Department of Civil and Environmental Engineering, University of California, Davis, One Shields Ave., Engineering III, Davis, CA 95616, United States.
J Contam Hydrol. 2010 Mar 1;112(1-4):103-17. doi: 10.1016/j.jconhyd.2009.11.001. Epub 2009 Nov 20.
A quasi-two-dimensional model is presented for simulating transport and transformation of contaminant species in river waters and sediments, taking into account the effect of both biotic and abiotic geochemical reactions on the contaminant fate and mobility. The model considers the downstream transport of dissolved and sediment-associated species, and the mass transfer with bed sediments due to erosion and resuspension, using linked advection-dispersion-reaction equations. The model also couples both equations to the reactive transport within bed sediment phases. This is done by the use of a set of vertical one-dimensional columns representing sediment layers that take into account the reactive transport of chemicals, burial, sorption/desorption to/from the solid phase, and the diffusive transport of aqueous species. Kinetically-controlled reversible solid-water mass exchange models are adopted to simulate interactions between suspended sediments and bulk water, as well as the mass exchange between bed sediments and pore water. An innovative multi-time step approach is used to model the fully kinetic nonlinear reaction terms using a non-iterative explicit method. This approach enables the model to handle fast and near-equilibrium reactions without a significant increase in computational burden. At the end, two demonstration cases are simulated using the model, including transport of a sorbing, non-reactive trace metal and nitrogen cycling, both in the Colusa Basin Drain in the Central Valley of California.
提出了一个准二维模型来模拟河水中污染物物种的迁移和转化,同时考虑了生物和非生物地球化学反应对污染物归宿和迁移性的影响。该模型考虑了溶解态和悬浮态物质的下游输运,以及由于侵蚀和再悬浮作用导致的与底泥的质量转移,采用了链接的对流-弥散-反应方程。该模型还将这些方程与底泥相内的反应性传输耦合起来。这是通过使用一组代表底泥层的垂直一维柱来实现的,这些柱考虑了化学物质的反应性传输、埋藏、从固相到固相的吸附/解吸,以及水相物质的扩散传输。采用动力学控制的可逆固-水质量交换模型来模拟悬浮泥沙与主体水之间的相互作用,以及底泥与孔隙水之间的质量交换。采用一种创新的多时间步方法,使用非迭代显式方法来模拟完全动力学非线性反应项。这种方法使模型能够处理快速和近平衡反应,而不会显著增加计算负担。最后,使用该模型模拟了两个演示案例,包括在加利福尼亚州中央谷的科卢萨流域中吸附、非反应性痕量金属和氮循环的输运。