CONCLUSIONS TO BE DRAWN FROM THESE FACTS.

The negative results just mentioned have an especial interest. It is

established that red phosphorus has a higher specific gravity than

white phosphorus, that of the former being 1.96, and that of the

latter 1.82. The author's former researches (_Bulletins de l'Académie

Royale de Belgique_, 49, p. 323, 1880) have shown that if sufficient

pressure is applied to a body capable of assuming several allotropic

states, it takes under pressure the state corresponding to its greatest

density. It is consequently impossible to transform red phosphorus into

white phosphorus by pressure. But we know, on the other hand, that

red sulphur and red phosphorus may be mixed with impunity at common

temperatures without combination ensuing; to produce combination the

temperature must be raised to about 260°, the point of transformation

of red phosphorus into white phosphorus.

It is thus established that red phosphorus must first be changed from

its allotropic condition before entering into combination with sulphur.

The pressure opposing this change renders also the act of combination

impossible; red phosphorus appears to us like a body which has lost its

chemical faculties.

Thus, the combination of an element with itself, _i. e._, its

polymerization, has really the effect of extinguishing its energy,

rendering it incapable of fulfilling certain functions. The chemistry

of red phosphorus, more simple than that of white phosphorus, may be

considered as the chemistry of a deadened body. The phosphorus which

is found in combination with sulphur is phosphorus sulphides, and

that which enters into combinations of other kinds, is certainly not

phosphorus in the red state; it is even possible, if not probable, that

it is not even white phosphorus, but a substance still unknown in the

free state.

We arrive at a similar but more complete conclusion as to the nature

of carbon. It is known that the affinity of carbon for sulphur and

even for oxygen only becomes manifest at a temperature bordering upon

redness. Is not this tantamount to saying that, in order to enter

into combination with another body, carbon, like red phosphorus, must

first change its allotropic condition? This view is supported by the

following considerations: The specific heat of amorphous carbon, and,

_a fortiori_, that of graphite and diamond, form exceptions to the

law of Dulong and Petit; they are too small by more than one-half.

They would be normal if the atomic weight of carbon were greater than

it really is; in other words, free carbon were a polymer of combined

carbon. Rose has found that at a temperature of about 500° the

specific heat of carbon agrees with the law of Dulong and Petit. At

this temperature carbon undergoes a beginning of depolymerization, _i.

e._, its chemical affinities reappear, and it burns readily in oxygen.

Do not these facts show a complete parallelism between the chemical

history of phosphorus and that of carbon?

Crystalline carbon, and even free amorphous carbon, are without

chemical activity at the ordinary temperature; but when, in consequence

of a rise of temperature, they take another state, they are transformed

into a new kind of carbon, constituting a fourth allotropic state, and

endowed with a prodigious capacity of combination. If these conclusions

are well founded, we may venture a step further and ask, if the carbon

which enters into the composition, not of mere organic compounds,

but of organized bodies, is not a carbon of still another allotropic

state characterized by the appearance of new properties or forms of

combination which find their expression in the vital phenomena.

In other words, a derivative of carbon, before forming part of a living

body, must first undergo in its atoms a transformation similar to that

which permits amorphous carbon to enter into the composition of organic

compounds. In this order of ideas the carbon of organic chemistry would

be merely a first deadened form of the carbon of biological chemistry,

while free carbon is merely the defunct remains of the carbon of

organic chemistry.--_Bulletin de la Société Chimique de Paris; Chem.

News._

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Scientific American, September 29, 1883 Supplement. No. 404 · 第 48 / 75 题