Experimental investigation of intermittent airflow separation and microscale wave breaking in wavy two-phase pipe flow. (18th September 2019)

• Record Type: Journal Article
• Authors: Vollestad, P.; Ayati, A. A.; Jensen, A.
• Is Part Of: Journal of fluid mechanics. Volume 878(2019)
• Page Start: 796
• Page End: 819
• Publication Date: 2019-09-18
• Subjects: gas/liquid flows, -- wave breaking, -- wind–wave interactions; Fluid mechanics -- Periodicals; 532.005
• DOI: 10.1017/jfm.2019.660
• Languages: English
• ISSNs: 0022-1120

Abstract

Abstract : We perform an experimental analysis of co-current, stratified wavy pipe flow, with the aim of investigating the effect of small scale wave breaking (microscale breaking) on the airflow. Particle image velocimetry is applied simultaneously in the gas and liquid phases. Active wave breaking is identified by high levels of vorticity on the leeward side of individual waves, and the statistics of the airflow above breaking and non-breaking waves are extracted from the gas-phase velocity fields. Keeping the liquid superficial velocity constant ( $U_{sl}=0.1~\text{m}~\text{s}^{-1}$ ), we consider two experimental cases of different gas flow rates. The lowest flow rate ( $U_{sg}=1.85~\text{m}~\text{s}^{-1}$ ) is slightly higher than the onset of microscale breaking, while the higher flow rate ( $U_{sg}=2.20~\text{m}~\text{s}^{-1}$ ) is within the regime where wave breaking is observed to be frequent, and the root-mean-square interface elevation $\unicode[STIX]{x1D702}_{rms}$ is independent of gas flow rate. Results show that for the lowest gas flow rate considered, active wave breaking has a stabilizing effect on the airflow above the waves, reducing the sheltered region on the leeward side of the wave and the turbulence above the wave crest compared with non-breaking waves at similar steepness. At the higher gas flow rate the effect of active wave breaking is found to be small, and the main geometrical properties of the waves are found to dominate the evolution of the separated flow region.