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绿色雨水基础设施将除冰盐从地表水引至地下水。

Green stormwater infrastructure redirects deicing salt from surface water to groundwater.

机构信息

Department of Engineering Systems and Environment, University of Virginia, 351 McCormick Rd., Charlottesville, VA 22904, United States.

Department of Engineering Systems and Environment, University of Virginia, 351 McCormick Rd., Charlottesville, VA 22904, United States.

出版信息

Sci Total Environ. 2020 Aug 10;729:138736. doi: 10.1016/j.scitotenv.2020.138736. Epub 2020 Apr 23.

Abstract

Winter deicing salt application has led to water quality impairment as stormwater carries salt ions (Na and Cl) through watersheds. Green infrastructure (GI) is a promising urban stormwater management practice, but its efficacy in managing salt is unknown. GI is not yet designed to remove salt, but may have potential to mitigate its loading to surface waters. Two roadside infiltration-based GI practices in Northern Virginia (bioretention and bioswale) were monitored year-round over 28 precipitation events to investigate the transport of salt through modern stormwater infrastructure. Stormwater runoff volumes and concentrations of salt ions entering and exiting each GI were monitored to determine reductions of salt ions. Both the bioretention and bioswale significantly reduced effluent surface loads of Cl and Na (76% to 82%), displaying ability to temporarily retain and infiltrate salts and delay their release to surface waters. Changes in bioretention soil chemistry revealed a small percentage of Na was stored long-term by ion exchange, but no long-term Cl storage was observed. Limited soil storage along with groundwater observations suggest the majority of salt removed from stormwater by the bioretention infiltrates into groundwater. Infiltration GI can buffer surface waters from salt, but are also an avenue for groundwater salt loading.

摘要

冬季融雪盐的使用导致了水质恶化,因为雨水将盐离子(Na 和 Cl)带入流域。绿色基础设施(GI)是一种有前途的城市雨水管理实践,但它在管理盐分方面的效果尚不清楚。GI 尚未设计用于去除盐分,但可能有潜力减轻其对地表水的负荷。弗吉尼亚北部的两种基于路边渗透的 GI 实践(生物滞留和生物沟)在 28 次降水事件中进行了全年监测,以调查盐分通过现代雨水基础设施的迁移。监测了进入和离开每个 GI 的雨水径流量和盐离子浓度,以确定盐离子的减少量。生物滞留和生物沟都显著降低了 Cl 和 Na 的出流水面负荷(76%至 82%),显示出暂时保留和渗透盐分并延迟其释放到地表水的能力。生物滞留土壤化学的变化表明,一小部分 Na 通过离子交换被长期储存,但未观察到 Cl 的长期储存。有限的土壤储存以及地下水观测表明,生物滞留从雨水去除的大部分盐分渗透到地下水中。渗透 GI 可以缓冲地表水免受盐分的影响,但也是地下水盐分负荷的途径。

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