Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa
The complicated composition of unsaturated clay, e.g., solid mineral particles, water, and air, makes it difficult to get its precise equation of state (EOS) over a wide pressure range. In this paper, the high-pressure EOS of unsaturated clay was discussed at the mesoscale. With the original clay ex...
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MDPI AG
2022-01-01
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Online Access: | https://www.mdpi.com/2073-4352/12/1/119 |
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author | Xianwen Ran Xuan Zou Jingyuan Zhou Wenhui Tang |
author_facet | Xianwen Ran Xuan Zou Jingyuan Zhou Wenhui Tang |
author_sort | Xianwen Ran |
collection | DOAJ |
description | The complicated composition of unsaturated clay, e.g., solid mineral particles, water, and air, makes it difficult to get its precise equation of state (EOS) over a wide pressure range. In this paper, the high-pressure EOS of unsaturated clay was discussed at the mesoscale. With the original clay extracted from the southern suburbs of Luoyang city, China, three unsaturated clays with moisture contents of 0%, 8%, and 15%, respectively, were remolded. Their Hugoniot parameters in the pressure range of 0–30 GPa were measured using a one-stage or two-stage light gas gun. With the measured Hugoniot parameters, a high-pressure EOS of the unsaturated clay up to 30 GPa was developed and it is in good agreement with the experimental data. |
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format | Article |
id | doaj.art-ffe8ab66451a405cbb1ac8c91e20f807 |
institution | Directory Open Access Journal |
issn | 2073-4352 |
language | English |
last_indexed | 2024-03-10T01:40:56Z |
publishDate | 2022-01-01 |
publisher | MDPI AG |
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series | Crystals |
spelling | doaj.art-ffe8ab66451a405cbb1ac8c91e20f8072023-11-23T13:25:31ZengMDPI AGCrystals2073-43522022-01-0112111910.3390/cryst12010119Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPaXianwen Ran0Xuan Zou1Jingyuan Zhou2Wenhui Tang3College of Liberal Arts and Sciences, National University of Defense Technology, Changsha 410073, ChinaCollege of Liberal Arts and Sciences, National University of Defense Technology, Changsha 410073, ChinaCollege of Liberal Arts and Sciences, National University of Defense Technology, Changsha 410073, ChinaCollege of Liberal Arts and Sciences, National University of Defense Technology, Changsha 410073, ChinaThe complicated composition of unsaturated clay, e.g., solid mineral particles, water, and air, makes it difficult to get its precise equation of state (EOS) over a wide pressure range. In this paper, the high-pressure EOS of unsaturated clay was discussed at the mesoscale. With the original clay extracted from the southern suburbs of Luoyang city, China, three unsaturated clays with moisture contents of 0%, 8%, and 15%, respectively, were remolded. Their Hugoniot parameters in the pressure range of 0–30 GPa were measured using a one-stage or two-stage light gas gun. With the measured Hugoniot parameters, a high-pressure EOS of the unsaturated clay up to 30 GPa was developed and it is in good agreement with the experimental data.https://www.mdpi.com/2073-4352/12/1/119unsaturated claymoisture contentHugoniot parametershigh-pressure EOS |
spellingShingle | Xianwen Ran Xuan Zou Jingyuan Zhou Wenhui Tang Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa Crystals unsaturated clay moisture content Hugoniot parameters high-pressure EOS |
title | Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa |
title_full | Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa |
title_fullStr | Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa |
title_full_unstemmed | Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa |
title_short | Shock Properties of One Unsaturated Clay and Its Equation of State Up to 30 GPa |
title_sort | shock properties of one unsaturated clay and its equation of state up to 30 gpa |
topic | unsaturated clay moisture content Hugoniot parameters high-pressure EOS |
url | https://www.mdpi.com/2073-4352/12/1/119 |
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