Riscassi Ami, Miller Carrie, Brooks Scott
Environmental Sciences Division, Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA.
Environ Toxicol Chem. 2016 Jun;35(6):1386-400. doi: 10.1002/etc.3310. Epub 2016 Mar 31.
Sediments and floodplain soils in the East Fork Poplar Creek watershed (Oak Ridge, TN, USA) are contaminated with high levels of mercury (Hg) from an industrial source at the headwaters. Although baseflow conditions have been monitored, concentrations of Hg and methylmercury (MeHg) during high-flow storm events, when the stream is more hydrologically connected to the floodplain, have yet to be assessed. The present study evaluated baseflow and event-driven Hg and MeHg dynamics in East Fork Poplar Creek, 5 km upstream of the confluence with Poplar Creek, to determine the importance of hydrology to in-stream concentrations and downstream loads and to ascertain whether the dynamics are comparable to those of systems without an industrial Hg source. Particulate Hg and MeHg were positively correlated with discharge (r(2) = 0.64 and 0.58, respectively) and total suspended sediment (r(2) = 0.97 and 0.89, respectively), and dissolved Hg also increased with increasing flow (r(2) = 0.18) and was associated with increases in dissolved organic carbon (r(2) = 0.65), similar to the dynamics observed in uncontaminated systems. Dissolved MeHg decreased with increases in discharge (r(2) = 0.23) and was not related to dissolved organic carbon concentrations (p = 0.56), dynamics comparable to relatively uncontaminated watersheds with a small percentage of wetlands (<10%). Although stormflows exert a dominant control on particulate Hg, particulate MeHg, and dissolved Hg concentrations and loads, baseflows were associated with the highest dissolved MeHg concentration (0.38 ng/L) and represented the majority of the annual dissolved MeHg load. Environ Toxicol Chem 2016;35:1386-1400. Published 2015 Wiley Periodicals, Inc. on behalf of SETAC. This article is a US Government work, and as such, is in the public domain in the United States of America.
美国田纳西州橡树岭市白杨溪东支流域的沉积物和河漫滩土壤受到源头工业源排放的高浓度汞(Hg)污染。尽管已对基流状况进行了监测,但在高流量暴雨事件期间,当溪流与河漫滩的水文联系更为紧密时,汞和甲基汞(MeHg)的浓度尚未得到评估。本研究评估了白杨溪东支(与白杨溪汇合处上游5公里处)的基流以及事件驱动的汞和甲基汞动态,以确定水文状况对溪流中汞浓度和下游负荷的重要性,并确定这些动态是否与没有工业汞源的系统相当。颗粒态汞和甲基汞与流量呈正相关(r²分别为0.64和0.58),与总悬浮沉积物也呈正相关(r²分别为0.97和0.89),溶解态汞也随流量增加而升高(r² = 0.18),并且与溶解有机碳的增加有关(r² = 0.65),这与在未受污染系统中观察到的动态相似。溶解态甲基汞随流量增加而降低(r² = 0.23),且与溶解有机碳浓度无关(p = 0.56),这种动态与湿地比例较小(<10%)的相对未受污染的流域相当。尽管暴雨径流对颗粒态汞、颗粒态甲基汞和溶解态汞的浓度及负荷起主要控制作用,但基流与最高溶解态甲基汞浓度(0.38 ng/L)相关,且占年度溶解态甲基汞负荷的大部分。《环境毒理学与化学》2016年;35:1386 - 1400。2015年由威利期刊公司代表SETAC出版。本文为美国政府作品,因此在美国属于公共领域。