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

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M. Altmann,K. S. de Boer,H. Edelmann07–0.14 m. The standard deviation of the grain size distribution was variable δ=1.8–3.2..The presented investigations concern the floods, when the maximum water flow was Q.=5.50 m./s, Q.=2.75 m./s, Q.=5.75 m./s, Q.=5.90 m./s. The amounts of the transported bed material during these floods were: G.=6
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Mikhail V. Tonkov,N. N. Filippovl sediment load results from gravitational processes, which mainly occur in winter during ablation periods. Therefore an alternation of sediment production by gravitational processes in winter and removal by fluvial processes during summer can be assumed.
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