence into the sewer and on down to the river or

wherever it is that the sewers are emptied. You see, it depends very

much on what the earth’s surface is covered with at the place where

the rain falls. When it strikes where there is vegetation a great deal

of it stays in the soil at a depth of comparatively few feet. If it is

soil where trees and other plants grow a great deal of it is sucked up

from the ground by this vegetation and given back into the air through

the leaves and flowers. Some of the rain keeps sinking on down into the

earth until it strikes some substance like rock or clay, through which

it cannot sink, and then it follows along this until it finds something

it can get through and collects in a pool and forms an underground

lake, and may cause a spring to flow. Then there are also worms and

other forms of animal life in the earth which use up some of the water.

But it all gets back into the air eventually to come down some time

again in the form of rain.

Why Does Rain Make the Air Fresh?

The main answer to this question must be that the rain in coming down

through the air drives the dust and other impurities which are in the

air before it, and so cleans the air and makes it absolutely clean.

In addition to this it is now stated that since very often rain is

produced by electrical changes in the air, and that these electrical

changes produce a gas called ozone, which has a delightfully fresh

smell, it is this ozone that makes us say the air has become fresh.

The air above our cities is almost constantly filled with smoke,

containing various poisonous gases, and these are driven away by the

falling rain.

Then, too, there is always a greater or less accumulation of dirt,

garbage and other things in the cities which give off offensive smells

constantly, but which we do not notice always because we become used to

them. When the rain comes down it washes the streets and destroys these

smells, and that makes the air fresh and delightful to take into the

lungs.

In the country the air is more nearly pure all the time, because the

things which spoil the air in the city are not present.

Is a Train Harder to Stop Than to Start?

The answer is yes. It is harder to stop a train than to start it, or

rather it takes more power. The speed of a train depends upon the

motive power. When a train is stopped and you wish to start it, you

must apply enough motive power to start it going. There must be enough

power to move the weight of the train and overcome the friction of the

wheels on the track. It is, of course, easier to move a thing that

weighs less than a heavier one. If you throw a ball ten feet into the

air, it will perhaps not sting your hand when you catch it on its

return; but, if you throw it one hundred feet into the air, it will

sting your hands when you catch it. Besides, it will come down faster

the last ten feet of the way than the ball which you threw only ten

feet into the air. This is because when movement is applied to anything

you add power to it. The ball which comes down from one hundred feet

in the air acquires more power in falling and it takes more power to

stop it. A train in motion has not only the power of the weight of the

train behind it, but also the additional weight which the movement of

the train has given it. Therefore, it takes more power to stop it than

to start it. To stop a train you must apply the same amount of power as

is in the moving train because the power to stop any moving thing must

always be at least as great as the power which is moving it.

What Makes the Knots In Boards?

We find knots in the boards which we notice in a lumber pile or in any

other place where boards happen to be, because the smaller limbs which

grow away from the larger limbs of trees grow from the inside as well

as the outside of the tree.

When you see a knot in a board it means that before the tree was cut

down and the log sawed up into boards, a limb was growing out from the

inside of the tree at the spot where the knot occurs.

You will also find that the wood in the knot is harder generally than

the rest of the board. This is because more strength is required at the

base of a limb and in the part of the limb which grew inside the tree

than in other parts, for the limb must be strong enough to support not

only the limb itself, but also the smaller limbs which grow out of it.

How Many Stars Are There?

Man may never know how many stars there are. The best we can do is

to figure on the number that can be seen with the largest telescopes

which have been invented, for, of course, you know there must be many

millions of them which to us are invisible. We have counted the stars

so far as we can see them; or, rather, so far as we can photograph

them. Astronomers have found that a photographic plate exposed to the

stars will show more of them than can be seen by the naked eye. This

is because the materials on a photographic plate are more sensitive

to the light of the stars than the human eye. By this method man has

been able in a way to count the stars he can see. It adds up to more

than a hundred million of them. Astronomers found this out by taking

photographs of the heavens at night, devoting one picture to each

section, until the entire heavens had been covered, and then counting

them.

[Illustration: WHERE PAINT COMES FROM

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