Slope stability analysis along the proposed Kathmandu-Hetauda Road with tunnel sections

Authors

  • I. R. Humagain Department of Engineering Geology and Hydrogeology in Aachen University of Technology, Lochner Str. 4 - 20, D-52056 Aachen, Germany
  • K. Schetelig Department of Engineering Geology and Hydrogeology in Aachen University of Technology, Lochner Str. 4 - 20, D-52056 Aachen, Germany
  • M. P. Sharma Tribhuvan University Central Office, Kirtipur, Kathmandu
  • B. N. Upreti Department of Geology, Tri-Chandra Campus, Tribhuvan University, Ghantaghar, Kathmandu
  • M. Langer Bundesanstalt fuer Geowissenschaften und Rohstoffe (BGR), Stilleweg – 2, D-30655 Hannover, Germany

DOI:

https://doi.org/10.3126/jngs.v22i0.32345

Keywords:

Road tunnel, Slope stability, Rock discontinuity, Kathmandu-Hetauda Road, Nepal

Abstract

The proposed Kathmandu-Hetauda Road alignment passes through Thankot, Chitlang, Kulekhani, Bhimphedi, and Bhaisedobhan. It is the shortest as well as least hazardous route very suitable for a standard highway. It has the following three tunnel sections: the Thankot Tunnel (3.2 km long), the Kulekhani Tunnel (500 m long), and the Chisapani Tunnel (3.8 km long). The alignment passes through the Kathmandu Nappe, Upper Nawakot Group of the Lesser Himalaya, and the Siwaliks. It also crosses the Main Boundary Thrust and the Mahabharat Thrust, four major faults/shear zones, and a major fold axis.

The areas of plane sliding, wedge sliding, and toppling are delimited on the basis of the study of discontinuities along the proposed alignment. The stability analysis show s that 60-75% of the total road length is stable, 20-30% is fair, 5- 15% is weak, and 2-5% is critical.

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Published

2000-12-01

How to Cite

Humagain, I. R., Schetelig, K., Sharma, M. P., Upreti, B. N., & Langer, M. (2000). Slope stability analysis along the proposed Kathmandu-Hetauda Road with tunnel sections. Journal of Nepal Geological Society, 22, 187–200. https://doi.org/10.3126/jngs.v22i0.32345

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Section

Articles