Mapping of cracked soils and lateral water flow characteristics through a network of cracks

When a cohesive soil is dried, its volume tends to shrink in three directions. Shrinkage of the soil causes tensile stresses to develop and desiccation cracks will start to develop. The occurrence of cracks can significantly influence the lateral flow of water through the soil. It is important to un...

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Bibliographic Details
Main Authors: Krisnanto, S., Rahardjo, H., Fredlund, D. G., Leong, E. C.
Other Authors: School of Civil and Environmental Engineering
Format: Article
Language:English
Published: 2014
Subjects:
Online Access:https://hdl.handle.net/10356/101959
http://hdl.handle.net/10220/19815
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Institution: Nanyang Technological University
Language: English
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