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Studies on two-phase co-current air/non-Newtonian shear-thinning fluid flows in inclined smooth pipes
Authors:Jing-yu Xu  Ying-xiang Wu  Zai-hong Shi  Li-yun Lao  Dong-hui Li
Institution:1. Division of Engineering Sciences, Institute of Mechanics, Chinese Academy of Sciences, Beijing 100080, China;2. Petroleum Exploration and Production Research Institute, Sinopec Corp, Beijing 100083, China;3. BP Institute for Multiphase Flows, University of Cambridge, Madingley Road, Cambridge CB3 0EZ, UK
Abstract:In this work, co-current flow characteristics of air/non-Newtonian liquid systems in inclined smooth pipes are studied experimentally and theoretically using transparent tubes of 20, 40 and 60 mm in diameter. Each tube includes two 10 m long pipe branches connected by a U-bend that is capable of being inclined to any angle, from a completely horizontal to a fully vertical position. The flow rate of each phase is varied over a wide range. The studied flow phenomena are bubbly flow, stratified flow, plug flow, slug flow, churn flow and annular flow. These are observed and recorded by a high-speed camera over a wide range of operating conditions. The effects of the liquid phase properties, the inclination angle and the pipe diameter on two-phase flow characteristics are systematically studied. The Heywood–Charles model for horizontal flow was modified to accommodate stratified flow in inclined pipes, taking into account the average void fraction and pressure drop of the mixture flow of a gas/non-Newtonian liquid. The pressure drop gradient model of Taitel and Barnea for a gas/Newtonian liquid slug flow was extended to include liquids possessing shear-thinning flow behaviour in inclined pipes. The comparison of the predicted values with the experimental data shows that the models presented here provide a reasonable estimate of the average void fraction and the corresponding pressure drop for the mixture flow of a gas/non-Newtonian liquid.
Keywords:Two-phase flow  Shear-thinning fluid  Flow pattern  Void fraction  Pressure drop  Inclination flow
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