Effect of Temperature on the Diffusion and Sorption of Cations in Clay Vermiculite

التفاصيل البيبلوغرافية
Parent link:ACS Omega
Vol. 7, iss. 14.— 2022.— [P. 11596-11605]
مؤلف مشترك: Национальный исследовательский Томский политехнический университет Инженерная школа ядерных технологий Отделение ядерно-топливного цикла
مؤلفون آخرون: Wang Cailun, Myshkin (Mishkin) V. F. Vyacheslav Fedorovich, Khan V. A. Valery Alekseevich, Poberezhnikov A. D. Andrey Dmitrievich, Baraban A. P. Aleksandr Petrovich
الملخص:Title screen
The MD method for modeling vermiculite containing Na+, Rb+, Cs+, Mg2+, and Ba2+ cations shows the following: With a weak swelling of clay, the temperature has no significant effect on the diffusion of water and cations through vermiculite. With a high content of water in vermiculite, the effect of temperature on the diffusion coefficient of water is greater than that of cations. We studied the structure of RDF ions in Na+-vermiculite, in which some of the cations are replaced by Rb+, Cs+, Mg2+, and Ba2+. Cations of alkali and alkaline earth metals compete with Na+ ions for adsorption sites on the surface of the clay layer. The alkaline earth metal cations are in the middle between the clay layers due to their higher charge and stronger hydration. In this case, Na+ is localized at the surface of the clay layer. Thus, cations of alkaline earth metals have little effect on the temperature dependence of the diffusion coefficient Na+.
Режим доступа: по договору с организацией-держателем ресурса
اللغة:الإنجليزية
منشور في: 2022
الموضوعات:
الوصول للمادة أونلاين:https://doi.org/10.1021/acsomega.1c06059
التنسيق: الكتروني فصل الكتاب
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=668138

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200 1 |a Effect of Temperature on the Diffusion and Sorption of Cations in Clay Vermiculite  |f Wang Cailun, V. F. Myshkin (Mishkin), V. A. Khan [et al.] 
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300 |a Title screen 
320 |a [References: 57 tit.] 
330 |a The MD method for modeling vermiculite containing Na+, Rb+, Cs+, Mg2+, and Ba2+ cations shows the following: With a weak swelling of clay, the temperature has no significant effect on the diffusion of water and cations through vermiculite. With a high content of water in vermiculite, the effect of temperature on the diffusion coefficient of water is greater than that of cations. We studied the structure of RDF ions in Na+-vermiculite, in which some of the cations are replaced by Rb+, Cs+, Mg2+, and Ba2+. Cations of alkali and alkaline earth metals compete with Na+ ions for adsorption sites on the surface of the clay layer. The alkaline earth metal cations are in the middle between the clay layers due to their higher charge and stronger hydration. In this case, Na+ is localized at the surface of the clay layer. Thus, cations of alkaline earth metals have little effect on the temperature dependence of the diffusion coefficient Na+. 
333 |a Режим доступа: по договору с организацией-держателем ресурса 
461 |t ACS Omega 
463 |t Vol. 7, iss. 14  |v [P. 11596-11605]  |d 2022 
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701 0 |a Wang Cailun 
701 1 |a Myshkin (Mishkin)  |b V. F.  |c Physicist  |c Professor of Tomsk Polytechnic University, Doctor of physical and mathematical sciences  |f 1962-  |g Vyacheslav Fedorovich  |3 (RuTPU)RU\TPU\pers\31492  |9 15653 
701 1 |a Khan  |b V. A.  |c physicist  |c Associate Professor of Tomsk Polytechnic University, Doctor of technical sciences  |f 1952-  |g Valery Alekseevich  |3 (RuTPU)RU\TPU\pers\31988  |9 16048 
701 1 |a Poberezhnikov  |b A. D.  |c physicist  |c Senior Lecturer, Tomsk Polytechnic University  |f 1981-  |g Andrey Dmitrievich  |3 (RuTPU)RU\TPU\pers\37337  |9 20256 
701 1 |a Baraban  |b A. P.  |g Aleksandr Petrovich 
712 0 2 |a Национальный исследовательский Томский политехнический университет  |b Инженерная школа ядерных технологий  |b Отделение ядерно-топливного цикла  |3 (RuTPU)RU\TPU\col\23554 
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