Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China

Abstract Superficial weathering in the form of granular disaggregation, powdering and flaking on stone surface is one of the most serious damages to stone heritages, since the surface carries most of the artistic, historical information. The determination of the thickness of the superficially weathe...

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Main Authors: Xuemei Wang, Hongjie Luo, Haidong Yu, Can Xiong, Hui Dai, Bo Rong, Xiao Huang
Format: Article
Language:English
Published: SpringerOpen 2024-03-01
Series:Heritage Science
Subjects:
Online Access:https://doi.org/10.1186/s40494-024-01206-4
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author Xuemei Wang
Hongjie Luo
Haidong Yu
Can Xiong
Hui Dai
Bo Rong
Xiao Huang
author_facet Xuemei Wang
Hongjie Luo
Haidong Yu
Can Xiong
Hui Dai
Bo Rong
Xiao Huang
author_sort Xuemei Wang
collection DOAJ
description Abstract Superficial weathering in the form of granular disaggregation, powdering and flaking on stone surface is one of the most serious damages to stone heritages, since the surface carries most of the artistic, historical information. The determination of the thickness of the superficially weathered layer of historical stones is critical to their conservation. However, the methodology for quantitative analyses of such thickness remains very limited. In this study, we carefully study the vapor absorption and pore structure evolution of historical sandstones from Guanzhong area with respect to their weathering. We find out that the thickness of superficial weathered layer of Guanzhong sandstones can be derived by following the changes in vapor absorption or pore structure. Such data achieved from various methods developed in this work are consistent with each other and in good agreement with the results obtained by using current techniques such as drilling resistance measurement, the Ruxton method and ultrasonic testing. Among all methods used, pore size distribution analysis requires less sample preparation and measures the thickness of superficial weathered layer of Guanzhong sandstones around 7 mm.
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spelling doaj.art-82cafbc98f084172b0a97076ed5391532024-03-24T12:29:00ZengSpringerOpenHeritage Science2050-74452024-03-0112111010.1186/s40494-024-01206-4Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in ChinaXuemei Wang0Hongjie Luo1Haidong Yu2Can Xiong3Hui Dai4Bo Rong5Xiao Huang6School of Materials Science and Engineering, Shanghai UniversitySchool of Materials Science and Engineering, Shanghai UniversityChongqing Key Laboratory of Paleontology and Paleoenvironment Co-evolution (Sichuan-Chongqing Joint Construction)Chongqing Key Laboratory of Paleontology and Paleoenvironment Co-evolution (Sichuan-Chongqing Joint Construction)Chongqing Key Laboratory of Paleontology and Paleoenvironment Co-evolution (Sichuan-Chongqing Joint Construction)School of Materials Science and Engineering, Shanghai UniversityInstitute for the Conservation of Cultural Heritage, Shanghai UniversityAbstract Superficial weathering in the form of granular disaggregation, powdering and flaking on stone surface is one of the most serious damages to stone heritages, since the surface carries most of the artistic, historical information. The determination of the thickness of the superficially weathered layer of historical stones is critical to their conservation. However, the methodology for quantitative analyses of such thickness remains very limited. In this study, we carefully study the vapor absorption and pore structure evolution of historical sandstones from Guanzhong area with respect to their weathering. We find out that the thickness of superficial weathered layer of Guanzhong sandstones can be derived by following the changes in vapor absorption or pore structure. Such data achieved from various methods developed in this work are consistent with each other and in good agreement with the results obtained by using current techniques such as drilling resistance measurement, the Ruxton method and ultrasonic testing. Among all methods used, pore size distribution analysis requires less sample preparation and measures the thickness of superficial weathered layer of Guanzhong sandstones around 7 mm.https://doi.org/10.1186/s40494-024-01206-4Superficial weatheringVapor absorptionPore structureThickness of weathered layer
spellingShingle Xuemei Wang
Hongjie Luo
Haidong Yu
Can Xiong
Hui Dai
Bo Rong
Xiao Huang
Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
Heritage Science
Superficial weathering
Vapor absorption
Pore structure
Thickness of weathered layer
title Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
title_full Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
title_fullStr Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
title_full_unstemmed Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
title_short Determination on the thickness of superficially weathered layer of historical stones from Guanzhong area in China
title_sort determination on the thickness of superficially weathered layer of historical stones from guanzhong area in china
topic Superficial weathering
Vapor absorption
Pore structure
Thickness of weathered layer
url https://doi.org/10.1186/s40494-024-01206-4
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