Identification of flow regime and estimation of volume fraction independent of liquid phase density in gas-liquid two-phase flow

2017 ◽  
Vol 98 ◽  
pp. 29-37 ◽  
Author(s):  
G.H. Roshani ◽  
E. Nazemi ◽  
M.M. Roshani
2020 ◽  
Vol 61 (10) ◽  
Author(s):  
Yongchao Zhang ◽  
Amirah Nabilah Azman ◽  
Ke-Wei Xu ◽  
Can Kang ◽  
Hyoung-Bum Kim

2021 ◽  
Author(s):  
Yang Gao ◽  
Haoyuan Gao ◽  
Bin Li ◽  
Tongyao Wei ◽  
Zhuang Li

Abstract During a landslide, the multi-phase nature of landslide debris defines its mobility. Eventually, frictional forces cause the slide energy to dissipate, and contact forces transmit the energy into nearby material. To analyze the dynamic characteristics of high-velocity long-runout landslides, we conducted flume model tests to empirically determine the mobility characteristics of flow-like landslides with various slide materials. Our conclusions are as follows: (1) Liquid-phase flow-like landslides are highly mobility and have long runout; solid-phase flow-like landslides are highly destructive because of their higher kinetic energy; and two-phase flow-like landslides are both highly mobility. (2) During a two-phase flow-like landslide, the mobility ability of the liquid-phase material is stronger than that of the solid-phase material; when the liquid slide volume fraction is sufficiently large, the liquid phase exerts a drag force on the solid phase. (3) Various liquids exert different drag effects on the solid; the solid-liquid velocity difference and the liquid viscosity determine the drag intensity and the mobility and depositional characteristics of the landslide.


1994 ◽  
Vol 59 (12) ◽  
pp. 2595-2603
Author(s):  
Lothar Ebner ◽  
Marie Fialová

Two regions of instabilities in horizontal two-phase flow were detected. The first was found in the transition from slug to annular flow, the second between stratified and slug flow. The existence of oscillations between the slug and annular flows can explain the differences in the limitation of the slug flow in flow regime maps proposed by different authors. Coexistence of these two regimes is similar to bistable behaviour of some differential equation solutions.


2003 ◽  
Vol 125 (4) ◽  
pp. 544-544 ◽  
Author(s):  
Sang Young Son ◽  
Jeffrey S. Allen ◽  
Kenneth O. Kihm

Author(s):  
F Bakhtar ◽  
H Mashmoushy ◽  
O C Jadayel

During the course of expansion of steam in turbines the fluid first supercools and then nucleates to become a two-phase mixture. The liquid phase consists of a large number of extremely small droplets which are difficult to generate except by nucleation. To reproduce turbine two-phase flow conditions requires a supply of supercooled vapour which can be achieved under blow-down conditions by the equipment employed. This paper is the third of a set describing an investigation into the performance of a cascade of rotor tip section profiles in wet steam and presents the results of the wake traverses.


2011 ◽  
Vol 32 (1) ◽  
pp. 164-175 ◽  
Author(s):  
J. Enrique Julia ◽  
Basar Ozar ◽  
Jae-Jun Jeong ◽  
Takashi Hibiki ◽  
Mamoru Ishii

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