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-------+ Water in coal. The amount of water present in freshly raised coals varies very considerably. It is generally largest in lignites, which may sometimes contain 30% or even more, while in the coals of the coal measures it does not usually exceed from 5 to 10%. The loss of weight by exposure to the atmosphere from drying may be from 1/2 to 3/4 of the total amount of water contained. TABLE III.--_Composition of Fuels (assuming Carbon = 100)._ +------------------------------+-------+---------+---------+-----------+ | | | | |Disposable | | |Carbon.|Hydrogen.| Oxygen. | Hydrogen. | +------------------------------+-------+---------+---------+-----------+ | Wood | 100 | 12.18 | 83.07 | 1.80 | | Peat | 100 | 9.85 | 55.67 | 2.89 | | Lignite | 100 | 8.37 | 42.42 | 3.07 | | Thick Coal, S. Staffordshire | 100 | 6.12 | 21.23 | 3.47 | | Hartley Steam Coal | 100 | 5.91 | 18.32 | 3.62 | | South Wales Steam Coal | 100 | 4.75 | 5.28 | 4.09 | | American Anthracite | 100 | 2.84 | 1.74 | 2.63 | +------------------------------+-------+---------+---------+-----------+ Origin of Coal. Coal is the result of the transformation of woody fibre and other vegetable matter by the elimination of oxygen and hydrogen in proportionally larger quantity than carbon, so that the percentage of the latter element is increased in the manner shown in Table III., given by J. Percy, the mineral matter being also changed by the removal of silica and alkalis and the substitution of substances analogous in composition to fire-clay. The causes and methods of these changes are, however, not very exactly defined. According to the elaborate researches of B. Renault (_Bulletin de la Societe de l'Industrie minerale_, 3 ser. vol. xiii. p. 865), the agents of the transformation of cellulose into peaty substances are saprophytic fungi and bacterial ferments. As the former are only active in the air while the latter are anaerobic, the activity of either agent is conditioned by variation in the water level of the bog. The ultimate term of bacterial activity seems to be the production of ulmic acid, containing carbon 65.31 and hydrogen 3.85%, which is a powerful antiseptic
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