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Multiphase flow involves flow of more than one phase or component. In
multiphase flow, a phase can be defined as an identifiable class of material that has a
particular inertial response to and interaction with the flow and the potential field in which it
is immersed. For example, different-sized solid particles of the same material can
be treated as different phases because each collection of particles with the same size
will have a similar dynamical response to the flow field. Two-phase flow is a case
of multiphase flow in which the two phases may exist in the four combinations of
gas-liquid, gas-solid, liquid-solid and liquid-liquid. Among these, analysis of
gas-liquid two-phase flow is complex due to the fact that the interface between the two
phases changes its shape with respect to time and space.
Mandhane et al. (1974), and Taitel and Dukler (1976) experimentally
captured various air-water type two-phase flow patterns. They developed the flow
pattern map by varying the mass flow rate of the gas and liquid phase. The flow pattern
map showed various flow regimes and their transitions. Kaminsky (1999), and Ghajar
and Tang (2007) reestablished these flow pattern maps using sophisticated
instrumentation and highly accurate measurement facility. They could capture various
intermittent regimes which were not observed previously. In addition, the pressure drop and
heat transfer characteristics for different flow patterns were measured.
Due to the advancement in computational techniques and numerical
algorithms, the practical experimentation is being replaced by numerical experimentation
(Lun et al., 1996). The numerical analysis involved in the two-phase flow includes
algorithms to locate the interface, drift velocity, and the momentum and energy exchange at
the interface (Hetsroni, 1982). Various numerical models have been proposed
in literature. These include Euler-Lagrange and Euler-Euler approaches. Efforts
have been made to model various flow patterns independently by various
researchers (Neti and Mohamed, 1990; Ghorai and Nigam, 2006; Schepper et al., 2008; and Vallee et al., 2008). |