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若干学者在考察近岸地区的泥沙运动,特别是推移质运动时,认为在海底附近范围内的流速分布,仍可用对数公式:
When investigating the sediment movement in the nearshore area, especially the thrusting movement, some scholars think that the distribution of the flow velocity in the vicinity of the sea bottom can still be expressed by the logarithmic formula: