(562e) Comparison of Meso Scale Subsea Gas Release with Multiphase Euler-Lagrangian CFD Model
AIChE Annual Meeting
2015
2015 AIChE Annual Meeting Proceedings
Engineering Sciences and Fundamentals
Turbulent and Reactive Flows
Wednesday, November 11, 2015 - 1:30pm to 1:45pm
Objectives/Scope: The primary objective of the present study is to characterize the
dynamics of subsea starting plumes and compare experimental observations with
multiphase computational fluid dynamics (CFD) simulations.
Methods and Procedures: Meso scale experiments were performed under controlled conditions
in the Trondheims Fjord during the spring of 2014. The release depth was 30 m
and the gas (ambient air) rates were varied between 18-72 Nm3/min through a
2" nozzle. Instrumentation was mounted on a frame that allowed
measurements to be taken at virtually any position inside and outside the
plume. The frame was deployed from a barge (65 x 17.5 m) using a heavy lifting
crane. Two air compressors supplied the gas at 10 bar. The instrumentation
included flow vanes, video cameras and a high speed camera system enabling
estimation of void, bubble size and bubble tracking. In addition surface
dynamics were probed using wave guides and cameras, enabling monitoring of
surface elevation and surface flow dynamics. A novel sonar imaging system was
employed to image the evolution of the bubble plume throughout the water
column. A transient 3D CFD model consisting of an Eulerian VOF model for
tracking the large scale interface between the ocean and atmosphere coupled to
a Lagrangian description of the dispersed bubble phase was used to model the
rising bubble plume. The Lagrangian model used to track the dispersed bubble
phase does not model individual bubbles but rather statistical parcels each
containing a large number of bubbles. The model accounts for gas
compressibility, mass transfer, employs a dynamic bubble size model accounting
for breakup and coalescence, damping of turbulence close to the ocean surface
and ocean stratification.
Results, Observations and Conclusions: We investigate the effects of release rate on overall plume
dynamics such as rise time, surface spreading, fountain height and plume angle
and compare CFD simulations with experimental observations done during the 2014
field trail on subsea gas blowout and literature data. We find that progress in
sonar imaging now allows subsea gas plumes to be visualized in detail and may
prove a very useful tool in field situations. The CFD model captures all the
main features observed in the experiments. However, we note that the CFD model
is sensitive to the initial ambient ocean conditions.
Novel/Additive Information: To our knowledge no studies have presented an equally detailed
experimental characterization of the evolution of starting plumes using
"3D sonar" imaging, nor have they been able to compare experiments
with equally detailed three dimensional transient multiphase CFD simulations.
The near shore meso scale experiment described in this study was conducted as a
qualification of instrumentation and initial validation of a CFD model before
progressing to full scale offshore experiments.
Figure 1:
Simultaneous tracking of bubble plume using sonar imaging looking at subsea
plume from the side (left) and visual imaging looking vertically down onto the
ocean surface (right).