1) sediment pick-up flux
泥沙上扬通量
1.
Turbulent bursting-based sediment pick-up flux from loose bed;
基于湍流猝发的床面泥沙上扬通量
2) pick-up flux
上扬通量
1.
An energy equilibrium model of uniform sediment pick-up flux;
均匀沙上扬通量的能量平衡模型
3) sediment flux
泥沙通量
1.
According to the measured data of sediment of many important hydrological stations in the middle and lower stream of the Yellow River for more than 50 years,the multi-method of hydrology,mechanics of sediment transport,fluvial process and statistics are applied to study the patterns of variations in the sediment flux in recent 50 years.
根据黄河中下游多个主要水文控制站50多年的实测资料,利用水文学、泥沙运动力学、河床演变学和经验统计相结合的分析方法,分析黄河中下游泥沙通量的变化规律。
2.
The paper summarizes the present status of study on delta sediment flux both at home and abroad,involving hydro-sediment statistical model,deposition dynamics and mathematical model.
总结了国内外河口泥沙通量研究的现状,内容涉及到水文泥沙统计模型、沉积动力学与数学模型。
3.
The errors of the crosssectional sediment flux estimation mainly origin from survey site layout and flux calculation method.
断面泥沙通量估算的误差主要来源于计算方法、测点布局等,通量模式应该建立在通量估算统计误差最小的原则基础之上。
4) sediment flux ratio
泥沙通量比
1.
Similar conditions of deposition and suspension for distorted model are incompatible and from theoretical analysis,it is demonstrated that both of the above two similar conditions are not tenable,and a similar condition of vertical sediment flux ratio is presented as a substitute.
理论分析表明 ,在变态模型中该两个相似条件均不能成立 ,替代它们的是一个所谓垂向泥沙通量比相似条件。
5) bed load resuspension
泥沙悬扬
6) critical conditionsfor sediment suspension
泥沙扬动
补充资料：传质通量
分子式：
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
CAS号：
性质：又称传质通量。单位时间、单位面积所传过去的物质质量，用符号N表示，其单位为kg/(m2·s)。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条