CHAPTER V

PUTTING RIVERS TO WORK

FLOWING water exerts a strange fascination upon mankind, even to the

present day. Tourists travel hundreds of miles to view the glorious

spectacle of a riotous tumbling cataract. Is it strange, then, that in

the olden times, when the world was peopled with gods and genii and

strange spirits, the ancients looked upon ceaselessly flowing rivers as

the symbol of life? It was most natural for them to covet the endless

power of a river and eventually, despite their superstitions, to try to

utilize some of its energy.

It may be that sailboats antedate the first water wheel, but it seems

much more probable that flowing water was the first inanimate power

harnessed by man. Windmills were certainly a later development. They

possessed the advantage that they could be located anywhere while the

water mill had of necessity to be built along the bank of a stream.

However, the power of the wind is so unreliable and fluctuates so

widely that it was little used, except in flat countries, where there

was little if any available water power.

Water power predominated until the steam engine was introduced, when

it had to give way to an even more reliable power and one which could

be located at any place to which fuel could be transported. Now,

however, we are going back to our first power, seeking it out in the

most inaccessible mountainous regions, because we have discovered the

means of taking the power it yields and transmitting it hundreds of

miles, over hills and plains to the point where we can put it to useful

service. Hydroelectric power has very aptly been termed “white coal.”

The first prime motor was the current wheel, that is, a wheel fitted

with paddles, which was journaled over a stream with the paddles

projecting into the water. This was a very inefficient machine; it

converted very little of the energy of a stream into useful mechanical

power. The idea of damming the stream and letting the waters flow

over the dam through a raceway upon a water wheel was a much later

development.

WATER WHEELS

Three types of water wheel which were in universal use before the

advent of the steam engine were the undershot wheel, the overshot

wheel, and the breast wheel (Figure 30). In the undershot wheel the

water stored back of a dam is let out near the bottom of the dam and

strikes the under side of the wheel, so that the top of the wheel turns

toward the dam. In the overshot wheel, the water flows over the wheel

striking the paddles or buckets on top and on the forward side, so that

the wheel turns forward. In the breast wheel, the water strikes the

paddles half way up the wheel on the rear side and drives the wheel in

the same direction as that of the undershot wheel.

When we speak of water power we are apt to think of the water as

actually furnishing the energy. As a matter of fact, it is not water

but gravity that drives the wheel, the water being merely the medium

that gravity acts upon. By having the water drop from a great height,

its velocity is greatly increased and the power it imparts to the wheel

is much higher. In mountainous regions it is easy to obtain a high head

of water and thus generate a great deal of power from a relatively

small stream. However, the ancient type of wheel with its paddles or

buckets has now practically passed out of existence, being superseded

by the Pelton wheel for high heads and the turbine for low heads of

water.

[Illustration: FIG. 30.--UNDERSHOT, OVERSHOT, AND BREAST WHEELS]

INVENTION OF THE PELTON WHEEL

[Illustration: FIG. 31.--SECTIONAL VIEW OF A PAIR OF PELTON WHEEL

BUCKETS SHOWING HOW THE WATER JET IS DIVIDED AND FOLLOWS THE CONTOUR OF

THE BUCKETS]

In California, a number of years ago, they made use of what was known

as the hurdy-gurdy wheel. This consisted of an ordinary wheel with

bucket-shaped paddles against which was directed a stream of water

at high velocity through a nozzle. There was a carpenter, named L.

A. Pelton, who used to make a business of building and repairing

such wheels and the flumes that carried the water to them. Although

uneducated, he was possessed of considerable native ingenuity and was a

very observant man. One day, when he was called in to repair a wheel,

he noticed that one of the buckets which had been misplaced received

the water from the nozzle without any splashing. The water struck the

edge of the bucket with practically no shock, whereas the other buckets

produced a great deal of splashing. Pelton had enough knowledge of

the principles of mechanics to realize that a splash means a waste of

energy, and that here was a bucket which, although out of plumb and

apparently defective, was really more efficient than any of the others

in the wheel. It occurred to him then that instead of having the jet of

water strike the middle of the buckets it ought to strike the edge, so

that all its power would be absorbed without any wasteful splashing. He

might have displaced the jet laterally so as to accomplish this result,

but he realized that that would have produced a considerable side

thrust on the wheel, which, of course, would have been objectionable,

and so he hit upon the plan of using double buckets and letting the

stream of water strike the pair of buckets along their dividing line.

(See Figure 31.) This would split the stream in two and let each half

strike the slanting face of the bucket, and follow the surface around

in the same way that it did on the single misplaced bucket, but the

reaction or side thrust on one bucket would be counteracted by that

on the other. This idea proved successful and out of it has grown

the Pelton wheel which is now universally used in all power plants

employing high heads of water.

A 4,000-FOOT HEAD OF WATER

A notable illustration of such a plant is the great installation at

Big Creek, Cal. Big Creek, despite its name, used to be a small stream

flowing down the mountains into a canyon. One would hardly suppose that

it was capable of yielding much power, but it had its source high up in

the Sierras and was fed mainly by melting snows. In the springtime, it

swelled to a good-sized torrent. By building three dams near the top of

the mountain, a lake was formed in which the water of the melting snow

was impounded, so that a steady stream of water could be supplied the

year round for power purposes. But even so, the stream hardly amounts

to very much if we consider only the quantity of water that passes

through it. The particular advantage of this installation is the fact

that in a distance of six miles from the dam the creek falls 4,000 feet.

An inhabitant of the Eastern States who is unused to mountain

heights may gain some conception of the meaning of this elevation by

gazing up to the pinnacle of the Woolworth Tower, which rises 795

feet above street level, then mentally multiplying its altitude by

five. Evidently even a small stream of water dropping from such an

elevation would develop an enormous amount of power. In fact, it was

considered inexpedient to use the entire fall at a single drop and so

it was divided into two stages. The water is carried through a tunnel

three-quarters of a mile long and then through a flow pipe along the

face of the mountain to a point where it may drop 2,000 feet to the

first power plant. After passing through this plant the water is

discharged into the creek and is then diverted into a second tunnel

four miles long and a series of steel conduits to a point from which it

may drop 2,000 feet more to the second power plant. In each power house

there are two electric generators, each fitted with a pair of Pelton

wheels. These wheels are a little less than eight feet in diameter and

each one develops 23,000 horsepower.

The water is directed into the buckets of the Pelton wheel in a stream

six inches in diameter, and it issues from the nozzle with a velocity

of 300 feet per second or about 210 miles per hour. A jet of water is

almost like a solid bar of wood. In fact, it is impossible to chop

through it with an ax. The water would swing the ax out of one’s hand

before it got part way through the jet. Traveling at such a high speed

the friction is so great that it would tear the skin off one’s hands,

if it did not actually tear the hand off the arm, and yet it strikes

the buckets of the wheels with no shock at all, for the first part of

the bucket it touches is nearly parallel to the jet, and as the water

sweeps around the curved face of the bucket it loses practically all of

its pressure and velocity and falls into the tail race. The electric

power generated by the two plants is stepped up to 150,000 volts and

sent out over transmission lines to points of service. The street cars

of Los Angeles are connected by a 240-mile electric harness to the

hydraulic horses of Big Creek.

Powerful as this stream is, a still higher head is used in Switzerland,

at Lake Fully, where there is a drop of over a mile in a distance of

2.8 miles. The water is carried by a short tunnel through the mountain,

and then makes a drop of over 5,000 feet to the power plant, where it

strikes the Pelton wheels at a velocity of 400 miles per hour, or about

seven times the speed of a fast express train.

HARNESSING THE MISSISSIPPI

In contrast to such high heads, we have the low-head power plants

which are employed where a large volume of water is available. The

most notable installation of this type, and the largest in the world,

is that at Keokuk, Iowa, where a dam has been thrown across the

Mississippi River. For many years it was thought impossible to make

any use of the vast volume of water that flows through this great

river. But above Keokuk there used to be a rapid extending back about

twelve miles. By building a dam across the river just below the rapid

it was possible to obtain a working head of about thirty-two feet, and

with the enormous volume of water available this provided sufficient

energy to make the development worth while. In marked contrast to

the installation at Big Creek, it is volume rather than velocity

that is employed, and hence turbines rather than Pelton wheels are

used. More water goes through a single turbine than is used in the

whole of the city of New York with all its elaborate aqueduct system.

Enormous turbines are used, fifteen feet in diameter, and when the

installation is complete there will be thirty units, each yielding

10,000 horsepower, or a total of 300,000 horsepower. A turbine, it may

be explained, differs from the ordinary water wheel in the fact that

the water runs through the wheel instead of around it (Figure 32). The

water may enter at the center and then flow out at the periphery, or

it may enter at the periphery and then be discharged from the center

of the wheel, or it may run axially through the wheel. In a Pelton

wheel there is a single jet which strikes but one pair of buckets at a

time, but in a turbine there are many jets distributed all around the

circumference of the wheel. The water is divided into a series of jets

by being forced through a stationary set of curved vanes. The blades of

the rotor or revolving part of the turbine are oppositely curved. If

the rotor were immovable the jets would have to change their direction

in passing through the rotor, but as the rotor is free to turn, the

jets react against these blades and set the wheel to revolving. The

turbine may be designed to run either on a horizontal axis or on a

vertical one.

[Illustration: FIG. 32.--TURBINE WHEELS; INFLOW TYPE SHOWN ON THE LEFT

AND OUTFLOW TYPE ON THE RIGHT]

The turbines used at the Keokuk plant are of the inflow type. The rotor

is mounted on a vertical shaft in a scroll-shaped concrete chamber,

something like a snail shell. Water pouring into this chamber is thus

given a swirling motion in the direction of rotation of the wheel. As

it flows into the wheel it passes first through a ring of fixed vanes,

which divide it into the jets.

The highest velocity of a wheel is naturally at the periphery and the

advantage of an inflowing turbine such as this is that the water is

traveling at its highest velocity when it strikes the periphery of the

rotor. As it loses its velocity it flows in toward the slower-moving

portions of the rotor. Finally it reaches the center, after giving up

practically all its energy, and falls into the tail pool through a

draft tube at the center of the rotor.

The scroll chambers at Keokuk are thirty-nine feet in diameter and the

draft tubes are eighteen feet in diameter. Water enters the scroll

chambers with a velocity of fourteen feet per second and comes out of

the draft tubes into the tail pool with its velocity cut down to but

four feet per second. Compare this with the velocity of the water jets

at Big Creek!

The current generated at Keokuk goes to St. Louis and surrounding towns

and serves a population of 1,120,000.

Now that we have learned how to transmit electrical power without

serious loss over enormous distances, it is only a question of time

before all the water power in the world is harnessed and put to the

service of man. The power costs nothing after once the plant has been

built; the only expense is that of maintaining the machinery and

keeping it in repair. It is estimated that there is some 200,000,000

horsepower available in this country, but this includes all flowing

water, much of which it would be impracticable, if not almost

impossible, to utilize. However, there is about 60,000,000 horsepower

commercially available, according to the figures of the U. S.

Geological Survey, of which we have developed so far only 6,000,000

horsepower.

The ancients used flowing streams not so much for power purposes as

to lift water to a higher level so that it would flow into their

irrigating ditches. Nowadays, electricity, steam, or air is used for

elevating water, but we have a very ingenious machine which makes

the stream lift a part of itself. This machine is very different in

principle from the old Egyptian noria. It depends upon the kinetic

energy of water in motion. You cannot push a nail into a piece of wood

with a hammer but you can easily drive it in by striking it with the

hammer. As the hammer is swung it acquires what we term kinetic energy

or energy of motion.

SETTING KITCHEN FAUCETS TO WORK

It is not generally realized that water in motion also acquires kinetic

energy. Whenever a faucet is turned off very quickly, there is a

hammering sound which is due to the fact that the moving water in the

water pipe is brought to an abrupt stop. This puts a severe strain on

the piping. A great deal of trouble was experienced from this source in

the early days of plumbing. At a hospital in Bristol, England, there

was a lead pipe leading from a cistern in one of the upper stories

to the kitchen. Every time the faucets were turned off abruptly the

momentum of the water caused the lead pipe to expand, and every now and

then the pipe was burst. In order to relieve the situation, a plumber

connected a pipe to the faucet and carried it up the side of the

building to the level of the cistern. His idea was that whenever the

water was turned off suddenly it would have a vent leading up to the

level of the water reservoir. Much to his surprise, the water issued

from the pipe in a jet of considerable height. To prevent the escape

of the water, he extended the pipe considerably, and still a jet of

water would issue from it. Eventually the relief pipe was carried up

twice the height of the cistern and even then the water would squirt

out occasionally when the faucets in the kitchen were turned off very

suddenly. Then the idea was conceived of placing a reservoir on one of

the upper floors of the hospital and letting the jet of water fill this

reservoir. Every time the faucet was operated in the kitchen a certain

amount of water flowed into the new cistern, and in this way it was

kept supplied with enough water to furnish that which was required for

the upper floors of the hospital.

[Illustration: FIG. 33.--SECTIONAL VIEW OF A WATER RAM]

It is on this principle that the hydraulic ram operates. Water from a

stream is made to flow down a pipe, and as it gains velocity a check

valve suddenly stops the flow which produces enough pressure to force

open a valve in an air chamber and let some of the water enter the

chamber. As soon as the pressure is relieved the check valve opens

and the valve into the chamber closes automatically until a moment

later the stream of water has gained sufficient velocity to repeat the

performance. Thus an intermittent jet of water is forced into the air

chamber and thence through a pipe to a reservoir. The height to which

the water will rise depends entirely upon the velocity of the water

flowing through the system. The air chamber is necessary to cushion

the action of the hydraulic ram and provide a fairly steady pressure

upon the water that flows up through the vent pipe. The check valve is

entirely automatic. It is held open against the pressure of the water

by a spring or a weight, but when the water is in motion is dragged

shut, only to spring open again when the pressure is reduced by the

escape of the water into the air chamber.

[Illustration: FIG. 34.--THE GYRATING WATER METER]

There is a very ingenious water-driven motor which is employed merely

to record the amount of water flowing through it. This is the Thomson

water meter which is illustrated in Figure 34. It consists of a

circular chamber with inwardly dished or conical top and bottom walls.

In the chamber is a flat disk with a ball and socket bearing. At one

side there is a vertical diaphragm in the chamber which passes through

a slot in the disk. This prevents the disk from revolving, but it

is free to oscillate. It has a motion similar to the gyrations of a

top when it is beginning to lose speed and die down, except that the

disk does not revolve. When the disk is in contact with the bottom

wall of the chamber on one side it contacts with the top wall on the

other so that the chamber is virtually divided into two compartments

by the disk, but by gyrating the disk these compartments are made to

revolve. Water enters at one side and discharges at the other side of

the vertical diaphragm. Now, if the disk is in the position shown in

Figure 34, the water, on entering, bears upon the upper face of the

inclined disk and wedges its way between the disk and the upper wall

of the chamber, making the disk oscillate on its ball center. As the

edge of the disk rises across the face of inlet port the water entering

the chamber bears against the under side of the disk, continuing the

gyratory motion. The water cut off on the upper side of the disk is

carried around to the outlet and discharges, while a fresh supply flows

in on the other side of the vertical partition and at the next half

turn the water in the lower compartment discharges at the outlet side

of the partition, while the compartment is filling on the other side of

the partition. A measured amount of water flows through the chamber at

each gyratory oscillation of the disk. A train of gearing is driven by

the gyrating disk which operates a set of dial pointers and a measure

of the amount of water passing through the meter is indicated.

DIGGING WITH WATER JETS

We have referred to the enormous velocity of the jets used to drive

Pelton wheels. Where high heads of water are obtainable water jets are

used very effectively for excavating purposes, particularly in mining

plants for washing down gold-bearing gravel banks. If water is not

found near such banks expensive canals, flumes, and pipe lines are

constructed and even tunnels are bored to bring the water to the point

where it can be utilized. Some of the giant nozzles spout streams from

2 to 8 inches in diameter with a pressure of from 50 to 200 pounds per

square inch. The powerful streams tear into the gravel banks, washing

them away into sluices in which riffle boxes are placed to catch the

precious metal. The back pressure of these nozzles is very heavy and

the larger ones have to be provided with strong anchorages. Water in

motion resists any change of direction and long levers have to be

provided to permit the miners to guide the nozzles.

The hydraulic jet is also used for general excavating wherever water

power is available. Sometimes it is employed under water when clearing

a channel to level down piles of stones that are too large to be picked

up by a suction dredge. Hollow iron piles are driven into a sandy

bottom by means of hydraulic jets. No hammer is needed. Water is pumped

into the pile and on issuing from the bottom of the pile it carries

sand with it, making a hole into which the pile sinks. Wooden piles

are driven in the same way by loosely attaching a water pipe to them

so that the pipe may be withdrawn when the pile has been driven far

enough. The pile is grooved at the lower end so that the pipe outlet

may be centered at the bottom of the pile.

COMPRESSING AIR WITH WATER

[Illustration: FIG. 35.--HOW THE VENA CONTRACTA RAISES WATER]

A very ingenious apparatus for compressing air was invented in the

earliest years of the iron age to furnish a continuous blast of air for

the Catalan forges. This compressor, known as a “trompe,” can hardly

be termed a machine because it contains no moving parts except water,

which is the motive power, and the air which it traps and compresses.

To understand its operation we must look into a peculiar property of

water flowing out of a reservoir into a pipe or nozzle. There is a

converging motion that tends to contract the jet of water just after it

leaves the pipe. This is known as the _vena contracta_. It produces

a partial vacuum in the pipe. If air ports are opened into the pipe

at this point, air will be sucked in to fill the vacuum and will be

carried out of the pipe by the friction of the water. In Figure 35 a

pipe is shown running from the _vena contracta_ to a water tank below.

The rise of water in this pipe indicates the degree of vacuum produced

by the jet.

[Illustration: FIG. 36.--THE “TROMPE” BY WHICH COMPRESSED AIR WAS

FURNISHED FOR CATALAN FORGES]

This principle is used in the hydraulic-air compressor or “trompe” as

it is called. Water flows out of one reservoir through a pipe into

another reservoir lower down. (See Figure 36.) Air enters the pipe

through ports at the point where the vein of water contracts and is

carried down into the second reservoir. This reservoir is sealed so

that the air is trapped in it. The water passes out through a pipe

which is carried high enough to keep a certain pressure of air in the

reservoir and prevent it from blowing out.

[Illustration: FIG. 37.--DIAGRAMMATIC SECTION OF A LARGE HYDRAULIC AIR

COMPRESSOR IN MICHIGAN]

There is a compressor of this type, constructed on an enormous scale,

in the northern part of Michigan. A sketch of the compressor is given

in Figure 37. The air reservoir in this case is a huge underground

rock-walled chamber nearly 350 feet below the surface, 8 feet wide, 26

feet high, and about 280 feet long. There are three intake pipes, 5

feet in diameter, each filled with an annular funnel-shaped head, which

sucks air into the water and carries it down into the chamber. At the

bottom of each intake pipe there is a concrete block with a conical

top projecting up into the pipe. The column of water flowing down the

pipe is spread out into an annular stream by the conical block and the

bubbles of air escape into the chamber. The water outlet of the chamber

is an inclined shaft which leads up about 270 feet to the surface of

the ground where it discharges into the tail race. The water is forced

up this inclined shaft by the pressure of the air trapped in the

chamber. The mouth of the shaft is, of course, below the level of the

water in the chamber so that there is no chance for the air to escape

unless the pressure becomes excessively high, when it will force the

water level below the mouth of the shaft and blow out. The discharge

sometimes forms a geyser 700 feet high. The air will continue to blow

until the pressure is reduced enough for the water level to rise and

cut off access of the air to the mouth of the shaft. Under normal

conditions there is a fall of 343 feet from the water level at the top

of the intake pipe to the water level in the chamber, and a vertical

rise of 271 feet from the water level in the chamber to the tail-water

level. The difference, or 72 feet, represents the working head. With

all three intakes operating, a total of 5,000 horsepower is developed.

Each intake delivers 11,930 cubic feet of air per minute at a pressure

of 128 pounds. Air enters the intake heads through tubes ⅜ inch in

diameter and there are 1,800 of them to each head. The air is employed

to operate machinery and tools in an adjacent mine.

One advantage of this type of air compressor is that it cools the air

while compressing it. This was hardly an advantage in the Catalan

forges, but when the air is used to drive machinery it is important

that it be precooled. When air is compressed by mechanical means

a great deal of heat is generated and the machines must be water

jacketed to extract this heat, but in the hydraulic compressor the

air bubbles are compressed as they pass down with the water to the

reservoir and the water absorbs the heat, delivering cool compressed

air at the bottom of the intake pipe.

Mechanics: The Science of Machinery · 第 5 / 22 章