Eingang zum Volltext in OPUS

Home | Suche | Browsen

Lizenz

Bitte beziehen Sie sich beim Zitieren dieses Dokumentes immer auf folgende
URN: urn:nbn:de:kobv:517-opus-60226
URL: http://opus.kobv.de/ubp/texte_eingeschraenkt_verlag/2012/6022/


Lindenmaier, Falk ; Zehe, Erwin ; Dittfurth, Angela ; Ihringer, Jürgen

Process identification at a slow-moving landslide in the Vorarlberg Alps

pdf-Format:
Dokument 1.pdf (1.409 KB)
Zugriffsbeschränkung: Universitätsverlag - eingeschränkter Zugriff


Kurzfassung in Deutsch

A fine-grained slope that exhibits slow movement rates was investigated to understand how geohydrological processes contribute to a consecutive development of mass movements in the Vorarlberg Alps, Austria. For that purpose intensive hydrometeorological, hydrogeological and geotechnical observations as well as surveying of surface movement rates were conducted during 1998–2001. Subsurface water dynamics at the creeping slope turned out to be dominated by a three-dimensional pressure system. The pressure reaction is triggered by fast infiltration of surface water and subsequent lateral water flow in the south-western part of the hillslope. The related pressure signal was shown to
propagate further downhill, causing fast reactions of the piezometric head at 5Ð5 m depth on a daily time scale. The observed pressure reactions might belong to a temporary hillslope water body that extends further downhill. The
related buoyancy forces could be one of the driving forces for the mass movement. A physically based hydrological model was adopted to model simultaneously surface and subsurface water dynamics including evapotranspiration and runoff production. It was possible to reproduce surface runoff and observed pressure reactions in principle. However, as soil hydraulic functions were only estimated on pedotransfer functions, a quantitative comparison between observed and simulated subsurface dynamics is not feasible. Nevertheless, the results suggest that it is possible to reconstruct important spatial structures based on sparse observations in the field which allow reasonable simulations with a physically based hydrological model. Copyright  2005 John Wiley & Sons, Ltd.

KEY WORDS rainfall-induced landslides; soil creep; hydrological modelling; Vorarlberg; Austria; pressure propagation

Institut 1: Institut für Geoökologie
Institut 2: Extern
Institut 3: Extern
Institut 4: Extern
DDC-Sachgruppe: Geowissenschaften
Dokumentart: c Postprint
Quelle: Hydrological Process. - ISSN 1099-1085 . - 19 (2005), S. 1635–1651.
Sprache: Englisch
Erstellungsjahr: 2004
Publikationsdatum: 03.07.2012
Bemerkung: This is a postprint of an article who was published in Hydrological Process. - ISSN 1099-1085 . - 19 (2005), S. 1635–1651. Online First Publication, December 22, 2004. DOI: 10.1002/hyp.5592 2005 Copyright John Wiley & Sons, Ltd.
Lizenz: Diese Nutzungsbedingung gilt nicht, wenn in den Metadaten eine modifizierende Lizenz genannt ist. Keine Nutzungslizenz vergeben - es gilt das deutsche Urheberrecht


Home | Leitlinien | Impressum | Haftungsausschluss | Statistik | Universitätsverlag | Universitätsbibliothek
Ihr Kontakt für Fragen und Anregungen:
Universitätsbibliothek Potsdam
powered by OPUS  Hosted by KOBV  Open
Archives Initiative  DINI Zertifikat 2007  OA Netzwerk