Application of fitting parameters in best fit equation

Soil-water characteristic curve (SWCC) contains key information for the application of unsaturated soil mechanics principles to engineering practice. SWCC variables such as air-entry value, residual suction and residual saturation are commonly referred to for estimation of other unsaturated soil pro...

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Main Authors: Qian, Zhai, Rahardjo, Harianto
Other Authors: Delage, P.
Format: Article
Language:English
Published: 2019
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Online Access:https://hdl.handle.net/10356/81157
http://hdl.handle.net/10220/50062
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-811572020-03-07T11:43:30Z Application of fitting parameters in best fit equation Qian, Zhai Rahardjo, Harianto Delage, P. Cui, Y.-J. Ghabezloo, S. Pereira, J.-M. Tang, A.-M. School of Civil and Environmental Engineering Fitting Parameters Soil-water Characteristic Curve Engineering::Environmental engineering Soil-water characteristic curve (SWCC) contains key information for the application of unsaturated soil mechanics principles to engineering practice. SWCC variables such as air-entry value, residual suction and residual saturation are commonly referred to for estimation of other unsaturated soil properties. Though there are clear definitions for these SWCC variables, it is difficult to measure them directly in laboratory and these SWCC variables are commonly estimated from SWCC. Hydraulic conductivity of unsaturated soil is the major property that controls water flow in soil. The laboratory measurement of hydraulic conductivity is time consuming and costly. Therefore, hydraulic conductivity is also commonly estimated from SWCC. Normally, SWCC is represented by a best fit equation which is typically governed by few fitting parameters. These fitting parameters can be obtained from a best fit procedure and are proven to be dependent on each other. Fredlund and Xing’s (1994) equation is one of the popular equations commonly used by researchers and there are only three fitting parameters such as “a”, “n”, “m” in this equation. Correlation equations between SWCC variables, hydraulic conductivity and the fitting parameters such as “a”, “n” and “m” are presented in this paper. In addition, the variability in the determined SWCC variables and hydraulic conductivity due to the variation in these fitting parameters is also discussed in this paper. Published version 2019-10-01T04:52:49Z 2019-12-06T14:22:38Z 2019-10-01T04:52:49Z 2019-12-06T14:22:38Z 2016 Journal Article Qian, Z., & Rahardjo, H. (2016). Application of fitting parameters in best fit equation. E3S Web of Conferences, 9, 10008-. doi:10.1051/e3sconf/20160910008 https://hdl.handle.net/10356/81157 http://hdl.handle.net/10220/50062 10.1051/e3sconf/20160910008 en E3S Web of Conferences © 2016 The Author(s) (Published by EDP Sciences). This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. 6 p. application/pdf
institution Nanyang Technological University
building NTU Library
country Singapore
collection DR-NTU
language English
topic Fitting Parameters
Soil-water Characteristic Curve
Engineering::Environmental engineering
spellingShingle Fitting Parameters
Soil-water Characteristic Curve
Engineering::Environmental engineering
Qian, Zhai
Rahardjo, Harianto
Application of fitting parameters in best fit equation
description Soil-water characteristic curve (SWCC) contains key information for the application of unsaturated soil mechanics principles to engineering practice. SWCC variables such as air-entry value, residual suction and residual saturation are commonly referred to for estimation of other unsaturated soil properties. Though there are clear definitions for these SWCC variables, it is difficult to measure them directly in laboratory and these SWCC variables are commonly estimated from SWCC. Hydraulic conductivity of unsaturated soil is the major property that controls water flow in soil. The laboratory measurement of hydraulic conductivity is time consuming and costly. Therefore, hydraulic conductivity is also commonly estimated from SWCC. Normally, SWCC is represented by a best fit equation which is typically governed by few fitting parameters. These fitting parameters can be obtained from a best fit procedure and are proven to be dependent on each other. Fredlund and Xing’s (1994) equation is one of the popular equations commonly used by researchers and there are only three fitting parameters such as “a”, “n”, “m” in this equation. Correlation equations between SWCC variables, hydraulic conductivity and the fitting parameters such as “a”, “n” and “m” are presented in this paper. In addition, the variability in the determined SWCC variables and hydraulic conductivity due to the variation in these fitting parameters is also discussed in this paper.
author2 Delage, P.
author_facet Delage, P.
Qian, Zhai
Rahardjo, Harianto
format Article
author Qian, Zhai
Rahardjo, Harianto
author_sort Qian, Zhai
title Application of fitting parameters in best fit equation
title_short Application of fitting parameters in best fit equation
title_full Application of fitting parameters in best fit equation
title_fullStr Application of fitting parameters in best fit equation
title_full_unstemmed Application of fitting parameters in best fit equation
title_sort application of fitting parameters in best fit equation
publishDate 2019
url https://hdl.handle.net/10356/81157
http://hdl.handle.net/10220/50062
_version_ 1681043829919055872