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liquid combination, enough water to hydrate the quick-blood which has circulated through a muscle in action is lime is incorporated by agitation, the temperature be- less than one-fourth of that contained in blood which has comes considerably raised, and in a few hours the entire traversed a muscle at rest, while there is a corresponding mass solidifies into a very homogenous pill-like consis- increase, not of course an equal increase, in the volume of tence. The proportion of water required is almost its carbonic acid; that the irritability of muscular fibre exactly a third of the lime employed. out of the body is arrested by its removal from oxygen, and again manifested on its re-exposure thereto; and lastly, that other things being equal, the amount of urea the lungs, is proportionate to the muscular activity of the excreted by the kidneys, and of carbonic acid excreted by individual. Seeing, then, that muscular exertion is really dependent upon muscular oxidation, we have to consider what should be the products, and what the value of its oxidation.

On repeating the previous experiment with ordinary calcined magnesia, M. Roussin established-1. That divers commercial balsams of copaiba contain a consider able proportion of water, which they will lose if exposed for a long time under a glass receiver, enclosing fragments of chloride of calcium or of carbonate of potash; 2. That the commercial calcined magnesia readily attracts the moisture of the air, and, after having been some time in a badly stopped vessel, always contains considerable quantities of water, sometimes to the extent of 15 and 20

per cent.

Unfortunately, the precise molecular formula-the exact chemical constitution-of muscle is at present unknown. But in muscle, as in all the albuminoid class of bodies, we do know the ratio in which the constituent carbon and nitrogen stand to one another. Thus it is established beyond all question that the ratio of the number of atoms of carbon to the number of the atoms of nitrogen in muscle is as nearly as possible, if not quite exactly, four to one. In the most minute fragment of muscle, then, for every single atomic proportion of nitrogen there are four atomic

If a specimen of good balsam of copaiba is divided into two equal parts, and having properly dried the first portion under a receiver, and sufficiently hydrated the other by placing it in a damp vessel, each portion is then mixed with one-sixteenth its weight of recently calcined magnesia, the dried portion remains liquid, and the mag-proportions of carbon, thus :nesia in great part even sinks to the bottom of the vessel, while the second portion, on the contrary, becomes a hard mass of pillular consistence.

The above facts show the necessity of the agency of water in order to bring about the combination of the resin of the balsam of copaiba with the lime and the magnesia. M. Roussin purposes to develope these results in a more extended investigation.

PROCEEDINGS OF SOCIETIES.

COLLEGE OF PHYSICIANS.

It will be more convenient, however, to express this ratio 4 CARBON to I NITROGEN.

four to one, we will adopt eight to two, as our expression by the doubles of the above numbers, so that, instead of of the atomic ratio of carbon to hydrogen in every particle of muscle:

8 CARBON to 2 NITROGEN. Admitting, as a result of its ultimate metamorphosis, that the whole of the nitrogen of muscle is converted into urea, let us first consider what proportion of its carbon of muscle must be associated with this nitrogen, and what proportion be left for excretion in the form of carbonic acid. Now, although the molecular constitution of muscle

"On Animal Chemistry." A course of Six Lectures by is undetermined, that of urea is perfectly definite.* WILLIAM ODLING, M.B., F.R.S., F.R.C.P.

Wednesday, May 10, 1865.
LECTURE 5.

As shown by its formula, CH NO, the molecule of urea consists of one atom of carbon, four atoms of hydrogen, two atoms of nitrogen, and one atom of oxygen. In other words, leaving out of consideration its hydrogen and

in urea have one atom of carbon associated with them; so as one to two. Accordingly, every two atoms of nitrogen that if we take the two proportions of nitrogen existing in muscle and add thereto the one proportion of carbon necessary to form urea, we shall have seven proportions of carbon left for conversion into carbonic acid, thus:

7-CARBON to

{2-NITROGEN.

of muscle is the appearance of one-eighth of its carbon in The theoretical result, then, of the complete oxidation the form of urea, and of seven-eighths of its carbon in the

Muscular action dependent on muscular metamorphosis-oxygen, the atomic ratio of carbon to nitrogen in urea is Theoretic oxidation of muscle into one proportion of urea and seven of carbonic acid-Practical results-Dynamic value of muscle oxidation-Quantities of heat producible by combustion of hydrogen and carbon-Difference between quantity and intensity of heat-Unit of heat equivalent to 430 kilogram-metres of motion Quantities of motion producible by combustion of hydrogen and carbon Economy of muscle as a motive exponent of combustionReciprocity of heat and motion in muscular action Muscular force traceable to the sun-Amount of force derivable from muscle proportional to degree of its oxidation-Imperfect knowledge of natural process of oxidation -Artificial oxidation of muscle-Nature of intermediate products-Relations of aldehydes and nitriles to acidsSimple constitution of acids obtained by muscle oxidation -Production of both fatty and aromatic compounds-fed Natural occurrence of leucine and tyrosine-Their formation by indirect oxidation of nitrogeneous tissue Leucine the most elaborate of fatty, and tyrosine of aromatic animal products- Constitution and analogies of leucine-Probable constitution of tyrosine-Its relation to hippuric acid.

THAT muscular exertion is dependent on muscular metamorphosis or oxidation is a subject rather for the physiologist than the chemist to dilate upon. Perhaps, however, I may be permitted to remind you of such observations as the following-that a free supply of thoroughly oxygenated arterial blood is essential for complete well-developed muscular action; that the volume of oxygen contained in

form of carbonic acid.

series of experiments made by Bischof and Voit, and Now, let us see what is the actual result. We have two Pettenkofer and Voit respectively, in which lean dogs were

exclusively upon a moderate diet of flesh. In the first series of experiments a small proportion of fat left in the experiments the fat was entirely removed. The general flesh was duly allowed for; while in the second series of results of these two series of experiments are shown

below:-
:-

C. of carb, acid.

C. of urea.

[blocks in formation]

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Thus the ratio of carbon excreted in the form of carbonic acid to carbon excreted in the form of urea was as 729 to 1 in the first series of experiments, as 6'85 to 1 in the second series, and as 7'07 to 1 in the mean of the two. Theoretically, then, the ratio of carbon in carbonic acid to carbon in urea is as 7 to 1; experimentally it is found | to be as 7'07 to 1-a striking mutual corroboration of the two methods of calculation and research.

rusting of a given weight of iron is considerably greater than that evolved by its rapid combustion in oxygen, the resulting compound being not only more highly oxidised, but in a state of hydration, or combination with solid water. I may illustrate this to you by a very ordinary experiment. When a plate of copper is immersed in a jar of chlorine gas, for instance, the chlorine gradually combines with the metal, and there is no evident rise of temperature; but when very thin copper leaf is immersed in chlorine gas, the combination takes place instantaneously, with evolution of sufficient heat to render the leaf luminous-with vivid combustion, in fact-as you perceive. Now, the amount of heat given out under these opposite circumstances is identical; the only difference is in its intensity -in the quantity of heat associated with a given quantity of matter at a given moment. In the last case, the action being instantaneous, and the quantity of matter to be heated very small, we have what we call an intense heat-that is, the momentary association of a large quantity of heat with a small quantity of matter; whereas in the other case, the action being gradual, the development of heat is likewise gradual, spread over a long period of time, and asso. ciated with a large quantity of matter; the increased temperature of which is, therefore, at no one moment very perceptible. The terms quantity and intensity of heat are strictly analogous to the terms quantity and velocity of motion. In a pound weight of iron raised to 1000-the melting point of silver, or ten pounds weight raised to 100°-the boiling point of water,-the quantity of heat capable of being imparted—say, to a gallon of cold water substantially the same, though the intensity of the heat is ten times as great in the one case as the other; just as the quantity of motion is the same in a pound weight moving at the rate of 1000 feet, or a ten pound weight moving at the rate of 100 feet per second, although the velocity of motion is ten times as great in the one case as the other. We come, then, to this conclusion-that chemical action, whether rapid or slow, provided only that the same substances react and the same products result, always furnishes the same amount of heat.

With regard to the dynamic value of muscle oxidation, I told you in my last lecture that by the separation of oxygen from carbo-hydrogen a certain amount of heat force was absorbed and rendered latent in the separated bodies, which, by the re-combination of these bodies, was again liberated and rendered sensible. Now, we find that in all re-combinations of separated constituents, the quantity of heat evolved is perfectly definite and invariable. Confining our attention to hydrogen, and speaking in round numbers, we may say that the heat evolved by burning a cubic foot of hydrogen-that is, by combining a cubic foot of hydrogen with half a cubic foot of oxygen-will raise the temperature of 5 cubic feet of water one degree Fahrenheit; or that the heat of burning hydrogen is capable of raising the temperature of 5 times its bulk of water one degree. But we know that the quantity of matter in a body is proportionate to its weight, and accordingly we get a much better idea of the amount of heat developed, by comparing the items gravimetrically rather than volumetrically. Thus we find that the combustion of one part by weight of hydrogen will evolve an amount of heat sufficient to raise the temperature of more than 60,000 parts of water one degree Fahren--is heit, or 34,000 parts of water one degree centigrade. Now, in comparing the amounts of heat given out by the combustion of different substances, it is convenient to have some definite standard of comparison; and the usual continental standard is altogether, perhaps, the most convenient. According to this standard, the amount of heat given out by one kilogramme of water in cooling one degree centigrade, or, of course, the amount of heat absorbed by one kilogramme of water in rising one degree centigrade is called the unit of heat. We find, then, that when one gramme of hydrogen gas is burned into water it gives out 34 units of heat; or it will raise the temperature of 34 kilogrammes-that is, 34,000 times its own weight of water one degree centigrade.

Turning our attention to carbon, we find that one gramme of carbon, in being oxidised or burned into carbonic anhydride, gives out 8 units of heat, or will raise the temperature of 8 kilogrammes that is to say, 8000 times its own weight-of water one degree. Now, the quantity of heat evolved during the oxidation of a given weight of hydrogen, carbon, or any other combustible, is perfectly independent of the rapidity or slowness of the action. Provided only that the same products are formed, the same amount of heat is liberated in their production, whether it takes place rapidly or slowly, violently or gradually. It is only the intensity of the heat, and not its quantity, which varies with the rapidity of the combination. When a stout piece of iron rusts in the air we get oxide of iron produced as the result of the slow burning of the metal, but there is no obvious rise of temperature! On the other hand, when a piece of iron wire is burned in oxygen gas, we have a brilliant combustion, with an intense development of heat. In reality, the products formed in these two cases are not identical, but only allied. Assuming them, however, to be identical, the amount of heat given out in the rapid burning of the metal would be identical with that given out during its slow rusting. The difference is merely that in the one case all the heat is given out in the course of a few seconds, that there is a great quantity of heat produced in a short time; while in the other case this same quantity of heat is developed only during a long series of years. As a matter of fact, the quantity of heat evolved by the slow

Now, let us apply this to hydrogen, one of the fuel constituents burnt in our tissues. If we inflame a mixture of oxygen and hydrogen gases, the combination and evolution of heat being alike instantaneous, we obtain the most intense degree of heat capable of being produced by direct chemical action. On the other hand, if we take the same mixture of oxygen and, hydrogen gases, and cause them to unite slowly by means of spongy platinum, the oxidation is spread over a considerable period of time, and, the heat being developed during a period of many minutes, there is no great manifestation of temperature at any one instant. The quantity of heat is, however, the same in both cases. One gramme of hydrogen in combining with oxygen, whether quickly or slowly, will always evolve 34 units of heat; and one gramme of carbon in combining with oxygen, whether quickly or slowly, will always evolve 8 units of heat. The slow oxidation of so much carbon and hydrogen in the human body will always produce its due amount of heat, or an equivalent in some other form of energy; for while the latent force liberated in the combustion of the carbon and hydrogen of fat is expressed solely in the form of heat, the combustion of an equal quantity of the carbon and hydrogen of voluntary muscle is expressed chiefly in the form of motion. You may remember that I referred in my last lecture to the equivalency subsisting between heat and motion--to the circumstance that so much heat was convertible into so much motion. Accordingly, when we burn hydrogen or carbon, instead of getting the heat force which was exerted in separating them from oxygen remanifested in the form of heat, under certain circumstances we get it manifested in the form of motion.

Let us next consider what are the quantitative relations subsisting between heat and motion. We have taken as

our unit of heat the quantity of heat absorbed or evolved by one gramme of water in rising or falling through one centigrade degree of temperature. Now, this is found by experiment to be the exact quantity of heat generated by collision with the earth of a kilogramme weight falling from a height of 430 metres. The mechanical force, then, of a kilogramme weight which has fallen through 430 metres, or, in other words, the mechanical force necessary to lift a kilogramme weight to the height of 430 metres, is equal to, interchangeable for, and convertible into the heat force evolved or absorbed by a kilogramme of water in changing its temperature one degree. Or the arrest of one unit of motion would raise the temperature of a kilogramme of water at zero 1 degree, and conversely, the absorption of one unit of heat would lift a kilogramme weight to the height of 430 metres. Of course, the force necessary to lift 1 kilo. through 430 metres, or 10 kilos. through 43 metres, or 430 kilos. through I metre, is the same; whence it is convenient to apply the expression kilogram-metre to the product of the kilos. lifted into the metres of height, and to say that the heat evolved by the cooling of a kilogramme of water one degree is equal to 430 kilogram-metres of motion, and vice versa. Or we may adopt Mr. Joule's original standard, and say that the heat evolved by the cooling of a pound of water one degree Fahrenheit is equal to 772 foot-pounds of motion.

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The applicability of these considerations to the combustions of hydrogen and carbon taking place in the animal body is obvious. We have said that the combustion of 1 gramme of hydrogen evolves 34 units of heat, and that a unit of heat is equal to 430 kilogram-metres of motion; so that the combustion of 1 gramme of hydrogen will produce 34 × 430 = 14,600 kilogram-metres of motion; or will serve to lift 1 kilogramme weight through 14,600 metres of height, or 14,600 kilogrammes through 1 metre of height, &c., &c. Similarly, the combustion of 1 gramme of carbon will suffice to produce 3440 kilogram-metres of motion, thus:—

One gramme
burnt.

HYDROGEN
CARBON

34 x 430 8 × 430

Kilogram-metres

=

of motion. 14,600 = 3,440

pro

In this way, then, we can form some idea of the mechanical power generated, or quantity of motion ducible, by the combustion of the hydrogen and carbon of our muscles into water, and carbonic acid or urea respectively. Our knowledge of the intimate constitution of muscle is, however, too imperfect to allow of our estimating the amount of motion producible by its oxidation with any degree of exactitude; but, as the result of a rough calculation, it may be taken that the combustion of the unburnt carbo-hydrogen of one gramme of dry muscle, free from fat, is capable of furnishing 1950 kilogram-metres of motion, or will suffice to lift 1950 kilogrammes to the height of 1 metre.‡

The heat produced by the conversion of carbon into urea is doubtless that producible by its conversion into carbonic anhydride CO2, and not merely that producible by its conversion into carbonic oxide CO, as sometimes represented.

Assuming for muscle the formula C12H19N304x6, and subtracting all the oxygen and nitrogen, with the necessary hydrogen, in the forms of water and ammonia, so as to leave a residue of C12H2 x6, 269 grammes of muscle would leave 144 grammes of carbon and 2 grammes of hydrogen for oxidation, which should furnish 524,560 kilo-gram-metres of motion, thus:

CARBON

HYDROGEN

Grammes.

Kilogram-metres.

144 X 3,440 495.360 2 X 14,600 = 29,200 524.560

Hence one gramine of muscle should furnish 524, 560-:-269-1590 kilogram-metres of motion. Accepting this result, it would follow from the experimental determinations of Valentin and Pousseuille, and the calculations of Mayer, who, together with Mr. Joule, is the great apostle of energetics, that the entire substance of the ventricles would be consumed in maintaining little more than two days' work of the beart. Of course some of the data on which this calculation is based are but very roughly approximative.

Now, although the ratio of the amount of motion actually produced to that theoretically producible by the combustion of a given weight of muscle, has not, I believe, been satisfactorily ascertained, this much is certain,—that muscular tissue is, without exception, by far the most perfect of machines for manifesting the force liberated by chemical action in the form of motion. No artificial contrivance with which we are acquainted is at all comparable to it in economy-that is to say, in the proportion of mechanical work performed to the total force liberated. The steam-engine, for instance, is an artificial machine, expressly intended for the conversion of chemical force into motion. Heat is generated in the boiler-furnace by a combination of the carbo-hydrogen of the coal with the oxygen of the air, but only a certain amount of this heat is absorbed in the evaporated water, and then only a certain amount of the heat so absorbed is translated into motion. Now it appears that by burning, or consuming, or oxidating a given weight of muscle in our bodies, we obtain a quantity of available motive force which would require for its production the combustion of at least five or six times its weight of coal in the most perfect steam-engine that ever was constructed.

The superior economy of muscle over any artificial contrivance, as a motive machine, seems to depend in great measure upon the circumstance of the force liberated by its oxidation being expressed directly in motion, instead of first appearing in some intermediate form of energy. Thus, in a steam-engine, the immediate effect of the oxidation is not motion, but heat, some of which eventually or intermediately appears as external motion. In this case, the combination produces heat, and the heat is afterwards transformed into motion; whereas, in muscular tissue, the the combination first produces motion, which is afterwards, in many cases, transformed into heat. The force liberated by the combustion of the muscular fibre of the heart, for instance, is expressed directly in the contraction of its ventricles, and the consequent propulsion of the blood through the greater and less circulations. But by the time the blood gets back to the heart, it has given up all its motion, and requires to be again propelled by another contraction of the ventricles, and so on. Now, what becomes of the motion received by the blood at each

contraction?

The

It appears in the form of heat. blood circulating through the vessels and capillaries undergoes a certain amount of friction. It is brought to a state of rest gradually by the hindrance to its motion, just as a bullet is brought to rest suddenly by the hindrance to its motion; and, in both cases, that which was motion becomes heat. The quantity of heat finally produced by the friction of the blood is generated as truly by the combustion of the heart-fibre, as if we had burnt it directly in a furnace, without any intermediate manifestation of motion. In some cases, indeed, the oxidation of muscle within our bodies produces a direct liberation of heat instead of motion. Thus, in the case of a person lifting a weight, the combustion of his tissue is expressed in the motion of the weight; but suppose he only attempts to lift a weight which is too heavy for him, there is then no production of motion, but instead of it a corresponding increase of temperature in the muscle. In tetanus, again, where the violent contraction of the muscles produces no external motion, their temperature has been observed to increase as much as six degrees centigrade or eleven degrees Fahrenheit above the normal state. Conversely, in the case of a man working a treadmill, although the amount of heat evolved from his person is absolutely larger, its proportion, relatively to the amount of tissue burned, is smaller than in the case of a person at rest, by a difference equivalent to the external work performed. But in fever, where there is a rapid destruction of tissue without any corresponding mechanical effect, we have a high degree of external heat.

Thus we return once again to the conclusion which

I brought more prominently under your notice in my last lecture. We perceive that muscular exertion does not result from vital force generated within the body, or, indeed, from force of any kind generated within the body, but only from a liberation within the body of pent-up solar force, which at some time or other had been rendered latent in the separated carbo-hydrate of our food on the one hand, and oxygen of our breath on the other. As well observed by Dr. Tyndall,— "It is at his (i.e., the sun's) cost that animal heat is produced, and animal motion accomplished. Not only is the sun chilled, that we may have our fires, but he is likewise chilled that we may have our powers of locomotion.' From the terms in which, upon that occasion, I referred to the fiction of vital force, some physiologists who honoured me by their presence seemed to infer that chemists and physicists were insensible to those important distinctions existing between living and dead matter, which they profess to explain by declaring the former to be possessed, and the latter dispossessed, of vital force. I believe, however, that chemists appreciate in its fullest extent what may be termed the mystery of life, but they look upon the physiologists' explanation as a mere periphrasis, -as only another mode of saying that dead matter differs from living matter because it is dead, while living matter differs from dead matter because it is alive. Chemists and physicists are well assured that, be life what it may, it is not a generator, but only a transformer, of external force. In the vegetable kingdom solar force is absorbed, in the animal kingdom it is liberated by the eremacausis of our fat and muscle.

Besanez's experiments upon the oxidation effected by ozone in alkaline liquids, whether or not a series of bodies intermediate between the initial substance and final carbonic acid are really formed, we are quite incapable of detecting them, and, consequently, of tracing their metamorphoses. The constituent carbon atoms of the original substance seem, at any rate, to become at once completely isolated, and oxidised. Whether, therefore, the more complex molecules formed by natural tissue-oxidation are to be regarded as direct, but intermediate, products of the principal oxidation, or as bye products resulting from subsidiary processes, is at present an open question, though the balance of evidence with regard to certain products, at any rate, seems to be in favour of the latter view. In any case, however, the formation and even excretion of some or other of these bodies, in greater or less proportion, according to the nature of the organism,-uric acid largely in birds and land reptiles, hippuric acid largely in herbivora, and both acids sparingly in mankind-are obviously normal or healthy actions. By the excretion of such imperfectly burned substances, indeed, a certain amount of force does not become utilised within the animal, but this prodigality of force in organic nature is far inferior to that which we observe in the inorganic world.

(To be continued.)

BRITISH ASSOCIATION. Birmingham Meeting, President, Professor PHILLIPS, M.A., &c., &c.

union of fresh discoveries and new inventions with the

President's Address, delivered September 6. Now, the full realisation of the force derivable from a given weight of muscle depends upon its complete oxida- ASSEMBLED for the third time in this busy centre of industion into water and carbonic acid or urea. Should it be trious England, amid the roar of engines and the clang of only converted into sugar, or kreatine, or uric acid, these hammers, where the strongest powers of nature are trained are imperfectly burned substances, which still retain a to work in the fairy chains of art, how softly falls upon certain amount of potential energy liberable from them by the ear the accent of Science, the friend of that art, and further oxidation. They still contain associated with them the guide of that industry! Here, where Priestley anasome portion of the latent force put into the original tissue-lysed the air, and Watt obtained the mastery over steam, constituents at the period of their formation, and accord- it well becomes the students of nature to gather round the standard which they carried so far into the fields of knowingly, by their further oxidation, we are capable of getting an additional amount of work out of them. ledge. And when, on other occasions, we meet in quiet In order, therefore, to obtain the full equivalent of heat colleges and academic halls, how gladly welcome is the force or motive force to which we are entitled by the waste of our tissues, it is important that this waste should be solid and venerable truths which are there treasured and thorough, that both the hydrogen and carbon should be taught. Long may such union last; the fair alliance of converted into the most completely oxidised compounds cultivated thought and practical skill; for by it labour is they are susceptible of forming, the whole of the hydro- dignified and science fertilised, and the condition of human gen into water, and the whole of the carbon into its society exalted! most stable mono-carbon compound, namely, carbonic acid, or the ammoniated form of this acid, namely, urea. In some cases of imperfect oxidation, however, we get less oxidised, and more complex, dicarbon molecules produced, such, for example, as oxalic acid, which occurs either in its normal saline state, or colligated with urea in the form of allantoine, oxaluric acid, &c. In cases of yet more imperfect oxidation, we meet with still less oxidised tricarbon molecules, such, for example, as the mesoxalic compound, which forms uric acid by its colligation with urea. We may even have tetracarbon molecules such as succinic acid, pentacarbon molecules such as amido-valeric acid or phocine, hexacarbon compounds such as amido-caproic acid or leucine, and heptacarbon compounds such as the benzoic residue of hippuric acid, and the salicic residue of tyrosine.

In certain processes of artificial oxidation to which I referred in a former lecture, we obtain, as you may remember, from any particular substance a series of less and less complex bodies terminating in carbonic acid; or, to use again the words of Gerhardt, we gradually descend the scale of complexity, converting the original substance into more and more simple products by successively burning off a portion of its carbon and hydrogen. In other cases, however, as in Gorup

Through this happy union of science and art, the young life of the British Association,-one-third of a century,inventions in a degree never surpassed. How else could has been illustrated by discoveries and enriched by useful we have gained that knowledge of the laws of nature which has added to the working strength of a thousand millions of men the mightier power of steam*, extracted from the buried ruins of primeval forests their treasured elements of heat and light and colour, and brought under the control of the human finger, and converted into a messenger of man's gentlest thoughts, the dangerous mystery of the lightning ?†

How many questions have we asked-not always in vain regarding the constitution of the earth, its history as a planet, its place in creation ;-now probing with sharpened

The quantity of coal dug in Great Britain in the year 1864 appears by the returns of Mr. R. Hunt to have been 92,787,873 tons. This would yield, if employed in steam engines of good construction, an amount of available force about equal to that of the whole human race. But in the combustion of coal not less than ten times this amount of force is actually set free-nine-tenths being at present unavailable, according to the statement of Sir William Armstrong, in

his address to the meeting at Newcastle in 1863.

The definite magnetic effect of an electrical current was the discovery of Oersted in 1819; Cooke and Wheatstone's patent for an electric telegraph is dated in 1837; the first message across the Atlantic was delivered in 1858. Tantæ molis erat.

eyes the peopled space around--peopled with a thousand times ten thousand stars ;-now floating above the clouds in colder and clearer air;-now traversing the polar icethe desert sand-the virgin forest- the unconquered mountain ;-now sounding the depths of the ocean, or diving into the dark places of the earth. Everywhere curiosity, everywhere discovery, everywhere enjoyment, everywhere some useful and therefore some worthy result. Life in every form, of every grade, in every stage; man in every clime and under all conditions; the life that now surrounds us, and that which has passed away;-these subjects of high contemplation have been examined often, if not always, in the spirit of that philosophy which is slowly raising, on a broad security of observed facts, sure inductions, and repeated experiments, the steady columns of the temple of physical truth.

Few of the great branches of the study of nature on which modern philosophy is intent were left unconsidered in the schools of Athens; hardly one of them was, or, indeed, could be, made the subject of accurate experiment. The precious instruments of exact research-the measures of time, and space, and force, and motion-are of very modern date. If, instead of the few lenses and mirrors of which traces appear in Greek and Roman writers, there had been even the first Galilean or the smallest Newtonian telescope in the hands of Hipparchus, Eratosthenes, or Ptolemy, would it have been left to their remote successors to be still struggling with the elements of physical astronomy, and waiting with impatience till another quarter of a century shall have rolled away, and given us one more good chance of measuring the distance of the sun by the transit of Venus? Had such instruments as Wheatstone's chronoscope been invented, would it have been left to Foucault to condense into his own apartment an experimental proof of the velocity of light, and within a tract of thirty feet to determine the rate of its movement through all the vast planetary space of millions and thousands of millions of miles, more exactly than had been inferred by astronomers from observations of the satellites of Jupiter By this experiment the velocity of light appears to be less, sensibly less, than was previously admitted; and this conclusion is of the highest interest; for, as by assuming too long a radius for the orbit of Jupiter, the calculated rate of light-movement was too great, so now, by employing the more exact rate and the same measures of time, we can correct the estimated distance of Jupiter and all the other planets from the sun. We have, in fact, a really independent measure of planetary space; and it concurs with observations of the parallax of Mars, in requiring a considerable reduction of the assumed diameters of the planetary paths. The distance of the earth from the sun must be reduced from above ninety-five to less than ninety-three millions of miles, and by this scale the other space-measures of the solar system, excepting the diameter of the earth and the distance and diameter of the moon, may be corrected.

The effect of lenses or globes of glass or crystal (vaλos) in collecting the solar rays to a point are familiarly referred to by Aristophanes in the Nubes, 766; and the ornamental use of convex and concave reflectors is known by the curious discussions in the IVth Book of Lucretius.

§ Fizeau performed experiments on the velocity of light between Suresnes and the Butte Montmartre, by means of the oxyhydrogen light, reflected back in its own path. The space was 28,324 ft. Engl. Twice this distance was traversed in 1000 of a second = 167,528 geogr. miles in a second. From obscrvations of Jupiter's satellites, Delambre inferred 167,976 miles, Struve 166,096. The experiment of M. Foucault gives 298,000,000 metres = 160,920 geogr. miles.

Estimates of the earth's distance from the sun have varied much. Cassini and Flamsteed, using observations of the parallax of Mars, ascribe to it ten or eleven thousand diameters of the earth = 79 or 89 millions of miles. Huyghens estimated it at twelve thousand 95 millions of miles. In 1745, Buffon reported it as the common opinion of astronomers at 30 millions of leagues (Fr.) = 90 millions miles (Engl.), but after the transit of Venus in 1769, he allowed 33 millions. Such was the effect of that now supposed erroneous experiment on the opinions of astronomers. (Epoques de la Nature.)

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The light and heat which are emitted from the sun reach the earth without great diminution by the absorptive action of the atmosphere; but the waste of heat from the surface of our planet through radiation into space is prevented, or rather lessened by this same atmosphere. Many transparent bodies admit freely heat rays derived from a source of high temperature, but stop the rays which emanate from bodies only slightly warmed. The atmosphere possesses this quality in a remarkable degree, and owes it to the presence of diffused water and vapour; a fact which Dr. Tyndall has placed in the clear light of complete and varied experiment. The application of this truth to the history of the earth and of the other planets is obvious. The vaporous atmosphere acts like warm clothing to the earth. By an augmented quantity of vapour dissolved, and water suspended in the air, the waste of surface-heat of the earth would be more impeded; the soil, the water, and the lower parts of the atmosphere would grow warmer; the climates would be more equalised; the general conditions more like what has been supposed to be the state of land, sea, and air, during the geological period of the coal-measures.

Such an augmentation of the watery constituents in the atmosphere would be a natural consequence of that greater flow of heat from the interior, which by many geologists, mathematicians, and chemists is supposed to have happened in the earlier periods of the history of the earth.

By the same considerations we may understand how the planet Mars, which receives not half so much heat from the sun ** as the earth does, may yet enjoy, as in fact it seems to enjoy, nearly a similar climate, with snows alternately gathering on one or the other of its poles, and spreading over large spaces around, but not, apparently, beyond the latitude of 50° or 40°; the equatorial band of 30° or 40° North or South being always free from snowmasses bright enough and large enough to catch the eye of the observer. Mars may, therefore, be inhabited, and we may see in the present state of this inquiry reason to pause before refusing the probability of any life to Jupiter and even more distant planets.

The history of suns and planets is in truth the history of the effects of light and heat manifested in them or emanating from them. Nothing in the universe escapes their influence; no part of space is too distant to be penetrated by their energy; no kind of matter is able to resist their transforming agency. Many, if not all, the special forces which act in the particles of matter are found to be reducible into the general form of heat; as this is convertible, and practically is converted, into proportionate measures of special energy. Under this comprehensive idea of convertibility of force, familiar to us now by the researches of Joule,tt the reasonings of Grove ++ and Helmholtz, and the theorems of Rankine,§§ it has been attempted by Mayer, Waterston, and Thomson || to assign a cause for the maintenance of the heat-giving power of the sun in the appulse of showers of aerolites and small masses of matter, and the extinction of their motion on the surface of the luminary. By calculations of the same order, depending on the rate of radiation of heat into space, the past antiquity of the earth and the future duration of sunshine have been expressed in thousands or millions of centuries.¶¶ In like manner the physical

Proc. of Roy. Soc. 1861. The Rumford Medal was adjudged to Dr. Tyndall in 1864. ** The proportion is about 19f according to the received measure of the mean distance.

tt Phil. Mag., 1843; Reports of the British Association, 1845; Trans. of the Royal Society, 1850.

# Grove, on the Correlation of Physical Forces, 1846.

$$ Rankine, Trans. of the Royal Society of Edinburgh, 1850-1; Phil. Trans., 1854.

ill Communication to the Royal Society of Edinburgh, 1854. Professor Thomson assigns to the sun's heat, supposing it to be maintained by the appulse of masses of matter, a limit of 300,000 years; and to the period of cooling of the earth from universal fusion to its actual state 98,000,000 years. These are the lowest estimates sanctioned by any mathematician.

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