Article ID Journal Published Year Pages File Type
1754231 International Journal of Coal Geology 2007 23 Pages PDF
Abstract
It has been concluded that, barring the effect of pressure, the changes due to heat effect on coking coals, whether in situ or laboratory carbonization, are almost similar. Organic and inorganic constituents undergoing changes at a particular temperature are nearly similar in both conditions. In case of pronounced overburden pressure, flow structures develop in the natural coke groundmass. Higher reflectance and very strong anisotropy, as evidenced in completely baked coking coals with fine to very coarse mosaic structures, may be a good criterion to explore these heat altered coals for the carbon artifact industry and further efforts are required to be made in this line.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
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