Experimental study of two and three phase flows in large diameter inclined pipes

被引:219
作者
Oddie, G
Shi, H
Durlofsky, LJ
Aziz, K
Pfeffer, B
Holmes, JA
机构
[1] Schlumberger Cambridge Res Ltd, Cambridge CB3 0EL, England
[2] Stanford Univ, Dept Petr Engn, Stanford, CA 94305 USA
[3] ChevronTexaco EPTC, San Ramon, CA 94583 USA
[4] Schlumberger GeoQuest, Abingdon OX14 1DZ, Oxon, England
关键词
two phase; three phase; large diameter; inclined; steady-state; transient; water-gas; oil-water; oil-water-gas; wellbore; holdup; flow pattern; mechanistic model;
D O I
10.1016/S0301-9322(03)00015-6
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Steady-state and transient experiments of water-gas, oil-water and oil-water-gas multiphase flows were conducted on a transparent I I in long, 15 cm, diameter, inclinable pipe using kerosene, tap water and nitrogen. The pipe inclination was varied from 0degrees (vertical) to 92degrees and the flow rates of each phase were varied over wide ranges. Fast-acting valves enabled the trapping of the fluid flowing in the pipe, which in turn allowed for the accurate measurement of the absolute volumetric fraction (holdup) of each phase. A nuclear densitometer, as well as ten electrical probes at various locations along the pipe, provided additional steady-state and transient measurements of the holdup. A total of 444 tests were conducted, including a number of repeated tests. Bubble, churn, elongated-bubble, slug, and stratified/stratified-wavy flows were observed for water-gas and oil-water-gas flows, while dispersed/homogeneous, mixed/semi-mixed and segregated/semi-segregated flows were observed for oil-water flows. Extensive results for holdup as a function of flow rates, flow pattern and pipe inclination are reported, and the various techniques for measuring holdup are compared and discussed. The flow pattern and shut-in holdup are also compared with the predictions of a mechanistic model. Results show close agreement between observed and predicted flow pattern, and a reasonable level of agreement in holdup. (C) 2003 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:527 / 558
页数:32
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