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PNEUMATICS.

CHAPTER I.

that surface by means of the piston, it will be found that no pres- fig. 1.

Division of Bodies-Subject of Pneu sure which can be produced

matics.

(1.) MATERIAL SUBSTANCES, in refer ence to their mechanical properties, are divided into solids and fluids.

Wood, stone, metal in its ordinary state, are instances of solids. One of the most striking mechanical peculiarities of this class is that, if to such a body any force be applied, the whole mass will be moved without suffering any change in its figure or shape. Water, quicksilver, melted metal, air, steam, are instances of fluids. This class of bodies differ essentially in their mechanical properties from the former. That cohesion of parts which is the cause of the preservation of the figure of a solid, notwithstanding the application of a force tending to change the figure, has here no existence whatever. The parts of a fluid are perfectly free to move among each other, and immediately yield upon the application of the smallest force. Fluids easily allow solid bodies to pass through them, and their surfaces always compose themselves into a perfect level. On the other hand, the cohesion of the parts of solids do not permit the passage of another body through them unless extraordinary force be used, and their surfaces maintain any position with respect to a level or horizontal plane in which they may happen to be placed.

(2.) Fluids are divided into two very distinct classes, denominated, from their characteristic mechanical properties, elastic and inelastic.

If a strong cylindrical vessel, of which AB (fig. 1.) is a section, be filled to the height C with water, and a piston or plug D, accurately fitting the vessel, and capable of moving water-tight in it, be introduced over the surface of the water, and a pressure be exerted on

will force the surface of the water lower in the vessel than its original height C.

Now let us suppose the water discharged from the vessel A B, and its place occupied by common air. Let the piston, as before, be introduced into the cylinder, fitting it so that no air can escape between the piston and the cylinder. A pressure being now exerted on the piston it will immediately descend; but the moment the pressure is removed, it will again ascend, and resume its first position.

(3.) The property, in virtue of which the water resisted the descent of the piston and would not admit of a diminished bulk, is called incompressibility; and, on the other hand, the property by which the air admitted the descent of the piston and was forced into a less bulk, is called compressibility. Again, the property manifested by the air in forcing back the piston when the pressure was removed, and resuming its original bulk, is called elasticity.

It appears, therefore, that elasticity supposes compressibility, and a body which is incompressible must necessarily be also inelastic. Hence water is an inelastic, air an elastic fluid.

Strictly speaking, neither water, nor any other liquid which we know of, is perfectly incompressible or inelastic. It was long supposed that water possessed neither of these properties; but accurate experiments have shown, that it and other liquids are both compressible and elastic. A pressure of 15lbs. on each square inch of surface, reduces the bulk of water by one part in 21740. The degrees of compressibility, however, which

B

are found in liquids, are so inconsider able, that the quality of compressibility in these substances is rather to be looked upon as a philosophical fact, than as a property to be taken into account in mechanical investigations. Accordingly, in all mechanical treatises, liquids and aëriform bodies are considered to be distinguished as we have already explained; and when their properties are expressed mathematically, the formulæ for the one are founded on the supposition of their being inelastic, and for the other of their being elastic.

The same property of incompressibility which we have just explained in water, is common to all that class of fluids which are called liquids, such as mercury, alcohol, &c.; and the property of elasticity explained in the instance of air is common to all fluids of the gaseous or vaporous form, such as all the gases, steam raised by heat from all species of liquids, &c.

This manifest and important mechanical distinction between the two classes of fluids gives rise to a corresponding division in that part of mechanical philosophy which treats of their properties. That which treats of the mechanical properties of elastic fluids, and which forms the subject of the present treatise, is called Pneumatics, from the Greek word μ, (pneuma,) which signifies breath or air.

(4.) The various elastic fluids differ one from another in many respects. One of the most striking distinctions is, that some are permanently elastic, and others not. Those which are incapable by any known means of being converted into a liquid are called permanently elastic fluids. Such, for example, is air. On the other hand, those which, by being submitted to pressure or exposed to cold, are reduced to liquids, are not permanently elastic, and are generally called vapours. Such, for example, is steam. Besides this, there are many other distinctions between elastic fluids, arising out of their chemical properties. It will not, however, be necessary here to inquire into these, since the mechanical properties which we shall have to consider in the present treatise are common to all elastic fluids, whatever be their differences as to permanent elasticity or any other properties. The elastic fluid with which we are most familiar is atmospheric air, and it possesses all the mechanical properties which we shall have to notice in any elastic fluid. For

this and other reasons it will be convenient to adopt it as the representative of elastic fluids in general, and there will be no difficulty in applying to them the conclusions to which we may arrive.

CHAPTER II.

Air possesses the universa! Properties of Matter-Impenetrability, Inertia, Mobility, and Weight.

(5.) Air being apparently an invisible, intangible substance in which we freely move, it may at first be doubted whether it be matter or not. It should be observed, that the properties of substances, even those with which we are most habitually conversant, do not always offer themselves immediately to the observation of the senses, and that in noticing them our senses must often be guided by philosophical considerations. Not that these philosophical considerations add any thing to the certitude derived from the senses, but rather that they direct the senses to the proper objects of attention. Let us then consider how we should use the senses in deciding the question, whether air be material or not? We know that there are certain properties which any thing must have in order to be material, and that having these properties it is necessarily one of that class of beings which we denote by the term matter. Air, then, will be material or not, according as it is found to possess or not these requisite qualifications. The principal of these properties are, impenetrability, inertia, mobility, and weight.

(6.) Impenetrability is that property by which a body occupies any space to the exclusion of every other body, or so that no other body can fill that space until the other deserts it.

(7.) Air is impenetrable.

There are various experimental proofs of this proposition. Let A B (fig 2.) be a glass receiver, or cylindrical vessel, containing water to the level B, and let CD (fig. 3.) be a smaller vessel of the same kind empty, and having an aperture in the bottom furnished with a stopcock at F. Let a cork or other light body be placed floating on the surface of the water at G, and the stop-cock F being closed, let the vessel CD be inverted over the cork G, (as at fig 4.) and let its mouth D be pressed into the water to any convenient depth. It will

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be found that the water will not enter the inverted receiver, except to a very limited height as E, as will be made visible by the cork floating on the surface and seen through the glass. Thus the air in the receiver which occupies the space CE excludes the water. That this is the cause of its exclusion will be rendered apparent by opening the stopcock F, by which the air which hitherto prevented the ascent of the water be yond the level E will escape, and the water will immediately rise until it assumes the same level in both receivers. Again, if the piston described in (2.) be forced against the air confined in the cylinder, it will be found that no force whatever will compel it to reach the bottom; however strong the apparatus may be, it will burst or break before this can happen.

(8.) In both of these experiments it might seem that the air was partially penetrable, since in the former the water entered the cylinder to the height E, and in the latter, although the piston could not be forced to the bottom, yet it was found to approach it. These effects, however, were not produced by the penetration of the air contained in the respective vessels, but by its compression. The air in both cases yielded to the body, which entered the cylinder and contracted itself into a smaller space.

It would be very easy to multiply proofs of the existence of this property in air, but it is the less necessary, as additional proofs of it will be perceived in many of the experiments which we shall have to describe for other purposes. The same, indeed, may be said of all the other properties of air which we are about to establish, and such is ever the nature of principles established by philosophical investigation. They are continually reappearing and soliciting our notice when we are not seeking them, and we recognise fresh proofs of them an investigations apparently the most

remote from those in which they first originated.

The quality in air which we have called impenetrability, is sometimes called solidity, and air is said to be solid. There is, however, an objection to the use of this term in this sense. Solid has already been used in opposition to fluid, and air is of the latter class. The word solid would thus be used in two different senses, which should be avoided. We have, therefore, in the present instance, thought it better to express that universal property of all species of matter by which it refuses admission of other matter to the space it fills until it has deserted it, by the negative term impenetrability.

(9.) Air is inert and moveable.

The quality of inertia which is known as an universal property of matter, is that in virtue of which it requires a certain effort or force to produce motion in matter if it be at rest, and to destroy or modify any motion which it has if not at rest.

That air possesses inertia we have numerous and familiar proofs. Wind is nothing but air in motion. Any obstacle which opposes this motion sustains a considerable pressure, and must exert a proportionate resistance, otherwise it will be carried forward with the body of moving air. Such are the effects of wind on balloons and other bodies floating in the atmosphere. Also on ships and all bodies floating on water which present sufficient surfaces in opposition to the wind, such as sails. Nay, we find, notwithstanding the extreme thinness of the atmosphere which surrounds us, that it is capable of exerting very powerful degrees of force when it acquires sufficient velocity: witness the effects of hurricanes in agitating the waters of the ocean, in tearing up by the roots the largest trees, in overthrowing buildings, &c. These effects establish beyond question the

great force which is necessary to destroy or modify the motion of air.

If the atmosphere be quiescent and there be no wind, there is a resistance opposed by it to the passage of any body through it. This resistance is produced by the force exerted by the body so passing through it in displacing the air in its progress. When the motion is slow, and the surface of the body which faces the direction of the motion not very great in proportion to the whole body, this resistance is perhaps not sen sibly felt. But if the motion be accelerated or the surface much enlarged, it is instantly perceived. In walking at a moderate pace on a calm day we do not easily feel the resistance of the air, but if we increase our speed and run, we find the same effect as if a wind were blowing in our face; this effect increases in proportion to the speed, and is very obvious when riding or driving rapidly.

pressing the piston to the bottom of the cylinder, the air contained in the cylinder will be forced through the valve in the piston. Let us then suppose the piston in close contact with the bottom and sides of the cylinder, all air having been excluded: upon attempting to draw the piston up, it will be found that very considerable force will be necessary; and that when sufficient effort has been used, and the piston has been brought to the top of the cylinder, if it be disengaged from the agent which This drew it up, it will descend with great force and strike the bottom. effect plainly indicates the weight of the air pressing on the upper surface of the piston. This is what is vulgarly called suction; as if there were some force within the cylinder which drew the piston to the bottom. But within the cylinder is nothing but empty space, and it is plainly unreasonable to ascribe to empty space any mechanical influence. If a large fan or an open umbrella be: That it is the weight of the incumbent moved slowly against the calm air, the atmosphere pressing on the upper surresistance will be instantly felt, and a face of the piston which forces it to the considerable exertion will be necessary bottom of the cylinder, is still further proved by the fact, that if the upper to sustain the motion. surface of the piston be increased, the force which presses it down will be also increased, and what is more, will be increased in precisely the same proportion as the surface of the piston. In fact, it is found that when all air or other elastic fluid has been expelled from beneath the piston, there will be a pressure amounting to about fifteen pounds on every square inch of the upper surface of the piston; from which we may infer that a column of air, having a square inch for its base, and which extends from the surface of the earth to the top of the atmosphere, weighs about fifteen pounds*. The atmospheric engine is a machine whose efficacy depends on the principle which we have been just explaining. In this machine the weight of the atmosphere is used as a first mover in pressing a piston to the bottom of a cylindert.

(10.) Air has weight.

If our object be merely to establish the fact that air is heavy, the most direct method is to weigh it by the But if it be usual means, a balance. required to ascertain with great nicety its degree of weight or specific gravity, other less direct but more accurate means must be resorted to. In the present instance we shall be content with establishing the fact that air has weight.

There are some very obvious effects which plainly indicate this. It is shown in our treatise on Hydrostatics, that when a lighter body is placed in a fluid it asoends in it, and that if it so ascend. it must be lighter than the fluid in which it moves. Now there can be no doubt that a balloon has weight, and yet it ascends in the atmosphere. The atmosphere must then, bulk for bulk, be heavier than the balloon. Besides this, the clouds which we see floating in the atmosphere are generally composed of water, as is proved by their frequently falling in rain. They have therefore weight, but yet must be lighter than the atmosphere in which they are sus. pended.

If a piston move in a cylinder so as to be air-tight and be provided with a valve which opens upwards, upon

Its weight varies within narrow limits, as will appear hereafter. Fifteen pounds may be considered

an average in round numbers.

+In calculating the atmospheric pressure on any surface, it is necessary to determine the number of square inches in the surface. As it often happens that the surface thus to be measured is circular, it may be useful to have a short and easy rule, by which the number of square inches in a circle of a given diameter may be found. The following rule will be found to serve this purpose:

Let half the diameter of the circle expressed inches be found, and its square taken, and let this square be multiplied by the number 3.1415, and the

But there is a still more conclusive argument that it is the weight of the atmosphere which presses down the piston If, by a valve in the bottom of the cylinder, the air be admitted below the piston, it will no longer be pressed down, or rather it will be pressed both upwards and downwards by equal forces, and will be indifferent as to its ascent or descent, except so far as the weight of the piston itself will produce the effect. This is owing to a property of air, by which it presses equally in every direction, which we shall explain more fully hereafter. (13.)

The most direct proof, however, that air is a heavy substance is, that it can be directly weighed.

water, it follows that, bulk for bulk, water is about 840 times the weight of air.

(11.) Many effects with which we are familiar, and which often excite our curiosity, are accounted for by the gra vitation of the atmosphere. If the nozzle and the valve-hole of a pair of bellows be stopped, it will be found that a very considerable force will be necessary to separate the boards. This is owing to the air not being permitted to enter at the usual apertures, to resist the pressure of the atmosphere on the external surfaces of the boards. Shellfish which adhere to rocks, snails, and other animals, have a power by muscular exertion of expelling the air from between the surface of the rock and the surface which they apply to it, in conse quence of which they are pressed upon the rock by the atmosphere with a force of about fifteen pounds for every square inch in the surface of contact. The same cause enables flies and other animals to walk on a perpendicular plane of glass or on the lower surface of an horizontal plane, apparently suspended by their feet, and with their bodies downwards. This has lately been proved to arise from a power of expelling the air from between their feet and the surface on which they tread, so as to obtain a pressure from the atmosphere proportionate to the magnitude of the soles of their feet.

Let a phial be provided, containing not less than two quarts, and having a stop-cock screwed upon its neck. By means of the air-pump or exhausting syringe, which will be described hereafter, the air may be withdrawn from this vessel. When this has been done, and the stop-cock closed, let it be suspended from one arm of a very accurate balance, and an exact counterpoise placed in the opposite scale-pan. The empty phial is thus balanced. When the beam ceases to vibrate and becomes steady, open the stop-cock and admit the air into the phial. It will immediately preponderate, and it will be found that to restore the equilibrium a weight must be placed in the opposite pan, at the rate of about 523 grains for every cubic foot of air contained by the bottle. Since there are 1000 ounces in a cubic foot of of the Weight of the Atmosphere-The

product will be the number of square inches in the circle.

This rule will give the area of the circle to within one 10,000th part of the square of half its diameter. The following example will serve to show the appli

cation of this, rule. Let the diameter of the circle be 21 inches. The square of half this is 12x12=144. Hence the area will be found thus:

144

3.1415

720

144

576

144

432

452.3760

which expresses the number of square inches in the cirele to within one hundred and forty-four 10,000th of an inch.

The area may be found without decimals by the following rule: Let the diameter of the circle be squared, and its square divided by 14. If the quote be multiplied by 11, the product will be the area nearly. Thus, in the preceding example, the diameter is 24, the square of which is 576; this, divided by 14, gives 41, which, being multiplied by 11, gives 152 4.

CHAPTER III.

Barometer.

(12.) Having in the last chapter considered in a general way those properties which elastic fluids have in common with every species of matter, we shall now examine more particularly the weight of the atmosphere and the methods of measuring it. It will be neces. sary first, however, to mention a quality of all fluids, whether elastic or inelastic, to which we shall have occasion to allude.

(13.) One of the most striking properties by which fluids are distinguished from solids, and that indeed which has been adopted in mechanical science as the definition of a fluid, is the quality by which it is capable of transmitting pressure equally in every direction.

To explain this, let us suppose a vessel of any shape completely filled with a fluid and closed at every part, so that

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