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Influence of preferred orientation of clay particles on the diffusion of water in kaolinite porous media at constant porosity

机译：粘土粒子优选取向对恒孔稳态桥质岩多孔介质中水中的影响

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Thomas Dabat; Patrice Porion; Fabien Hubert; Erwan Paineau; Baptiste Dazas; Brian Grégoire; Emmanuel Tertre; Alfred Delville; Eric Ferrage;
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1. Influence of preferred orientation of clay particles on the diffusion of water in kaolinite porous media at constant porosity [J] . Dabat Thomas, Porion Patrice, Hubert Fabien, Applied clay science . 2020,第Jana期

机译：恒定孔隙度下粘土颗粒优选取向对水在高岭石多孔介质中扩散的影响
2. Role of interlayer porosity and particle organization in the diffusion of water in swelling clays [J] . Asaad A., Hubert F., Ferrage E., Applied clay science . 2021,第Juna期

机译：层间孔隙率和粒子组织在膨胀粘土中扩散的作用
3. Influence of clay particles on Al2O3 and TiO2 nanoparticles transport and retention through limestone porous media: measurements and mechanisms [J] . Bayat Ali Esfandyari, Junin Radzuan, Mohsin Rahmat, Journal of nanoparticle research: An interdisciplinary forum for nanoscale science and technology . 2015,第5期

机译：粘土颗粒对Al2O3和TiO2纳米颗粒通过石灰石多孔介质的传输和保留的影响：测量和机理
4. The influence of pressure diffusion effects on absorbing properties of porous media with double porosity [C] . X.Olny, C.Boutin International congress on noise control engineering . 2000

机译：压力扩散效应对双孔隙率多孔介质吸收性能的影响
5. Three-Dimensional Measurement of Porosity and Solute-Concentration Distributions during Diffusion in Porous Geologic Media Using X-ray Micro-Computed Tomography [D] . Agbogun, Henry Mosimabale Degussa 2012

机译：使用X射线微计算机断层扫描技术在多孔地质介质中扩散过程中孔隙度和溶质浓度分布的三维测量
6. Mineral precipitation-induced porosity reduction and its effect on transport parameters in diffusion-controlled porous media [O] . Aurélie Chagneau, Francis Claret, Frieder Enzmann, 2015

机译：扩散控制的多孔介质中矿物沉淀引起的孔隙度降低及其对输运参数的影响
7. Role of interlayer porosity and particle organization in the diffusion of water in swelling clays [O] . A. Asaad, F. Hubert, E. Ferrage, 2021

机译：层间孔隙率和粒子组织在膨胀粘土中扩散的作用

Influence of preferred orientation of clay particles on the diffusion of water in kaolinite porous media at constant porosity

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