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Trace metal distribution and mobility in drill cuttings and produced waters from Marcellus Shale gas extraction: Uranium,arsenic, barium
Institution:1. U.S. Geological Survey, Leetown Science Center, 11649 Leetown Rd., Kearneysville, WV 25430, United States;2. The Nature Conservancy, Global Lands Team, 117 E. Mountain Avenue, Suite 201, Fort Collins, CO 80524, United States;3. Nicholas Institute for Environmental Policy Solutions at Duke University, 2111 Campus Drive, Durham, NC 27708, United States;4. Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin, 10100 Burnet Road, Building 130, Austin, TX 78758, United States;5. Department of Biology, University of Central Arkansas, 201 Donaghey Avenue, Conway, AR 72035, United States;6. The Nature Conservancy, 1101 West River Parkway, Suite 200, Minneapolis, MN 55415, United States;7. Environmental Policy Initiative, Harvard Law School, #4123 Wasserstein Hall, Cambridge, MA 02138, United States;8. Department of Civil, Environmental and Architectural Engineering, University of Colorado Boulder, UCB 607, Boulder, CO 80309, United States;9. The Nature Conservancy, Africa Program, 820G Rieveschl Hall, Cincinnati, OH 45221, United States;10. School of Forestry and Environmental Studies, Yale University, 195 Prospect St., New Haven, CT 06511, United States;11. Florida State University College of Law, 425 W. Jefferson Street, Tallahassee, FL 32306, United States
Abstract:Development of unconventional shale gas wells can generate significant quantities of drilling waste, including trace metal-rich black shale from the lateral portion of the drillhole. We carried out sequential extractions on 15 samples of dry-drilled cuttings and core material from the gas-producing Middle Devonian Marcellus Shale and surrounding units to identify the host phases and evaluate the mobility of selected trace elements during cuttings disposal. Maximum whole rock concentrations of uranium (U), arsenic (As), and barium (Ba) were 47, 90, and 3333 mg kg?1, respectively. Sequential chemical extractions suggest that although silicate minerals are the primary host for U, as much as 20% can be present in carbonate minerals. Up to 74% of the Ba in shale was extracted from exchangeable sites in the shale, while As is primarily associated with organic matter and sulfide minerals that could be mobilized by oxidation. For comparison, U and As concentrations were also measured in 43 produced water samples returned from Marcellus Shale gas wells. Low U concentrations in produced water (<0.084–3.26 μg L?1) are consistent with low-oxygen conditions in the wellbore, in which U would be in its reduced, immobile form. Arsenic was below detection in all produced water samples, which is also consistent with reducing conditions in the wellbore minimizing oxidation of As-bearing sulfide minerals.Geochemical modeling to determine mobility under surface storage and disposal conditions indicates that oxidation and/or dissolution of U-bearing minerals in drill cuttings would likely be followed by immobilization of U in secondary minerals such as schoepite, uranophane, and soddyite, or uraninite as conditions become more reducing. Oxidative dissolution of arsenic containing sulfides could release soluble As in arsenate form under oxic acidic conditions. The degree to which the As is subsequently immobilized depends on the redox conditions along the landfill flow path. The results suggest that proper management of drill cuttings can minimize mobilization of these metals by monitoring and controlling Eh, pH and dissolved constituents in landfill leachates.
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