Study on the Motion Characteristics of Particles Transported by a Horizontal Pipeline in Heterogeneous Flow

被引:4
|
作者
Wang, Jiayi [1 ]
Li, Yitian [1 ]
Lai, Zhiqiang [2 ,3 ]
Zhao, Lianjun [2 ,3 ]
Wang, Zhongmei [2 ,3 ]
机构
[1] Wuhan Univ, State Key Lab Water Resources & Hydropower Engn S, Wuhan 430072, Peoples R China
[2] Yellow River Conservancy Commiss, Yellow River Inst Hydraul Res, Zhengzhou 450003, Peoples R China
[3] Minist Water Resources, Key Lab Lower Yellow River Channel & Estuary Regu, Zhengzhou 450003, Peoples R China
基金
中国国家自然科学基金;
关键词
self-priming pipe; pipeline velocity; pipeline sand drainage; particle motion; sediment transport rate; NUMERICAL-SIMULATION; PRESSURE-DROP; LIQUID; DEPOSITION; VELOCITY; SOLIDS; SLURRY;
D O I
10.3390/w14193177
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The worldwide problem of reservoir sedimentation has perplexed the water conservancy industry. The problem of reservoir sedimentation is particularly serious in sandy rivers in China and directly affects the normal function of reservoirs. Due to its effect on the economy and environmental protection, the self-priming pipeline dredging and sediment discharge technology has broad application prospects. Nevertheless, there are pressing problems in the transportation of slurry particles in the pipeline system of this new technology. The purpose of this study is to use physical model tests to analyze the influence of the sediment transport rate and pipeline velocity on the motion state of particles (aggregation transport, jump transport, and suspension transport) when a heterogeneous flow with different particle sizes is transported in the pipeline. The results indicate that under the same pipeline velocity and sediment transport rate, the thickness of the static particle accumulation layer decreases with the increase in particle size in the state of aggregation and transportation, and the smaller the particle size, the greater the particle movement speed in the case of aggregation and suspension transportation. During jump transportation, the velocity of particles above the critical inflection point Y' increases with the decrease in particle size. The opposite is found below the critical inflection point Y'. At the same particle size and sediment transport rate, when the pipeline velocity increases, the particle transport transits from aggregation transport to jump transport and then to suspension transport. The larger the pipeline velocity, the greater the overall movement speed of particles. When gathering and conveying, if the pipeline flow rate increases by 1.5, the maximum movement speed of particles increases by 3.3. The curvature of the vertical velocity curve of the particles during jump transportation is not affected by the pipeline velocity. The particle velocity at the highest point increases with the increase in the pipeline velocity. During suspension transportation, the difference between the maximum and minimum vertical particle distribution velocities is exponentially related to the pipeline velocity. At the same pipe velocity and particle size, the overall particle velocity decreases with the increase in sediment transport rate.
引用
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页数:16
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