International Journal of Coal Geology, Vol.38, No.3, 261-284, 1999
Influence of environments of coal deposition on phosphorous accumulation in a high latitude, northern Alaska, coal seam
Although phosphorus is a very important biogenic element, its concentration in coal is generally low. Phosphorus (P) concentrations typically range from 0.001% to 0.229% in raw coals of the contiguous 48 states [Glick, D.C., Davis, A., 1984. Variability in the inorganic content of United States coals-a multivariate statistical study of final report, Part 10 (DOE-30013-Flo) to the US Dept. of Energy under contract no. DE-AC22-80PC 30013, 404 pp.]. Some Alaskan coal seams contain horizons that are unusually high in phosphorus. The present paper focuses on a bituminous coal from northern Alaska, where 0.15 m subsections of this coal seam have shown high phosphorous in certain subsections. In order to investigate the lateral extent of such high phosphorous bands in coal, the authors obtained three drill cores up to 3 gm apart from the coal seam. A detailed investigation of the cores was undertaken to determine the nature and mode of occurrence of phosphorous minerals. Maceral composition allowed interpretation of environments of coal deposition. Acid-extractable phosphorous analysis of the subsections identified the high phosphorous horizons. Electron microprobe analyses identified the phosphorous mineral as crandallite. Correlation of high phosphorous intervals with corresponding environments of deposition suggests that phosphorous precipitation is promoted by an oxidizing environment with a lowered water table during the peat stage. A study of thin sections from high phosphorous samples showed that crandallite is associated with structured vitrinite and as cell fillings in fusinite. The study confirms the potential for using high phosphorous horizons for the correlation of coal seams, as noted in previous work by the authors (Rao and Walsh, 1997). A high phosphorous horizon is found at 0.45 m above the bottom of the seam in all of the drill holes, indicating a uniformity of the coal forming environment and the availability of crandallite constituent elements over the entire 3 km. The uniformity of high phosphorous concentrations through the top 2 m of the three drill holes also shows a distinct correlation.