  We explore the role of gravitational settling on inertial particle
concentrations in a wall-bounded turbulent flow. While it may be thought that
settling can be ignored when the settling parameter $Sv\equiv v_s/u_\tau$ is
small ($v_s$ - Stokes settling velocity, $u_\tau$ - fluid friction velocity),
we show that even in this regime the settling may make a leading order
contribution to the concentration profiles. This is because the importance of
settling is determined, not by the size of $v_s$ compared with $u_\tau$ or any
other fluid velocity scale, but by the size of $v_s$ relative to the other
mechanisms that control the vertical particle velocity and concentration
profile. We explain this in the context of the particle mean-momentum equation,
and show that in general, there always exists a region in the boundary layer
where settling cannot be neglected, no matter how small $Sv$ is (provided it is
finite). Direct numerical simulations confirm the arguments, and show that the
near-wall concentration is highly dependent on $Sv$ even when $Sv\ll 1$, and
can reduce by an order of magnitude when $Sv$ is increased from $O(10^{-4})$
and $O(10^{-2})$. The results also show that the preferential sampling of
ejection events in the boundary layer by inertial particles when $Sv=0$ is
profoundly altered as $Sv$ is increased, and is replaced by a preferential
sampling of sweep events due to the onset of the preferential sweeping
mechanism.
