AËRONAUTICS.

Recent British papers and correspondents bring very pleasing accounts of

a balloon ascension, which took place in London on the 9th of October.

This adventure is the more interesting to us, from the fact that the

well-known and experienced aëronauts, Messrs. Coxwell and Glaisher, were

accompanied in their celestial excursion by several private individuals

of distinction, and among the rest by the Hon. Robert J. Walker, of this

country, whose able contributions have done so much to enhance the value

of THE CONTINENTAL. Some years ago, this gentleman had the

scientific curiosity to descend to the bottom of the sea, in a new

diving apparatus, just then invented; and recently he has been driven

through a tunnel on a railway, by the pneumatic process, which in

certain locations and conditions, will probably hereafter be substituted

for the ordinary power of the locomotive engine. He seems to be not only

ready to welcome all valuable improvements in science and mechanics, but

is ready himself to take the risks of dangerous exploration in the

pursuit of knowledge and for the promotion of progress.

But of all such adventures, that into the regions of the atmosphere is

by far the most interesting. Living immersed in this great ocean of air

and moisture which surrounds the earth, and is the theatre of all the

grand, beautiful, benignant, and often terrific phenomena of

meteorology, it is no more than a very natural curiosity which induces

us to seek by aërial exploration to understand its physical

peculiarities, and to make use of the vast resources which it will

doubtless soon afford to the genius and enterprise of the human race.

Until recently, we believe, it has been considered a settled fact, that

the atmosphere was limited to the height of about forty-five miles, that

being estimated as the limit at which the earth's attraction would be

balanced by the expansive force of the particles of air. But in this

problem there is an element of complication in the rotation of the

atmosphere with the earth on its axis. Near the surface, and for a great

distance upward, the air is but a part of the solid globe, or rather an

appendage to it, moving with it in all respects like the denser fluid

which constitutes the mighty ocean. But there must be a point in the

ascent upward, where the centrifugal force of the particles of air, in

the diurnal rotation, must over-balance the power of gravitation; and

from that limit, the motions of the atmosphere must be subject to a law

of a wholly different character--partaking of the nature of planetary

revolution, rather than of axial rotation. The latest speculations as to

the height of the atmosphere, seem to have reached only this degree of

certainty, viz., that it does not extend so far as the orbit of the

moon. Otherwise, it is argued, the superior attraction of that body, in

its immediate vicinity, would aggregate a considerable quantity of the

air about it, which would tend to retard the motions of the satellite in

its orbit, and of the earth on its axis; whereas, the revolutions and

rotations of both are known to have been uniform for a period as far

back as authentic observation extends.

But these speculations, however curious and interesting, are of no

practical importance. We shall never be able to traverse the air to any

great distance above the earth's surface. Independent of mechanical

difficulties, two great impediments will forever prevent the realization

of any such ambitions aspirations. These are the increase of cold and

decrease of pressure in the upper regions of the air, and the deficiency

of oxygen in the rarefied element for the support of animal life. It is

well known that at the earth's surface, the pressure on all parts of the

body, internal and external, by the weight of the superincumbent

atmosphere, is no less than 14½ pounds to every square inch. The

structure of the human body is physiologically conformed by nature to

this pressure, and it cannot survive with any very great change of this

amount, either by increase or diminution. When one descends into the

water, the pressure is doubled at about 32 feet of depth. In ascending

in the atmosphere, the pressure is diminished much less rapidly, of

course, but quite sensibly when the altitude becomes very great.

Messrs. Coxwell and Glaisher are said to have ascended in 1862 to a

height of seven and a half miles. One of these gentlemen became entirely

insensible from cold and want of oxygen, and the other very nearly so,

being obliged to open the valve of the balloon with his teeth for want

of the use of his hands.

Nature provides a partial remedy for the difficulty of breathing in the

upper regions of the atmosphere. In the effort to breathe, the lungs are

found to expand and to develop air cells not ordinarily used, so as to

bring a larger quantity of the rarefied air into contact with the blood.

It has been proposed to assist this effort of nature, and, in order to

enable the aëronaut to reach a greater altitude with safety, to carry up

in bags a supply of oxygen for breathing. As air is carried or forced

down into the water to enable the diver to breathe, so it may be

conveyed upward for the benefit of the aërial adventurer.

But with all possible expedients, it is not probable that man will ever

be able to get far away from the surface of the earth which is his

natural place of abode. If he can explore the lower strata immediately

adjoining his own theatre of action--the strata in which all the great

and important phenomena of meteorology take place--and if he can succeed

in traversing it at his pleasure with safety and some degree of

celerity, as we doubt not he will eventually, this great achievement

will subserve all the useful purposes possible to be derived from such

skill and knowledge.

The atmosphere will still be the vast reservoir of oxygen, nitrogen, and

carbon, from winch all living things in the air, on the earth, or in the

depths of the boundless ocean, whether animal or vegetable, draw far the

greater part of their nutriment. We can never reach the surface of this

atmospheric ocean, for that would be for us a region of inanity and

death; but there is scarcely a doubt that we shall freely use it in the

future for purposes of locomotion, at the same time that we breathe and

assimilate it as the very pabulum and substance of our mortal bodies.

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The Continental Monthly, Vol. 4, No. 6, December 1863 Devoted to Literature and National Policy · 第 42 / 80 题