Pore-Scale Modeling of Water and Ion Diffusion in Partially Saturated Clays

被引:5
作者
Yang, Yuankai [1 ]
Churakov, Sergey V. [2 ,3 ]
Patel, Ravi A. [4 ]
Prasianakis, Nikolaos [3 ]
Deissmann, Guido [1 ]
Bosbach, Dirk [1 ]
Poonoosamy, Jenna [1 ]
机构
[1] Forschungszentrum Julich, Inst Energy & Climate Res Nucl Waste Management IE, JARA, CSD, Julich, Germany
[2] Paul Scherrer Inst, Lab Waste Management, Villigen, Switzerland
[3] Univ Bern, Inst Geol Sci, Bern, Switzerland
[4] Karlsruhe Inst Technol KIT, Inst Bldg Mat & Concrete Struct IMB, Karlsruhe, Germany
基金
欧洲研究理事会;
关键词
diffusion; pore-scale model; partially saturated clays; Lattice Boltzmann method; electrical double layer; REACTIVE TRANSPORT; AQUEOUS-SOLUTIONS; COMPACTED ILLITE; SURFACE; BENTONITE; MONTMORILLONITE; PERMEABILITY; HTO; COEFFICIENT; ADSORPTION;
D O I
10.1029/2023WR035595
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
An accurate mechanistic understanding of solute diffusion in partially saturated clays is critical for assessing the safety of deep geological repositories for radioactive waste. In this study, a pore-scale numerical framework is developed to simulate water and ion diffusion in partially saturated clays. First, the two-phase Shan-Chen Lattice Boltzmann method is employed to establish the liquid-gas distribution in a reconstructed three-dimensional pore geometry of a clay. An equivalent solute method is also developed and validated to improve the numerical stability of the solution at the liquid/gas interface corresponding to steep variations of the concentration and diffusion coefficient of the water tracer. By using a mobility-distance relationship from molecular simulations, Fick's law is numerically solved to simulate water diffusion in nanopores, while the coupled Poisson-Boltzmann-Nernst-Planck equations are solved to simulate ion diffusion under the influence of the electrical double layer (EDL). Our model reveals that the decrease of relative effective diffusion coefficients during the desaturation is more pronounced for ions than for water, due to the additional transport pathway of water tracers in the gas phase. The obtained effective diffusion coefficients of tritiated water and ions agree well with reported data from compacted sedimentary rocks. By comparing the local electric potential and the distribution of ion concentrations in single pores, the simulation results suggest that the EDL in unsaturated clays has a more complex influence on ion distribution than under fully water-saturated conditions. This study provides critical insights into the coupled transport processes of solutes in partially saturated clays. Development of a pore-scale numerical framework to simulate water and ion diffusion in partially saturated claysDerivation of an equivalent solute method to improve the numerical stability caused by the discontinuities at the water/vapor interfaceThe electrical double layer has a stronger effect on ion transport under unsaturated conditions than under water saturated conditions
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页数:23
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