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多组分重质非水相液体对地下水污染的控制现场试验:溶解羽流阻滞作用

A controlled field experiment on groundwater contamination by a multicomponent DNAPL: dissolved-plume retardation.

作者信息

Rivett Michael O, Allen-King Richelle M

机构信息

Earth Sciences, School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK.

出版信息

J Contam Hydrol. 2003 Oct;66(1-2):117-46. doi: 10.1016/S0169-7722(03)00006-8.

Abstract

A natural gradient emplaced-source (ES) controlled field experiment was conducted at the Borden aquifer research site, Ontario, to study the transport of dissolved plumes emanating from residual dense nonaqueous-phase liquid (DNAPL) source zones. The specific objective of the work presented here is to determine the effects of solute and co-solute concentrations on sorption and retardation of dissolved chlorinated solvent-contaminant plumes. The ES field experiment comprised a controlled emplacement of a residual multicomponent DNAPL below the groundwater table and intensive monitoring of dissolved-phase plumes of trichloromethane (TCM), trichloroethylene (TCE), and perchloroethylene (PCE) plumes continuously generated in the aquifer down gradient from gradual source dissolution. Estimates of plume retardation (and dispersion) were obtained from 3-D numerical simulations that incorporated transient source input and flow regimes monitored during the test. PCE, the most retarded solute, surprisingly exhibited a retardation factor approximately 3 times lower than observed in a previous Borden tracer test by Mackay et al. [Water Resour. Res. 22 (1986) 2017] conducted approximately 150 m away. Also, an absence of temporal trend in PCE retardation contrasted with the previous Borden test. Supporting laboratory studies on ES site core indicated that sorption was nonlinear and competitive, i.e. reduced sorption of PCE was observed in the presence of TCE. Consideration of the effects of relatively high co-solute (TCE) concentration (competitive sorption) in addition to PCE concentration effects (nonlinear sorption) was necessary to yield laboratory-based PCE retardation estimates consistent with the field plume values. Concentration- and co-solute-based sorption and retardation analysis was also applied to the previous low-concentration pulse injection test of Mackay et al. [Water Resour. Res. 22 (1986) 2017] and was able to successfully predict the temporal field retardation trends observed in that test. While it is acknowledged that other "nonideal transport" effects may contribute, our analysis predicts differences in the PCE retardation magnitude and trend between the two experiments that are consistent with field observations based on the marked solute concentration differences that resulted from contrasting source conditions. Solute and co-solute concentration effects have heretofore received little attention, but may have wide significance in aquifers contaminated by point-source pollutants because many plumes contain mixed solutes over wide concentration ranges in strata that are likely subject to nonlinear sorption.

摘要

在安大略省的博登含水层研究地点进行了一次天然梯度注入源(ES)控制场实验,以研究源自残留重质非水相液体(DNAPL)源区的溶解羽状物的迁移。本文所述工作的具体目标是确定溶质和共溶质浓度对溶解的氯化溶剂污染物羽状物吸附和阻滞的影响。ES场实验包括在地下水位以下控制注入残留的多组分DNAPL,并对含水层中因源逐渐溶解而在下游持续产生的三氯甲烷(TCM)、三氯乙烯(TCE)和全氯乙烯(PCE)溶解相羽状物进行密集监测。羽状物阻滞(和弥散)的估计值来自三维数值模拟,该模拟纳入了测试期间监测到的瞬态源输入和水流状态。PCE是阻滞作用最强的溶质,令人惊讶的是,其阻滞因子比麦凯等人[《水资源研究》22(1986)2017]在约150米外进行的前一次博登示踪剂测试中观察到的低约3倍。此外,PCE阻滞作用不存在时间趋势,这与前一次博登测试形成对比。对ES场地岩心的支持性实验室研究表明,吸附是非线性且具有竞争性的,即在TCE存在的情况下,观察到PCE的吸附减少。除了PCE浓度效应(非线性吸附)外,考虑相对较高的共溶质(TCE)浓度(竞争性吸附)的影响对于得出与现场羽状物值一致的基于实验室的PCE阻滞估计值是必要的。基于浓度和共溶质的吸附和阻滞分析也应用于麦凯等人[《水资源研究》22(1986)2017]之前的低浓度脉冲注入测试,并能够成功预测该测试中观察到的现场阻滞时间趋势。虽然承认其他“非理想迁移”效应可能起作用,但我们的分析预测了两个实验之间PCE阻滞幅度和趋势的差异,这与基于对比源条件导致的显著溶质浓度差异的现场观测结果一致。溶质和共溶质浓度效应迄今为止很少受到关注,但在受点源污染物污染的含水层中可能具有广泛意义,因为许多羽状物在可能存在非线性吸附的地层中含有浓度范围广泛的混合溶质。

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