Role of confining pressure on the hydraulic properties of compacted soil

The effects of confining pressure on the hydraulic properties of two types of compacted soils, namely Sand-Kaolin and Sand-Kaolin-Mica, are investigated. The compacted soil specimens are saturated, consolidated by net confining pressures of 50 kPa and 200 kPa separately, and subsequently suction-dri...

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Main Author: Tanuwidjaja, Samuel Winson
Other Authors: Harianto Rahardjo
Format: Final Year Project
Language:English
Published: Nanyang Technological University 2021
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Online Access:https://hdl.handle.net/10356/149002
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1490022021-05-11T05:22:23Z Role of confining pressure on the hydraulic properties of compacted soil Tanuwidjaja, Samuel Winson Harianto Rahardjo School of Civil and Environmental Engineering CHRAHARDJO@ntu.edu.sg Engineering::Civil engineering::Geotechnical The effects of confining pressure on the hydraulic properties of two types of compacted soils, namely Sand-Kaolin and Sand-Kaolin-Mica, are investigated. The compacted soil specimens are saturated, consolidated by net confining pressures of 50 kPa and 200 kPa separately, and subsequently suction-dried to generate the drying SWCCs. The drying SWCC corresponding to zero confining pressure is derived from the results of Zhao (2020). The SWCCs are then be compared in terms of their key parameters namely air-entry value (AEV), geometric standard deviation (s) and inflection point (ψ_m), especially those that correspond to the second sub-curve of the bimodal SWCC. For Sand-Kaolin, the 2nd AEV increases with increasing confining pressure, whereas the 2nd geometric standard deviation and the 2nd inflection point decreases linearly with increasing confining pressure. These relationships between the variation in Sand-Kaolin’s SWCC with varying confining pressures are further supported by the results of the pore-size distribution (PSD) of the Sand-Kaolin specimens. For Sand-Kaolin-Mica, the 2nd AEV and the 2nd geometric standard deviation decreases linearly with increasing confining pressure, while the 2nd inflection point increases linearly with increasing confining pressure. PSD data cannot be used to justify the variations in Sand-Kaolin-Mica’s SWCC as the elastic nature of the mica particles negates the effects of confining pressure on the soil structure once the confining pressure is removed. However, inferences are made with regards to the effects of confining pressure on mica-influenced soil structure, which may help explain the macro-scale behaviour exhibited in the SWCC. Bachelor of Engineering (Civil) 2021-05-11T05:22:23Z 2021-05-11T05:22:23Z 2021 Final Year Project (FYP) Tanuwidjaja, S. W. (2021). Role of confining pressure on the hydraulic properties of compacted soil. Final Year Project (FYP), Nanyang Technological University, Singapore. https://hdl.handle.net/10356/149002 https://hdl.handle.net/10356/149002 en GE-07 application/pdf Nanyang Technological University
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Engineering::Civil engineering::Geotechnical
spellingShingle Engineering::Civil engineering::Geotechnical
Tanuwidjaja, Samuel Winson
Role of confining pressure on the hydraulic properties of compacted soil
description The effects of confining pressure on the hydraulic properties of two types of compacted soils, namely Sand-Kaolin and Sand-Kaolin-Mica, are investigated. The compacted soil specimens are saturated, consolidated by net confining pressures of 50 kPa and 200 kPa separately, and subsequently suction-dried to generate the drying SWCCs. The drying SWCC corresponding to zero confining pressure is derived from the results of Zhao (2020). The SWCCs are then be compared in terms of their key parameters namely air-entry value (AEV), geometric standard deviation (s) and inflection point (ψ_m), especially those that correspond to the second sub-curve of the bimodal SWCC. For Sand-Kaolin, the 2nd AEV increases with increasing confining pressure, whereas the 2nd geometric standard deviation and the 2nd inflection point decreases linearly with increasing confining pressure. These relationships between the variation in Sand-Kaolin’s SWCC with varying confining pressures are further supported by the results of the pore-size distribution (PSD) of the Sand-Kaolin specimens. For Sand-Kaolin-Mica, the 2nd AEV and the 2nd geometric standard deviation decreases linearly with increasing confining pressure, while the 2nd inflection point increases linearly with increasing confining pressure. PSD data cannot be used to justify the variations in Sand-Kaolin-Mica’s SWCC as the elastic nature of the mica particles negates the effects of confining pressure on the soil structure once the confining pressure is removed. However, inferences are made with regards to the effects of confining pressure on mica-influenced soil structure, which may help explain the macro-scale behaviour exhibited in the SWCC.
author2 Harianto Rahardjo
author_facet Harianto Rahardjo
Tanuwidjaja, Samuel Winson
format Final Year Project
author Tanuwidjaja, Samuel Winson
author_sort Tanuwidjaja, Samuel Winson
title Role of confining pressure on the hydraulic properties of compacted soil
title_short Role of confining pressure on the hydraulic properties of compacted soil
title_full Role of confining pressure on the hydraulic properties of compacted soil
title_fullStr Role of confining pressure on the hydraulic properties of compacted soil
title_full_unstemmed Role of confining pressure on the hydraulic properties of compacted soil
title_sort role of confining pressure on the hydraulic properties of compacted soil
publisher Nanyang Technological University
publishDate 2021
url https://hdl.handle.net/10356/149002
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