Though nitrogen gas is, by itself, so noxious to animals, it answers an important end when mixed with oxygen gas in atmospheric air. Were it not for this large quantity of nitrogen in the atmosphere, the blood would flow with too great rapidity through the vessels, and all animals would have too great spirits; the consequence of which would be, that the life of man would not be protracted to the length that it now is. “If the proportions of oxygen and nitrogen were reversed in the atmospheric air, says Dr. Lambe, the air taken in by respiration would be more stimulant, the circulation would become accelerated, and all the secretions would be increased: but the tone of the vessels, thus stimulated to increased action, would be destroyed by over-excitement; and, if the supply from the stomach were not equal to the consumption, the body must inevitably waste and decay.” Hence the wisdom of God is remarkably displayed in the constitution of the atmospheric air! See Parke’s Chemical Catechism, chap. ii.
59
— “Mr. Cavendish,” says Dr. O. Gregory, “is the first who endeavored to establish that the proportions of the two principal elements of the atmospheric air were constant. The observations since made by M. de Mairy in Spain, M. Berthollet, in Egypt and in France; Mr. Davy, in England; and by Dr. Beddoes on the air brought from the coast of Guinea, seem to have confirmed this grand result. But one of the finest experiments made on this subject is that of Gay Lussac, in France, who, having been elevated alone in a balloon to the height of 6,900 metres, the greatest ever attained by any person, brought some atmospheric air from these regions. This air, being analysed at his return, comparatively with that on the surface of the earth, gave the same principles in the same proportions; a proof that the chemical constitution of the atmosphere at these great heights, is the same as at the surface of the earth. This result has been since confirmed by the experiments made by Messrs. Humboldt and Gay Lussac on eudiometry. The air of the surface of the earth, analysed at different days, at various hours and temperatures, presented no change in its composition: it always contained 0.21 of oxygen in volume, 0.783 of azote, 0.003 of hydrogen, and 0.004 of carbonic acid. Biot and Arrago have also lately verified this grand result. The atmospheric air, analysed in places the most distant from each other, in deep valleys, on high mountains, on banks of lakes, and in the glaciers of Chamouny, always presented to them the same composition.” Haüy’s Natural Philosophy, Note, vol. i. p. 218.
60
— Sturm’s Reflections, vol. iv. p. 49.
61
— “Galileo, to whom was reserved the glory of preparing, long before, the way for the theory of Newton, by the discovery of the law to which the acceleration of heavy bodies is subjected, having let fall from a great height different balls of gold, of lead, of copper, or porphyry, with a ball of wax, observed that all these bodies employed nearly the same time in falling to the earth. The ball of wax, the only one that was sensibly retarded, was no more than four inches from the earth at the end of the fall of the other bodies. Galileo, considering that this difference was very far from being proportional to that of the weights, concluded that it depended solely on the resistance of the air. This conjecture has been since verified by direct experiments, consisting in letting fall from the top of a tube, within which the vacuum has been made the most perfect possible, bodies of different materials, such as lead, iron, wood, cork, feathers, wool, &c., and it has been found that none of these bodies will then permit of our perceiving any sensible difference in the duration of their fall. As to bodies which raise themselves in air, such as smoke, it is known that their ascension is occasioned by the circumstance of their being specifically lighter than air: they are with respect to this fluid, situated as a piece of cork is with respect to water, which when immersed in that water to a certain depth, and then left to itself, rises again to the surface. The vulgar regard all as being without gravity which rises instead of falling: whence Newton remarked that the weight of the vulgar was the excess of the absolute weight of a body above the weight of the air. The ascent of air-balloons in the midst of the air is well calculated to undeceive the partisans of this theory of bodies without heaviness.” Haüy’s Natural Philosophy, vol. i. p. 48.
62
— To Otto Guericke, a burgo-master of Magdeburgh, we are indebted for the invention of the pneumatic machine, or air-pump.
63
— The atmosphere presses equally on the whole surface of the water in the well, until the rod of the pump is moved; but, by forcing the rod down, the bucket compresses the air in the lower part of the pump tree, which being elastic, forces its way out of the tree through the valve; so that when the bucket is again raised, that part of the pump tree under the bucket is void of air; and the weight of the atmosphere, pressing on the body of water in the well, forces up a column of water to supply its place; the next stroke of the pump rod causes another column of water to rise; and as long as the bucket fits the pump tree close enough to produce a vacuum, a constant stream of water may be drawn from below. Parkes’s Chemical Catechism, pp. 47, 418.
64
— As the earth’s surface contains, observes Mr. Ferguson, in round numbers, 200,000,000 square miles, must contain no less than 5,575,680,000,000,000 square feet; which being multiplied by 2,160, the numbers of pounds on each square foot, amounts to 12,043,468,800,000,000,000 pounds, for the weight of the whole atmosphere. Mr. Coates computed that the weight of the air which pressed upon the whole surface of the earth, is equal to that of a globe of lead sixty miles in diameter.
The following simple experiments within the reach of every one’s observation, show clearly the weight or gravitating power of the air. Let any one lay his hand on the top of a long perpendicular pipe, such as a pump filled to the brim with water, which is at first prevented from running out by the valve below: then let the valve be opened, so that the water may descend, and he will find his hand so hard pressed to the top of the pipe that he cannot draw it away. The prop is now gone; he has no pressure under his hand; a column of air, 45 miles high forces it down by its weight; and he must let in the air under it before the hand can be withdrawn.—If we shut the nozzle and valve-hole of a pair of bellows after having squeezed the air out of them, we shall find that a very great force, even some hundred pounds, is necessary for separating the boards; they being kept together by the pressure of the air which surrounds them.—If any one will apply the open end of a syringe to his hand, and then draw up the piston, he will find his hand sucked into the syringe with great force, and it will give pain, and the soft part of the hand will swell into it, being pressed in by the neighboring parts, which are subject to the action of the external air.
65
— A heavy air is more favorable to health than a light one, because it promotes the circulation of the blood, and insensible perspiration. When the air is heavy, it is generally clear; whereas a light air is generally accompanied with clouds, rain, or snow, which render it damp. Too great a dryness of the air is very injurious to the human body; but this seldom happens for any length of time, except in sandy countries. A damp air is very unwholesome, because it relaxes the fibres, obstructs insensible perspiration, and if heat accompany the dampness, it disposes the humors to putrefy. An air too hot dilates all the fluids of the body, and occasions sweatings, which bring on weakness and oppression. On the other hand, when the air is to cold, the solid parts contract excessively, and the fluids are condensed; hence result obstructions and inflammations. The best air is that which is neither too heavy nor too light, too moist nor too dry, and which is not impregnated with noxious vapors. Sturm’s Reflections, vol. iv, p. 50.
66
— “The most ingenious theories of the periodical winds we recollect, are those of Mr. Hadley, first proposed in Phil. Trans. vol. xxxix, p. 58, and lately revised by Mr. Dalton, in his Meteorological Essays,—and of Dr. Halley, first published in Phil. Transac. vol. xvi, p. 153, and recently defended by Dr. Kirwan, in his paper, ‘On the Variations of the Atmosphere.’ In the latter mentioned paper Kirwan has given some interesting information relative to variable winds, as westerly, easterly, southerly, northerly, and opposite concomitant winds; also relative to the succession of winds, and the Sirocco. See likewise the Philosophical Magazine, No. 60. Some curious facts respecting winds, and waves on the surface of the sea, are related by Mr. Horsburg in the Philosophical Journal, No. 60.” Haüy’s Nat. Phil. vol. i, pp. 285,286.
67
— Odyss. v. 295.
68
— A celebrated architect, born at Formio, in Italy. He was greatly esteemed by Julius Cæsar, and employed by Augustus in constructing public buildings and warlike machines. He wrote a valuable Treatise on Architecture.
69
— This division, with the several names on each point, was made by the Germans, as most commodious; but these names are not easily expressed in other languages. They are thus marked in English:
North.
East.
South.
West.
N and by E
E and by S
S and by W
W and by N
N N E
E S E
S S W
W N W
N E and by N
S E and by E
S W and by S
N W and by W
N E
S E
S W
N W
N E and by E
S E and by S
S W and by W
N W and by N
E N E
S S E
W S W
N N W
E and by N
S and by E
W and by S
N and by W
70
— “The most decisive circumstance tending to show the great velocity of brisk winds,” says Dr. O. Gregory, “is that of the rapid passage of the celebrated aëronaut M. Garnerin, from London to Colchester. On the 30th of June, 1802, the wind being strong, though not impetuous, M. Garnerin and another gentleman ascended with an inflammable air-balloon from Ranelagh Gardens, on the south-west of London, between four and five o’clock in the afternoon; and in exactly three-quarters of an hour they descended near the sea, at the distance of four miles from Colchester. The distance of the places of ascent and descent is at least 60 miles; so that, allowing no time for the elevation and depression of the balloon, but, supposing the whole period occupied in transferring it in a path nearly parallel to the earth’s surface, its velocity must have been at the rate of 80 miles per hour. If, therefore, the wind moved no faster than the balloon, its velocity was then 80 miles per hour, or 117½ feet per second; a celerity but little less than the greatest assigned by Kraaft: and hence it is probable, that the velocity of very impetuous winds is not less than 130 or 140 feet per second.” Haüy’s Nat. Phil. vol. i, p. 282.
71
— Mr. Bruce, who, in his journey through the desert, suffered from the simoon, gives of it the following graphical description. “At eleven o’clock, while we contemplated with great pleasure the rugged top of Chiggre, to which we were fast approaching, and where we were to solace ourselves with plenty of good water, Idris, our guide, cried out, with a loud voice, ‘Fall on your faces, for here is the simoon.’ I saw from the south-east a haze come, in color like the purple part of the rainbow, but not so compressed or thick. It did not occupy twenty yards in breadth, and was about twelve feet high from the ground. It was a kind of blush on the air, and it moved very rapidly: for I scarce could turn to fall on the ground with my head to the northward, when I felt the heat of its current on my face. We all lay flat on the ground as if dead, till Idris told us it was blown over. The meteor or purple-haze which I saw, was indeed passed, but the light air that still blew was of heat sufficient to threaten suffocation. For my part, I found distinctly in my breast that I had imbibed a part of it, nor was I free of an asthmatic sensation, till I had been some months in Italy, at the baths of Poretta, near two years afterwards.” Though the severity of this blast seems to have passed over them almost instantaneously, it continued to blow so as to exhaust them till twenty minutes before five in the afternoon, lasting through all its stages very near six hours, and leaving them in a state of the utmost despondency.
Fatal Simoon.—Extract of a letter from Smyrna:—We have received intelligence of a dreadful calamity having overtaken the largest caravan of the season, on its route from Mecca to Aleppo. The caravan consisted of 2,000 souls, merchants and travellers from the Red Sea and Persian Gulf, pilgrims returning from Mecca, and a numerous train of attendants; the whole escorted by 400 military. The march was in three columns. On the 15th of August last, they entered the great Arabian Desert, in which they journeyed seven days, and were already approaching its edge. A few hours more would have placed them beyond danger; but on the morning of the 23d, just as they had struck their tents, and commenced their march, a wind arose from the north-east, and blew with tremendous violence. They increased the rapidity of their march to escape the threatening danger; but the fatal Kamsin had set in. On a sudden dense clouds were observed, whose extremity obscured the horizon, and swept the face of the desert. They approached the columns, and obscured the line of march. Both men and beast, struck with a sense of common danger, uttered loud cries. The next moment they fell beneath its pestiferous influence lifeless corpses. Of 2,800 souls, composing the caravan, not more than 20 escaped this calamity; they owed their safety to the swiftness of their dromedaries. Literary Panorama, for January, 1814.
72
— See Baptist Magazine, for December, 1816.
73
— So the word is translated Luke xix, 10; 2 Cor. iv, 3.
74
— Benson on Gen. i, 9, 10.
75
— Contemplative Philosopher, vol. ii, pp. 177-179.
76
— M. Savary, in his instructive and entertaining Letters on Greece, has the following pertinent reflections: “We enjoy the finest weather imaginable; not a cloud obscures the sky, and a south-east wind wafts us directly towards the port to which our wishes tend. We have now entirely lost sight of land, and, as far as the eye can reach, only view the immense abyss of the waters, and the vast expanse of the heavens. How awful is this sight! How does it inspire the mind with great ideas! How adventurous is man, who trusts his fortune and his life to this frail vessel he has built, which a worm may pierce, or a single blast dash to pieces against a rock. Yet in this he braves the fury of the ocean! But how admirable is his ingenuity! He commands the winds, enchains them in the canvas, and forces them to conduct him where he pleases. He sails from one end of the world to the other, and traverses the immense liquid plains without any signals to direct him. He reads his course in the heavens. A needle, which wonderfully points perpetually to the pole, and the observation of the stars, inform him where he is. A few lines and points mark out to him the islands, coasts, and shoals, which his skill enables him to approach or avoid at pleasure. Yet has he cause to tremble, notwithstanding all his science and all his genius! The fire of the clouds is kindling over his head, and may consume his dwelling. Unfathomable gulfs are yawning beneath his feet, and he is separated from them only by a single plank. His confidence might make us imagine he knew himself immortal; yet he must die—die never to revive again, except in another state of being.”
77
— As it is sometimes necessary to preserve sea water in casks for bathing and other purposes, it is of importance to know how to keep it from putrefaction. Dr. Henry from many experiments made by him for the preservation of sea water from putrefaction, has concluded, that two scruples of quick-lime are sufficient to preserve a quart of sea water. The proportions, however, may vary a little according to the strength of quick-lime employed.
78
— “Frosts often occasion a scantiness of water in our fountains and wells. This is sometimes erroneously accounted for by supposing that the water freezes in the bowels of the earth. But this, as Dr. Robison remarks, is a great mistake: the most intense cold of a Siberian winter would not freeze the ground two feet deep; but a very moderate frost will consolidate the whole surface of a country, and make it impervious to the air; especially if the frost have been preceded by rain, which has soaked the surface. When this happens, the water which was flittering through the ground is all arrested, and kept suspended in its capillary tubes by the pressure of the air.” Haüy’s Nat. Phil. p. 198.
79
— Dr. Black’s Lectures, vol. i. p. 69.
80
— See Ellis’s voyage to Hudson’s Bay.
81
— St. Pierre’s Studies, vol. i, pp. 129-132.
82
— See 21st volume of the Philosophical Magazine.
83
— The specific gravity of water is as follows; a wine-pint measure weighs one pound; consequently a cubic foot of water weighs about 1,000 ounces, or 62½ pounds, avoirdupois. It is 816 times heavier than atmospheric air.
84
— Parkes’s Chemical Catechism, p. 108.
85
— Haüy’s Natural Philosophy, vol. i. pp. 197, 198.
86
— Parkes’s Chemical Catechism, pp. 94, 95.
87
— Parkes’s Chemical Catechism, p. 92.
88
— Driessen on the Nature of Snow.
89
— Thomson’s Chemistry, vol. i, p. 365.
90
— “The English word hail, in Latin grando, in Greek χαλαζα, gives us no information about the nature of the thing: but, if we take the word ברד BeReD in Hebrew, it resolves itself into ב..רד, which signifies in descensu, and so describes to us the physiological formation of hail: which, as philosophers agree, is first formed into drops of rain, and, as it falls, is frozen into hail.” Jones’s Letter on the Use of the Hebrew Language.
91
— Dr. Clarke on Exod. ix, 18.
92
— See Dr. Paley’s Natural Theology, p. 407.
93
— There are hot spouting springs of water in Iceland, of which a traveller says, “Near Laugervatan, a small lake about two days’ journey distant from Mount Hecla, we beheld the steam of the hot springs rising in eight different places, one of which of which continually threw up into the air a column of water from eighteen to twenty-four feet high. The water was extremely hot, so that a piece of mutton and some salmon trouts were almost boiled to pieces in it in six minutes.