A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition

Kozeny–Carman (KC) equation is a well-known relation between hydraulic conductivity and pore properties in porous material. The applications of KC equation to predicting saturated hydraulic conductivities of sands and non-expansive soils are well documented. However, KC equation is incapable of pred...

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Main Authors: Kunlin Ruan, Xian-Lei Fu
Format: Article
Language:English
Published: Elsevier 2022-06-01
Series:Journal of Rock Mechanics and Geotechnical Engineering
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674775521001475
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author Kunlin Ruan
Xian-Lei Fu
author_facet Kunlin Ruan
Xian-Lei Fu
author_sort Kunlin Ruan
collection DOAJ
description Kozeny–Carman (KC) equation is a well-known relation between hydraulic conductivity and pore properties in porous material. The applications of KC equation to predicting saturated hydraulic conductivities of sands and non-expansive soils are well documented. However, KC equation is incapable of predicting saturated hydraulic conductivity of expansive soil (e.g. bentonite) well. Based on a new dual-pore system, this study modified KC equation for improving the prediction of saturated hydraulic conductivities of bentonites. In this study, an assumption that inter-layer space (micropore) has limited effect on fluid flow performance of compacted bentonite was adopted. The critical parameters including total porosity and total tortuosity in conventional KC equation were replaced by macroporosity and tortuosity of macropore, respectively. Macroporosity and microporosity were calculated by basal spacing of compacted bentonite, which was estimated by assuming that specific surface area is changeable during saturation process. A comprehensive comparison of bentonite's saturated hydraulic conductivity predictions, including modified KC equation proposed in this study, conventional KC equation, and prediction method based on diffuse double layer (DDL) theory, was carried out. It was found that the predicted saturated hydraulic conductivity of bentonites calculated using modified KC equation fitted the experimental data better than others to a certain extent.
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spelling doaj.art-4a82554338714ea89ecf5d812cca71b92022-12-22T00:36:43ZengElsevierJournal of Rock Mechanics and Geotechnical Engineering1674-77552022-06-01143984993A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined conditionKunlin Ruan0Xian-Lei Fu1Department of Civil and Environmental Engineering, Waseda University, Tokyo, 169-8555, JapanJiangsu Key Laboratory of Urban Underground Engineering and Environmental Safety, Institute of Geotechnical Engineering, Southeast University, Nanjing, 210096, China; Corresponding author.Kozeny–Carman (KC) equation is a well-known relation between hydraulic conductivity and pore properties in porous material. The applications of KC equation to predicting saturated hydraulic conductivities of sands and non-expansive soils are well documented. However, KC equation is incapable of predicting saturated hydraulic conductivity of expansive soil (e.g. bentonite) well. Based on a new dual-pore system, this study modified KC equation for improving the prediction of saturated hydraulic conductivities of bentonites. In this study, an assumption that inter-layer space (micropore) has limited effect on fluid flow performance of compacted bentonite was adopted. The critical parameters including total porosity and total tortuosity in conventional KC equation were replaced by macroporosity and tortuosity of macropore, respectively. Macroporosity and microporosity were calculated by basal spacing of compacted bentonite, which was estimated by assuming that specific surface area is changeable during saturation process. A comprehensive comparison of bentonite's saturated hydraulic conductivity predictions, including modified KC equation proposed in this study, conventional KC equation, and prediction method based on diffuse double layer (DDL) theory, was carried out. It was found that the predicted saturated hydraulic conductivity of bentonites calculated using modified KC equation fitted the experimental data better than others to a certain extent.http://www.sciencedirect.com/science/article/pii/S1674775521001475Kozeny–carman (KC) equationSaturated hydraulic conductivityBentonitePore size distribution (PSD)Specific surface area
spellingShingle Kunlin Ruan
Xian-Lei Fu
A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
Journal of Rock Mechanics and Geotechnical Engineering
Kozeny–carman (KC) equation
Saturated hydraulic conductivity
Bentonite
Pore size distribution (PSD)
Specific surface area
title A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
title_full A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
title_fullStr A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
title_full_unstemmed A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
title_short A modified Kozeny–Carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
title_sort modified kozeny carman equation for predicting saturated hydraulic conductivity of compacted bentonite in confined condition
topic Kozeny–carman (KC) equation
Saturated hydraulic conductivity
Bentonite
Pore size distribution (PSD)
Specific surface area
url http://www.sciencedirect.com/science/article/pii/S1674775521001475
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