首页> 外文会议>International Waste Management and Landfill Symposium >ANALYTICAL MODELS FOR CONTAMINANT TRANSPORT IN LANDFILL CLAY LINERS CONSIDERING COUPLED EFFECT OF CONSOLIDATION, DIFFUSION AND DEGRADATION
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ANALYTICAL MODELS FOR CONTAMINANT TRANSPORT IN LANDFILL CLAY LINERS CONSIDERING COUPLED EFFECT OF CONSOLIDATION, DIFFUSION AND DEGRADATION

机译:考虑耦合耦合,扩散和降解耦合效果的垃​​圾填埋粘土衬里中污染物运输分析模型

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Mathematical models for organic contaminant transport in clayey soils are developed to investigate the behavior of organic transport in the landfill clay liner system considering coupled effect of consolidation, diffusion and degradation. The bottom boundary conditions are assumed to be zero concentration or zero flux. Degradation and porosity changing of the organic contaminants in the porous media is considered. The bottom concentration and flux of the soil liners can be greatly reduced when the degradation effect and porosity changing is considered. For the case under steady-state, the bottom flux and concentration for the case with t1/2=10 years can be 2.8 and 4.5 times larger than those of the case with t1/2=100 years, respectively. The bottom concentration and flux of the soil liners can be greatly reduced when the coefficient of volume compressibility decreases. For quasi-steady-state and with t1/2=10 years, the bottom flux and concentration for the case with mv=0.02Mpa-1 can be 17.4 and 19.6 times lower than the case with mv =0.5Mpa-1. This may be due to the fact that the true fluid velocity induced by consolidation is greater for the case with high coefficient of volume compressibility. The proposed analytical model is relatively simple, and can be used for verification of more complicated numerical models and assessment of the coupled effect of diffusion, consolidation and degradation on contaminant transport in clay liners.
机译:制定了粘土土壤中有机污染物运输的数学模型,以研究垃圾填埋粘土衬垫系统的有机运输的行为考虑耦合耦合,扩散和降解的耦合作用。假设底部边界条件为零浓度或零通量。考虑了多孔介质中有机污染物的劣化和孔隙率改变。当考虑降解效果和孔隙率变化时,可以大大降低土壤衬里的底部浓度和磁通量。对于稳态下的情况,具有T1 / 2 = 10年的壳体的底部通量和浓度可以分别比T1 / 2 = 100年大的情况大2.8%和4.5倍。当压缩系数减小时,可以大大降低土壤衬里的底部浓度和磁通量。对于准稳态和T1 / 2 = 10年,底部通量和MV = 0.02MPa-1的壳体的浓度可以是17.4和19.6倍,而mV = 0.5MPa-1的情况。这可能是由于在具有高卷压缩性的情况下通过固结引起的真正流体速度更大。所提出的分析模型相对简单,可用于验证更复杂的数值模型和对粘土衬里污染物输送的扩散,固结和降解的耦合效果的评估。

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