Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil

Flood season embankment due to long-term high water immersion environment creates situations where its soil properties will deteriorate, quickly triggering bank slope instability and other dangerous situations. In order to study embankment slope soil in the disintegration and permeability characteri...

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Main Authors: Kun Zhang, Di Feng
Format: Article
Language:English
Published: MDPI AG 2023-08-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/13/17/9819
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author Kun Zhang
Di Feng
author_facet Kun Zhang
Di Feng
author_sort Kun Zhang
collection DOAJ
description Flood season embankment due to long-term high water immersion environment creates situations where its soil properties will deteriorate, quickly triggering bank slope instability and other dangerous situations. In order to study embankment slope soil in the disintegration and permeability characteristics under the long-term water immersion process, disintegration tests and variable head infiltration tests were carried out on embankment-disturbed clays in Jiangxinzhou, Nanjing, Jiangsu Province, China. The results showed that the disintegration rate decreased with increasing dry density. Moreover, the samples gained weight quickly when the water content was low. Moreover, there is a threshold water content of around 20%, and it is assumed that the disintegration pattern of the soil may be significantly different depending on the optimum moisture content. The effect of moisture content on the disintegration of the samples was more significant. There were three main typical disintegration modes of the samples. The primary influencing factors resulting in the various disintegration patterns are the soil matrix suction, the change in consistency following water immersion, and the water membrane on the surface of the clay particles. The coefficient of permeability decreases with increasing dry density, and the variation of the coefficient of permeability with dry density coincides with the exponential function relationship. Long-term immersion conditions will change the permeability of the soil. An electron microscope test of immersed and unimmersed samples shows that the internal structure change is an essential factor affecting the permeability. After water immersion, with the dissolution of cementing material between soil particles, the particles move to fill the intergranular pore space so that the permeability coefficient decreases.
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spelling doaj.art-ea15d0f512be461c9b470584ee6f78282023-11-19T07:52:14ZengMDPI AGApplied Sciences2076-34172023-08-011317981910.3390/app13179819Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment SoilKun Zhang0Di Feng1Department of Civil and Transportation Engineering, Hohai University, Nanjing 210098, ChinaDepartment of Civil and Transportation Engineering, Hohai University, Nanjing 210098, ChinaFlood season embankment due to long-term high water immersion environment creates situations where its soil properties will deteriorate, quickly triggering bank slope instability and other dangerous situations. In order to study embankment slope soil in the disintegration and permeability characteristics under the long-term water immersion process, disintegration tests and variable head infiltration tests were carried out on embankment-disturbed clays in Jiangxinzhou, Nanjing, Jiangsu Province, China. The results showed that the disintegration rate decreased with increasing dry density. Moreover, the samples gained weight quickly when the water content was low. Moreover, there is a threshold water content of around 20%, and it is assumed that the disintegration pattern of the soil may be significantly different depending on the optimum moisture content. The effect of moisture content on the disintegration of the samples was more significant. There were three main typical disintegration modes of the samples. The primary influencing factors resulting in the various disintegration patterns are the soil matrix suction, the change in consistency following water immersion, and the water membrane on the surface of the clay particles. The coefficient of permeability decreases with increasing dry density, and the variation of the coefficient of permeability with dry density coincides with the exponential function relationship. Long-term immersion conditions will change the permeability of the soil. An electron microscope test of immersed and unimmersed samples shows that the internal structure change is an essential factor affecting the permeability. After water immersion, with the dissolution of cementing material between soil particles, the particles move to fill the intergranular pore space so that the permeability coefficient decreases.https://www.mdpi.com/2076-3417/13/17/9819disintegration characteristicsdisintegration modeslong-term immersionpermeabilityslope instability
spellingShingle Kun Zhang
Di Feng
Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
Applied Sciences
disintegration characteristics
disintegration modes
long-term immersion
permeability
slope instability
title Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
title_full Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
title_fullStr Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
title_full_unstemmed Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
title_short Study on Disintegration and Infiltration Characteristics of Nanjing Jiangxinzhou Embankment Soil
title_sort study on disintegration and infiltration characteristics of nanjing jiangxinzhou embankment soil
topic disintegration characteristics
disintegration modes
long-term immersion
permeability
slope instability
url https://www.mdpi.com/2076-3417/13/17/9819
work_keys_str_mv AT kunzhang studyondisintegrationandinfiltrationcharacteristicsofnanjingjiangxinzhouembankmentsoil
AT difeng studyondisintegrationandinfiltrationcharacteristicsofnanjingjiangxinzhouembankmentsoil