Engineering Geological Investigation of dam site of proposed Sunkoshi-2 Hydropower Project, Khurkot area, eastern Nepal

Authors

  • Bipin Adhikari Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu
  • Ujjwal Acharya Center for Geo-environment and Engineering Research, Kupondole, Lalitpur
  • Kamala Kant Acharya Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu
  • Subesh Ghimire Central Department of Geology, Tribhuvan University, Kirtipur, Kathmandu

DOI:

https://doi.org/10.3126/jngs.v58i0.24603

Keywords:

Discontinuity Survey, Tawa Khola Formation, Rock Mass Characterization, RMR, DMR

Abstract

The dam site of proposed Sunkoshi-2 Hydropower Project and its surrounding mainly comprise the Tawa Khola Formation, which is the basal formation of the Bhimphedi Group. Although garnet schist and micaceous quartzite bands are the main rock types; three rock units namely- Schist Unit, Quartzite Unit, and Gneiss Unit were identified. Engineering geological mapping followed by discontinuity survey were carried out. The result exhibited differences in fracture intensity and discontinuity characteristics of rock masses according to rock type. Since joint orientations were found to be consistent over fairly large areas, surface studies of joints were used in predicting subsurface orientations. Rock mass classification was made in line with the Rock Mass Rating System (RMR) and the Dam Mass Rating (DMR) classification for the dam foundation. The rock masses were classified onto fair to good rock classes according to RMR value. Dam foundation analysis regarding stability against sliding using DMR classification helped in selection of suitable dam-axis among two alternatives. Water Quality Standards (2005).

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Published

2019-06-25

How to Cite

Adhikari, B., Acharya, U., Acharya, K. K., & Ghimire, S. (2019). Engineering Geological Investigation of dam site of proposed Sunkoshi-2 Hydropower Project, Khurkot area, eastern Nepal. Journal of Nepal Geological Society, 58, 181–188. https://doi.org/10.3126/jngs.v58i0.24603

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