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有机污染物的溶解度归一化联合吸附-分配吸附等温线

Solubility-normalized combined adsorption-partitioning sorption isotherms for organic pollutants.

作者信息

Kleineidam Sybille, Schüth Christoph, Grathwohl Peter

机构信息

Center for Applied Geoscience, University of Tübingen, Germany.

出版信息

Environ Sci Technol. 2002 Nov 1;36(21):4689-97. doi: 10.1021/es010293b.

Abstract

Equilibrium sorption isotherms were measured for five different low-polarity organic compounds (benzene, trichloroethene, 1,2- and 1,4-dichlorobenzene, and phenanthrene) over a wide concentration range. The investigated sorbents can be grouped into the following three classes: (1) humic soil organic matter, which shows linear sorption isotherms (solely partitioning, as observed in the peat sample); (2) carbon materials, which were thermally altered (due to their natural history or industrial production) and thus contain a high specific surface area and exhibit nonlinear isotherms, and (3) pure engineered microporous materials (e.g., zeolites and activated carbon), where adsorption is solely due to a pore-filling process. Sorption of all compounds was fitted very well by the Polanyi-Dubinin-Manes (PDM) model, which for sorbents containing humic organic matter (e.g., peat) was combined with linear partitioning. Both the partitioning and the Polanyi-Dubinin-Manes model predict unique sorption isotherms of similar compounds if the solubility-normalized aqueous concentration is used. In addition, an inverse linear relationship between the distribution coefficient (Kd) and water solubility, which was very well confirmed by the data, is obtained. This also leads to unit-equivalent Freundlich sorption isotherms and explains the often observed apparent correlation between sorption capacity at a given concentration (e.g., Freundlich coefficient) and sorption nonlinearity (Freundlich exponent).

摘要

在很宽的浓度范围内,对五种不同的低极性有机化合物(苯、三氯乙烯、1,2 - 二氯苯、1,4 - 二氯苯和菲)测量了平衡吸附等温线。所研究的吸附剂可分为以下三类:(1)腐殖质土壤有机物,其呈现线性吸附等温线(如泥炭样品中观察到的仅为分配作用);(2)碳材料,其经过热改性(由于其自然历史或工业生产),因此具有高比表面积并呈现非线性等温线,以及(3)纯工程微孔材料(如沸石和活性炭),其吸附仅归因于孔填充过程。所有化合物的吸附都能很好地用波兰尼 - 杜比宁 - 马内斯(PDM)模型拟合,对于含有腐殖有机物的吸附剂(如泥炭),该模型与线性分配相结合。如果使用溶解度归一化的水相浓度,分配模型和波兰尼 - 杜比宁 - 马内斯模型都能预测相似化合物独特的吸附等温线。此外,数据很好地证实了分配系数(Kd)与水溶性之间的反比线性关系。这也导致了单位等效的弗伦德利希吸附等温线,并解释了在给定浓度下吸附容量(如弗伦德利希系数)与吸附非线性(弗伦德利希指数)之间经常观察到的明显相关性。

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