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MASS TRANSFER PROCESS IN THE SATURATED SUBSURFACE WITH A GROUNDWATER CIRCULATION FLOW FIELD

机译:地下水循环流场在饱和地下岩体中的传质过程

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Vertical circulation flow systems induced by groundwater circulation wells are anestablished in-situ groundwater pollution remediation technique. For a effectiveremediation of a groundwater pollution with a groundwater circulation well it wasnecessary to unterstand the influence of a circulation flow field on the mass transferprocess. Therefore one-dimensional soil column experiments and two-dimensional tankexperiments with a circulation flow field have been carried out to systematicallyinvestigate the mass transfer process between the residual NAPL and the aqueousphase. A dissolution model to describe the mass transfer process has been developed.This model assumes that the each residual NAPL phase has a spherical shape and ishomogeneously distributed in the porous medium. With this model it was possible todetermine the mass removed during the experiments and to estimate from experimentaldata the initial NAPL mass in the contamination source.
机译:地下水循环井诱发的垂直循环流系统是一种成熟的地下水污染修复方法。为了用地下水循环井有效地修复地下水污染,必须了解循环流场对传质过程的影响。因此,已经进行了一维土柱实验和具有循环流场的二维储罐实验,以系统地研究残留NAPL与水相之间的传质过程。建立了描述传质过程的溶出模型,该模型假设每个残留的NAPL相为球形,并且均匀分布在多孔介质中。使用该模型,可以确定实验过程中去除的质量,并根据实验数据估算污染源中的初始NAPL质量。

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