Abstract

Ultra-fast Magnetic Resonance Imaging (MRI) is used to image liquid distribution during air–water, co-current downflow through a fixed bed of cylindrical porous pellets of length and diameter 3 mm, packed within a 43 mm internal diameter column in both the trickle- and pulsing-flow regimes. Two different data acquisition times are used, 20 ms and 6.4 s, giving two-dimensional images of in-plane spatial resolution 1.4 mm × 2.8 mm and 351 μ m × 351 μ m , respectively. Superficial gas velocities in the range 27 – 275 mm s - 1 ( 0.033 – 0.338 kg m - 2 s - 1 ) and superficial liquid velocities in the range 0.4 – 13.3 mm s - 1 ( 0.4 – 13.3 kg m - 2 s - 1 ) were used. This work reports images of local pulsing events within the bed occurring during the trickle-to-pulse flow transition. The evolution of the local instabilities is studied as a function of increasing and decreasing liquid velocity, at constant gas velocity. Temporal fluctuations in local liquid holdup were seen even in the trickle flow regime; these fluctuations had much shorter time periods than the pore-scale liquid pulses, and are perhaps associated with fluctuations in local surface wetting of the packing elements. A preliminary assessment of the effect of periodic operation on liquid distribution within the bed is also reported.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.