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Effect of Elevated Temperature on Rhyolitic Rocks’ Properties
The effect of high temperatures on rock’s thermophysical and mechanical properties is critical to the design of underground geotechnical applications. The current work investigates the impact of temperature on rhyolitic turf rock’s physical and mechanical properties. Intact cylindrical core rock sam...
Autores principales: | , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
MDPI
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9101199/ https://www.ncbi.nlm.nih.gov/pubmed/35591538 http://dx.doi.org/10.3390/ma15093204 |
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author | Ahmed, Haitham M. Hefni, Mohammed A. Ahmed, Hussin A. M. Adewuyi, Sefiu O. Hassani, Ferri Sasmito, Agus P. Saleem, Hussein A. Moustafa, Essam B. Hassan, Gamal S. A. |
author_facet | Ahmed, Haitham M. Hefni, Mohammed A. Ahmed, Hussin A. M. Adewuyi, Sefiu O. Hassani, Ferri Sasmito, Agus P. Saleem, Hussein A. Moustafa, Essam B. Hassan, Gamal S. A. |
author_sort | Ahmed, Haitham M. |
collection | PubMed |
description | The effect of high temperatures on rock’s thermophysical and mechanical properties is critical to the design of underground geotechnical applications. The current work investigates the impact of temperature on rhyolitic turf rock’s physical and mechanical properties. Intact cylindrical core rock samples were heated to different temperatures (200, 400, 600, and 800 °C). The uniaxial compressive strength (UCS) and elastic modulus of unheated and heated samples were determined as important mechanical properties. In addition, the effect of temperature on the physical properties of rhyolite rock (density, color, and absorption) was investigated in conjunction with its microstructural properties. The hardening of the rhyolitic rock samples was observed below 600 °C, at which point the UCS and elastic modulus decreased to 78.0% and 75.9%, respectively, at 800 °C. The results also show that heating does not significantly affect the density and volume of permeable pore space, but a color change can be observed at 400 °C and above. A microscopic analysis shows the change in microstructural properties of rhyolite rock after heating to 600 °C. Furthermore, the SEM observations of heated materials show structural particle displacements and microcracking, leading to apparent surface cracks. |
format | Online Article Text |
id | pubmed-9101199 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | MDPI |
record_format | MEDLINE/PubMed |
spelling | pubmed-91011992022-05-14 Effect of Elevated Temperature on Rhyolitic Rocks’ Properties Ahmed, Haitham M. Hefni, Mohammed A. Ahmed, Hussin A. M. Adewuyi, Sefiu O. Hassani, Ferri Sasmito, Agus P. Saleem, Hussein A. Moustafa, Essam B. Hassan, Gamal S. A. Materials (Basel) Article The effect of high temperatures on rock’s thermophysical and mechanical properties is critical to the design of underground geotechnical applications. The current work investigates the impact of temperature on rhyolitic turf rock’s physical and mechanical properties. Intact cylindrical core rock samples were heated to different temperatures (200, 400, 600, and 800 °C). The uniaxial compressive strength (UCS) and elastic modulus of unheated and heated samples were determined as important mechanical properties. In addition, the effect of temperature on the physical properties of rhyolite rock (density, color, and absorption) was investigated in conjunction with its microstructural properties. The hardening of the rhyolitic rock samples was observed below 600 °C, at which point the UCS and elastic modulus decreased to 78.0% and 75.9%, respectively, at 800 °C. The results also show that heating does not significantly affect the density and volume of permeable pore space, but a color change can be observed at 400 °C and above. A microscopic analysis shows the change in microstructural properties of rhyolite rock after heating to 600 °C. Furthermore, the SEM observations of heated materials show structural particle displacements and microcracking, leading to apparent surface cracks. MDPI 2022-04-29 /pmc/articles/PMC9101199/ /pubmed/35591538 http://dx.doi.org/10.3390/ma15093204 Text en © 2022 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). |
spellingShingle | Article Ahmed, Haitham M. Hefni, Mohammed A. Ahmed, Hussin A. M. Adewuyi, Sefiu O. Hassani, Ferri Sasmito, Agus P. Saleem, Hussein A. Moustafa, Essam B. Hassan, Gamal S. A. Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title | Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title_full | Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title_fullStr | Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title_full_unstemmed | Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title_short | Effect of Elevated Temperature on Rhyolitic Rocks’ Properties |
title_sort | effect of elevated temperature on rhyolitic rocks’ properties |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9101199/ https://www.ncbi.nlm.nih.gov/pubmed/35591538 http://dx.doi.org/10.3390/ma15093204 |
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