Computational and experimental study of an oil jet in crossflow: coupling population balance model with multifluid large eddy simulation

被引:5
作者
Daskiran, Cosan [1 ]
Cui, Fangda [1 ]
Boufadel, Michel C. [1 ]
Liu, Ruixue [1 ]
Zhao, Lin [2 ]
Ozgokmen, Tamay [3 ]
Socolofsky, Scott [4 ]
Lee, Kenneth [5 ]
机构
[1] New Jersey Inst Technol, Ctr Nat Resources, Civil & Environm Engn Dept, Newark, NJ 07102 USA
[2] ExxonMobil Upstream Res Co, Houston, TX 77389 USA
[3] Univ Miami, Dept Ocean Sci, Miami, FL 33149 USA
[4] Texas A&M Univ, Zachry Dept Civil Engn, College Stn, TX 77843 USA
[5] Fisheries & Oceans Canada, Dartmouth, NS B2Y 4A2, Canada
基金
美国国家科学基金会;
关键词
breakup/coalescence; drops; multiphase flow; DROPLET FORMATION; BUOYANT JETS; SUBSEA OIL; CRUDE-OIL; EVOLUTION; DYNAMICS; INJECTION; VELOCITY; TENSION; SCALAR;
D O I
10.1017/jfm.2021.1002
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Understanding the size of oil droplets released from a jet in crossflow is crucial for estimating the trajectory of hydrocarbons and the rates of oil biodegradation/dissolution in the water column. We present experimental results of an oil jet with a jet-to-crossflow velocity ratio of 9.3. The oil was released from a vertical pipe 25 mm in diameter with a Reynolds number of 25 000. We measured the size of oil droplets near the top and bottom boundaries of the plume using shadowgraph cameras and we also filmed the whole plume. In parallel, we developed a multifluid large eddy simulation model to simulate the plume and coupled it with our VDROP population balance model to compute the local droplet size. We accounted for the slip velocity of oil droplets in the momentum equation and in the volume fraction equation of oil through the local, mass-weighted average droplet rise velocity. The top and bottom boundaries of the plume were captured well in the simulation. Larger droplets shaped the upper boundary of the plume, and the mean droplet size increased with elevation across the plume, most likely due to the individual rise velocity of droplets. At the same elevation across the plume, the droplet size was smaller at the centre axis as compared with the side boundaries of the plume due to the formation of the counter-rotating vortex pair, which induced upward velocity at the centre axis and downward velocity near the sides of the plume.
引用
收藏
页数:38
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