Use of Acoustic Backscatter to characterize the roughness of porous soil surfaces outdoors.


Michael L. Oelze, Ph.D.

Department of Physics and Astronomy

National Center for Physical Acoustics

University of Mississippi

Oxford, MS

Friday May 19, 2000

11 am

4269 Beckman Institute

Work has been done to determine acoustically the pore properties of soils, such as porosity, permeability and tortuosity. Early methods used probe microphones to determine the soil pore characteristics by looking at the attenuation and phase change of sound propagating through the soil pores. The attenuation and phase change of the sound were then related to a surface impedance that incorporated the soil pore properties. Seeking noninvasive means of finding these properties, forward scattering or acoustic level difference experiments were performed. It was observed that sound propagated over porous surfaces is reduced by the surface impedance and by the surface roughness. Theories have been developed to take into account the reduction in acoustic signal due to the finite surface impedance. Difficulties have arisen in separating the signal loss due to impedance and the signal loss from roughness scattering in the forward direction. Acoustic backscatter has been used to study the roughness statistics of soil surfaces in an effort to determine the effects of roughness apart from the surface impedance effects. The effects of the pore properties on acoustic backscatter are examined theoretically. After accounting for the effects of the pore properties, roughness statistics obtained via acoustic backscatter are then compared with alternate non-acoustic methods for examining surface roughness.