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利用高分辨率质谱法评估工程渗流带中新兴有机污染物的去除。

Evaluating emerging organic contaminant removal in an engineered hyporheic zone using high resolution mass spectrometry.

机构信息

Interdisciplinary Arts and Science, University of Washington Tacoma, Tacoma, WA, 98421, USA; Center for Urban Waters, Tacoma, WA, 98421, USA.

Department of Civil and Environmental Engineering, Colorado School of Mines, Golden, CO, 80401, USA.

出版信息

Water Res. 2019 Mar 1;150:140-152. doi: 10.1016/j.watres.2018.11.050. Epub 2018 Nov 23.

Abstract

The hyporheic zone (HZ), located at the interface of surface and groundwater, is a natural bioreactor for attenuation of chemical contaminants. Engineered HZs can be incorporated into stream restoration projects to enhance hyporheic exchange, with flowpaths optimized to promote biological habitat, water quantity, and water quality improvements. Designing HZs for in-stream treatment of stormwater, a significant source of flow and contaminant loads to urban creeks, requires assessment of both the hydrology and biogeochemical capacity for water quality improvement. Here, we applied tracer tests and high resolution mass spectrometry (HRMS) to characterize an engineered hyporheic zone unit process, called a hyporheic design element (HDE), in the Thornton Creek Watershed in Seattle, WA. Dye, NaCl, and bromide were used to hydrologically link downwelling and upwelling zones and estimate the hydraulic retention time (HRT) of hyporheic flowpaths. We then compared water quality improvements across hydrologically-linked surface and hyporheic flowpaths (3-5 m length; ∼30 min to >3 h) during baseflow and stormflow conditions. We evaluated fate outcomes for 83 identified contaminants during stormflow, including those correlated with an urban runoff mortality syndrome in coho salmon. Non-target HRMS analysis was used to assess holistic water quality improvements and evaluate attenuation mechanisms. The data indicated substantial water quality improvement in hyporheic flowpaths relative to surface flow and improved contaminant removal with longer hyporheic HRT (for ∼1900 non-target compounds detected during stormflow, <17% were attenuated >50% via surface flow vs. 59% and 78% via short and long hyporheic residence times, respectively), and strong contributions of hydrophobic sorption towards observed contaminant attenuation.

摘要

位于地表水和地下水交界处的地下河流域(HZ)是化学污染物衰减的天然生物反应器。人工地下河流域可以纳入溪流恢复项目中,以增强地下河流域的交换,优化水流路径以促进生物栖息地、水量和水质改善。设计用于处理城市溪流中雨水的地下河流域,这是流量和污染物负荷的重要来源,需要评估水文和生物地球化学改善水质的能力。在这里,我们应用示踪剂测试和高分辨率质谱(HRMS)来描述一个工程化的地下河流域单元过程,称为地下河流域设计元素(HDE),该过程位于西雅图的桑顿溪流域。使用染料、NaCl 和溴化物来在下降区和上升区之间进行水文链接,并估计地下水流路径的水力停留时间(HRT)。然后,我们比较了基流和暴流条件下地下和地表水流路径(3-5m 长度;约 30 分钟至>3 小时)的水质改善情况。我们评估了暴流期间 83 种已识别污染物的命运结果,包括与银鲑鱼城市径流死亡率综合征相关的污染物。非靶向 HRMS 分析用于评估整体水质改善情况并评估衰减机制。数据表明,地下水流路径相对于地表水流具有较大的水质改善,并且随着地下河流域 HRT 的延长,去除效果更好(在暴流期间检测到的约 1900 种非目标化合物中,<17%通过地表流被衰减>50%,而通过短和长地下停留时间分别为 59%和 78%),并且疏水性吸附对观察到的污染物衰减有很大的贡献。

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