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001445034 001__ 1445034
001445034 003__ OCoLC
001445034 005__ 20230310003809.0
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001445034 020__ $$a9783658370732$$q(electronic bk.)
001445034 020__ $$a3658370734$$q(electronic bk.)
001445034 020__ $$z3658370726
001445034 020__ $$z9783658370725
001445034 0247_ $$a10.1007/978-3-658-37073-2$$2doi
001445034 035__ $$aSP(OCoLC)1302696987
001445034 040__ $$aYDX$$beng$$cYDX$$dGW5XE$$dEBLCP$$dOCLCO$$dOCLCF$$dUKAHL$$dOCLCQ
001445034 0411_ $$aeng$$beng$$bger$$heng
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001445034 049__ $$aISEA
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001445034 1001_ $$aKainz, Simon.
001445034 24510 $$aCharacterizing groundwater flow dynamics and storage capacity in an active rock glacier /$$cSimon Kainz.
001445034 260__ $$aWiesbaden, Germany :$$bSpringer Spektrum,$$c2022.
001445034 300__ $$a1 online resource
001445034 4901_ $$aBestMasters
001445034 504__ $$aIncludes bibliographical references.
001445034 5050_ $$aIntroduction -- Study site -- Methods -- Results and interpretation -- Discussion -- Conclusion -- Outlook.
001445034 506__ $$aAccess limited to authorized users.
001445034 520__ $$aAlpine aquifers play a critical role in the hydrology of mountainous areas by sustaining base flow in downstream rivers during dry periods and retarding flood propagation after heavy precipitation events. Progressing climate change alters climatic and meteorological boundary conditions as well as the hydraulic response of alpine catchments by ablating glaciers and thawing permafrost. Rock glaciers exert a controlling influence on the catchment response due to their prominent groundwater storage and complex drainage characteristics. This thesis investigates the hydrogeology and internal structure of the active rock glacier Innere Olgrube (Otztal Alps), which governs catchment runoff and is affected by permafrost degradation. A 3D geometrical model of its internal structure is obtained by combining geophysical data and permafrost creep modelling. Available data and new results are integrated into a conceptual hydrogeological model providing a sound basis for the implementation of a prospective numerical groundwater flow model. Hydraulic properties of the hydrostratigraphic units constituting the rock glacier are estimated and groundwater recharge fluxes quantified. Fundamental properties of the heterogeneous groundwater flow system within the rock glacier are discussed and compared to existing rock glacier studies. About the author Simon Kainz is currently working on alpine water resources and climate change as PhD student at the University of Graz, Austria. His educational background is geosciences, focusing on hydrogeology and engineering geology at the Universities of Graz, Leoben, and Waterloo (ON).
001445034 546__ $$aAbstract in German and English.
001445034 588__ $$aOnline resource; title from PDF title page (SpringerLink, viewed March 18, 2022).
001445034 650_0 $$aHydrogeology$$zÖtztal Alps (Austria and Italy)
001445034 650_0 $$aRock glaciers$$zÖtztal Alps (Austria and Italy)
001445034 650_6 $$aHydrogéologie$$zAlpes d'Ötztal (Autriche et Italie)
001445034 650_6 $$aGlaciers de pierres$$zAlpes d'Ötztal (Autriche et Italie)
001445034 655_0 $$aElectronic books.
001445034 77608 $$iPrint version: $$z3658370726$$z9783658370725$$w(OCoLC)1296419845
001445034 830_0 $$aBestMasters.
001445034 852__ $$bebk
001445034 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-658-37073-2$$zOnline Access$$91397441.1
001445034 909CO $$ooai:library.usi.edu:1445034$$pGLOBAL_SET
001445034 980__ $$aBIB
001445034 980__ $$aEBOOK
001445034 982__ $$aEbook
001445034 983__ $$aOnline
001445034 994__ $$a92$$bISE