分析了多来多排的机理后认为：临界流速的非单值性是挟沙能力多值性的深层原因；
It deems after analyzing the mechanism of desilting as much as coming that non-uniqueness of critical velocity is the deep reason of multi-value of sediment carrying capacity and;
分析了多来多排的机理后认为：临界流速的非单值性是挟沙能力多值性的深层原因；
It deems after analyzing the mechanism of desilting as much as coming that non-uniqueness of critical velocity is the deep reason of multi-value of sediment carrying capacity and;
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