Spatial variation of shear strength properties incorporating auxiliary variables
Soil shear strength is a critical parameter in slope stability. Shear strength properties may vary significantly over large areas. Thus, the spatial estimates of shear strength properties are necessary for deterministic slope susceptibility mapping over large areas. However, measurements of shear st...
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sg-ntu-dr.10356-1598252022-07-06T06:55:27Z Spatial variation of shear strength properties incorporating auxiliary variables Ip, Sabrina Chui Yee Satyanaga, Alfrendo Rahardjo, Harianto School of Civil and Environmental Engineering Engineering::Civil engineering::Geotechnical Regression Kriging Spatial Variability Sampling Density Random Forest Soil Shear Strength Soil shear strength is a critical parameter in slope stability. Shear strength properties may vary significantly over large areas. Thus, the spatial estimates of shear strength properties are necessary for deterministic slope susceptibility mapping over large areas. However, measurements of shear strength parameters are often limited as compared to other soil properties such as Atterberg limit, bulk density and grain size distribution. Multivariate methods have been shown to improve prediction accuracy, but these methods have rarely been used to predict shear strength. In this study, attempts were made to evaluate the effectiveness of using the aforementioned soil properties in predicting the spatial variation of shear strength properties: effective cohesion (c’) and effective friction angle (ϕ’). The performance of ordinary kriging (OK), Random Forest (RF) and regression kriging (RK) in predicting c’ and ϕ’ of residual soils in Singapore were compared and evaluated. In addition, the sensitivity of the three methods to the sample size was investigated. The results of RF analysis revealed that the northing coordinate and percentage of fines were the most important variables for predicting ϕ’. The spatial coordinates and ϕ’ were also important variables for predicting c’. The predicted c’ and ϕ’ using RF and RK resulted in higher spatial heterogeneity than OK. Overall, RF had the smallest error as compared to OK and RK in predicting c’ and ϕ’ at all sample sizes, except for the prediction of ϕ’ using the largest sample size. This study also showed that RF and RK were more sensitive to sample size than OK. These results highlight the benefits of using auxiliary variables when mapping shear strength properties. Submitted/Accepted version 2022-07-06T06:55:26Z 2022-07-06T06:55:26Z 2021 Journal Article Ip, S. C. Y., Satyanaga, A. & Rahardjo, H. (2021). Spatial variation of shear strength properties incorporating auxiliary variables. CATENA, 200, 105196-. https://dx.doi.org/10.1016/j.catena.2021.105196 0341-8162 https://hdl.handle.net/10356/159825 10.1016/j.catena.2021.105196 200 105196 en CATENA © 2021 Elsevier B.V. All rights reserved. This paper was published in CATENA and is made available with permission of Elsevier B.V. application/pdf |
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Engineering::Civil engineering::Geotechnical Regression Kriging Spatial Variability Sampling Density Random Forest Soil Shear Strength |
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Engineering::Civil engineering::Geotechnical Regression Kriging Spatial Variability Sampling Density Random Forest Soil Shear Strength Ip, Sabrina Chui Yee Satyanaga, Alfrendo Rahardjo, Harianto Spatial variation of shear strength properties incorporating auxiliary variables |
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Soil shear strength is a critical parameter in slope stability. Shear strength properties may vary significantly over large areas. Thus, the spatial estimates of shear strength properties are necessary for deterministic slope susceptibility mapping over large areas. However, measurements of shear strength parameters are often limited as compared to other soil properties such as Atterberg limit, bulk density and grain size distribution. Multivariate methods have been shown to improve prediction accuracy, but these methods have rarely been used to predict shear strength. In this study, attempts were made to evaluate the effectiveness of using the aforementioned soil properties in predicting the spatial variation of shear strength properties: effective cohesion (c’) and effective friction angle (ϕ’). The performance of ordinary kriging (OK), Random Forest (RF) and regression kriging (RK) in predicting c’ and ϕ’ of residual soils in Singapore were compared and evaluated. In addition, the sensitivity of the three methods to the sample size was investigated. The results of RF analysis revealed that the northing coordinate and percentage of fines were the most important variables for predicting ϕ’. The spatial coordinates and ϕ’ were also important variables for predicting c’. The predicted c’ and ϕ’ using RF and RK resulted in higher spatial heterogeneity than OK. Overall, RF had the smallest error as compared to OK and RK in predicting c’ and ϕ’ at all sample sizes, except for the prediction of ϕ’ using the largest sample size. This study also showed that RF and RK were more sensitive to sample size than OK. These results highlight the benefits of using auxiliary variables when mapping shear strength properties. |
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School of Civil and Environmental Engineering |
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School of Civil and Environmental Engineering Ip, Sabrina Chui Yee Satyanaga, Alfrendo Rahardjo, Harianto |
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Article |
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Ip, Sabrina Chui Yee Satyanaga, Alfrendo Rahardjo, Harianto |
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Ip, Sabrina Chui Yee |
title |
Spatial variation of shear strength properties incorporating auxiliary variables |
title_short |
Spatial variation of shear strength properties incorporating auxiliary variables |
title_full |
Spatial variation of shear strength properties incorporating auxiliary variables |
title_fullStr |
Spatial variation of shear strength properties incorporating auxiliary variables |
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Spatial variation of shear strength properties incorporating auxiliary variables |
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spatial variation of shear strength properties incorporating auxiliary variables |
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2022 |
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https://hdl.handle.net/10356/159825 |
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