Compound-specific carbon isotopic fractionation during transport of phthalate esters in sandy aquifer

被引:9
|
作者
Liu, Hui [1 ,2 ]
Li, YanXi [1 ,2 ]
He, Xi [1 ,2 ]
Sissou, Zakari [1 ,2 ]
Tong, Lei [1 ,2 ]
Yarnes, Chris [3 ]
Huang, Xianyu [4 ]
机构
[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China
[2] China Univ Geosci, Sch Environm Studies, Wuhan 430074, Peoples R China
[3] UC Davis Stable Isotope Facil, Dept Plant Sci, Davis, CA 95616 USA
[4] China Univ Geosci, Fac Earth Sci, Dept Geog, Wuhan 430074, Peoples R China
基金
中国国家自然科学基金;
关键词
Carbon isotope; Isotopic fractionation; Phthalate esters; Sediment; Transport simulation; ORGANIC CONTAMINANTS; GROUNDWATER CONTAMINATION; SORPTION; BIODEGRADATION; LANDFILL; SOIL;
D O I
10.1016/j.chemosphere.2015.10.080
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The present paper aims to evaluate the carbon isotopic fractionation of phthalate esters (PAEs) during transport in an sandy aquifer. Breakthrough curves of di-methyl phthalate (DMP), di-ethyl phthalate (DEP), and di-n-butyl phthalate (DBP) in mixed solution were determined by miscible displacement experiment, and simulated using HYDRUS-1D software. The stable carbon isotopes (delta C-13) of 3 PAEs in effluent were analyzed at different times. Results showed that, in the transport process in sandy sediment, PAEs are mainly trapped into the pore space instead of being adsorbed on the surface of particles. At the initial stage of transport, PAEs with lighter carbon tend to run faster in the sandy sediment, and PAEs with heavier carbon run after. However, there is no priority for the transport of PAEs with different carbon isotopes at Stage II with mainly time-limited sorption. So the transport-based isotope fractionation occurs in the front area of contaminant plume. This effect may be relevant for interpreting carbon isotope signatures in the real contaminant site. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1831 / 1836
页数:6
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