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Mixing induced reactive transport in fractured crystalline rocks

机译:裂隙结晶岩中混合诱导的反应输运

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摘要

In this paper the solute retention properties of crystalline fractured rocks due to mixing-induced geochemical reactions are studied. While fractured media exhibit paths of fast flow and transport and thus short residence times for conservative solutes, at the same time they promote mixing and dilution due to strong heterogeneity, which leads to sharp concentration contrasts. Enhanced mixing and dilution have a double effect that favors crystalline fractured media as a possible host medium for nuclear waste disposal. Firstly, peak radionuclide concentrations are attenuated and, secondly, mixing-induced precipitation reactions are enhanced significantly, which leads to radionuclide immobilization. An integrated framework is presented for the effective modeling of these flow, transport and reaction phenomena, and the interaction between them. In a simple case study, the enhanced dilution and precipitation potential of fractured crystalline rocks are systematically studied and quantified and contrasted it to retention and attenuation in an equivalent homogeneous formation.
机译:本文研究了由于混合诱发的地球化学反应而产生的结晶性裂隙岩石的溶质保留特性。破裂的介质表现出快速流动和运输的路径,因此对于保守的溶质而言停留时间短,同时由于强烈的异质性,它们也促进了混合和稀释,这导致了明显的浓度对比。增强的混合和稀释具有双重作用,有利于晶体破裂介质作为核废料处置的可能宿主介质。首先,峰值放射性核素浓度降低,其次,混合诱导的沉淀反应显着增强,这导致放射性核素固定化。提出了一个集成的框架,用于对这些流动,传输和反应现象以及它们之间的相互作用进行有效建模。在一个简单的案例研究中,系统地研究和量化了裂隙结晶岩增强的稀释和沉淀潜力,并将其与等效均质地层中的保留和衰减进行了对比。

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