Abstract
The petrographic composition of sized coal produced through the progressive grinding of a Central Appalachian high-volatile bituminous coal blend was analyzed for multiple sets either by removing fine, −200-mesh, coal after each test iteration or by retaining the fine coal in progressive test fractions. With prolonged grinding, coarser fractions tend to become depleted in vitrinite and vitrinite-rich microlithotypes, leading to progressively harder-to-grind coal remaining in the oversize, +200-mesh, fractions. The latter trend is shown both by the maceral and microlithotype composition of the coal and by the increased slope and fractal dimension of size-frequency distribution, implying an increase in hardness and resistance to grinding of the oversize coal.
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Trimble, A.S., Hower, J.C. Maceral/microlithotype analysis of the progressive grinding of a Central Appalachian high-volatile bituminous coal blend. Mining, Metallurgy & Exploration 17, 234–243 (2000). https://doi.org/10.1007/BF03403240
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DOI: https://doi.org/10.1007/BF03403240