|
|
 |
|||||||||||||||||
|
|||||||||||||||||
 |
|||||||||||||||||
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
SPECIAL SECTION: HYDROGEOPHYSICS |
a Department of Environmental Sciences and Land Use Planning, Catholic University of Louvain, Croix du Sud 2, Box 2, B-1348 Louvain-la-Neuve, Belgium
b TNO Physics and Electronics Laboratory, P.O. Box 96864, 2509 JG The Hague, The Netherlands
c Microwave Laboratory, Catholic University of Louvain, Place du Levant 3, B-1348 Louvain-la-Neuve, Belgium
d Department of Geotechnology, Delft University of Technology, Mijnbouwstraat 120, 2628 RX Delft, The Netherlands
Correspondence: * Corresponding author (lambot{at}geru.ucl.ac.be)
Received for publication 13 January 2004. We explore the possibility of measuring a continuously variable soil moisture profile by inversion of a ground penetrating radar (GPR) signal. Synthetic experiments were conducted to demonstrate the well-posedness of the inverse problem for the specific case of identifying a soil moisture profile in hydrostatic equilibrium with a water table. In this case, the profile agrees with the water retention curve of the soil. The analysis subsequently extends to an actual case study in controlled outdoor conditions on a large tank filled with sand. Due to the presence of a discontinuity in the actual dielectric profile, inversion of the continuous model (Model 1) led to poor results. Only the surface soil moisture was well estimated. Including the observed discontinuity in the model (Model 2) led to a good estimation of the water content profile. Finally, we observed that the surface water content can be accurately estimated using a simplified three-layer model (Model 3). Generally, the observed confidence intervals on the estimated parameters are large, which denotes a lack of model sensitivity to the soil parameters. We attributed the low sensitivity to the high operating frequency range. Lower frequencies would have been required to obtain more information from the larger depths. Nevertheless, high frequencies allowed for an accurate estimation of the surface soil moisture, which offers particularly promising perspectives in humanitarian demining and agricultural applications.
Abbreviations: CMP, common midpoint • GMCS, global multilevel coordinate search • GPR, ground penetrating radar • NMS, Nelder–Mead simplex • SFCW, stepped frequency continuous wave • TEM, transverse electromagnetic • UWB, ultrawide band • VNA, vector network analyzer
This article has been cited by other articles:
|
|
 |
|
  S. Lambot, E. Slob, J. Rhebergen, O. Lopera, K. Z. Jadoon, and H. Vereecken Remote Estimation of the Hydraulic Properties of a Sand Using Full-Waveform Integrated Hydrogeophysical Inversion of Time-Lapse, Off-Ground GPR Data Vadose Zone J., August 11, 2009; 8(3): 743 - 754. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
F. Soldovieri, G. Prisco, and R. Persico Application of Microwave Tomography in Hydrogeophysics: Some Examples Vadose Zone J., February 25, 2008; 7(1): 160 - 170. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
C. P. Oden, G. R. Olhoeft, D. L. Wright, and M. H. Powers Measuring the Electrical Properties of Soil Using a Calibrated Ground-Coupled GPR System Vadose Zone J., February 25, 2008; 7(1): 171 - 183. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
A. Saintenoy, S. Schneider, and P. Tucholka Evaluating Ground Penetrating Radar Use for Water Infiltration Monitoring Vadose Zone J., February 25, 2008; 7(1): 208 - 214. [Abstract] [Full Text] [PDF]
|
|
|
|
|
|
H. Vereecken, S. Hubbard, A. Binley, and T. Ferre Hydrogeophysics: An Introduction from the Guest Editors Vadose Zone J., November 1, 2004; 3(4): 1060 - 1062. [Full Text] [PDF]
|
|
| JOURNAL HOME | HELP | CONTACT PUBLISHER | SUBSCRIBE | ARCHIVE | SEARCH | TABLE OF CONTENTS |
