Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite
This paper aims to study the effect of cyclic heating and flowing-water cooling conditions on the physical properties of granite. Ultrasonic tests, gas measured porosity, permeability, and microscope observations were conducted on granite after thermal treatment. The results showed that the velocity...
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doaj-bf24eaa5985c4f8fbc61d8d943d568092020-11-25T02:36:29ZengMDPI AGEnergies1996-10732020-04-01132136213610.3390/en13092136Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of GraniteXiangchao Shi0Leiyu Gao1Jie Wu2Cheng Zhu3Shuai Chen4Xiao Zhuo5State Key Lab of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, ChinaState Key Lab of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, ChinaState Key Lab of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, ChinaDepartment of Civil & Environmental Engineering, Rowan University, Glassboro, NJ 08028, USAState Key Lab of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, ChinaState Key Lab of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu 610500, ChinaThis paper aims to study the effect of cyclic heating and flowing-water cooling conditions on the physical properties of granite. Ultrasonic tests, gas measured porosity, permeability, and microscope observations were conducted on granite after thermal treatment. The results showed that the velocity of P- and S-waves decreased as the number of thermal cycles increased. The porosity increased with the number of the thermal cycles attained at 600 °C, while no apparent changes were observed at 200 and 400 °C. The permeability increased with the increasing number of thermal cycles. Furthermore, microscope observations showed that degradation of the granite after thermal treatment was attributed to a large network of microcracks induced by thermal stress. As the number of thermal cycles increased, the number of transgranular microcracks gradually increased, as well as their length and width. The quantification of microcracks from cast thin section (CTS) images supported the visual observation.https://www.mdpi.com/1996-1073/13/9/2136granitephysical characteristicscyclicthermal treatmentwater cooling |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Xiangchao Shi Leiyu Gao Jie Wu Cheng Zhu Shuai Chen Xiao Zhuo |
spellingShingle |
Xiangchao Shi Leiyu Gao Jie Wu Cheng Zhu Shuai Chen Xiao Zhuo Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite Energies granite physical characteristics cyclic thermal treatment water cooling |
author_facet |
Xiangchao Shi Leiyu Gao Jie Wu Cheng Zhu Shuai Chen Xiao Zhuo |
author_sort |
Xiangchao Shi |
title |
Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite |
title_short |
Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite |
title_full |
Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite |
title_fullStr |
Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite |
title_full_unstemmed |
Effects of Cyclic Heating and Water Cooling on the Physical Characteristics of Granite |
title_sort |
effects of cyclic heating and water cooling on the physical characteristics of granite |
publisher |
MDPI AG |
series |
Energies |
issn |
1996-1073 |
publishDate |
2020-04-01 |
description |
This paper aims to study the effect of cyclic heating and flowing-water cooling conditions on the physical properties of granite. Ultrasonic tests, gas measured porosity, permeability, and microscope observations were conducted on granite after thermal treatment. The results showed that the velocity of P- and S-waves decreased as the number of thermal cycles increased. The porosity increased with the number of the thermal cycles attained at 600 °C, while no apparent changes were observed at 200 and 400 °C. The permeability increased with the increasing number of thermal cycles. Furthermore, microscope observations showed that degradation of the granite after thermal treatment was attributed to a large network of microcracks induced by thermal stress. As the number of thermal cycles increased, the number of transgranular microcracks gradually increased, as well as their length and width. The quantification of microcracks from cast thin section (CTS) images supported the visual observation. |
topic |
granite physical characteristics cyclic thermal treatment water cooling |
url |
https://www.mdpi.com/1996-1073/13/9/2136 |
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