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Simulating the transfer and fate of hexachlorocyclohexane in recent 50 years in Beijing, China

机译:模拟近50年六氯环己烷在中国北京的转移和命运

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Taking Beijing as a study area, a dynamic fugacity model was used to simulate the transfer and fate of technical HCHs according to the physic-chemical properties of the studying environment and HCH isomers. Dynamic changes of the transfer fluxes and concentrations of HCH isomers during 1952-2003 were simulated and the model results suggest good agreement between the calculated and measured concentrations of HCH isomers. During 1952-1983, the average input and output amount of HCHs through agricultural application and degradation are 130 t and 150 t respectively. The dominant transfer processes of HCHs in the study area are air-soil deposition, soil erosion and soil-air diffusion, transfer fluxes of these processes are 80 t·a~(-1), 16 t·a~(-1) and 11 t·a~(-1) which account for 92% of total transfer fluxes of HCHs isomers. There were approximately 253t HCHs in all environmental compartments of the study area during this period and 97% of which existed in soil compartment. Air and water advection became the dominant input sources of HCHs after 1984 when the application of technical HCHs was prohibited, concentration of HCHs quickly descended to a quite low level in several years. Total amount of HCHs isomers remaining in the study area environment now is less than 5% that before 1983, and this percentage may descend to 0.5% after 20 years by prediction.
机译:以北京为研究区域,根据研究环境和六氯环己烷异构体的理化性质,采用动态逸度模型模拟了六氯环己烷的转移和去向。模拟了1952-2003年间六氯环己烷的转移通量和浓度的动态变化,模型结果表明,六氯环己烷异构体的计算浓度和实测浓度之间具有很好的一致性。在1952-1983年期间,通过农业应用和降解产生的六氯环己烷的平均输入和输出量分别为130 t和150 t。研究区六氯环己烷的主要转移过程是空气-土壤沉积,土壤侵蚀和土壤-空气扩散,这些过程的转移通量分别为80 t·a〜(-1),16 t·a〜(-1)和11 t·a〜(-1)占六氯环乙烷异构体总转移通量的92%。在此期间,研究区域所有环境隔间中大约有253t六氯环己烷,其中97%存在于土壤隔间中。 1984年禁止使用技术性六氯环己烷后,空气和水的平流成为六氯环己烷的主要输入来源,几年来,六氯环己烷的浓度迅速下降到相当低的水平。现在,研究区环境中残留的六氯环己烷异构体总量不到1983年之前的5%,而根据预测,这一百分比在20年后可能降至0.5%。

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