Analysis of slope instability along Rangsit-Nakhon Nayok highway

By: Call Number: AIT Thesis no.GT-92-09 Contributor(s): Material type: TextSeries: Asian Institute of Technology. Thesis ; no. GT-92-09Publication details: Bangkok : Asian Institute of Technology, 1993Description: 138 leaves + 1 online resourceSubject(s): Online resources: Dissertation note: Thesis (M.Eng.) - Asian Institute of Technology, 1993 Summary: Slope failure of· Rangsit-Nakhon Nayok highway was analysed in detail to identify the causes. Crucial field and laboratory tests were accomplished to obtain essential soil parameters required for slope stability analysis. The original soil is relatively uniform soft clay layer. A number of assumed cases were analysed using the Simplified Bishop's method. Results show that a combination of a rapid drop of water level in the canal during the summer season, and slope face shrinkage crack was principal cause of the failure. This effect caused retrogressive failure of some of the steeper slopes starting from the toe upward however at the lowest water level, the stability of the overall slope was also not stable.
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20-AIT Publication Asian Institute of Technology Library AIT Publications AIT Thesis no.GT-92-09 (Browse shelf(Opens below)) 3 Available 30050120712780
22-AIT Thesis (Replacement) Asian Institute of Technology Library AIT Publications AIT Thesis no.GT-92-09 (Browse shelf(Opens below)) 4 Available 30050120708242
40-Archives Asian Institute of Technology Library Archives AIT Thesis no.GT-92-09 (Browse shelf(Opens below)) 1 Available 30050120308654

A thesis submitted in partial fulfillment of the requirement for the degree of Master of Engineering, School of Engineering and Technology

Thesis (M.Eng.) - Asian Institute of Technology, 1993

Slope failure of· Rangsit-Nakhon Nayok highway was analysed in detail to identify the causes. Crucial field and laboratory tests were accomplished to obtain essential soil parameters required for slope stability analysis. The original soil is relatively uniform soft clay layer. A number of assumed cases were analysed using the Simplified Bishop's method. Results show that a combination of a rapid drop of water level in the canal during the summer season, and slope face shrinkage crack was principal cause of the failure. This effect caused retrogressive failure of some of the steeper slopes starting from the toe upward however at the lowest water level, the stability of the overall slope was also not stable.

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