蔡喜运

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教授

博士生导师

硕士生导师

性别:男

毕业院校:浙江大学

学位:博士

所在单位:环境学院

学科:环境工程. 环境科学

办公地点:环境学院环境楼B411室

联系方式:电话:0411-84707193 (Office) Email:xiyuncai@dlut.edu.cn QQ:1851430298或xycai1978@163.com

电子邮箱:xiyuncai@dlut.edu.cn

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Application of a level IV fugacity model to simulate the long-term fate of hexachlorocyclohexane isomers in the lower reach of Yellow River basin, China

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论文类型:期刊论文

发表时间:2009-01-01

发表刊物:CHEMOSPHERE

收录刊物:SCIE、EI、PubMed

卷号:74

期号:3

页面范围:370-376

ISSN号:0045-6535

关键字:Fugacity model; Environmental fate; Yellow River; HCHs

摘要:A level IV multimedia fugacity model was established to simulate the fate and transfer of hexachlorocyclohexane (HCH) isomers in the lower reach of the Yellow River basin, China, during 1952-2010. The predicted concentrations of HCHs are in good agreement with the observed ones, as indicated by the residual errors being generally lower than 0.5 logarithmic units. The effects of extensive agricultural application and subsequent prohibition of HCHs are reflected by the temporal variation of HCHs predicted by the model. It is predicted that only 1.8 tons of HCHs will be left in 2010, less than 0.06% of the highest contents (in 1983) in the study area, and about 99% of HCHs remain in soil. The proportions of HCH isomers in the environment also changed with time due to their different physicochemical properties. Although beta-HCH is not the main component of the technical HCHs, it has become the most abundant isomer in the environment because of its persistence. The dominant transfer processes between the adjacent compartments were deposition from air to soil, air diffusion through the air-water interface and runoff from soil to water. Sensitivity analysis showed that degradation rate in soil, parameters related to major sources, and thickness of soils had the strongest influence on the model result. Results of Monte Carlo simulation indicated the overall uncertainty of model predictions, and the coefficients of variation of the estimated concentrations of HCHs in all the compartments ranged from 0.5 to 5.8. (C) 2008 Elsevier Ltd. All rights reserved.