Small-Scale Seismic Monitoring of Varying Water Levels in Granular Media
Physical properties of soils in the vadose zone, and especially their water content, are characterized by strong spatial and temporal variations mostly driven by weather and anthropogenic activities. To understand this variability and help water resource management, seismic methods have been recently suggested as a complement to electrical and electromagnetic techniques. The simultaneous in situ estimation of pressure (P) and shear (S) wave velocities (VP and VS, respectively) and their ratio (VP/VS) offers novel perspectives for the monitoring of space and time variations of vadose zone mechanical properties. However, the seismic response in partially saturated and unconsolidated soils remains complex and deserves to be studied both theoretically and experimentally. In this study, we tested the sensitivity of seismic measurements (i.e., P-wave travel times and surface-wave phase velocities) to water saturation variations using controlled physical models at the laboratory scale. Ultrasonic techniques were used to reproduce a small-scale seismic acquisition setup at the surface of glass bead layers with varying water levels. Travel times and phase velocity measurements obtained at the dry state were validated with both theoretical models and numerical simulations and serve as reference datasets. The increasing water level clearly affected the recorded wave field in both its phase and amplitude. In these cases, the collected data cannot yet be inverted in the absence of a comprehensive theoretical model for such partially saturated granular media. The differences in travel time and phase velocity observed between the dry and wet models show patterns that interestingly match the observed water level and depth of the capillary fringe, thus offering attractive perspectives for studying soil water content variations.
Copyright © Soil Science Society of America 5585 Guilford Rd., Madison, WI 53711 USA. All rights reserved.
(Sylvain Pasquet1, Ludovic Bodet2, Paolo Bergamo3, Roger Guérin2, Roland Martin4, Régis Mourgues5, and Vincent Tournat6)
- Sorbonne Univ., UPMC Univ Paris 06, CNRS, EPHE, UMR 7619 METIS, 4 place Jussieu, 75005 Paris, France, and now at Wyoming Center for Environmental Hydrology and Geophysics and Dep. of Geology and Geophysics, Univ. of Wyoming, Laramie, WY 85071
- Sorbonne Universités, UPMC Univ Paris 06, CNRS, EPHE, UMR 7619 METIS, 4 place Jussieu, 75005 Paris
- School of Planning Architecture and Civil Engineering, Queen’s Univ. Belfast, Belfast, UK
- CNRS, Univ. Paul Sabatier, Observatoire Midi-Pyrénées, UMR 5563 GET, 31000 Toulouse, France
- LUNAM Univ., Univ. du Maine, UMR 6112 LPG, 72000 Le Mans, France
- LUNAM Univ., CNRS, Univ. du Maine, UMR 6613 LAUM, 72000 Le Mans, France