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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Main Authors: Xiangchao Shi, Leiyu Gao, Jie Wu, Cheng Zhu, Shuai Chen, Xiao Zhuo
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Energies
Subjects:
Online Access:https://www.mdpi.com/1996-1073/13/9/2136
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spelling 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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