Hardgrove grindability study of Powder River Basin and Appalachian coal components in a Midwestern power station blend

摘要

Five coals blended at a Midwestern United States power station were subjected to detailed analysis of their Hardgrove grindability. The coals, representing four distinct coal beds, are a low-sulfur, high-volatile A bituminous Upper Elkhorn No.3 coal (Pike County, Kentucky); a medium-sulfur, high-volatile A bituminous Pittsburgh coal (southwestern Pennsylvania); a low-sulfur, subbituminous coal from the northern powder river basin (Montana); and two low-sulfur, subbituminous Wyodak coals from two different mines located in the eastern Powder River Basin (Campbell County, Wyoming). All samples that were processed in the Hardgrove grindability tests were also analyzed for their maceral and microlithotype content.The high-vitrinite Pittsburgh coal and the relatively petrographically complex Upper Elkhorn No.3 coal exhibited different grindability behavior. The petrographic compositions of the Pittsburgh raw feed, the 16 x 30-mesh fraction(HGI test fraction) and the -30-mesh fraction (HGI test Ct) are similar, suggesting that the HGI test fraction 'es the whole feed. The eastern Kentucky test sample is as representative of the whole feed, with the HGI test lion having lower vitrinite amounts than the rejected -30-fraction. The Powder River Basin coals are high in vitrinite content and show behavior similar to the Pittsburgh