Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts

A study of the weathering process of three types of stones, sandstone, marble, and granite, which are commonly found in artifacts worldwide, is presented. Freeze–thaw cycles are used to accelerate changes in the stone’s physical properties, such as the surface morphology, mass, and porosity. Pulsed...

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Main Authors: Jia’nan Zhang, Xue Yang, Beichen Chen, Xiangyu Wang, Gangbo Hu, Ning Tao, Jiangang Sun
Format: Article
Language:English
Published: MDPI AG 2023-03-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/14/4/666
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author Jia’nan Zhang
Xue Yang
Beichen Chen
Xiangyu Wang
Gangbo Hu
Ning Tao
Jiangang Sun
author_facet Jia’nan Zhang
Xue Yang
Beichen Chen
Xiangyu Wang
Gangbo Hu
Ning Tao
Jiangang Sun
author_sort Jia’nan Zhang
collection DOAJ
description A study of the weathering process of three types of stones, sandstone, marble, and granite, which are commonly found in artifacts worldwide, is presented. Freeze–thaw cycles are used to accelerate changes in the stone’s physical properties, such as the surface morphology, mass, and porosity. Pulsed infrared thermography, as an in situ non-destructive testing method, is adopted to measure the stone’s thermal properties, such as the diffusivity, effusivity, and conductivity. These thermal parameters influence the natural weathering process, and in turn can change with the decay of the stone materials. Preliminary experimental results show that all three types of stone experience a process of mass loss and porosity increase after the freeze–thaw cycles, and their thermal properties change differently depending on their types. Since the thermal effusivity can be obtained non-destructively by reflectance thermography, we propose for the first time the use of thermal effusivity to characterize the influence of the weathering process and as an indicator of the aging degree of stone artifacts.
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spelling doaj.art-7971a2f3ae7f47599d9f3fb92dd7d2a62023-11-17T18:17:05ZengMDPI AGAtmosphere2073-44332023-03-0114466610.3390/atmos14040666Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone ArtifactsJia’nan Zhang0Xue Yang1Beichen Chen2Xiangyu Wang3Gangbo Hu4Ning Tao5Jiangang Sun6School of History, Capital Normal University, Beijing 100089, ChinaKey Laboratory of Terahertz Optoelectronics, Ministry of Education, Beijing Advanced Innovation Center for Imaging Theory and Technology, Department of Physics, Capital Normal University, Beijing 100048, ChinaSchool of History, Capital Normal University, Beijing 100089, ChinaKey Laboratory of Terahertz Optoelectronics, Ministry of Education, Beijing Advanced Innovation Center for Imaging Theory and Technology, Department of Physics, Capital Normal University, Beijing 100048, ChinaKey Laboratory of Terahertz Optoelectronics, Ministry of Education, Beijing Advanced Innovation Center for Imaging Theory and Technology, Department of Physics, Capital Normal University, Beijing 100048, ChinaKey Laboratory of Terahertz Optoelectronics, Ministry of Education, Beijing Advanced Innovation Center for Imaging Theory and Technology, Department of Physics, Capital Normal University, Beijing 100048, ChinaKey Laboratory of Terahertz Optoelectronics, Ministry of Education, Beijing Advanced Innovation Center for Imaging Theory and Technology, Department of Physics, Capital Normal University, Beijing 100048, ChinaA study of the weathering process of three types of stones, sandstone, marble, and granite, which are commonly found in artifacts worldwide, is presented. Freeze–thaw cycles are used to accelerate changes in the stone’s physical properties, such as the surface morphology, mass, and porosity. Pulsed infrared thermography, as an in situ non-destructive testing method, is adopted to measure the stone’s thermal properties, such as the diffusivity, effusivity, and conductivity. These thermal parameters influence the natural weathering process, and in turn can change with the decay of the stone materials. Preliminary experimental results show that all three types of stone experience a process of mass loss and porosity increase after the freeze–thaw cycles, and their thermal properties change differently depending on their types. Since the thermal effusivity can be obtained non-destructively by reflectance thermography, we propose for the first time the use of thermal effusivity to characterize the influence of the weathering process and as an indicator of the aging degree of stone artifacts.https://www.mdpi.com/2073-4433/14/4/666stone artifactfreeze–thaw cycleweatheringporosityinfrared thermographythermal diffusivity
spellingShingle Jia’nan Zhang
Xue Yang
Beichen Chen
Xiangyu Wang
Gangbo Hu
Ning Tao
Jiangang Sun
Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
Atmosphere
stone artifact
freeze–thaw cycle
weathering
porosity
infrared thermography
thermal diffusivity
title Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
title_full Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
title_fullStr Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
title_full_unstemmed Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
title_short Study of the Freeze–Thaw Weathering’s Influence on Thermal Properties of Stone Artifacts
title_sort study of the freeze thaw weathering s influence on thermal properties of stone artifacts
topic stone artifact
freeze–thaw cycle
weathering
porosity
infrared thermography
thermal diffusivity
url https://www.mdpi.com/2073-4433/14/4/666
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AT xiangyuwang studyofthefreezethawweatheringsinfluenceonthermalpropertiesofstoneartifacts
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