Institute of Environmental Assessment and Water Research (IDÆA), Spanish Council of Scientific Research (CSIC), Barcelona, Spain.
J Contam Hydrol. 2011 Mar 1;120-121:1-17. doi: 10.1016/j.jconhyd.2010.05.002. Epub 2010 May 19.
Geological media exhibit heterogeneities in their hydraulic and chemical properties, which can lead to enhanced spreading and mixing of the transported species and induce an effective reaction behavior that is different from the one for a homogeneous medium. Chemical heterogeneities such as spatially varying adsorption properties and specific reactive surface areas can act directly on the chemical reaction dynamics and lead to different effective reaction laws. Physical heterogeneities affect mixing-limited chemical reactions in an indirect way by their impact on spreading and mixing of dissolved species. To understand and model large-scale reactive transport the interactions of these coupled processes need to be understood and quantified. This paper provides a brief review on approaches of non-reactive and reactive transport modeling in geological media.
地质介质在水力和化学性质上表现出非均质性,这会导致迁移物种的扩散和混合增强,并诱导出与均匀介质不同的有效反应行为。化学非均质性,如空间变化的吸附特性和特定的反应表面积,可直接作用于化学反应动力学,并导致不同的有效反应定律。物理非均质性通过影响溶解物种的扩散和混合,间接地影响混合限制的化学反应。为了理解和模拟大规模的反应性传输,需要理解和量化这些耦合过程的相互作用。本文简要回顾了地质介质中非反应性和反应性传输建模的方法。