Soil cracking propagation due to dryness and its relation to suction

Investigation of Crack Intensity Factor is essential as it affects the mechanical and hydraulic behaviour of soils. Soil water coming from the wet seasons or from the water table, is removed by evaporation during the driest season. The loss of water provokes a significant increase in suction. When i...

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Main Authors: Oliveira Elisangela do Prado, Soecki Karoline, Faro Vitor Pereira, Kormann Alessander Christopher Morales
Format: Article
Language:English
Published: EDP Sciences 2021-01-01
Series:MATEC Web of Conferences
Online Access:https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_01021.pdf
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spelling doaj-70e9e627f6984525920bc3e93e2c126c2021-05-04T12:21:53ZengEDP SciencesMATEC Web of Conferences2261-236X2021-01-013370102110.1051/matecconf/202133701021matecconf_PanAm-Unsat2021_01021Soil cracking propagation due to dryness and its relation to suctionOliveira Elisangela do PradoSoecki Karoline0Faro Vitor Pereira1Kormann Alessander Christopher Morales2Federal University of Paraná, Pontal do Paraná Campus, Center for Marine StudiesGraduate Program in Civil Construction Engineering, Federal University of ParanáGraduate Program in Civil Construction Engineering, Federal University of ParanáInvestigation of Crack Intensity Factor is essential as it affects the mechanical and hydraulic behaviour of soils. Soil water coming from the wet seasons or from the water table, is removed by evaporation during the driest season. The loss of water provokes a significant increase in suction. When it exceeds the tensile strength of the soil, cracks occur that can modify the mechanical and mainly hydraulic properties of the soil, creating preferred paths for water infiltration. Little research is conducted on quantifying cracking in soil relating it to its hydraulic properties. This research aims to investigate the cracking of soils with focus on analysing its relation to water content and soil suction. Soils from a specific region in Brazil with clay predominance are collected and characterized. Unsaturated soil specimens are prepared and subjected to environmental real conditions in order to progressively check the consequences caused by the environment in soils with different clay content during four weeks. The Crack Intensity Factor is measured along the time through image processing. The water content is monitored through volume water content sensors. The measured results are evaluated to correlate crack intensity factor as function of weather variables and soil water content.https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_01021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Oliveira Elisangela do Prado
Soecki Karoline
Faro Vitor Pereira
Kormann Alessander Christopher Morales
spellingShingle Oliveira Elisangela do Prado
Soecki Karoline
Faro Vitor Pereira
Kormann Alessander Christopher Morales
Soil cracking propagation due to dryness and its relation to suction
MATEC Web of Conferences
author_facet Oliveira Elisangela do Prado
Soecki Karoline
Faro Vitor Pereira
Kormann Alessander Christopher Morales
author_sort Oliveira Elisangela do Prado
title Soil cracking propagation due to dryness and its relation to suction
title_short Soil cracking propagation due to dryness and its relation to suction
title_full Soil cracking propagation due to dryness and its relation to suction
title_fullStr Soil cracking propagation due to dryness and its relation to suction
title_full_unstemmed Soil cracking propagation due to dryness and its relation to suction
title_sort soil cracking propagation due to dryness and its relation to suction
publisher EDP Sciences
series MATEC Web of Conferences
issn 2261-236X
publishDate 2021-01-01
description Investigation of Crack Intensity Factor is essential as it affects the mechanical and hydraulic behaviour of soils. Soil water coming from the wet seasons or from the water table, is removed by evaporation during the driest season. The loss of water provokes a significant increase in suction. When it exceeds the tensile strength of the soil, cracks occur that can modify the mechanical and mainly hydraulic properties of the soil, creating preferred paths for water infiltration. Little research is conducted on quantifying cracking in soil relating it to its hydraulic properties. This research aims to investigate the cracking of soils with focus on analysing its relation to water content and soil suction. Soils from a specific region in Brazil with clay predominance are collected and characterized. Unsaturated soil specimens are prepared and subjected to environmental real conditions in order to progressively check the consequences caused by the environment in soils with different clay content during four weeks. The Crack Intensity Factor is measured along the time through image processing. The water content is monitored through volume water content sensors. The measured results are evaluated to correlate crack intensity factor as function of weather variables and soil water content.
url https://www.matec-conferences.org/articles/matecconf/pdf/2021/06/matecconf_PanAm-Unsat2021_01021.pdf
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AT soeckikaroline soilcrackingpropagationduetodrynessanditsrelationtosuction
AT farovitorpereira soilcrackingpropagationduetodrynessanditsrelationtosuction
AT kormannalessanderchristophermorales soilcrackingpropagationduetodrynessanditsrelationtosuction
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