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Assessment of interfacial mass transfer in water-unsaturated soils during vapor extraction

机译:蒸汽萃取过程中非饱和土壤中界面传质的评估

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This paper presents results of a numerical investigation of soil vapor extraction (SVE) systems at the laboratory scale. The SVE technique is used to remove volatile chlorinated hydrocarbons (VCHC) from the water-unsaturated soil zone. The developed numerical model solves equations of flow, transport and interfacial mass transfer regarding an isothermal n-component and three-phase system. The mathematical model is based on a simple pore network and phase distribution model and designed to be scaled by a characteristic length. All mathematical expressions are structured into VCHC specific and VCHC non-specific parameters. Furthermore, indicators are introduced that help to separate thermodynamic equilibrium from thermodynamic non-equilibrium domains and to determine the controlling physical parameters. For numerical solution, the system of partial differential equations is discretized by a finite volume method and an implicit Euler time stepping scheme. Computational effort is reduced notably through techniques that enable spatial and temporal adaptivity, through a standard multigrid method as well as through a problem-oriented sparse-matrix storage concept. Computations are carried out in two dimensions regarding the laboratory experiment of Fischer et al. [Water Resour. Res. 32 (12) 1996 3413]. By varying the characteristic length scale of the pore network and phase distribution model, it is shown that the experimental gas phase concentrations cannot be explained only by the volatility and diffusivity of the VCHC. The computational results suggest a sorption process whose significance grows with the aqueous activity of the less or non-polar organic compounds.
机译:本文介绍了实验室规模的土壤蒸汽提取(SVE)系统的数值研究结果。 SVE技术用于从水不饱和土壤带中去除挥发性氯代烃(VCHC)。所开发的数值模型解决了等温n成分和三相系统的流动,传输和界面传质方程。数学模型基于简单的孔网络和相分布模型,并设计为按特征长度进行缩放。所有数学表达式都构造为VCHC特定参数和VCHC非特定参数。此外,引入了有助于将热力学平衡与热力学非平衡域分开并确定控制物理参数的指示剂。对于数值解,偏微分方程组通过有限体积法和隐式欧拉时间步进方案离散化。通过实现空间和时间适应性的技术,标准的多重网格方法以及面向问题的稀疏矩阵存储概念,显着减少了计算工作量。关于Fischer等人的实验室实验,计算在两个维度上进行。 [水资源。 Res。 32(12)1996 3413]。通过改变孔隙网络的特征长度尺度和相分布模型,表明仅通过VCHC的挥发性和扩散性不能解释实验气相浓度。计算结果表明,吸附过程的重要性随着较少或非极性有机化合物的水活性而增长。

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