  The hydrodynamics of bubble columns in the heterogeneous regime is revisited.
Focusing on air-water systems at large aspect ratio, we show from dimensional
analysis that buoyancy equilibrates inertia, and that velocities scale as
$(gD\varepsilon)^{1/2}$, where $D$ is the bubble column diameter, $\varepsilon$
the void fraction and $g$ the gravitational acceleration.
  From new experiments in a $0.4$m diameter column with ${\cal{O}}(10^3)$
particle Reynolds number bubbles and from a detailed analysis of published
data, we confirm the self-organization prevailing in the heterogeneous regime,
and that the liquid flow rate is only set by the column diameter $D$. Besides,
direct liquid and gas velocity measurements demonstrate that the relative
velocity increases above the terminal velocity $U_T$ in the heterogeneous
regime, and that it tends to $\sim 2.4 U_T$ at very large gas superficial
velocities $V_{sg}$. The proposed velocity scaling is shown to hold for liquid
and gas mean velocities and for their standard deviations. Furthermore, it is
found to be valid over a wide range of conditions, corresponding to Froude
numbers $Fr=V_{sg}/(gD)^{1/2}$ from 0.02 to 0.5. Then, the relevance of this
scaling for coalescing media is discussed. Moreover, following the successful
prediction of the void fraction with a Zuber \& Findlay approach at the
beginning of the heterogeneous regime, we show how the void fraction is
correlated with $Fr$. Further investigations are finally suggested to connect
the increase in relative velocity with meso-scale structures known to exist in
the heterogeneous regime.
