Causes of catastrophic failure of Tam Pokhari moraine dam in the Mt. Everest region |
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Authors: | Osti Rabindra Bhattarai Tara Nidhi Miyake Katsuhito |
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Institution: | (1) International Centre for Water Hazard and Risk Management, Public Works Research Institute, Minamihara 1-6, Tsukuba 305-8516, Japan;(2) Department of Geology, Tribhuvan University, Tri-Chandra Campus, Ghantaghar, Kathmandu, Nepal |
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Abstract: | The moraine dam of the Tam Pokhari glacial lake breached on 3 September 1998 and caused a catastrophic flood in the downstream
areas. To learn from the event, a field survey was conducted. The survey team found that a landslide, which is considered
to be responsible for the outburst flood, occurred in the northeast-facing slope of the moraine dam. The dam internal structure
played a crucial role in forming a landslide that triggered the excess overflow and finally the breach of the dam. The internal
structure of the dam was made of alternating layers of finer and coarser sediments inclining at 30° downstream and layers
are truncated in the upslope direction by a huge pile of unconsolidated and structureless moraine materials. Since the upstream
slope angle of the dam i.e., 40° is larger than the angle of repose i.e. 35° of sediments, the increased pore water pressure
in the dam triggered a landslide. The rainfall and seismological activities of that particular day, which hit the record high,
were crucial in triggering the failure. It is estimated that the dam’s north and northeast-facing slopes completely slid involving
about 30,000 m3 of sediment mass of unconsolidated moraine materials above the shear plane. A slope stability analysis was also performed.
The calculated safety factor was 0.85, and the calculated slip circle agreed with the shear plane marked in the dam. About
18 million cubic metres of water was swiftly released due to the sudden breach of the moraine dam. |
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