Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site
In the context of deep waste disposals, the geological barrier (i.e., the host rock) will be exposed to saline plumes from bituminous waste and alkaline plumes from concrete degradation. These chemical disturbances will affect the hydraulic and mechanical properties of the clay rock by modifying its...
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Format: | Article |
Language: | English |
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EDP Sciences
2023-01-01
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Series: | E3S Web of Conferences |
Online Access: | https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_11002.pdf |
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author | Barakat Yara Mokni Nadia Cui Yu-Jun Delage Pierre Bernier Frédéric |
author_facet | Barakat Yara Mokni Nadia Cui Yu-Jun Delage Pierre Bernier Frédéric |
author_sort | Barakat Yara |
collection | DOAJ |
description | In the context of deep waste disposals, the geological barrier (i.e., the host rock) will be exposed to saline plumes from bituminous waste and alkaline plumes from concrete degradation. These chemical disturbances will affect the hydraulic and mechanical properties of the clay rock by modifying its microstructure. As a result, the self-sealing of the fractures created during excavation could be affected,further affecting the long-term safety of the repositories. To this end, the effect of salinity and alkalinity on the microstructure of a partially saturated Opalinus Clay from the lower sandy facies of Mont Terri was investigated. It was found that at 𝑤 = 4.1%, salinity decreases the density and the peak of the mesopores compared to the synthetic water. This is due to the water transfer from the meso to the macro pores and to the decrease of the thickness of the diffuse double layer. For the same water content, alkalinity generates meso and macro pores. The dissolutions of clay and non-clay minerals are the main mechanisms involved. |
first_indexed | 2024-04-09T14:51:40Z |
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id | doaj.art-0f93467371f64d108261b64c7bd4fbe0 |
institution | Directory Open Access Journal |
issn | 2267-1242 |
language | English |
last_indexed | 2024-04-09T14:51:40Z |
publishDate | 2023-01-01 |
publisher | EDP Sciences |
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series | E3S Web of Conferences |
spelling | doaj.art-0f93467371f64d108261b64c7bd4fbe02023-05-02T09:28:10ZengEDP SciencesE3S Web of Conferences2267-12422023-01-013821100210.1051/e3sconf/202338211002e3sconf_unsat2023_11002Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri siteBarakat Yara0Mokni Nadia1Cui Yu-Jun2Delage Pierre3Bernier Frédéric4Institut de Radioprotection et de Sûreté Nucléaire (IRSN), PSE-ENV/SEDRE/LETISInstitut de Radioprotection et de Sûreté Nucléaire (IRSN), PSE-ENV/SEDRE/LETISNavier, Ecole des Ponts, Univ Gustave Eiffel, CNRSNavier, Ecole des Ponts, Univ Gustave Eiffel, CNRSAgence Fédérale de Contrôle Nucléaire (AFCN)In the context of deep waste disposals, the geological barrier (i.e., the host rock) will be exposed to saline plumes from bituminous waste and alkaline plumes from concrete degradation. These chemical disturbances will affect the hydraulic and mechanical properties of the clay rock by modifying its microstructure. As a result, the self-sealing of the fractures created during excavation could be affected,further affecting the long-term safety of the repositories. To this end, the effect of salinity and alkalinity on the microstructure of a partially saturated Opalinus Clay from the lower sandy facies of Mont Terri was investigated. It was found that at 𝑤 = 4.1%, salinity decreases the density and the peak of the mesopores compared to the synthetic water. This is due to the water transfer from the meso to the macro pores and to the decrease of the thickness of the diffuse double layer. For the same water content, alkalinity generates meso and macro pores. The dissolutions of clay and non-clay minerals are the main mechanisms involved.https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_11002.pdf |
spellingShingle | Barakat Yara Mokni Nadia Cui Yu-Jun Delage Pierre Bernier Frédéric Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site E3S Web of Conferences |
title | Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site |
title_full | Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site |
title_fullStr | Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site |
title_full_unstemmed | Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site |
title_short | Impact of salinity and alkalinity on the microstructure of partially saturated Opalinus Clay from the lower sandy facies (LSF) of Mont Terri site |
title_sort | impact of salinity and alkalinity on the microstructure of partially saturated opalinus clay from the lower sandy facies lsf of mont terri site |
url | https://www.e3s-conferences.org/articles/e3sconf/pdf/2023/19/e3sconf_unsat2023_11002.pdf |
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