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Reaction front formation in contaminant plumes

机译:污染物羽流中的反应前沿形成

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The formation of successive fronts in contaminated groundwater plumes by subsoil bacterial action is a commonly accepted feature of their propagation, but it is not obviously clear from a mathematical standpoint quite how such fronts are formed or propagate. In this paper we show that these can be explained by combining classical reaction-diffusion theory involving just two reactants (oxidant and reductant), and a secondary reaction in which a reactant on one side of such a front is (re-)formed on the other side of the front via diffusion of its product across the front We give approximate asymptotic solutions for the reactant profiles, and the propagation rate of the front.
机译:受土壤下的细菌作用在受污染的地下水羽流中形成连续的前沿是它们传播的普遍接受的特征,但是从数学的角度来看,尚不清楚这种前沿是如何形成或传播的。在本文中,我们证明了这些可以通过结合仅涉及两种反应物(氧化剂和还原剂)的经典反应扩散理论以及在反应前沿的一侧(再)形成反应物的二次反应进行解释。通过其产物在前端的扩散,可以得到前端的另一侧。我们给出了反应物分布和前端的传播速率的近似渐近解。

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