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1)  releasing from sediment
底泥起动
2)  moveable muddy bed
活动底泥
3)  sediment disturbance
底泥扰动
1.
Effect of sediment disturbance on the phosphorus forms migration under different water temperature
不同水温时底泥扰动对不同形态磷分布的影响
4)  sediment incipience
泥沙起动
1.
Homogenous turbulence structure near the wall and sediment incipience;
各向同性均匀湍流近壁结构及泥沙起动
2.
Assuming that the instantaneous bed shear stress is the hydrodynamic mechanism of sediment incipience and transportation,the numerical model of the local scour under the complex flows around the structures is presented.
以床面瞬时剪应力作为泥沙起动及输运的水动力机制,建立了结构物周围复杂流场下床面局部冲刷的数学模型。
3.
As one of the most basic problems in the sediment transport theory, the mechanism of the sediment incipience is also needed to be understood for the study of local scouring process.
泥沙起动是泥沙运动理论中最基本的问题之一,也是研究泥沙输运及局部冲刷时必需解决的问题。
5)  sediment incipient motion
泥沙起动
1.
Experimental study on the sediment incipient motion in circulating flow;
回流泥沙起动规律的试验研究
2.
Because the resistance in sediment incipient motion is the sand-grain resistance,it is proposed that computation of the sand-grain resistance is based on resistance of sediment incipient motion.
利用泥沙起动的Shields曲线与明渠阻力特性之间的相似性,结合实测泥沙起动资料给出了沙粒阻力的计算公式。
3.
The motion characteristics of the sand group are researched from the perspective of theory and the dynamic condition for sediment incipient motion is obtained by determining the critical Shearing Stress, which can get rid of the influence of experiential factors and the research of sediment will radically start strict theoretical exploration.
根据波浪作用下的推移质群体泥沙运动方程可以看出推移质运动具有明显的非线性特性,对非线性动力学特性进行分析得到了考虑离散力时泥沙起动的希尔兹(Shields)曲线及一般形式的推移质输沙公式。
6)  incipient motion
泥沙起动
1.
The hydraulic gradients and flow directions were varied in tests to investigate the effects of the seepage on the incipient motion of the sand.
结果表明,泥沙起动流速曲线存在明显的转折点,可以解释崩岸的突发性;向坡外的渗流将大幅降低岸坡泥沙起动条件;冲刷水流方向也影响泥沙起动流速,在接近零流速破坏坡角时影响显著。
2.
During the fluvial processes of the alternate deposition and erosion, one of the key technologies predicting the bed’s deformation is how the location characteristics of bed material affects incipient motion for non-uniform sediment and transport rate for bed lo.
卵石滩床沙粗化对泥沙起动和推移质输沙能力影响较大,而各条河道的床沙粗化程度不尽相同,因而输沙能力相差也较大;即使同一河段的不同时期,河床粗化程度也不相同,输沙能力也不尽相同,这也是目前卵石起动、推移质输沙计算和实际情况差别较大的主要原因之一。
补充资料:阿泥底耶
【阿泥底耶】
 (天名)A^ditya,日天子之梵名。见不空罥索经四。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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