Analytical expressions for thermo-osmotic permeability of clays
| Publication Date: |
2018-01-09
|
|---|---|
| Publisher: |
Wiley-Blackwell
|
| Print ISSN: |
0094-8276
|
| Electronic ISSN: |
1944-8007
|
| Topics: |
Geosciences
Physics
|
| Published by: |
| _version_ | 1836398740987969536 |
|---|---|
| autor | J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa |
| beschreibung | In this study, a new formulation for the thermo-osmotic permeability of natural pore solutions containing monovalent and divalent cations is proposed. The mathematical formulation proposed here is based on the theoretical framework supporting thermo-osmosis which relies on water structure alteration in the pore space of surface-charged materials caused by solid-fluid electrochemical interactions. The ionic content balancing the surface charge of clay minerals causes a disruption in the hydrogen bond network when more structured water is present at the clay surface. Analytical expressions based on our heuristic model are proposed and compared to the available data for NaCl solutions. It is shown that the introduction of divalent cations reduces the thermo-osmotic permeability by one third compared to the monovalent case. The analytical expressions provided here can be used to advantage for safety calculations in deep underground nuclear waste repositories. |
| citation_standardnr | 6133876 |
| datenlieferant | ipn_articles |
| feed_copyright | American Geophysical Union (AGU) |
| feed_copyright_url | http://www.agu.org/ |
| feed_id | 4905 |
| feed_publisher | Wiley-Blackwell |
| feed_publisher_url | http://www.wiley.com/wiley-blackwell |
| insertion_date | 2018-01-09 |
| journaleissn | 1944-8007 |
| journalissn | 0094-8276 |
| publikationsjahr_anzeige | 2018 |
| publikationsjahr_facette | 2018 |
| publikationsjahr_intervall | 7984:2015-2019 |
| publikationsjahr_sort | 2018 |
| publisher | Wiley-Blackwell |
| quelle | Geophysical Research Letters |
| relation | http://onlinelibrary.wiley.com/resolve/doi?DOI=10.1002%2F2017GL075904 |
| search_space | articles |
| shingle_author_1 | J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa |
| shingle_author_2 | J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa |
| shingle_author_3 | J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa |
| shingle_author_4 | J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa |
| shingle_catch_all_1 | Analytical expressions for thermo-osmotic permeability of clays In this study, a new formulation for the thermo-osmotic permeability of natural pore solutions containing monovalent and divalent cations is proposed. The mathematical formulation proposed here is based on the theoretical framework supporting thermo-osmosis which relies on water structure alteration in the pore space of surface-charged materials caused by solid-fluid electrochemical interactions. The ionic content balancing the surface charge of clay minerals causes a disruption in the hydrogen bond network when more structured water is present at the clay surface. Analytical expressions based on our heuristic model are proposed and compared to the available data for NaCl solutions. It is shown that the introduction of divalent cations reduces the thermo-osmotic permeability by one third compared to the monovalent case. The analytical expressions provided here can be used to advantage for safety calculations in deep underground nuclear waste repositories. J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa Wiley-Blackwell 0094-8276 00948276 1944-8007 19448007 |
| shingle_catch_all_2 | Analytical expressions for thermo-osmotic permeability of clays In this study, a new formulation for the thermo-osmotic permeability of natural pore solutions containing monovalent and divalent cations is proposed. The mathematical formulation proposed here is based on the theoretical framework supporting thermo-osmosis which relies on water structure alteration in the pore space of surface-charged materials caused by solid-fluid electrochemical interactions. The ionic content balancing the surface charge of clay minerals causes a disruption in the hydrogen bond network when more structured water is present at the clay surface. Analytical expressions based on our heuristic model are proposed and compared to the available data for NaCl solutions. It is shown that the introduction of divalent cations reduces the thermo-osmotic permeability by one third compared to the monovalent case. The analytical expressions provided here can be used to advantage for safety calculations in deep underground nuclear waste repositories. J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa Wiley-Blackwell 0094-8276 00948276 1944-8007 19448007 |
| shingle_catch_all_3 | Analytical expressions for thermo-osmotic permeability of clays In this study, a new formulation for the thermo-osmotic permeability of natural pore solutions containing monovalent and divalent cations is proposed. The mathematical formulation proposed here is based on the theoretical framework supporting thermo-osmosis which relies on water structure alteration in the pore space of surface-charged materials caused by solid-fluid electrochemical interactions. The ionic content balancing the surface charge of clay minerals causes a disruption in the hydrogen bond network when more structured water is present at the clay surface. Analytical expressions based on our heuristic model are proposed and compared to the available data for NaCl solutions. It is shown that the introduction of divalent cations reduces the thermo-osmotic permeability by one third compared to the monovalent case. The analytical expressions provided here can be used to advantage for safety calculations in deep underground nuclear waste repositories. J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa Wiley-Blackwell 0094-8276 00948276 1944-8007 19448007 |
| shingle_catch_all_4 | Analytical expressions for thermo-osmotic permeability of clays In this study, a new formulation for the thermo-osmotic permeability of natural pore solutions containing monovalent and divalent cations is proposed. The mathematical formulation proposed here is based on the theoretical framework supporting thermo-osmosis which relies on water structure alteration in the pore space of surface-charged materials caused by solid-fluid electrochemical interactions. The ionic content balancing the surface charge of clay minerals causes a disruption in the hydrogen bond network when more structured water is present at the clay surface. Analytical expressions based on our heuristic model are proposed and compared to the available data for NaCl solutions. It is shown that the introduction of divalent cations reduces the thermo-osmotic permeability by one third compared to the monovalent case. The analytical expressions provided here can be used to advantage for safety calculations in deep underground nuclear waste repositories. J. Gonçalvès, C. Ji Yu, J.-M. Matray, J. Tremosa Wiley-Blackwell 0094-8276 00948276 1944-8007 19448007 |
| shingle_title_1 | Analytical expressions for thermo-osmotic permeability of clays |
| shingle_title_2 | Analytical expressions for thermo-osmotic permeability of clays |
| shingle_title_3 | Analytical expressions for thermo-osmotic permeability of clays |
| shingle_title_4 | Analytical expressions for thermo-osmotic permeability of clays |
| timestamp | 2025-06-30T23:31:53.781Z |
| titel | Analytical expressions for thermo-osmotic permeability of clays |
| titel_suche | Analytical expressions for thermo-osmotic permeability of clays |
| topic | TE-TZ U |
| uid | ipn_articles_6133876 |