Ch. 16: Formation of the Diamond

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FORMATION OF THE DIAMOND
139
common laws which govern other substances, and can be made volatile and fusible under certain conditions. He has demon­strated that the temperature necessary to volatilize pure carbon is about 36000 C, and that it passes into the gaseous state without liquefying, and he infers that, if sufficient pressure were applied with the high temperature, liquid carbon would be pro­duced which upon cooling would crystallize in diamonds. For this product the absence of oxygen is absolutely necessary, as the carbon would readily unite with it in the form of carbonic acid. It is a well-known fact that iron when melted dissolves carbon, and while Moissan discovered that other metals effect this dissolution, he found that iron was the best solvent.
Sir William Crookes went through the process of producing diamonds before the eyes of his audience, but was only able to show them the result of this experiment by reproducing a lantern slide of microscopical diamonds which he had made in the same way previously, for it takes a fortnight to separate them from the iron and other substances in which they are embedded. The scientific principle upon which this experiment rests, accord­ing to Sir William Crookes, is that molten iron absorbs carbon, and as iron increases in volume as it passes from the liquid to the solid state, if the outer crust of the iron is suddenly cooled and the centre remains in a liquid state, the enormous pressure caused by its expanding while cooling affords the two factors neces­sary for the crystallization of the diamond — heat and pressure.
Authorities differ somewhat as to the exact moment when molten iron expands on cooling, but it is the generally ac­cepted theory that expansion takes place at the moment of solidification. It is also a well-known fact that shrinkage or contraction takes place as the solidified metal cools. It is there­fore possible to obtain enormous pressure in the molten centre of a casting by the contraction of the outer shell which has been rapidly cooled and the expansion of the inner mass just as it begins to solidify.1
1 American Society Mechanical Engineers, Vol. XVIII, pp. 419 and 431. American Institute of Mining Engineers, Vol. XVII, 126 and 1015.
Ch. 16: Formation of the Diamond Page of 396 Ch. 16: Formation of the Diamond
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