Published February 1, 2017 | Version v1
Journal article

Environmental signatures and effects of an oil and gas wastewater spill in the Williston Basin, North Dakota

  • 1. U.S. Geological Survey, National Research Program, Reston, VA 20192 (United States)
  • 2. U.S. Geological Survey, National Research Program, Menlo Park, CA 94025 (United States)
  • 3. U.S. Geological Survey, Eastern Energy Resources Science Center, Reston, VA 20192 (United States)
  • 4. U.S. Geological Survey, Columbia Environmental Research Center, Jackson Field Research Station, Jackson, WY 83001 (United States)
  • 5. Department of Obstetrics, Gynecology and Women's Health, University of Missouri, Columbia, MO 65211 (United States)
  • 6. U.S. Geological Survey, Leetown Science Center, Kearneysville, WV 25430 (United States)
  • 7. U.S. Geological Survey, North Dakota Water Science Center, Bismarck, ND 58503 (United States)

Description

Wastewaters from oil and gas development pose largely unknown risks to environmental resources. In January 2015, 11.4 M L (million liters) of wastewater (300 g/L TDS) from oil production in the Williston Basin was reported to have leaked from a pipeline, spilling into Blacktail Creek, North Dakota. Geochemical and biological samples were collected in February and June 2015 to identify geochemical signatures of spilled wastewaters as well as biological responses along a 44-km river reach. February water samples had elevated chloride (1030 mg/L) and bromide (7.8 mg/L) downstream from the spill, compared to upstream levels (11 mg/L and < 0.4 mg/L, respectively). Lithium (0.25 mg/L), boron (1.75 mg/L) and strontium (7.1 mg/L) were present downstream at 5–10 times upstream concentrations. Light hydrocarbon measurements indicated a persistent thermogenic source of methane in the stream. Semi-volatile hydrocarbons indicative of oil were not detected in filtered samples but low levels, including tetramethylbenzenes and di-methylnaphthalenes, were detected in unfiltered water samples downstream from the spill. Labile sediment-bound barium and strontium concentrations (June 2015) were higher downstream from the Spill Site. Radium activities in sediment downstream from the Spill Site were up to 15 times the upstream activities and, combined with Sr isotope ratios, suggest contributions from the pipeline fluid and support the conclusion that elevated concentrations in Blacktail Creek water are from the leaking pipeline. Results from June 2015 demonstrate the persistence of wastewater effects in Blacktail Creek several months after remediation efforts started. Aquatic health effects were observed in June 2015; fish bioassays showed only 2.5% survival at 7.1 km downstream from the spill compared to 89% at the upstream reference site. Additional potential biological impacts were indicated by estrogenic inhibition in downstream waters. Our findings demonstrate that environmental signatures from wastewater spills are persistent and create the potential for long-term environmental health effects. - Highlights: • UOG wastewater (> 11 million liters) spilled into Blacktail Creek, ND in January 2015. • Elevated Na, Cl, Br, Sr, B, Li, NH4, and hydrocarbons were detected in creek waters. • Geochemical baseline deviations persist months after remediation efforts started. • B and Sr concentrations, and Ra activities were up to 15 times background in sediment downstream. • Biological impacts include reduced fish survival and estrogenic inhibition downstream.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2016.11.157

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2016.11.157;
PII
S0048-9697(16)32620-1;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
579
Journal Page Range
p. 1781-1793
ISSN
0048-9697
CODEN
STENDL

Optional Information

Copyright
Copyright (c) 2016 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.