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非饱和土质覆盖层多组分气体运移机理研究
引用本文:张旭俊,陈云敏,徐晓兵,詹良通,杨益彪. 非饱和土质覆盖层多组分气体运移机理研究[J]. 岩土工程学报, 2015, 37(10): 1917-1923. DOI: 10.11779/CJGE201510021
作者姓名:张旭俊  陈云敏  徐晓兵  詹良通  杨益彪
作者单位:1. 浙江大学岩土工程研究所,浙江 杭州 310058;2. 浙江大学软弱土与环境土工教育部重点试验室,浙江 杭州 310058
基金项目:国家重点基础研究发展计划(“973”计划)项目; (2012CB719805); 国家自然科学基金项目(41402249)
摘    要:为研究土质覆盖层中各组分气体的运移规律,进行了土柱注气试验,并通过多组分气体运移理论对试验结果进一步分析。分析结果表明:在注入气体总流量不变的情况下,改变注入气体的组分,会显著影响土柱中各组分气体分布;多组分气体运移理论能较好地预测各组分气体的运移;表观气相渗透系数不是一常数,与气压大小相关;体相扩散是影响各组分气体分布规律的主要因素,通过改变有效二元扩散系数,调整各组分气体分布,可以提高土质覆盖层中甲烷氧化效果。

关 键 词:气体运移  覆盖层  多组分气体  非饱和土  体相扩散  
收稿时间:2014-09-11

Mechanism of multi-component gas migration in unsaturated cover
ZHANG Xu-jun,CHEN Yun-min,XU Xiao-bing,ZHAN Liang-tong,YANG Yi-biao. Mechanism of multi-component gas migration in unsaturated cover[J]. Chinese Journal of Geotechnical Engineering, 2015, 37(10): 1917-1923. DOI: 10.11779/CJGE201510021
Authors:ZHANG Xu-jun  CHEN Yun-min  XU Xiao-bing  ZHAN Liang-tong  YANG Yi-biao
Affiliation:1. Institute of Geotechnical Engineering, Zhejiang University, Hangzhou 310058, China; 2. MOE Key Laboratory of Soft Soils and Geoenvironmental Engineering, Zhejiang University, Hangzhou 310058, China
Abstract:A multi-component gas migration model is presented for determining each component flux of landfill gas. The method to determine transport parameters in unsaturated soils is also given. A soil column test is conducted to simulate the progress of gas migration in landfill final cover. The test results are compared with the theoretical ones. It shows that the multi-component gas migration model can give the flux of each component more accurately. Change in the injected gas component fraction has a significant influence on the gas distribution in soils. Amount of apparent gas permeability depends on gas pressure. Bulk diffusion is the main factor to determine the distribution of each component in soils. Changing in effective diffusion coefficient may improve the methane oxidation capacity.
Keywords:gas transport  final cover  multi-component gas  unsaturated soil  bulk diffusion  
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