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Detecting the effects of coal mining,acid rain,and natural gas extraction in Appalachian basin streams in Pennsylvania (USA) through analysis of barium and sulfate concentrations
Authors:Niu  Xianzeng  Wendt  Anna  Li  Zhenhui  Agarwal  Amal  Xue  Lingzhou  Gonzales  Matthew  Brantley  Susan L
Institution:1.Earth and Environmental Systems Institute, Penn State University, EES Building, 2217, University Park, PA, 16802, USA
;2.College of Information Sciences and Technology, Penn State University, University Park, PA, 16802, USA
;3.Department of Statistics, Penn State University, University Park, PA, 16802, USA
;
Abstract:

To understand how extraction of different energy sources impacts water resources requires assessment of how water chemistry has changed in comparison with the background values of pristine streams. With such understanding, we can develop better water quality standards and ecological interpretations. However, determination of pristine background chemistry is difficult in areas with heavy human impact. To learn to do this, we compiled a master dataset of sulfate and barium concentrations (SO4], Ba]) in Pennsylvania (PA, USA) streams from publically available sources. These elements were chosen because they can represent contamination related to oil/gas and coal, respectively. We applied changepoint analysis (i.e., likelihood ratio test) to identify pristine streams, which we defined as streams with a low variability in concentrations as measured over years. From these pristine streams, we estimated the baseline concentrations for major bedrock types in PA. Overall, we found that 48,471 data values are available for SO4] from 1904 to 2014 and 3243 data for Ba] from 1963 to 2014. Statewide SO4] baseline was estimated to be 15.8 ± 9.6 mg/L, but values range from 12.4 to 26.7 mg/L for different bedrock types. The statewide Ba] baseline is 27.7 ± 10.6 µg/L and values range from 25.8 to 38.7 µg/L. Results show that most increases in SO4] from the baseline occurred in areas with intensive coal mining activities, confirming previous studies. Sulfate inputs from acid rain were also documented. Slight increases in Ba] since 2007 and higher Ba] in areas with higher densities of gas wells when compared to other areas could document impacts from shale gas development, the prevalence of basin brines, or decreases in acid rain and its coupled effects on Ba] related to barite solubility. The largest impacts on PA stream Ba] and SO4] are related to releases from coal mining or burning rather than oil and gas development.

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