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多环芳烃在粉质黏土中动态吸附和解吸的研究。

Study of dynamic sorption and desorption of polycyclic aromatic hydrocarbons in silty-clay soil.

机构信息

State Key Laboratory of Biogeology and Environmental Geology & School of Environmental Studies, China University of Geosciences, Wuhan 430074, China.

出版信息

J Hazard Mater. 2013 Jan 15;244-245:77-85. doi: 10.1016/j.jhazmat.2012.11.029. Epub 2012 Nov 21.

Abstract

This study reported a well controlled laboratory experiment of high concentration PAHs solute, containing fluorene, phenanthrene, fluoranthene and pyrene, through a nearly homogeneous soil column to reveal sorption and desorption behavior of these four PAHs in soil. The duration of the experiment was 64 days and the flow rate through the soil column was a constant which equals to 2000 mL d(-1). The result showed that the mechanism of isothermal sorption and desorption of fluorene can be perfectly described by the Langmuir model, and the correlation coefficients were greater than 0.997. The first-order Lagergren and the Bangham equation can precisely describe the rate of sorption of PAHs, while the rate of desorption can be represented by the second-order kinetics model. The results of the desorption experiment indicated that the desorption hysteresis of fluorene was evident. Few phenanthrene, fluoranthene and pyrene were desorpted to the aqueous phase for the chemical bond with the clay minerals. The most important process determining the behavior of PAHs in soils and their availability to further transformations was the sorption to soil solids with further sequestration and desorption to the aqueous phase.

摘要

本研究报告了一项针对高浓度多环芳烃溶质(包含芴、菲、荧蒽和芘)的实验室控制实验,该溶质通过近乎均匀的土壤柱进行实验,以揭示这些多环芳烃在土壤中的吸附和解吸行为。实验持续了 64 天,土壤柱的流速为恒定值,等于 2000 毫升/天。结果表明,芴的等温吸附和解吸机制可以用朗缪尔模型完美描述,相关系数大于 0.997。一级 Lagergren 和 Bangham 方程可以精确描述多环芳烃的吸附速率,而解吸速率可以用二级动力学模型来表示。解吸实验的结果表明,芴的解吸滞后现象明显。由于与粘土矿物形成化学键,很少有菲、荧蒽和芘被解吸到水相中。决定多环芳烃在土壤中行为及其进一步转化可用性的最重要过程是与土壤固体的吸附,以及进一步被固定到水相的解吸。

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