| 释义 |
Karman constant
基本例句
化卡曼常数
The results from this equation ofKarman constantagree with measured data.该卡门常数的理论公式与实测资料较为吻合。
Velocity distribution in sediment-laden flow,especially itsKarman constant,is one of the most important issues in fluvial hydraulics.挟沙水流的流速分布,特别是其中的卡门常数,一直是冲积河流水力学研究的热点问题之一。
The vonKarman constantof sediment-laden flows is one of the important parameters reflecting the influence of sediment movement on the flow structure.挟沙水流卡门常数是反映泥沙运动对水流结构影响的重要参数之一,本文回顾并讨论了挟沙水流卡门常数的计算公式及其影响因素。
Velocity distribution in sediment-laden flow, especially itsKarman constant, is one of the most important issues in fluvial hydraulics.摘要挟沙水流的流速分布，特别是其中的卡门常数，一直是冲积河流水力学研究的热点问题之一。
By use of this model, it is demonstrated that theKarman constantis varied in vertical distance from near 0.4 in near bed region to below 0.4 in main flow region.利用该流速分布模型，得到挟沙水流的卡门常数沿垂线是变化的结论，即从近底区的约0.;4渐变到主流区的小于0
By use of this model,it is demonstrated that theKarman constantis varied in vertical distance from near in near bed region to below in main flow region.利用该流速分布模型;得到挟沙水流的卡门常数沿垂线是变化的结论;即从近底区的约0.;4渐变到主流区的小于0 |