  The discharge of spherical grains from a hole in the bottom of a right
circular cylinder is measured with the entire system underwater. We find that
the discharge rate depends on filling height, in contrast to the well-known
case of dry non-cohesive grains. It is further surprising that the rate
increases up to about twenty five percent, as the hopper empties and the
granular pressure head decreases. For deep filling, where the discharge rate is
constant, we measure the behavior as a function of both grain and hole
diameters. The discharge rate scale is set by the product of hole area and the
terminal falling speed of isolated grains. But there is a small-hole cutoff of
about two and half grain diameters, which is larger than the analogous cutoff
in the Beverloo equation for dry grains.
