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Parameters that control the cleanup of fractured permeable aquifers

机译:控制压裂的渗透性含水层的参数

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This study develops a modeling approach for simulating and evaluating entrapped light nonaqueous-phase liquid (light NAPL-LNAPL) dissolution and transport of the solute in a fractured permeable aquifer (FPA). The term FPA refers to an aquifer made of porous blocks of high permeability that embed fractures. The fracture network is part of the domain characterized by high permeability and negligible storage. Previous studies show that sandstone aquifers often represent FPAs. The basic model developed in this study is a two-dimensional (2-D) model of permeable blocks that embed oblique equidistant fractures with constant aperture and orientation. According to this model, two major parameters govern NAPL dissolution and transport of the solute. These parameters are: 1) the dimensionless interphase mass transfer coefficient, K_(f0), and 2) the mobility number, N_(M0). These parameters represent measures of heterogeneity affecting flow, NAPL dissolution, and transport of the solute in the domain. The parameter K_(f0) refers to the rate at which organic mass is transferred from the NAPL into the water phase. The parameter N_(M0) represents the ratio of flow through the porous blocks to flow through the fracture network in regions free of entrapped NAPL. It also provides a measure of groundwater flow bypassing regions contaminated by entrapped NAPL. In regions contaminated by entrapped NAPL our simulations have often indicated very low permeability of the porous blocks, enabling a significant increase of the fracture flow at the expense of the permeable block flow. Two types of constitutive relationships also affect the rate of FPA cleanup: 1) the relationship between the saturation of the entrapped NAPL and the permeability of the porous blocks, and 2) the relationships representing effects of the entrapped NAPL saturation and the permeable block flow velocity on rates of interphase mass transfer. This study provides basic tools for evaluating the characteristics of pump-and-treat cleanup of FPAs by referring to sets of parameters and constitutive relationships typical of FPAs. The numerical simulations carried out in this study show that at high initial saturation of the entrapped NAPL, during initial stages of the FPA cleanup the contaminant concentration increases, but later it decreases. This phenomenon originates from significant groundwater bypassing the NAPL entrapped in the permeable blocks via the fracture network.
机译:这项研究开发了一种模拟方法,用于模拟和评估夹带的轻质非水相液体(轻质NAPL-LNAPL)在裂隙可渗透含水层(FPA)中的溶质溶解和迁移。术语FPA是指由高渗透性的多孔块嵌入裂缝形成的含水层。裂缝网络是以高渗透率和可忽略的储量为特征的区域的一部分。先前的研究表明,砂岩含水层通常代表FPA。在这项研究中开发的基本模型是二维(2-D)的可渗透块的模型,该块以恒定的孔径和方向嵌入倾斜的等距裂缝。根据该模型,两个主要参数控制着NAPL的溶解和溶质的运输。这些参数是:1)无量纲相间传质系数K_(f0),和2)迁移率数N_(M0)。这些参数表示影响流量,NAPL溶解和溶质在域中运输的异质性度量。参数K_(f0)是指有机物质从NAPL转移到水相的速率。参数N_(M0)表示在没有夹带NAPL的区域中,流过多孔块的流量与流过裂缝网络的流量之比。它还提供了一种措施,对被捕获的NAPL污染的地下水绕行区域进行测量。在被夹杂有NAPL污染的区域中,我们的模拟通常表明多孔块体的渗透率非常低,从而以增加了渗透性块体流为代价,使裂缝流量显着增加。两种类型的本构关系也会影响FPA净化率:1)夹带的NAPL饱和度与多孔块渗透率之间的关系,以及2)表示夹带的NAPL饱和度和渗透性块流速之间的关系关于相间传质的速率。该研究通过参考典型的FPA参数集和本构关系,为评估FPA的泵处理特征提供了基础工具。在这项研究中进行的数值模拟表明,在捕获的NAPL的初始饱和度较高时,在FPA净化的初始阶段,污染物浓度增加,但随后降低。这种现象源于大量的地下水通过裂缝网络绕过了渗透块中夹带的NAPL。

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