Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas

Abstract Background Drying and rewetting process, frequently occurred during climatic changes, is an important process in soil aggregate slacking and dissolution. The severer interference of human activities on global climate makes the extreme climate scenarios like drought and rainstorm occur frequ...

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Main Authors: Jie Xu, Yiqun Tang, Jie Zhou
Format: Article
Language:English
Published: SpringerOpen 2017-09-01
Series:Geoenvironmental Disasters
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40677-017-0084-y
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spelling doaj-249c886094a143e591337e5aebbe41132020-11-24T21:36:20ZengSpringerOpenGeoenvironmental Disasters2197-86702017-09-014111310.1186/s40677-017-0084-yEffect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areasJie Xu0Yiqun Tang1Jie Zhou2Department of Geotechnical Engineering, Tongji UniversityDepartment of Geotechnical Engineering, Tongji UniversityDepartment of Geotechnical Engineering, Tongji UniversityAbstract Background Drying and rewetting process, frequently occurred during climatic changes, is an important process in soil aggregate slacking and dissolution. The severer interference of human activities on global climate makes the extreme climate scenarios like drought and rainstorm occur frequently. Therefore, there is necessity to further our understanding on the impact of the drying–wetting cycles and initial water content on the breakdown of soil aggregates. The typical yellow–brown earth composed of water–stable and water–unstable aggregates is selected. Variations of water-stable aggregate size distributions after drying-wetting cycles are measured by wet sieving, under variable initial water content and cycles respectively. Results Drying-wetting cycles cause a significant aggregate slaking, especially within the first two cycles. After that, most aggregates show more slacking resistant. The variation curves of the proportion of water-stable aggregates with the size 1–5 mm shows a coexistence of slaking process and supplement. The critical initial water content (about 24%) and turning point (with the aggregate size of 0.3 mm) are proposed to describe the effects of initial water content on size distribution of water-stable aggregates. Overall, the increase of initial water content strengths the water stability. In addition, the mathematical model for the relative leakage ratio based on the drying–wetting cycle, initial water content and size distribution are established. Conclusions The findings reported in this paper may be capable of supporting the intensive study for the breakdown mechanism and assessing the leakage potential under the influence of climate change. However, there exists a certain mismatch between the drying-wetting cycles in the tests and in practice, mainly in the frequency and intensity, which should be paid more attention.http://link.springer.com/article/10.1186/s40677-017-0084-yDrying–wetting cyclesYellow–brown earthsWater stabilityAggregate breakdownRelative leakage ratio
collection DOAJ
language English
format Article
sources DOAJ
author Jie Xu
Yiqun Tang
Jie Zhou
spellingShingle Jie Xu
Yiqun Tang
Jie Zhou
Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
Geoenvironmental Disasters
Drying–wetting cycles
Yellow–brown earths
Water stability
Aggregate breakdown
Relative leakage ratio
author_facet Jie Xu
Yiqun Tang
Jie Zhou
author_sort Jie Xu
title Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
title_short Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
title_full Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
title_fullStr Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
title_full_unstemmed Effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
title_sort effect of drying–wetting cycles on aggregate breakdown for yellow–brown earths in karst areas
publisher SpringerOpen
series Geoenvironmental Disasters
issn 2197-8670
publishDate 2017-09-01
description Abstract Background Drying and rewetting process, frequently occurred during climatic changes, is an important process in soil aggregate slacking and dissolution. The severer interference of human activities on global climate makes the extreme climate scenarios like drought and rainstorm occur frequently. Therefore, there is necessity to further our understanding on the impact of the drying–wetting cycles and initial water content on the breakdown of soil aggregates. The typical yellow–brown earth composed of water–stable and water–unstable aggregates is selected. Variations of water-stable aggregate size distributions after drying-wetting cycles are measured by wet sieving, under variable initial water content and cycles respectively. Results Drying-wetting cycles cause a significant aggregate slaking, especially within the first two cycles. After that, most aggregates show more slacking resistant. The variation curves of the proportion of water-stable aggregates with the size 1–5 mm shows a coexistence of slaking process and supplement. The critical initial water content (about 24%) and turning point (with the aggregate size of 0.3 mm) are proposed to describe the effects of initial water content on size distribution of water-stable aggregates. Overall, the increase of initial water content strengths the water stability. In addition, the mathematical model for the relative leakage ratio based on the drying–wetting cycle, initial water content and size distribution are established. Conclusions The findings reported in this paper may be capable of supporting the intensive study for the breakdown mechanism and assessing the leakage potential under the influence of climate change. However, there exists a certain mismatch between the drying-wetting cycles in the tests and in practice, mainly in the frequency and intensity, which should be paid more attention.
topic Drying–wetting cycles
Yellow–brown earths
Water stability
Aggregate breakdown
Relative leakage ratio
url http://link.springer.com/article/10.1186/s40677-017-0084-y
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AT yiquntang effectofdryingwettingcyclesonaggregatebreakdownforyellowbrownearthsinkarstareas
AT jiezhou effectofdryingwettingcyclesonaggregatebreakdownforyellowbrownearthsinkarstareas
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