Mineralogy in the Waste Isolation Pilot Plant (WIPP) facility stratigraphic horizon
Author(s) -
Carol L. Stein
Publication year - 1985
Language(s) - English
Resource type - Reports
DOI - 10.2172/5203761
Subject(s) - halite , anhydrite , geology , mineralogy , gypsum , evaporite , geochemistry , horizon , sedimentary rock , geometry , paleontology , mathematics
Forty-six samples were selected for this study from two cores, one extending 50 ft up through the roof of the WIPP facility and the other penetrating 50 ft below the facility floor. These samples, selected from approximately every other foot of core length, represent the major lithologies present in the immediate vicinity of the WIPP facility horizon: ''clean'' halite, polyhalitic halite, argillaceous halite, and mixed polyhalitic-argillaceous halite. Samples were analyzed for non-NaCl mineralogy by determining weight percents of water- and EDTA-insoluble residues, which were then identified by x-ray diffraction. In general, WIPP halite contains at most 5 wt % non-NaCl residue. The major mineral constituents are quartz, magnesite, anhydrite, gypsum, polyhalite, and clays. Results of this study confirm that, in previous descriptions of WIPP core, trace mineral quantities have been visually overestimated by approximately an order of magnitude. 9 refs., 5 figs., 5 tabs.
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