Water Supply (May 2024)

Mitigation of tunnel support design risks for hydropower projects within high tectonic stress regimes – an empirical analysis

  • Aamir Hameed,
  • Mairaj Soomro,
  • Yaoying Huang,
  • Mian Sohail Akram,
  • Muhammad Sanaullah,
  • Luqman Ahmed,
  • Muhammad Jehangir Khan

DOI
https://doi.org/10.2166/ws.2024.081
Journal volume & issue
Vol. 24, no. 5
pp. 1425 – 1446

Abstract

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The study for the design of tunnels in similar geological settings, providing insights into potential challenges that may arise during excavation and offering strategies for mitigating risks in District Kalam on the Ushu River, Khyber Pakhtunkhwa, Pakistan. The methodology involved geological mapping, rock sampling, discontinuity surveys, and laboratory testing for empirical analysis of tunnel parameters at the Weir House, Powerhouse, and tunnel alignment locations. Empirical analysis of tunnel parameters using three rock classification systems, rock mass rating (RMR), rock quality tunneling index, and rock mass index (RMi). Based on the classification, the rock quality was found to be fair, indicating favorable rock properties. The Q-system rated the rock as poor to fair, suggesting low discontinuity intensity, medium rock strength, or medium deformation modulus. According to the RMi, rock was rated as medium to strong, indicating low discontinuity intensity, high rock strength, or low deformability. The support design for the tunnel is based on empirical analysis, it recommends support design for the tunnel reinforcement elements such as rock bolts, wire mesh, and shotcrete lining. Overall, the tunnel is stable and does not have complex structure and weak zones. HIGHLIGHTS The study has novel significant implications for the design of tunnels in similar geological settings, providing insights into potential challenges that may arise during excavation and offering strategies for mitigating risks.; Design of a tunnel for a hydropower in a high-tectonic stress regime, for tunnel engineering due to the potential for rock mass instabilities.;

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