COMPARISON OF 2D DEBRIS-FLOW SIMULATION MODELS WITH FIELD EVENTS

dc.contributor.authorRickenmann D.
dc.contributor.authorLaigle D.
dc.contributor.authorMcardell B.W.
dc.contributor.authorHübl J.
dc.date.accessioned2024-09-20T06:16:50Z
dc.date.available2024-09-20T06:16:50Z
dc.date.issued2006
dc.description.abstractThree two-dimensional (2D) debris-flow simulation models are applied to two large well-documented debris-flow events which caused major deposition of solid material on the fan. The models are based on a Voellmy fluid rheology reflecting turbulent-like and basal frictional stresses, a quadratic rheologic formulation including Bingham, collisional and turbulent stresses, and a Herschel–Bulkley rheology representing a viscoplastic fluid. The rheologic or friction parameters of the models are either assumed a priori or adjusted to best match field observations. All three models are capable of reasonably reproducing the depositional pattern on the alluvial fan after the models have been calibrated using historical data from the torrent. Accurate representation of the channel and fan topography is especially important to achieve a good replication of the observed deposition pattern.
dc.identifierhttps://www.elibrary.ru/item.asp?id=52840980
dc.identifier.citationComputational Geosciences, 2006, 10, 2, 241-264
dc.identifier.doi10.1007/s10596-005-9021-3
dc.identifier.issn1420-0597
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/45233
dc.subjectDEBRIS FLOW
dc.subjectFIELD OBSERVATION
dc.subjectFRICTION LAW
dc.subjectRHEOLOGIC PARAMETER
dc.subjectSIMULATION MODEL
dc.titleCOMPARISON OF 2D DEBRIS-FLOW SIMULATION MODELS WITH FIELD EVENTS
dc.typeСтатья

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