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Trace element distribution and oil yield data from the parachute creek member of the green river formation, colorado

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Environmental Geology and Water Sciences

Abstract

The determination of trace element concentrations in oil shale before mining and retorting is required for proper solid-waste management planning. Using routine Fischer assay oil yield data collected during resource characterization as indicators of potential trace element concentrations could lead to a standard method of identifying strata containing high trace element levels. In order to determine a correlation between trace element concentrations and oil yield, shale samples were selected from four statigraphic zones of the Parachute Creek Member of the Green River Formation for analysis. All samples were analyzed for total elemental concentrations, mineralogy, and Fischer assay oil yield. The results of these analyses demonstrated that the Mahogany zone shales contain significantly greater trace element concentrations (antimony, arsenic, cadmium, chromium, copper, lead, lithium, mercury, molybdenum, nickel, selenium, silver, and vanadium) than the other three shale zones. These high trace element concentrations have been identified within well-defined interbedded tuff deposits in the Mahogany zone. In addition, all trace elements evaluated, except boron, show either increasing or decreasing concentrations as oil yield increases within all oil shale zones. With an increased number of analyses of existing oil shale cores, oil yield data will be correlated to specific stratigraphic units containing high trace element concentrations.

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  1. Division of Environmental Chemistry Western Research Institute, University of Wyoming Research Corporation, 82071, Laramie, Wyoming

    Patrick J. Sullivan & Robert C. Donovan

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  1. Patrick J. Sullivan
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  2. Robert C. Donovan
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Sullivan, P.J., Donovan, R.C. Trace element distribution and oil yield data from the parachute creek member of the green river formation, colorado. Environ. Geol. Water Sci 10, 21–31 (1987). https://doi.org/10.1007/BF02588002

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