THE ORIGIN AND RELATIONS OF THE CARBON MINERALS.

[Footnote: Read before the New York Academy of Sciences, February 6,

1882.]

By J.S. NEWBERRY.

What are called the carbon minerals--peat, lignite, coal, graphite,

asphalt, petroleum, etc.--are, properly speaking, not minerals at

all, as they are organic substances, and have no definite chemical

composition or crystalline forms. They are, in fact, chiefly the

products or phases of a progressive and inevitable change in

plant-tissue, which, like all organic matter, is an unstable compound

and destined to decomposition.

In virtue of a mysterious and inscrutable force which resides in the

microscopic embryo of the seed, a tree begins its growth. For a brief

interval, this growth is maintained by the prepared food stored in the

cotyledons, and this suffices to produce and to bring into functional

activity--some root-fibrils below and leaves above, with which

the independent and self-sustained life of the individual begins.

Henceforward, perhaps for a thousand years, this life goes on, active in

summer and dormant in winter, absorbing the sunlight as a motive power

which it controls and guides. Its instruments are the discriminating

cells at the extremities of the root-fibrils, which search for, select,

and absorb the crude aliment adapted to the needs of the plant to which

they belong, and the chlorophyl cells--the lungs and stomach of the

tree--in the leaves. During all the years of the growth of the plant,

these organs are mainly occupied in breaking the strongly riveted bonds

that unite oxygen and carbon in carbonic acid; appropriating the carbon

and driving off most of the oxygen. In the end, if the tree is, e. g.,

a _Sequoia_, some hundreds of tons of solid, organized tissue have been

raised into a column hundreds of feet in height, in opposition to the

force of gravitation and to the affinities of inorganic chemistry.

The time comes, however, sooner or later, when the power which has

created and the life that has pervaded this wonderful structure

abandon it. The affinities of inorganic chemistry immediately reassert

themselves, in ordinary circumstances rapidly tearing down the ephemeral

fabric.

The disintegration of organic tissue, when deserted by the force which

has animated and preserved it, gives rise to the phenomena which form

the theme of this paper.

Most animal-tissue decomposes with great rapidity, and plant tissue,

when not protected, soon decays. This decay is essentially oxidation,

since its final result is the restoration to the atmosphere of carbonic

acid, which is broken up in plant-growth by the appropriation of its

carbon. Hence it is a kind of combustion, although this term is more

generally applied to very rapid oxidation, with the evolution of

sensible light and heat. But, whether the process goes on rapidly or

slowly, the same force is evolved that is absorbed in the growth of

plant-tissue; and by accelerating and guiding its evolution, we are able

to utilize this force in the production at will of heat, light, and

their correlatives, chemical affinity, motive power, electricity, and

magnetism. The decomposition of plants may, however, be more or less

retarded, and it then takes the form of a destructive distillation,

the constituents reacting upon each other, and forming temporary

combinations, part of which are evolved, and part remain behind. Water

is the great extinguisher of this as of the more rapid oxidation that we

call combustion; and the decomposition of plant-tissue under water is

extremely slow, from the partial exclusion of oxygen. Buried under thick

and nearly impervious masses of clay, where the exclusion of oxygen is

still more nearly complete, the decomposition is so far retarded that

plant-tissue, which is destroyed by combustion almost instantaneously,

and if exposed to "the elements"--moisture with a free access of

oxygen--decays in a year or two, may be but partially consumed when

millions of years have passed. The final result is, however, inevitable,

and always the same, viz., the oxidation and escape of the organic

mutter, and the concentration of the inorganic matter woven into its

composition--in it, but not of it--forming what we call the ash of the

plant.

Since the decomposition of organic matter commences the instant it is

abandoned by the creative and conservative vital force, and proceeds

uninterruptedly, whether slowly or rapidly, to the final result, it is

evident that each moment in the progress of this decomposition presents

us with a phase of structure and composition different from that which

preceded and from that which follows it. Hence the succession of these

phases forms a complete sliding scale, which is graphically shown in

the following diagram, where the organic constituents of plant

tissue--carbon, hydrogen, oxygen, and nitrogen--appear gradually

diminishing to extinction, while the ash remains nearly constant, but

relatively increasing, till it is the sole representative of the fabric.

[Illustration: DIAGRAM SHOWING THE GENETIC RELATIONS OF THE CARBON

MINERALS.]

We may cut this triangle of residual products where we please, and by

careful analysis determine accurately the chemical composition of a

section at this point, and we may please ourselves with the illusion, as

many chemists have done, that the definite proportions found represent

the formula of a specific compound; but an adjacent section above or

below would show a different composition, and so in the entire triangle

we should find an infinite series of formulae, or rather no constant

formulae at all. We should also find that the slice, taken at any point

while lying in the laboratory or undergoing chemical treatment, would

change in composition, and become a different substance.

In the same way we can snatch a brand from the fire at any stage of its

decomposition, or analyze a decaying tree trunk during any month of its

existence, and thus manufacture as many chemical formulae as we like,

and give them specific names; but it is evident that this is child's

play, not science. The truth is, the slowly decomposing tissue of the

plants of past ages has given us a series of phases which we have

grouped under distinct names, and we have called one group peat, one

lignite, another coal, another anthracite, and another graphite. We have

spaced off the scale, and called all within certain lines by a common

name; but this does not give us a common composition for all the

material within these lines. Hence we see that any effort to define or

describe coal, lignite, or anthracite accurately must be a failure,

because neither has a fixed composition, neither is a distinct

substance, but simply a conventional group of substances which form part

of an infinite and indivisible series.

But this sliding scale of solid compounds, which we designate by

the names given above, is not the only product of the natural and

spontaneous distillation of plant tissue. Part of the original organic

mass remains, though constantly wasting, to represent it; another part

escapes, either completely oxidized as carbonic acid and water, or in

a volatile or liquid form, still retaining its organic character, and

destined to future oxidation, known as carbureted hydrogen, olefiant

gas, petroleum, etc.

Hence, in the decomposition of vegetable tissue, two classes of

resultant compounds are formed, one residual and the other evolved; and

the genesis and relation of the carbon minerals may be accurately shown

by the following diagram:

PLANT TISSUE

_________________

|

_Residual Products_ | _Evolved Products_

|

Peat. }

| }

Lignite. }

| } { Carbonic Acid.

Bitumious Coal. } { Carbonic Oxide.

| } { Carbureted Hydrogen, etc.

Semi-bitumious " } { Water.

| } { {Maltha.

Anthracite. } { { |

| } { {Asphalt etc.

Graphitie Anthracite. } { Petro- { |

| } { leum {Asphaltic Coal.

Graphite. } { |

| } {Asphaltic Anthracite.

Ash. } { |

{ " Graphite.

[NOTE.--In this diagram, the vertical line connecting the names of the

residual products (and of the derivatives of petroleum) indicates that

each succeeding one is produced by further alteration from that which

precedes it, and not independently. Also, the arrangement of the braces

is designed to show that any or all of the evolved products are given

off at each stage of alteration.]

The theory here proposed has not been evolved from my inner

consciousness, but has grown from careful study, through many years, of

facts in the field. A brief sketch of the evidence in favor of it is all

that we have space for here.

Scientific American Supplement, No. 362, December 9, 1882 · 第 35 / 57 题