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水在污染土壤中烃类热解吸中的矛盾作用。

Ambivalent role of water in thermodesorption of hydrocarbons from contaminated soil.

机构信息

Helmholtz Centre for Environmental Research-UFZ, Department of Environmental Engineering, Leipzig, Germany.

出版信息

Environ Sci Technol. 2011 Jan 15;45(2):732-7. doi: 10.1021/es102778h. Epub 2010 Dec 6.

Abstract

Thermodesorption studies with soil samples from a former filling station for light crude oil contaminated with mineral oil hydrocarbons (mainly benzene, toluene, ethylbenzene, xylenes, naphthalene, alkylnaphthalenes, and C(10) to C(14) alkanes) have revealed an ambivalent influence of water on desorption rates. Particularly, the influences of soil moisture content, humidity of the purge gas, temperature, and content of soil organic matter (SOM) were studied. At low temperature, purge gas humidity strongly affected the mobility of hydrocarbons in the soil organic matter (SOM) leading to an enhanced release of contaminants at higher moisture contents. Heating resulted in a decrease of thermodesorption when connected with desiccation of soil, in spite of the strong temperature impact on the vapor pressure of contaminants. At high water content of the SOM, the transfer of the pollutant molecules into the gas phase was found to be markedly hindered by the formation of water films or pore-filling by bulk water, both acting as diffusion barriers.

摘要

从一座曾用于加注轻质原油的加油站的土壤样本中进行的热脱附研究表明,水对脱附速率有双重影响。特别是,研究了土壤湿度、吹扫气湿度、温度和土壤有机质(SOM)含量对脱附速率的影响。在低温下,吹扫气湿度强烈影响土壤有机质(SOM)中碳氢化合物的迁移性,导致在较高湿度时污染物的释放增加。尽管污染物的蒸气压受温度的强烈影响,但加热会导致土壤干燥,从而降低热脱附率。在 SOM 具有高含水量的情况下,污染物分子向气相中的转移明显受到水膜的形成或由体相水填充孔的阻碍,两者都起到扩散障碍的作用。

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