Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China

Abstract Granite residual soil in south and southeast China has obvious characteristic of disintegration, which induces collapse erosion and shallow landslide. Although the escape of pore air can be observed in the present hydrostatic water tests, and pore air and cementitious substance dissolution...

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Main Authors: Liping Liao, Dongming Yi, Yinghui Tan, Shaokun Ma, Yunchuan Yang, Zhengwei Liu
Format: Article
Language:English
Published: Nature Portfolio 2025-03-01
Series:Scientific Reports
Subjects:
Online Access:https://doi.org/10.1038/s41598-025-92578-5
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author Liping Liao
Dongming Yi
Yinghui Tan
Shaokun Ma
Yunchuan Yang
Zhengwei Liu
author_facet Liping Liao
Dongming Yi
Yinghui Tan
Shaokun Ma
Yunchuan Yang
Zhengwei Liu
author_sort Liping Liao
collection DOAJ
description Abstract Granite residual soil in south and southeast China has obvious characteristic of disintegration, which induces collapse erosion and shallow landslide. Although the escape of pore air can be observed in the present hydrostatic water tests, and pore air and cementitious substance dissolution is qualitatively confirmed to promote soil disintegration, these two factors fail to be monitored in real time throughout the whole disintegration process. Therefore, this study utilized two self-developed instruments to monitor the volume of escaping pore air and the process of soil disintegration, and observe the current variations in the solution during the soil disintegration. The disintegration patterns and rates of residual soils with various compaction levels and initial moisture contents were analyzed. The intrinsic affecting mechanisms of pore air escape and cementitious substance dissolution on the soil disintegration were revealed. The results consist of three aspects. (1) The initial moisture content has a significant impact on disintegration pattern, completion time and velocity. (2) The variance in the effect of the increase in compaction degree on the completion time and speed of disintegration is governed by the initial moisture content. (3) The escape of pore air and the dissolution of cementitious substances constitute two principal phenomena during the entire disintegration process of granite residual soil. (4) The repulsive stress generated by the compressed and escaping pore air being greater than the sum of suction stress and viscous stress generated by capillary water and cementitious substance is one of the primary causes for granite residual soil disintegration.
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spelling doaj-art-e7bf74d3125d427a871a9665188fcc952025-08-20T02:10:23ZengNature PortfolioScientific Reports2045-23222025-03-0115111410.1038/s41598-025-92578-5Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast ChinaLiping Liao0Dongming Yi1Yinghui Tan2Shaokun Ma3Yunchuan Yang4Zhengwei Liu5College of Civil Engineering and Architecture, Guangxi UniversityCollege of Civil Engineering and Architecture, Guangxi UniversityCollege of Civil Engineering and Architecture, Guangxi UniversityCollege of Civil Engineering and Architecture, Guangxi UniversityCollege of Civil Engineering and Architecture, Guangxi UniversityCollege of Civil Engineering and Architecture, Guangxi UniversityAbstract Granite residual soil in south and southeast China has obvious characteristic of disintegration, which induces collapse erosion and shallow landslide. Although the escape of pore air can be observed in the present hydrostatic water tests, and pore air and cementitious substance dissolution is qualitatively confirmed to promote soil disintegration, these two factors fail to be monitored in real time throughout the whole disintegration process. Therefore, this study utilized two self-developed instruments to monitor the volume of escaping pore air and the process of soil disintegration, and observe the current variations in the solution during the soil disintegration. The disintegration patterns and rates of residual soils with various compaction levels and initial moisture contents were analyzed. The intrinsic affecting mechanisms of pore air escape and cementitious substance dissolution on the soil disintegration were revealed. The results consist of three aspects. (1) The initial moisture content has a significant impact on disintegration pattern, completion time and velocity. (2) The variance in the effect of the increase in compaction degree on the completion time and speed of disintegration is governed by the initial moisture content. (3) The escape of pore air and the dissolution of cementitious substances constitute two principal phenomena during the entire disintegration process of granite residual soil. (4) The repulsive stress generated by the compressed and escaping pore air being greater than the sum of suction stress and viscous stress generated by capillary water and cementitious substance is one of the primary causes for granite residual soil disintegration.https://doi.org/10.1038/s41598-025-92578-5Granite residual soilPore air escapeCement dissolutionDisintegration mechanism
spellingShingle Liping Liao
Dongming Yi
Yinghui Tan
Shaokun Ma
Yunchuan Yang
Zhengwei Liu
Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
Scientific Reports
Granite residual soil
Pore air escape
Cement dissolution
Disintegration mechanism
title Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
title_full Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
title_fullStr Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
title_full_unstemmed Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
title_short Effect of pore air escape and cement dissolution on granite residual soil disintegration, southeast China
title_sort effect of pore air escape and cement dissolution on granite residual soil disintegration southeast china
topic Granite residual soil
Pore air escape
Cement dissolution
Disintegration mechanism
url https://doi.org/10.1038/s41598-025-92578-5
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AT yinghuitan effectofporeairescapeandcementdissolutionongraniteresidualsoildisintegrationsoutheastchina
AT shaokunma effectofporeairescapeandcementdissolutionongraniteresidualsoildisintegrationsoutheastchina
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