Moore Stephanie A, Hay Alex E
Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada.
J Acoust Soc Am. 2009 Sep;126(3):1046-56. doi: 10.1121/1.3180696.
Sound scattering by solid particles suspended in a turbulent jet is investigated. Measurements of the scattered amplitude were made in a bistatic geometry at frequencies between 1.5 and 4.0 MHz, and at scattering angles from 95 degrees to 165 degrees relative to the forward direction. Two types of particle were used: nearly spherical lead-glass beads and aspherical natural sand grains. For each particle type, experiments were carried out using approximately 200 and approximately 500 microm median diameter grain sizes, corresponding to 0.7 < or approximately ka < or approximately 4. The sphericity of the sand grains, defined as the ratio of projected perimeter size to projected area size, was 1.08. The lead-glass bead results are consistent with an elastic sphere model. A rigid movable sphere model provides the best fit to the sand data, and the best-fit diameter is within 4% of the equivalent volume size. However, the scattering pattern for sand is systematically smoother than predicted: that is, the undulations in the angular scattering pattern predicted by spherical scatterer theory are present, but muted. This observed departure from spherical scatterer theory is attributed to disruption of the interference among creeping waves by the irregular surfaces of natural sand grains.
