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Calcite-rich bituminous coal

Figure 3. XANES of calcite-rich bituminous coal (A), the Fust seam lignite (B), and calcium acetate (C). Figure 3. XANES of calcite-rich bituminous coal (A), the Fust seam lignite (B), and calcium acetate (C).
Rasa coal is exceptional because of its high sulfur content, most of which appears to be organic sulfur. The high organic sulfur content is characteristic of marine-influenced bituminous coals. Rasa coal appears to have been formed in a high-pH marine environment where bacteria thrived. This hypothesis is supported by the presence of substantial amounts of both calcite and dolomite in Rasa coal. The calcium- and magnesium-rich environment where Rasa coal formed is expected to have been alkaline. The... [Pg.271]


See other pages where Calcite-rich bituminous coal is mentioned: [Pg.170]    [Pg.170]    [Pg.161]    [Pg.166]    [Pg.166]   


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