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Experimental Study of Air-Water Flow in Undulating Pipeline and Implication on Sand Transport

机译:波纹管中空气水流的实验研究及对输沙的影响

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The study of multiphase flow is more difficult and complex in undulating pipelines due to flow interaction between differentrnpipe sections and influence of the specific angles being studied. While previous studies (Zheng et al., 1995; Al-Safran et al.,rn2005) are low angles of hilly pipeline, there is no adequate information on flow characteristics for high angles. Therncomplexity in sand transportation in multiphase flow is more aggravated in undulating pipelinernThis paper presents experimental investigations to understand the multiphase flow characteristics, conditions for slugrninitiation mechanism that would enhance sand transport in undulating pipes and assist pipeline design. The investigationsrnwere conducted using a 2-inch (ID=50.24 mm) dip facility which consists of a downhill pipeline (-24o), a lower elbow (dip)rnand an uphill pipeline (+24o).rnThe slug initiation mechanisms phenomena were investigated. New flow regimes were identified for different pipe sectionsrnusing both visual observation and statistical parameters. Sand transport characteristics in water and air-water were studied atrndifferent sand concentration. Also, flow condition to transport sand bed deposit at the dip was determined.rnThree slug behaviours were observed at the dip: complete stratified flow downhill with slug initiation at dip; stratified flowrn(with energetic ripple) downhill with slug initiation and slug growth at the dip; and aerated slug downhill and slug growth atrnthe dip. This behaviour is different from existing works on this subject with low angle of inclination.
机译:由于不同管段之间的流动相互作用以及所研究的特定角度的影响,在起伏的管道中进行多相流的研究更加困难和复杂。虽然以前的研究(Zheng等,1995; Al-Safran等,rn2005)是丘陵管道的低角度,但对于大角度的流动特性却没有足够的信息。在起伏的管道中,多相流中输沙的复杂性更加严重。本文提出了一些实验研究,以了解多相流的特性,形成团粒的机理条件,这些条件会增强起伏管道中的输沙并有助于管道设计。研究使用2英寸(ID = 50.24 mm)浸入设备进行,浸入设备由下坡管道(-24o),下肘(dip)和上坡管道(+ 24o)组成。研究了团状引发机制现象。利用目测和统计参数,为不同的管段确定了新的流态。在不同的沙浓度下,研究了水和空气中沙的迁移特征。并确定了在垂线下运沙床沉积物的流动条件。rn在垂线处观察到了三种团状行为:下坡完全分层流,在垂线处开始有团块;层状流(有高能量波纹)下坡,有团状萌生和凹陷处团状生长;以及下坡时充气的子弹和子弹的生长。这种行为不同于现有关于该主题的低倾斜角度的作品。

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