Effects of submergence depth on the growth and tuberization of Eleocharis ochrostachys Steud.

2021 ◽  
Vol 10 (5) ◽  
pp. 62-68
Author(s):  
Phuong Vo Thi ◽  
Sanh Nguyen Du ◽  
Truc Huynh Thi Thanh ◽  
Nhu Nguyen Thi Huynh ◽  
Mai Pham Thi Thanh ◽  
...  
Keyword(s):  
Author(s):  
Tianshi Liu ◽  
Min Zheng ◽  
Xinai Song ◽  
Ying Wu ◽  
Rong Zhang
Keyword(s):  
Oil Well ◽  

Author(s):  
Thiyam T. Devi ◽  
Annu P. Sinha ◽  
Meena Thakre ◽  
Bimlesh Kumar

Author(s):  
Ali Fakhri Kadhim ◽  
Hayder A. Al Thamiry

The pumping station is widely used in our modern life. The occurrence of the vortex at pumpsump, which is causing air entering pipe intake, is a common problem in the design of pumps. Thisphenomenon, including surface and sub-surface vortex, may lead to damage to the pumping structure, highpower consumption, and loss in pump performance. In some requirements, the multiple suction pipes areusing to get the required flow. Due to this arrangement, the performance of the suction pipes will influence.This paper is aimed to investigate the occurrence of vortices around the flow pattern of two pumps by usingComputational Fluid Dynamic (CFD) code Fluent. This CFD model is based on solving Navier-Stockequations by finite volume method. The model of double suction pipes was investigated under five differentsubmergence depth (S) and five different suction velocities (v). The SST k-ω turbulence model was selectedfor the turbulence. The results showed that the air entering vortex does not appear when the submergencedepth (S) is equal or greater than 1.5 times from the diameter of the bellmouth for intake pipe (D). Thesurface vortex appeared obviously when the submergence depth (S) equals to 1.25D and the Froude numberat the bell is equal to or greater than 1.028, and appeared clearly when the (S/D=1) and Froude number isequal to or more than 0.77. The nearer attached wall vortex does not appear when the space from the centerof the suction pipe to the sidewall (C) equals 2 times of bell diameter.


2016 ◽  
Author(s):  
Shengmu Yang ◽  
Jiuxing Xing ◽  
Daoyi Chen ◽  
Shengli Chen

Abstract. A mesoscale eddy's trajectory and its interaction with topography under the planetary β and nonlinear effects in the South China Sea are examined using the MITgcm. Warm eddies propagate to the southwest while cold eddies propagate to the northwest. The speed of both warm and cold eddies is about 2.4 km/day in the model. The eddy trajectory and its structure are affected by an island or a seamount, in particular, some eddies may split during the interaction with an island/seamount. Eddy-splitting is related to the size of the island and the submergence depth of the seamount. The results of sensitivity experiments of the interaction between an idealized eddy and an island/seamount indicate that the eddy would split in the qualitative range of 1/4 


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