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Assessment of nonequilibriu in gas-water mass transfer during advective gas-phase transport in soils

机译:平流气相在土壤中气水传质中的非平衡评价

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In soils advective gas flow may be due to natural processes, e.g., water-table fluctuations, or may be a result of remediation techniques, such as soil vapor extraction(SVE), which are used to remove volatile organic compounds(VOCs)from the vadose zone. Recently, multicomponent experiments as well as numerical simulations provided evidence that the efficiency of SVE operations can be limited by slow diffusion of VOCs from interparticle water into the gas phase. Using a first-order kinetics approach, we show that the degree of local nonequilibrium between the Two phases and, thus, of the validity of the local equilibrium assumption(LEA)can be Characterized by the prefix denominator, P_D, for gas-water mass transfer which is derived by the SKIT(Separation of the Kinetically Influened Term)procedure of Bahr and Rubin[Bahr, J.M., Rubin, J., 1987.
机译:在土壤中,对流气流可能是由于自然过程(例如,水位波动)引起的,也可能是补救技术(例如土壤蒸汽提取(SVE))的结果,该技术用于从土壤中去除挥发性有机化合物(VOC)。渗流区。最近,多组分实验和数值模拟提供了证据,表明SVE操作的效率可能受到VOC从颗粒间水缓慢扩散到气相中的限制。使用一阶动力学方法,我们表明两相之间的局部不平衡程度以及局部平衡​​假设(LEA)的有效性可以通过前缀分母P_D来表征。由Bahr和Rubin的SKIT(动力学影响项的分离)程序得出的转移[Bahr,JM,Rubin,J.,1987。

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