作者: S. A. SCHUMM , H. R. KHAN , B. R. WINKLEY , L. G. ROBBINS
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摘要: MODEL studies1 of the dependence river patterns on sediment load and inclination surface which model flows—the valley slope—show that at a constant discharge very different channel are formed slopes (Fig. 1). Although is also an important factor affecting sinuosity river, Fig. 1 shows abrupt change in slope should lead to pattern.