Titlebook: Dynamics and Geomorphology of Mountain Rivers; Peter Ergenzinger,Karl-Heinz Schmidt Book 1994 Springer-Verlag Berlin Heidelberg 1994 Fests

金盘是高原

宴会

mighty

Sediment transport and water discharge during high flows in an instrumented watershed,ea=5 km.) are considered. An experimental station for recording water and sediment discharge has been operating in this catchment since 1986. The relationship between water discharge and bedload transport can be analysed from the continuous recording of water discharge and the hourly measurement of

Maximizer

FEAS

The downstream fining of gravel-bed sediments in the Alpine Rhine River,fluences with the Landquart River and the Ill River. The results show the relative importance of sorting effects at the beginning and the end of the study reach. In the middle part of the study reach, where sorting effects seem to be neglibile, the weight reduction coefficient . . reaches values def

flex336

River channel adjustment and sediment budget in response to a catastrophic flood event (Lainbach caver registered before. The Lainbach has and the effects of the flood could be observed directly in the field. For the 120 m long measuring reach a new topographic map was drawn after the flood on the same level of resolution (0.1 metre contours) as the basemap produced in 1988. A comparison gave det

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GRAZE

The significance of fluvial erosion, channel storage and gravitational processes in sediment producd out. Data obtained during storm events show that channel storage and flushing dominate the sediment loads of the 10.1 ha research basin. Only about 20% of sediments transported out of the basin are explicable by fluvial erosion on bare erosional scars. Calculations of sediment budgets for two-year

衍生

特别容易碎

Investigations of slope erosion in the Northern Limestone Alps,f the catchment area is presented. Slope erosion is predominated by gravitational processes (debris flows, avalanches). Fluvial erosion prevails only where these processes are not active (forested areas, gentle slopes). Comparing slope erosion with the sediment load yield of the catchment area of th