Earth and Environmental Systems Institute, Penn State University, EES Building, 2217, University Park, PA, 16802, USA.
College of Information Sciences and Technology, Penn State University, University Park, PA, 16802, USA.
Environ Geochem Health. 2018 Apr;40(2):865-885. doi: 10.1007/s10653-017-0031-6. Epub 2017 Oct 13.
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 ([SO], [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 [SO] from 1904 to 2014 and 3243 data for [Ba] from 1963 to 2014. Statewide [SO] 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 [SO] 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 [SO] are related to releases from coal mining or burning rather than oil and gas development.
要了解不同能源的提取如何影响水资源,需要评估与原始溪流的背景值相比,水化学发生了怎样的变化。有了这样的认识,我们就能制定更好的水质标准和生态解释。然而,在人类活动影响严重的地区,确定原始背景化学性质是很困难的。为了学会这一点,我们从公开来源汇编了宾夕法尼亚州(美国)溪流中硫酸盐和钡浓度([SO],[Ba])的主数据集。选择这两种元素是因为它们可以分别代表与石油/天然气和煤炭有关的污染。我们应用了变化点分析(即似然比检验)来识别原始溪流,我们将其定义为多年来浓度变化较小的溪流。从这些原始溪流中,我们估计了宾夕法尼亚州主要基岩类型的基线浓度。总的来说,我们发现 1904 年至 2014 年有 48471 个[SO]数据值,1963 年至 2014 年有 3243 个[Ba]数据值。全州[SO]基线估计为 15.8±9.6mg/L,但不同基岩类型的范围为 12.4 至 26.7mg/L。全州[Ba]基线为 27.7±10.6µg/L,范围为 25.8 至 38.7µg/L。结果表明,大多数[SO]超过基线值的情况都发生在煤炭开采活动密集的地区,这证实了以前的研究。酸雨引起的硫酸盐输入也有记录。自 2007 年以来,[Ba]略有增加,与其他地区相比,天然气井密度较高的地区[Ba]较高,这可能记录了页岩气开发的影响、盆地卤水的流行,或酸雨及其对与重晶石溶解度相关的[Ba]的耦合效应的减少。对宾夕法尼亚州溪流[Ba]和[SO]影响最大的是煤炭开采或燃烧的排放,而不是石油和天然气的开发。