Measurements in two-phase, water–air bubble, grid turbulence have been conducted in a vertical water channel of square cross section. The water flow was directed upwards. A 30 mm mesh grid located at the entrance of the test section generated, in the absence of the dispersed phase, a nearly isotropic turbulent flow field occupying the central part of the channel. Air bubbles were injected in the flow from the grid. Velocity measurements of the liquid phase were obtained using Laser Doppler Velocimetry. The measured flow characteristics included mean velocity and statistical quantities such as turbulence intensity, probability distribution function, skewness and flatness factors, autocorrelation, macroscale and power spectra, for both the longitudinal and transverse velocity components. Local void fraction was measured with an optical probe as well as with hot film anemometry. Bubble velocity and size were estimated with photographic techniques. Presented measurements illustrate the upwards development of void fraction distribution at successive cross sections of the channel. The observed distributions indicate the presence of a mechanism responsible for capturing and redistributing the bubbles. Accordingly, physical mechanisms possibly responsible for the observed phenomenon such as a Segre–Silberberg effect, modified for deformable bubbles in the presence of buoyancy, or the action of large eddies present in the flow are discussed. The velocity field has been obtained on a cross-section at a distance of 30 mesh from the grid at a constant water volumetric flow rate. Based on the obtained experimental results, the influence of the dispersed phase on the initially isotropic turbulence field is identified and the physical processes responsible for the observed changes are discussed. The presence of the second phase appears to introduce inhomogeneities in the void fraction and flow property distributions leading to the emergence of two spatial regions controlled by different physical processes. Also, two distinct regimes in the measured quantities are observed, corresponding to low and high values of gas flow rate ratio. The described changes result in a significant departure from initial isotropy, followed by a tendency towards returning to a state characterised by nearly normal probability distributions and scales close to that of grid turbulence as the gas flow rate increases. Finally, the measured autocorrelation and power spectra offer information regarding the nature of the energy exchanging mechanism occurring between the liquid and dispersed phase.
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