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Modeling of multicomponent transport in groundwater and its application to chromium system.

机译:地下水中多组分迁移的建模及其在铬系统中的应用。

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The distribution of chromium in groundwater are determined by two processes: solute transport and chemical reactions. The transport of aqueous species is governed by a set of partial differential equations (PDEs), and the speciation of chemical species is governed by a set of nonlinear algebraic equations (AEs).; An efficient 1-D multicomponent transport model was developed using the direct substitution approach (DSA). The model incorporates aqueous complexation, surface complexation and precipitation/dissolution. PDEs governing transport processes were discretized and solved together with non-linear AEs for chemical reactions using the Newton-Raphson method. The Jacobian matrix was obtained analytically. The DSA model is about 100% more efficient than a model based on the sequential substitution approach (SIA) commonly used in practice. A 3-D multicomponent transport model was developed based on the 1-D model. The slow process of chromium migration into the soil matrix was modeled by a first order mass transfer process.; Groundwater flow is the driving force for chemical transport. A 3-D groundwater flow model was developed based on a multigrid finite difference method. The model is capable of simulating domains with irregular boundaries as well as fluctuating groundwater table, i.e., the cells are allowed to dry out and to be re-watered. The model saves about 30% in CPU time compared with MODFLOW.; Chromium contamination found at the National Chromium Inc. site, Putnam, Connecticut, was modeled. The groundwater flow at the site was calibrated, and simulated water table agreed well with the observed well water elevations. The chromium adsorption data from the isotherm studies were also modeled. Information from both isotherm study and sequential extraction study was used to simulate the site. A calibration framework was developed to assess heavy metal contamination sites of this kind where long term chromium contamination occurs. The hindcast technique was used for calibration, where most weight was given to chromium data on soil collected at the two multilevel nests since it represents the accumulative effect of chromium contamination over time. The simulated soil chromium concentrations were with the range of the observed chromium data at the two multilevel nests. A pump-and-treat remediation alternative was recommended.
机译:铬在地下水中的分布取决于两个过程:溶质迁移和化学反应。水性物质的运输受一组偏微分方程(PDE)支配,化学物质的形成受一组非线性代数方程(AE)支配。使用直接替代方法(DSA)开发了一种有效的一维多组分传输模型。该模型包括水络合,表面络合和沉淀/溶解。使用牛顿-拉夫森方法,将支配运输过程的PDE与非线性AE进行离散化并求解。通过解析获得雅可比矩阵。 DSA模型比基于实践中常用的顺序替换方法(SIA)的模型效率高约100%。在1-D模型的基础上开发了3-D多组分传输模型。铬迁移到土壤基质的缓慢过程是通过一阶传质过程建模的。地下水流是化学运输的驱动力。基于多网格有限差分法建立了3-D地下水流模型。该模型能够模拟边界不规则以及地下水位波动的区域,即允许细胞变干并重新浇水。与MODFLOW相比,该模型节省了大约30%的CPU时间。对位于康涅狄格州普特南市的国家铬业有限公司工厂中的铬污染进行了建模。对现场的地下水流量进行了校准,模拟地下水位与观测到的井水高程吻合得很好。还对等温线研究中的铬吸附数据进行了建模。等温线研究和顺序提取研究中的信息均用于模拟站点。开发了校准框架以评估发生长期铬污染的此类重金属污染部位。后铸技术用于标定,其中权重最大的是在两个多级巢穴收集的土壤中的铬数据,因为它代表了铬污染随时间的累积效应。模拟的土壤铬浓度在两个多层巢中的观测铬数据范围内。建议采用泵和治疗的替代方法。

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