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挥发性氯代烃在湿润土壤中的平衡吸附研究
引用本文:孟凡勇,刘锐,小林刚,万梅,余素林,陈吕军. 挥发性氯代烃在湿润土壤中的平衡吸附研究[J]. 环境科学, 2012, 33(4): 1361-1368
作者姓名:孟凡勇  刘锐  小林刚  万梅  余素林  陈吕军
作者单位:浙江清华长三角研究院生态环境研究所, 浙江省水质科学与技术重点实验室, 嘉兴 314006;浙江清华长三角研究院生态环境研究所, 浙江省水质科学与技术重点实验室, 嘉兴 314006;横滨国立大学大学院环境情报研究院, 横滨 240-8501;浙江清华长三角研究院生态环境研究所, 浙江省水质科学与技术重点实验室, 嘉兴 314006;浙江清华长三角研究院生态环境研究所, 浙江省水质科学与技术重点实验室, 嘉兴 314006;浙江清华长三角研究院生态环境研究所, 浙江省水质科学与技术重点实验室, 嘉兴 314006; 清华大学环境学院,北京 100084
基金项目:科技部国际科技合作项目(2008DFA91300)
摘    要:吸附是挥发性氯代烃(volatile chlorinated hydrocarbons,VCHs)赋存于土壤的主要机制之一.开展动态吸附实验,研究了4种常见VCHs污染物在我国8种典型土壤中的吸附平衡关系.结果表明,土壤在干燥条件下对VCHs气体的吸附能力要远大于湿润条件,且随含水率的升高吸附能力急剧下降,在含水率达到10%以后土壤吸附量趋于稳定.湿润土壤对三氯乙烯(TCE)、四氯乙烯(PCE)、1,1,1-三氯乙烷(MC)气体的吸附等温线符合Henry型吸附等温式,而1,1,2-三氯乙烷(1,1,2-TCA)符合Freundlich模型.VCHs在湿润土壤中的吸附量总体上与土壤有机碳(soil organic carbon,SOC)含量呈正相关,且受SOC类型和化合物极性影响较大.弱极性的TCE、PCE在土壤中的吸附能力与SOC含量呈严格正相关,而极性的MC、1,1,2-TCA在黑土等高碳土壤中不仅与SOC含量有关,还受到SOC物质组成的影响.建立了TCE和PCE在湿润土壤中的平衡吸附量预测模型,预测值与实测值相关性良好(n=80,R2=0.98).

关 键 词:挥发性氯代烃  湿润土壤  吸附等温线  土壤有机碳  土壤矿物
收稿时间:2011-06-15
修稿时间:2011-10-13

Study on Equilibrium Adsorption of Volatile Chlorinated Hydrocarbons on Humid Soils
Meng Fan-Yong,Liu Rui,Kobayashi Takeshi,Wan Mei,Yu Su-Lin,Chen Lü-Jun. Study on Equilibrium Adsorption of Volatile Chlorinated Hydrocarbons on Humid Soils[J]. Chinese Journal of Environmental Science, 2012, 33(4): 1361-1368
Authors:Meng Fan-Yong  Liu Rui  Kobayashi Takeshi  Wan Mei  Yu Su-Lin  Chen Lü-Jun
Affiliation:Zhejiang Provincial Key Laboratory of Water Science and Technology, Ecological and Environmental Research Department, Yangtze Delta Region Institute of Tsinghua University, Jiaxing 314006, China;Zhejiang Provincial Key Laboratory of Water Science and Technology, Ecological and Environmental Research Department, Yangtze Delta Region Institute of Tsinghua University, Jiaxing 314006, China;Graduate School of Environment and Information Sciences, Yokohama National University, Yokohama 240-8501, Japan;Zhejiang Provincial Key Laboratory of Water Science and Technology, Ecological and Environmental Research Department, Yangtze Delta Region Institute of Tsinghua University, Jiaxing 314006, China;Zhejiang Provincial Key Laboratory of Water Science and Technology, Ecological and Environmental Research Department, Yangtze Delta Region Institute of Tsinghua University, Jiaxing 314006, China;Zhejiang Provincial Key Laboratory of Water Science and Technology, Ecological and Environmental Research Department, Yangtze Delta Region Institute of Tsinghua University, Jiaxing 314006, China; School of Environment, Tsinghua University, Beijing 100084, China
Abstract:Adsorption is one of the principal mechanisms for soil contamination by volatile chlorinated hydrocarbons (VCHs). Dynamic adsorption experiments were carried out to study the equilibrium adsorption of four common VCHs pollutants onto eight typical soils in China. Results showed that dry soils had far greater adsorption capacity than humid soils. The soil adsorption capacity sharply decreased with the increase in the soil water content, and then reached a plateau as the water content rose to 10% or above. The adsorption isotherms of trichloroethylene (TCE), tetrachloroethylene (PCE) and 1,1,1-trichloroethane (MC) could be fitted with Henry's equation, while the adsorption isotherms of 1,1,2-trichloroethane (1,1,2-TCA) could be fitted with Freundlich model. The adsorption capacities of VCHs on humid soils were principally influenced by the content of soil organic carbon (SOC), but sometimes also impacted by the composition of SOC and the polarities of the VCHs molecules. Low polar molecules such as TCE and PCE showed adsorption capacities positively dependent on the SOC content. High polar molecules such as MC and 1,1,2-TCA displayed adsorption behavior not only influenced by SOC content but also by the SOC composition of high SOC content soils such as black soil. An adsorption equilibrium simulation model was developed for TCE and PCE on humid soils, the predicted values correlating well with the measured values (n=80, R2=0.98).
Keywords:volatile chlorinated hydrocarbons (VCHs)  humid soil  sorption isotherm  soil organic carbon  soil minerals
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