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Titel Holocene, subrecent and contemporary source-to-sink fluxes in a valley-fjord system, Erdalen and Bødalen site project (SedyMONT - Norway)
VerfasserIn Achim A. Beylich
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250032478
 
Zusammenfassung
The focus of this ESF-NFR funded Norwegian Individual Project (IP5, 2008-2013) within the European Science Foundation (ESF) SedyMONT (EUROCORES TOPO-EUROPE) Programme (http://www.esf.org/topoeurope) is on Holocene, subrecent and contemporary sedimentary fluxes and budgets in the Erdalen and Bødalen catchments in Nordfjord, western Norway (http://www.ngu.no/sedymont). The innovative approach of this research project is the integrated quantitative study of longer-term (Holocene), subrecent and contemporary source-to-sink fluxes and process rates using a novel combination of advanced methods and techniques. With respect to the main aims and objectives of ESF SedyMONT, the following main aims of the Erdalen and Bødalen site project can be stressed: - Analyse how the inheritance of the landscape due to the influence of the Last Glacial Maximum (LGM) has affected process rates over time (paraglacial system), - Document changes in process rates over different timescales by combining quantitative knowledge on Holocene process rates with newly generated data on subrecent and contemporary process rates. Monitoring of surface processes in Erdalen and Bødalen, in combination with repeated analyses of surface water chemistry, atmospheric solute inputs and granulometric analyses of suspended sediments provide high-resolution data to analyse and quantify present-day sedimentary and solute fluxes as well as sediment sources, denudation rates, and meteorological and topographic / landscape morphometric controls of denudative processes. In addition to standard methods for monitoring bedload transport, innovative techniques like impact sensors, PIT tags and biofilm analysis are applied to analyse channel stability / mobility and to estimate bedload transport rates in both valleys. The volume and composition of lake sediments are studied using echo-sounder, georadar and different coring techniques. Investigations on volumes and architecture of storage elements (talus cones, valley infills, deltas) using different geophysical methods like georadar and seismic refraction surveys are carried out to improve the quantitative knowledge on Holocene process rates. Detailed geomorphological mapping is performed and interpreted in combination with digital elevation models and data. The process and denudation rates in Erdalen and Bødalen are compared with process and denudation rates in the other SedyMONT test sites (Alps) (http://www.sedymont.eu) and with other cold environment catchments worldwide through the global SEDIBUD Programme (http://www.geomorph.org/wg/wgsb.html).