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Medientyp: E-Artikel Titel: Meso‐scale catchment sediment budgets: combining field surveys and modeling in the Dragonja catchment, southwest Slovenia Beteiligte: Keesstra, S. D.; Bruijnzeel, L. A.; van Huissteden, J. Erschienen: Wiley, 2009 Erschienen in: Earth Surface Processes and Landforms Sprache: Englisch DOI: 10.1002/esp.1846 ISSN: 0197-9337; 1096-9837 Schlagwörter: Earth and Planetary Sciences (miscellaneous) ; Earth-Surface Processes ; Geography, Planning and Development Entstehung: Anmerkungen: Beschreibung: <jats:title>Abstract</jats:title><jats:p>In this paper, we present a methodology to construct a sediment budget for meso‐scale catchments. We combine extensive field surveys and expert knowledge of the catchment with a sediment delivery model. The meso‐scale Mediterranean drainage basin of the Dragonja (91 km<jats:sup>2</jats:sup>), southwest Slovenia, was chosen as case study area.</jats:p><jats:p>During the field surveys, sheet wash was observed on sloping agricultural fields during numerous rainfall events, which was found to be the main source of sediment. With the sediment yield model WATEM/SEDEM the estimated net erosion on the hillslopes 4·1 t ha<jats:sup>–1</jats:sup> y<jats:sup>–1</jats:sup> (91% of inputs). The second source, bank erosion (4·2%; 0·25 t ha<jats:sup>–1</jats:sup> y<jats:sup>–1</jats:sup>) was monitored during several years with erosion pins and photogrammetric techniques. The last source, channel incision, was derived from geomorphological mapping and lichenomery and provided 3·8% (0·17 t ha<jats:sup>–1</jats:sup> y<jats:sup>–1</jats:sup>) of the sediment input.</jats:p><jats:p>The river transports its suspended sediment mainly during high‐flow events (sampled with automated water samplers). About 27% (1·2 t ha<jats:sup>–1</jats:sup> y<jats:sup>–1</jats:sup>) of the sediment delivered to the channel is deposited on floodplains and low terraces downstream (estimated with geomorphological mapping, coring and cesium‐137 measurements). The sediment transported as bedload disintegrates during transport to the outlet due to the softness of the bedrock material. As a result, the river carries no bedload when it reaches the sea.</jats:p><jats:p>The results imply a build‐up of sediment in the valleys catchment. However, extreme flood events may flush large amounts of sediment stored in the lower parts of the system. Geomorphological evidence exists in the catchment that such high magnitude, low frequency events have happened in the past. Copyright © 2009 John Wiley & Sons, Ltd.</jats:p>