CHAPTER XXIX

SOME RECENT APPLICATIONS OF ELECTRICITY--AN ELECTRIC PIPE LOCATOR

One of the great advantages of living in a town is the abundant supply

of gas and water. These necessary substances are conveyed to us along

underground pipes, and a large town has miles upon miles of such pipes,

extending in all directions and forming a most complex network. Gas

and water companies keep a record of these pipes, with the object of

finding any pipe quickly when the necessity arises; but in spite of

such records pipes are often lost, especially where the whole face of

the neighbourhood has changed since the pipes were laid. The finding

of a lost pipe by digging is a very troublesome process, and even when

the pipe is known to be close at hand, it is quite surprising how

many attempts are frequently necessary before it can be located, and

its course traced. As may be imagined, this is an expensive business,

and often it has been found cheaper to lay a new length of pipe than

to find the old one. There is now an electrical method by which

pipe locating is made comparatively simple, and unless it is very

exceptionally deep down, a pipe never need be abandoned on account of

difficulty in tracing it.

The mechanism of an electric pipe locator is not at all complicated,

consisting only of an induction coil with battery, and a telephone

receiver connected to a coil of a large number of turns of thin copper

wire. If a certain section of a pipe is lost, and has to be located,

operations are commenced from some fitting known to be connected with

it, and from some other fitting which may or may not be connected with

the pipe, but which is believed to be so connected. The induction coil

is set working, and its secondary terminals are connected one to each

of these fittings. If the second fitting is connected with the pipe,

then the whole length of the pipe between these two points is traversed

by the high-frequency current. The searcher, wearing the head telephone

receiver, with the coil hanging down from it so as to be close to the

ground, walks to and fro over the ground beneath which the pipe must

lie. When he approaches the pipe the current passing through the latter

induces a similar current in the suspended coil, and this produces

a sort of buzzing or humming sound in the telephone. The nearer he

approaches to the pipe the louder is the humming, and it reaches its

maximum when he is standing directly over the pipe. In this way the

whole course of the pipe can be traced without any digging, even when

the pipe is 15 or 20 feet down. The absence of any sounds in the

receiver indicates that the second fitting is not on the required pipe

line, and other fittings have to be tried until one on this line is

found.

AN ELECTRIC ICEBERG DETECTOR

Amongst the many dangers to which ships crossing the Atlantic are

exposed is that of collision with icebergs. These are large masses of

ice which have become detached from the mighty ice-fields of the north,

and which travel slowly and majestically southwards, growing smaller

and smaller as they pass into warmer seas. Icebergs give no warning

of their coming, and in foggy weather, which is very prevalent in the

regions where they are encountered, they are extremely difficult to

see until they are at dangerously close quarters.

Attempts have been made to detect the proximity of icebergs by noting

the variations in the temperature of the water. We naturally should

expect the temperature of the water to become lower as we approach a

large berg, and this is usually the case. On the other hand, it has

been found that in many instances the temperature near an iceberg is

quite as high as, and sometimes higher than the average temperature of

the ocean. For this reason the temperature test, taken by itself, is

not at all reliable. A much more certain test is that of the salinity

or saltness of the water. Icebergs are formed from fresh water, and

as they gradually melt during their southward journey the fresh water

mixes with the sea water. Consequently the water around an iceberg is

less salt than the water of the open ocean. The saltness of water may

be determined by taking its specific gravity, or by various chemical

processes; but while these tests are quite satisfactory when performed

under laboratory conditions, they cannot be carried out at sea with

any approach to accuracy. There is however an electrical test which

can be applied accurately and continuously. The electrical conducting

power of water varies greatly with the proportion of salt present. If

the conductivity of normal Atlantic water be taken as 1000, then the

conductivity of Thames water is 8, and that of distilled water about

1/22. The difference in conductivity between normal ocean water and

water in the vicinity of an iceberg is therefore very great.

[Illustration:

_By permission of_] [_Dr. Myer Coplans._

FIG. 43.--Diagram of Heat-compensated Salinometer.]

The apparatus for detecting differences in salinity by measuring the

conductivity of the water is called a “salinometer,” and its most

perfect form, known as the heat-compensated conductivity salinometer,

is due to Dr. Myer Coplans. Fig. 43 shows a diagram of this interesting

piece of apparatus, which is most ingeniously devised. Two insulated

electrodes of copper, with platinum points, are suspended in a U-tube

through which the sea water passes continuously, as indicated in

the diagram. A steady current is passed through the column of water

between the two platinum points, and the conductivity of this column

is measured continuously by very accurate instruments. Variations in

the conductivity, indicating corresponding variations in the saltness

of the water, are thus shown immediately; but before these indications

can be relied upon the instrument must be compensated for temperature,

because the conductivity of the water increases with a rise, and

decreases with a fall in temperature. This compensation is effected by

the compound bars of brass and steel shown in the vessel at the right

of the figure. These bars are connected with the wheel and disc from

which the electrodes are suspended. When the temperature of the water

rises, the bars contract, and exert a pull upon the wheel and disc, so

that the electrodes are raised slightly in the U-tube. This increases

the length of the column of water between the platinum points, and so

increases the resistance, or, what amounts to the same thing, lowers

the conductivity, in exact proportion to the rise in temperature.

Similarly, a fall in temperature lowers the electrodes, and decreases

the resistance by shortening the column of water. In this way the

conductivity of the water remains constant so far as temperature is

concerned, and it varies only with the saltness of the water. Under

ordinary conditions a considerable decrease in the salinity of the

water indicates the existence of ice in the near neighbourhood, but the

geographical position of the ship has to be taken into account. Rivers

such as the St. Lawrence pour vast quantities of fresh water into the

ocean, and the resulting decrease in the saltness of the water within a

considerable radius of the mouth of the river must be allowed for.

A “FLYING TRAIN”

Considerable interest was aroused last year by a model of a railway

working upon a very remarkable system. This was the invention of

Mr. Emile Bachelet, and the model was brought to London from the

United States. The main principle upon which the system is based is

interesting. About 1884, Professor Elihu Thompson, a famous American

scientist, made the discovery that a plate of copper could be attracted

or repelled by an electro-magnet. The effects took place at the moment

when the magnetism was varied by suddenly switching the current on or

off; the copper being repelled when the current was switched on, and

attracted when it was switched off. Copper is a non-magnetic substance,

and the attraction and repulsion are not ordinary magnetic effects,

but are due to currents induced in the copper plate at the instant

of producing or destroying the magnetism. The plate is attracted or

repelled according to whether these induced currents flow in the same

direction as, or in the opposite direction to, the current in the

magnet coil. Brass and aluminium plates act in the same way as the

copper plate, and the effects are produced equally well by exciting

the magnet with alternating current, which, by changing its direction,

changes the magnetism also. Of the two effects, the repulsion is much

the stronger, especially if the variations in the magnetism take place

very rapidly; and if a powerful and rapidly alternating current is

used, the plate is repelled so strongly that it remains supported in

mid-air above the magnet.

This repulsive effect is utilized in the Bachelet system (Plate XV.).

There are no rails in the ordinary sense, and the track is made up

of a continuous series of electro-magnets. The car, which is shaped

something like a cigar, has a floor of aluminium, and contains an iron

cylinder, and it runs above the line of magnets. Along each side of

the track is a channel guide rail, and underneath the car at each end

are fixed two brushes with guide pieces, which run in the guide rails.

Above the car is a third guide rail, and two brushes with guide pieces

fixed on the top of the car, one at each end, run in this overhead

rail. These guide rails keep the car in position, and also act as

conductors for the current. The repulsive action of the electro-magnets

upon the aluminium floor raises the car clear of the track, and keeps

it suspended; and while remaining in this mid-air position it is

driven, or rather pulled forward, by powerful solenoids, which are

supplied with continuous current. We have referred previously to the

way in which a solenoid draws into it a core of iron. When the car

enters a solenoid, the latter exerts a pulling influence upon the iron

cylinder inside the car, and so the car is given a forward movement.

This is sufficient to carry it along to the next solenoid, which gives

it another pull, and so the car is drawn forward from one solenoid to

another to the end of the line. The model referred to has only a short

track of about 30 feet, with one solenoid at each end; but its working

shows that the pulling power of the solenoids is sufficient to propel

the car.

[Illustration: PLATE XV.

_Photo by_ _Record Press._

BACHELET “FLYING TRAIN” AND ITS INVENTOR.]

To avoid the necessity of keeping the whole of the electro-magnets

energized all the time, these are arranged in sections, which are

energized separately. By means of the lower set of brushes working

in the track guides, each of these sections has alternating current

supplied to it as the car approaches, and switched off from it when

the car has passed. The brushes working in the overhead guide supply

continuous current to each solenoid as the car enters it, and switch

off the current when the car has passed through. The speed at which the

model car travels is quite extraordinary, and the inventor believes

that in actual practice speeds of more than 300 miles an hour are

attainable on his system.

Electricity · 第 29 / 31 章