2) high sand concentration sea water
高含沙海水
3) high turbid water with slit content
含沙高浊水
4) hyperconcentrated flows
高含沙水流
1.
Study of the spatial differentiation of hyperconcentrated flows frequency in the Loess Plateau;
黄土高原区高含沙水流发生频率空间分异及其影响因素
2.
Based on the data from Zizhou and Wangjiagou Experimental stations in the coarse sediment-producing area of the middle Yellow River drainage basin, this study deals with characteristics of hyperconcentrated flows in slope-channel systems in the gullied hilly areas.
以黄河中游多沙粗沙区子洲径流站和离石王家沟试验站的径流场观测资料为基础,对黄土高原丘陵沟壑区坡沟系统中高含沙水流特征进行了研究。
3.
Semi arid climate, poor vegetation cover and highly erodible loess can be regarded as the main natural factors responsible for the formation of hyperconcentrated flows in the Loess Plateau, China.
黄土高原半干旱的气候条件、稀疏的植被和疏松易蚀的黄土物质，是该地区高含沙水流形成的自然地理因素。
5) hyperconcentrated flow
高含沙水流
1.
Transfer and dissipation laws of turbulent energy in hyperconcentrated flow;
高含沙水流紊动能量转化与耗散规律
2.
The hyperconcentrated flow is an important factor to the high intensity erosion of the high-intensity and coarse sediment producing area of the Loess Plateau.
高含沙水流的频繁发生是黄土高原多沙粗沙区产生高强度侵蚀的重要原因。
3.
Compared with low concentration sediment flow, hyperconcentrated flow has its specific properties.
本文综述了高含沙水流的阻力特征、流速分布、紊动强度分布、能量分布等流动过程中所具有的特性 ,并和清水、低含沙水流作了对比分析。
6) hyperconcentration flow
高含沙水流
1.
In this paper, the resistance coefficient of pipe to transport hyperconcentration flow has been experimentaly studied by on_the_spot measurement.
作者利用实测管道压力、流量、含沙量等数据对高含沙水流阻力特性进行分析 ,取得了在管道粗糙过渡区泥浆沿程阻力系数受Re数、含沙量影响的基本认识 ,进一步给出了常规条件下沿程阻力系数与综合泥浆因子间相关关系及计算方法。
2.
The basic transport properties of Yellow River sediments and bakelite powders(which are used as the sediments in the model) are studied systematically, and the similarity relationships for hyperconcentration flows are developed.
首次提出了可应用于高含沙水流模型试验的相似关系，据此理论建造了黄河小浪底枢纽１：８０的正态泥沙模型。
补充资料：沙水
1.沙滩上的水。 2.沙与水。
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