27 research outputs found

    A mineralogical study of the Harmon lignite bed, Bullion Creek Formation (Paleocene), Bowman County, North Dakota

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    Study of the Harmon lignite bed at the Gascoyne Mine in Bowman County, North Dakota showed that most of the minerals in the coal lithobodies were detrital in origin and that variable ash deposition during combustion may be caused by variations in types and quantities of mineral phases. The Harmon bed is part of the Bullion Creek Formation (Paleocene). Objectives of this study included: to develop scanning electron microscope/microprobe techniques for the study of minerals in coal; to determine the origins of the mineral phases; to postulate a depositional environment for the Harmon lignite; and to ascertain whether variable ash deposition behavior of the Gascoyne lignite is related to mineral content. Scanning electron microscopy and electron microprobe analysis was used to identify and determine the abundance of minerals in the lignite. The average mineral content in weight percent was 44% quartz, 31% illite, 13% kaolinite, 5% montmorillonite, 5% pyrite, and 2% gypsum. The amount of mineral matter as discrete phases, not organically bound inorganic constituents, varied directly with total ash. The Blue Pit has a higher inorganic content than the White Pit because of a greater amount of quartz and clays in the B seam. This result demonstrates the lateral variability in inorganic content in the Gascoyne lignite. Minerals also varied in vertical distribution. Quartz and clay minerals were more abundant in lithologic layers that were adjacent to clay silt partings, overburden, and underclay. Quartz, illite, and kaolinite are primarily detrital in origin. Framboidal pyrite and possibly some kaolinite and phosphate minerals formed authigenically during early peat stages. Massive pyrite, gypsum, barite, celestite, siderite, and jarosite were probably epigenetic products which formed after seam compaction and coalification. The present mineral content of the Harmon lignite is probably the result of the characteristics of the depositional environment. Authigenic processes during early peat stages or after compaction and coalification had a minor influence on the current mineral content. The Harmon lignite was probably deposited as part of a lacustrine depositional environment. Periodic transgression and regression of the freshwater body would explain best the types of minerals observed and their distributions. Variations in ash deposition behavior within the Gascoyne Mine may be caused by the variation in types and quantities of discrete mineral phases

    Advanced SEM Techniques to Characterize Coal Minerals

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    Research at the University of North Dakota Energy and Environmental Research Center (EERC) has focused on methods to characterize the inorganic components in coals. Because the scanning electron microscope and electron probe microanalysis system (SEM/EPMA) provide both morphologic and chemical information, the SEM/EPMA system is well-suited to the characterization of discrete minerals in coal. Computer-controlled scanning electron microscopy (CCSEM), along with simultaneous automated digital image collection, is one means of gaining more detailed insight into coal mineralogy. Computer-stored images of coal surfaces already analyzed for minerals using CCSEM can be reanalyzed to discern mineral morphologies and coal-to-mineral associations. Limitations may exist when using just CCSEM to characterize chemically and physically complex clay minerals without complimentary data on the association of the minerals to the coal organic matrix. Mineralogic investigations of San Miguel and Beulah lignites and Upper Freeport bituminous coal using CCSEM and automated digital image collection are given with a particular reference to the clay minerals present. Total mineral quantities generated for the three coals were in good agreement with total ash content, provided that organically bound constituents were taken into account for the lignites. Classification of the more complex aluminosilicate minerals was aided by the use of distribution plots of Si/Al ratios and concentrations of ion exchangeable cations derived from the CCSEM analysis. Morphologic analysis of stored SEM images proved to be helpful in characterizing kaolinite group minerals

    EERC Center for Biomass Utilization 2006

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    The Center for Biomass Utilization (CBUî) 2006 project at the Energy & Environmental Research Center (EERC) consisted of three tasks related to applied fundamental research focused on converting biomass feedstocks to energy, liquid transportation fuels, and chemicals. Task 1, entitled Thermochemical Conversion of Biomass to Syngas and Chemical Feedstocks, involved three activities. Task 2, entitled Crop Oil Biorefinery Process Development, involved four activities. Task 3, entitled Management, Education, and Outreach, focused on overall project management and providing educational outreach related to biomass technologies through workshops and conferences

    Task 3.0 - Advanced Power Systems Subtask 3.18 - Ash Behavior in Power Systems

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    Ash behavior in power systems can have a significant impact on the design and performance of advanced power systems. The Energy & Environmental Research Center (EERC) has focused significant effort on ash behavior in conventional power systems that can be applied to advanced power systems. This initiative focuses on filling gaps in the understanding of fundamental mechanisms of ash behavior that has relevance to commercial application and marketable products. This program develops methods and means to better understand and mitigate adverse coal ash behavior in power systems and can act to relieve the U.S. reliance on diminishing recoverable oil resources, especially those resources that are not domestically available and are fairly uncertain
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