Acoustic assessment of flow patterns in unsaturated soil

Acoustic wavelengths in soils range from meters to millimeters, depending o n their frequencies. The spatial and temporal scales of pulse transmission through soils are well suited to investigate transient and presumably heter ogeneous water infiltration into and redistribution within soils. Acoustic pulses were transmitted through a column of an undisturbed and par tially water-saturated loess soil with height and diameter of 0.8 and 0.3 m , respectively. The maximum frequency of the arriving pulses was 10 kHz, wh ich corresponds to a wavelength of about 50 mm. Both travel velocities and absorption of the acoustic waves reacted in the expected ways on soil moist ure variations; however, the two temporal reaction patterns differed consid erably. Brutsaert's [J. Geophys. Res. 69 (1964) 243] model was successfully applied to the data. Dye tracers visualized the patterns of water distribu tion. Their scale compares well with theoretical considerations on the flow paths and the results from the acoustic investigations. (C) 2001 Elsevier Science B.V. All rights reserved.