Velocity fields of N2- and CO2-water bubbly flows in a quasi-2D bubble column
Investigation using BIV and PIV
D. Sarker (TU Delft - ChemE/Transport Phenomena, International University of Business Agriculture and Technology)
C. V. Schinkel (TU Delft - ChemE/O&O groep)
L. M. Portela (TU Delft - ChemE/Transport Phenomena)
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Abstract
This study reports the distribution of gas and liquid velocity fluctuations and flow structures in N2-water and CO2-water bubbly flows within a pseudo-2D bubble column reactor (BCR). PIV and BIV techniques, operating at a resolution of 750 Hz, were synchronized, and ensemble averaging of the recorded velocity fields was performed to mitigate distortions caused by light interference, reflections, and shadows. Probability density functions (PDF), power spectral density (PSD), and cross-correlation values of velocity fluctuations were calculated to analyze gas bubble interaction and dissolution in dilute to dense bubbly flow regimes. The singular value decomposition (SVD) technique was applied to correlate the flow structure distribution and energy content of velocity fluctuation. The results indicate that CO2-water bubbly flow exhibits a bimodal distribution of velocity fluctuation at low gas superficial velocity (Ug = 5.25 ± 1e-4 mm/s) due to bubble dissolution, whereas N2-water bubbly flow at Ug = 8.67 ± 0.035 mm/s shows unimodal distribution. At high gas superficial velocities (Ug> 20.91 ± 0.075 mm/s for N2 and Ug> 15.75 ± 0.05 mm/s for CO2), bubbly flows exhibit unimodal distribution of velocity fluctuations. The bimodal distribution is attributed to bubble coalescence and breakup. Experimental findings also suggest that recirculation zones near the BCR walls primarily contain small flow structures with the highest energy density and rapid structural decay. In contrast, larger flow structures are found in the center of the BCR, exhibiting slower decay. Detailed insights into CO2 bubble dissolution could enhance BCR design, thereby improving the efficiency of relevant industrial applications.
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