Impact of water–rock interaction on the pore structures of red-bed soft rock
Abstract The physical and mechanical properties of the reservoir bank slope are affected by the water–rock interaction. However, few studies considered the impact of long-term water–rock interaction on the evolution law of mesostructure. Therefore, in this study, the water–rock interaction test was...
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2021-04-01
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Online Access: | https://doi.org/10.1038/s41598-021-86815-w |
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doaj-2c871573f2004cee91d919c6b452eb482021-04-04T11:33:32ZengNature Publishing GroupScientific Reports2045-23222021-04-0111111510.1038/s41598-021-86815-wImpact of water–rock interaction on the pore structures of red-bed soft rockMeiling Zhou0Jianlin Li1Zuosen Luo2Jianbin Sun3Feng Xu4Qiao Jiang5Huafeng Deng6Key Laboratory of Geological Hazards on Three Gorges Reservoir Area of Ministry of Education, China Three Gorges UniversityKey Laboratory of Geological Hazards on Three Gorges Reservoir Area of Ministry of Education, China Three Gorges UniversityKey Laboratory of Geological Hazards on Three Gorges Reservoir Area of Ministry of Education, China Three Gorges UniversityChina International Water and Electric Co., Ltd.China International Water and Electric Co., Ltd.China Three Gorges Projects Development Co., Ltd.Key Laboratory of Geological Hazards on Three Gorges Reservoir Area of Ministry of Education, China Three Gorges UniversityAbstract The physical and mechanical properties of the reservoir bank slope are affected by the water–rock interaction. However, few studies considered the impact of long-term water–rock interaction on the evolution law of mesostructure. Therefore, in this study, the water–rock interaction test was conducted on a slightly weathered red-bed soft rock from the Three Gorges Reservoir area, considering the fluctuation in the reservoir water level. The corresponding pore structure parameters were measured and analyzed based on a scanning electron microscope (SEM) and digital image processing technology. The study showed that: (1) The pore size has been gradually increased, while the number of pores was increased initially and then decreased. Within 12 cycles, the maximum and average pore radius of the rock specimens was increased by 101.02% and 43.32%, respectively, and the porosity has been increased by 26.59%, whereas the number of pores decreased by 22.65%. This indicates the effect of water–rock interaction on the propagation of pores. (2) The pores were changed from oblate to slender by the water–rock interaction. The shape factor was decreased by about 15.79% within 12 cycles. In the meantime, the fractal dimension was increased from 1.20 to 1.28, and more complex structures of pores were observed. (3) The porosity evolution model for the red-bed soft rock was established based on the curve fitting technique. The results can be used as a reference to conceptualize the mesostructure damage of rocks under water–rock interaction.https://doi.org/10.1038/s41598-021-86815-w |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Meiling Zhou Jianlin Li Zuosen Luo Jianbin Sun Feng Xu Qiao Jiang Huafeng Deng |
spellingShingle |
Meiling Zhou Jianlin Li Zuosen Luo Jianbin Sun Feng Xu Qiao Jiang Huafeng Deng Impact of water–rock interaction on the pore structures of red-bed soft rock Scientific Reports |
author_facet |
Meiling Zhou Jianlin Li Zuosen Luo Jianbin Sun Feng Xu Qiao Jiang Huafeng Deng |
author_sort |
Meiling Zhou |
title |
Impact of water–rock interaction on the pore structures of red-bed soft rock |
title_short |
Impact of water–rock interaction on the pore structures of red-bed soft rock |
title_full |
Impact of water–rock interaction on the pore structures of red-bed soft rock |
title_fullStr |
Impact of water–rock interaction on the pore structures of red-bed soft rock |
title_full_unstemmed |
Impact of water–rock interaction on the pore structures of red-bed soft rock |
title_sort |
impact of water–rock interaction on the pore structures of red-bed soft rock |
publisher |
Nature Publishing Group |
series |
Scientific Reports |
issn |
2045-2322 |
publishDate |
2021-04-01 |
description |
Abstract The physical and mechanical properties of the reservoir bank slope are affected by the water–rock interaction. However, few studies considered the impact of long-term water–rock interaction on the evolution law of mesostructure. Therefore, in this study, the water–rock interaction test was conducted on a slightly weathered red-bed soft rock from the Three Gorges Reservoir area, considering the fluctuation in the reservoir water level. The corresponding pore structure parameters were measured and analyzed based on a scanning electron microscope (SEM) and digital image processing technology. The study showed that: (1) The pore size has been gradually increased, while the number of pores was increased initially and then decreased. Within 12 cycles, the maximum and average pore radius of the rock specimens was increased by 101.02% and 43.32%, respectively, and the porosity has been increased by 26.59%, whereas the number of pores decreased by 22.65%. This indicates the effect of water–rock interaction on the propagation of pores. (2) The pores were changed from oblate to slender by the water–rock interaction. The shape factor was decreased by about 15.79% within 12 cycles. In the meantime, the fractal dimension was increased from 1.20 to 1.28, and more complex structures of pores were observed. (3) The porosity evolution model for the red-bed soft rock was established based on the curve fitting technique. The results can be used as a reference to conceptualize the mesostructure damage of rocks under water–rock interaction. |
url |
https://doi.org/10.1038/s41598-021-86815-w |
work_keys_str_mv |
AT meilingzhou impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT jianlinli impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT zuosenluo impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT jianbinsun impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT fengxu impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT qiaojiang impactofwaterrockinteractionontheporestructuresofredbedsoftrock AT huafengdeng impactofwaterrockinteractionontheporestructuresofredbedsoftrock |
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