Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1754231 | International Journal of Coal Geology | 2007 | 23 Pages |
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.
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Authors
Ashok K. Singh, Mahendra P. Singh, Mamta Sharma, Sunil K. Srivastava,