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将非饱和带溶质运移模型集成到“用于MODFLOW的HYDRUS软件包”中。

Implementation of Solute Transport in the Vadose Zone into the "HYDRUS Package for MODFLOW".

作者信息

Beegum Sahila, Šimůnek Jiří, Szymkiewicz Adam, Sudheer K P, Nambi Indumathi M

机构信息

Department of Environmental Sciences, University of California, Riverside, CA.

Gdańsk University of Technology, Faculty of Civil and Environmental Engineering, Gdańsk, Poland.

出版信息

Ground Water. 2019 May;57(3):392-408. doi: 10.1111/gwat.12815. Epub 2018 Aug 22.

Abstract

The "HYDRUS package for MODFLOW" is an existing MODFLOW package that allows MODFLOW to simultaneously evaluate transient water flow in both unsaturated and saturated zones. The package is based on incorporating parts of the HYDRUS-1D model (to simulate unsaturated water flow in the vadose zone) into MODFLOW (to simulate saturated groundwater flow). The coupled model is effective in addressing spatially variable saturated-unsaturated hydrological processes at the regional scale. However, one of the major limitations of this coupled model is that it does not have the capability to simulate solute transport along with water flow and therefore, the model cannot be employed for evaluating groundwater contamination. In this work, a modified unsaturated flow and transport package (modified HYDRUS package for MODFLOW and MT3DMS) has been developed and linked to the three-dimensional (3D) groundwater flow model MODFLOW and the 3D groundwater solute transport model MT3DMS. The new package can simulate, in addition to water flow in the vadose zone, also solute transport involving many biogeochemical processes and reactions, including first-order degradation, volatilization, linear or nonlinear sorption, one-site kinetic sorption, two-site sorption, and two-kinetic sites sorption. Due to complex interactions at the groundwater table, certain modifications of the pressure head (compared to the original coupling) and solute concentration profiles were incorporated into the modified HYDRUS package. The performance of the newly developed model is evaluated using HYDRUS (2D/3D), and the results indicate that the new model is effective in simulating the movement of water and contaminants in the saturated-unsaturated flow domains.

摘要

“用于MODFLOW的HYDRUS软件包”是一个现有的MODFLOW软件包,它能使MODFLOW同时评估非饱和带和饱和带中的瞬态水流。该软件包是基于将HYDRUS - 1D模型的部分内容(用于模拟包气带中的非饱和水流)并入MODFLOW(用于模拟饱和地下水流动)而构建的。这种耦合模型在处理区域尺度上空间变化的饱和 - 非饱和水文过程方面很有效。然而,这种耦合模型的一个主要局限性在于它没有能力在模拟水流的同时模拟溶质运移,因此,该模型不能用于评估地下水污染情况。在这项工作中,已开发出一个改进的非饱和水流与运移软件包(用于MODFLOW和MT3DMS的改进型HYDRUS软件包),并将其与三维(3D)地下水流模型MODFLOW以及3D地下水溶质运移模型MT3DMS相链接。除了包气带中的水流外,新软件包还能模拟涉及许多生物地球化学过程和反应的溶质运移,包括一级降解、挥发、线性或非线性吸附、单点位动力学吸附、双点位吸附以及双动力学点位吸附。由于地下水位处存在复杂的相互作用,改进型HYDRUS软件包中纳入了与原始耦合相比在压力水头和溶质浓度剖面方面的某些修正。使用HYDRUS(2D/3D)对新开发模型的性能进行了评估,结果表明新模型在模拟饱和 - 非饱和水流区域中的水和污染物运移方面是有效的。

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