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Coupled chemical speciation-solute transport model for prediction of solute transport in clay buffers

机译:耦合化学形态-溶质运移模型预测黏土缓冲液中的溶质运移

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Modelling of the physico-chemical processes which occur in the buffer over a long time period is an invaluable tool as it is often not possible to conduct experiments over sufficiently long time scales to observe the long term leaching behaviour of waste. A coupled solute transport and chemical equilibrium speciation model has been developed. The model has the capability for simulating transport of multiple components of radioactive substances, thermodynamically reacting chemical species as they move, through a clay barrier system. It consists of two main modules, a finite difference transport module and an equilibrium geochemistry module which is a modified version of MINTEQA2. This linearizes the coupling between the physical and chemical processes and leads to a simple and efficient model to simulate the simultaneous processes of advective-dispersive transport (advection, diffusion, osmotic and ion restriction effect) and geochemical reactions (complexation, exchange, precipitation, adsorption and desorption) under different temperatures and pressures. In this research montmorillonite clay is employed as a buffer and strontium as a radioactive component for the simulation study. Two levels of temperature were chosen for simulation (25 ℃ and 100 ℃). The results indicated that the distribution and diffusion coefficients of Sr~(2+) are time-, space- and temperature-dependent and may not be considered as constant values.
机译:长时间在缓冲液中发生的物理化学过程的建模是非常宝贵的工具,因为通常不可能在足够长的时间内进行实验以观察废物的长期浸出行为。建立了耦合的溶质运移和化学平衡形态模型。该模型具有模拟放射性物质的多种成分的传输的能力,当化学物质移动通过粘土屏障系统时,它们会发生热力学反应。它由两个主要模块组成:有限差分传输模块和平衡地球化学模块,该模块是MINTEQA2的改进版本。这线性化了物理和化学过程之间的耦合,并导致一个简单而有效的模型来模拟对流-分散传输(对流,扩散,渗透和离子限制效应)和地球化学反应(复杂化,交换,沉淀,吸附)的同时过程和解吸)。在这项研究中,将蒙脱石粘土用作缓冲剂,将锶用作放射性成分进行模拟研究。选择两个温度水平进行仿真(25℃和100℃)。结果表明,Sr〜(2+)的分布和扩散系数与时间,空间和温度有关,因此不能视为常数。

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