含水层中有机化合物缓凝系数的测定方法

M. Maraqa
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引用次数: 0

摘要

吸附是影响有机化合物在地下环境中迁移的重要机制。被吸附的化合物的移动速度比地下水慢,导致它们的移动迟缓。准确测定含水层中有机化合物的阻滞系数(R)对于了解其运动、命运和修复至关重要。包括预测工具、实验室实验和现场实验在内的几种方法已被用于确定吸附相关的延迟。本文的目的是回顾和比较不同的方法用于测定有机化合物的R,重点是预测和实验室为基础的方法。预测工具基于定量结构-活性关系(qsar)的使用。实验室方法使用不同类型的反应器,包括间歇式,搅拌流,循环通过塔,或混相置换通过填充塔。此外,用不同的方法分析柱法的数据以确定r。不同方法或不同分析方法的结果之间的差异已被报道。这就造成了这些方法或所用分析方法的适用性的不确定性。本文强调了观察到的差异的可能原因,并确定了所使用的方法和分析方法的局限性和适当性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Methods of Determining Retardation Coefficients of Organic Compounds in Aquifers
Sorption is an important mechanism that affects the mobility of organic compounds in the subsurface environment. Sorbed compounds move slower than that of groundwater, causing retardation in their movement. Accurate determination of retardation coefficients (R) of organic compounds in aquifers is critical for understanding their movement, fate, and remediation. Several methods, including predictive tools, laboratory experiments, and field experiments have been utilized for determining sorption-related retardation. The objective of this paper was to review and compare between the different methods used for the determination of R of organic compounds, with emphasis on predictiveand laboratory-based approaches. Predictive tools are based on the use of quantitative structure-activity relationships (QSARs). Laboratory methods utilize different types of reactors including batch, stirred-flow, circulationthrough-column, or miscible displacement through packed columns. In addition, data from the column method have been analyzed in various ways to determine R. Discrepancies between results from different methods or from different analysis approaches have been reported. This create uncertainty about the suitability of some of these methods or the used analysis approaches. This paper highlights the possible causes for the observed discrepancy and establishes the limitations and appropriateness of the used methods and analysis approaches.
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