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- W2339190999 abstract "This study presents a hydrodynamic and sedimentary reconstruction and interpretation of the San Juan dam- break occurred in January 2001 in Altorricon (Huesca). Geomorphic processes as well as erosional and depositional forms created by released water and sediment are also described. Approximately 300,000 m 3 of water were released during the outflow following an estimated peak of 172 m 3 s -1 . As a consequence, 3,350 metric tones of sediment were entrained, 80% of them subsequently deposited as an alluvial fan at the dam-break footstep. Metric blocs were trans - ported by hyperconcentr ated flows around 1.35 t m -3 in density. Dam break and collapse were mainly triggered by hypodermic fluxes and piping. Non-adequate sealing of the dam bottom and the inappropiate location on top of highly- permeable Quaternary sediments can be pointed out as main causes of the disaster ." @default.
- W2339190999 created "2016-06-24" @default.
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- W2339190999 date "2001-01-01" @default.
- W2339190999 modified "2023-09-26" @default.
- W2339190999 title "INTERPRETACIÓN HIDRODINÁMICA Y SEDIMENTARIADE LA ROTURA DE LA BALSA DE SAN JUAN (ALTORRICÓN, HUESCA) Hydrodynamic and sedimentary interpretation of the San Juan Dam break (Altorricón, Huesca)" @default.
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- W2339190999 hasPublicationYear "2001" @default.
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