dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Analysis of the runout time and distance of slow-moving gravitational flows: possible modelling concepts and simulations.
VerfasserIn Th. W. J. van Asch, J.-P. Malet, S. Bégueria-Portuguès
Konferenz EGU General Assembly 2009
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 11 (2009)
Datensatznummer 250022197
 
Zusammenfassung
Mud/debris flows are in general fast-moving gravitational flows with a velocity from 1 to more than 10 m.s-1. A number of gravitational flows models have been developed based on a two dimensional finite difference solution of a depth–averaged form of the Navier-Stokes equations of fluid motion. In these models, the flows are treated as a one phase medium which behaviour is controlled by different rheological characteristics depending on the liquid/solid ratio. It appeared that these models are not able to describe accurately both the run-out time and the run-out distance of shear flows with a relatively lower velocity. For example, a mud flow with an initial volume of about 100m3 failed in May 5th 1999 suddenly from a secondary scarp of the Super-Sauze mudslide (Southern French Alps) and reached a distal point of 105 m from the source area. It flowed on the hillslope in the first 30 min with a mean velocity of 2 m.min-1 until a distance of 50 m from the source area, and then continued flowing at a slower mean velocity of 1 m.min-1. Similar patterns of velocity and runout distance for small volume mudflows triggered in May 2008 at Super-Sauze have also been observed. Three strategies are used to adapt the current run-out models to these relatively slow-moving gravitational flows. These are related to (1) a change in pore pressure dissipation rate and rheological behaviour during the run-out, (2) the ignorance of inertial forces in the equation of motion, (3) the assumptions of a rigid plug in the velocity profile and of low shear rates. The application of the model and results of the simulation to the case studies mentioned above are discussed.