1) sediment movement equation
泥沙运动方程
1.
Generation of body-fitted grids and transformation of the 2-D sediment movement equation in body-fitted coordinate regions;
贴体网格的生成与平面二维泥沙运动方程在贴体坐标区域中的变换
2) governing equation of sediment movement
泥沙运动基本方程
3) sediment transport
泥沙运动
1.
Study on the sediment transport direction on the beach of Taozi Bay,Yantai;
烟台套子湾海滩泥沙运动方向研究
2.
On the effective shear stress of sediment transport;
确定泥沙运动有效切应力方法的探讨
3.
The authors analyze the surface sediment diameter characteristics in the east of Haikou Bay using EOF method,and draw some conclusion on the sediment sources and main hydrodynamics factors which control the sediment transport in the east of Haikou Bay.
作者对海口湾东部表层沉积物的粒径用EOF方法进行了分析 ,得出了海口湾东部浅滩区的泥沙来源与控制泥沙运动的主要动力因素 ,为对海口湾东部浅滩区的科学整治提供了依据。
4) sediment movement
泥沙运动
1.
And it is found that the sediment movement is consistent with the action of waves.
发现大风天气海底泥沙对波浪作用反应灵敏,悬沙和底沙分布规律与波浪作用吻合,为波浪作用下海底泥沙运动的理论研究以及海区工程开发提供了科学依据。
2.
The total flow differential model of sediment density current is used to simulate the sediment movement in the reservoir at dam.
运用异重流总流微分模型预测水库坝址泥沙运动过程,在满足防洪安全的前提下,结合水库入库洪水过程,进行旨在水库排沙比最大的水沙联合调度研究,最后给出实例。
3.
The remote sensing image analysis of the sea area where Binzhou Port is located has revealed the characteristics of sediment distribution in the sea area and the pattern of sediment movement under different conditions.
从泥沙运动的角度而言,受已建导堤影响,落潮水流和风吹流、波生流等叠加可能形成较复杂的向外水流和环流,携带泥沙向外输运,使高含沙水体运动更远的距离,一般情况下可达-6 m等深线以远。
5) sediment motion
泥沙运动
1.
Analysis of near-bed sediment motion;
床面附近泥沙运动的分析
2.
Sediment problems in the environment, and enviromental problems caused by sediment motion are discussed in this paper.
从两个方面，即水环境中的泥沙问题和泥沙运动引起的环境问题出发，说明了环境中泥沙问题的普遍性，指出了结合泥沙运动研究环境问题和结合环境科学研究泥沙问题的重要性和必要性，并将这方面的工作概括为“环境泥沙学”。
3.
were separately applied in analyzing and investigating the sediment motion lawin the hydraulic fill area at the estuary of Zhuhai River and the influence on the channel.
本文分别采用了现场水文测验、抛泥追测实验以及中子活化示踪等多种测试手段，对珠江口伶仃洋挖泥水抛区的泥沙运动规律及其对航道的影响进行了分析研究。
6) silt kinematics
泥沙运动学
1.
According to the research result of silt kinematics and the creep character of sandy soil, the movement law of high silt?laden flow in the Yellow River and the deformation of sand foundation under the eroded riverbed were studied.
依据泥沙运动学及砂土蠕变的研究成果,对黄河高含沙水流运动规律及河床冲刷底面下砂基的变形进行了研究。
补充资料：土壤水分运动基本方程(见土壤水运动)
土壤水分运动基本方程(见土壤水运动)
turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
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