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Characterization of mineral matter in East Texas lignites

Technical Report ·
OSTI ID:5573778
The purpose of this project is to characterize the mineral matter in Texas lignites and in their ashes. Low temperature ashing is a practical way to burn the coal in order to separate the mineral matter in the form of low temperature ash (LTA) without any serious alterations. Twenty-seven LTA samples have been selected from four lignite cores drilled in Shelby, Nacogdoches, Panola, and Rusk Counties in East Texas from the Sabine Uplift, Wilcox Group. The mineral matter in these LTA samples have been studied with x-ray diffraction (XRD) and with analytical electron microscopy (AEM). Quartz, bassanite, kaolinite and halloysite are the main mineral components in these lignites. Pyrite, illite, smectite, chlorite, barite, and feldspars generally occur in small quantities. The silica phase consists mostly of authigenic microquartz and of some detrital quartz. Following the determination of the mineral phases, we searched for the particles carrying hazardous elements such as As, Cd, Cr, Co, Pb, Hg, Mn, Mo, Ni, Se, V, Ag, Zn, Ti, U and Th. Particulate matter with high concentration of selenium and lead is found and it has been identified as a Pb-Se compound known as clausthalite. Similarly, particles with high Pb-Sn content are found in the form of spherules of about 300 A in size. Manganese is found in association with iron oxides occurring in the form of minute spherules of 200 A. A mineral particle with high Zr and Si concentration is identified as zircon. Titanium-rich particles consist of needle-like crystals of rutile (or anatase) in the coal. 28 figures, 10 tables.
Research Organization:
Texas Tech Univ., Lubbock (USA). Dept. of Geosciences
OSTI ID:
5573778
Report Number(s):
TENRAC/EDF-103; ON: DE84900412
Country of Publication:
United States
Language:
English

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