journal article·2024-05-28Open access

Influence of Rock Slide Geometry on Stability Behavior during Reservoir Impounding

Christian Zangerl, Heidrun Lechner, Alfred Strauss

Applied Sciences· Volume 14· Issue 11

Abstract

Assessing the stability behavior of deep-seated rock slides in the surroundings of large dam reservoirs requires an understanding of the geometry, the kinematics, the groundwater situation, and the rock mass and shear zone properties. This study focuses on the influence of rock slide geometry on stability evolution during initial reservoir impounding. Therefore, nine different rock slide models, mainly taken from published case studies with a well-explored geometry, were analyzed. Based on the assumption that the rock slides are close to limit equilibrium in a no-reservoir scenario, reservoir impounding causes a reduction in the factor of safety (FoS). The results show a large impact of the water level for rotational slides where the majority of the rock mass is located at the lower part of the slope. This results in a maximum reduction in the FoS of up to 12%. In contrast to this, translational rock slides are less affected by reservoir impounding. The stability analysis shows that the change in FoS is strongly controlled by the kinematics of the rock slide and the geometry near the foot of the slope. Consequently, a comprehensive in situ investigation of the geometry and kinematics is necessary in order to reliably assess the influence of initial reservoir impounding.
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Research context

OpenAlex topics: Landslides and related hazards · Rock Mechanics and Modeling · Dam Engineering and Safety

SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.

Affiliations

Institute of Applied Geology, Department of Civil Engineering and Natural Hazards, BOKU University, Peter Jordan-Strasse 82, 1190 Vienna, Austria

Institute of Structural Engineering, Department of Civil Engineering and Natural Hazards, BOKU University, Peter Jordan-Strasse 82, 1190 Vienna, Austria

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