Permittivity measurements of multilayered media with monostatic pulse radar

Electromagnetic (EM) inversion is a useful tool for quantitative analysis in short-range applications of pulse radars. To estimate multilayered media properties using monostatic radar, two inverse scattering approaches are discussed: (a) layer-stripping algorithm by exploiting amplitude and time delay of radar echoes after their detection, and (b) EM inverse problem of parameter optimization by minimizing the mean square error between measured and modeled data. Redundancy in the estimation of media properties is given by spatial continuous measurements of the investigated media. This property is exploited in both the approaches investigated. In the layer-stripping approach the medium within each layer is homogeneous and the interfaces are assumed laterally continuous. In the inverse problem permittivity is assumed to be laterally smooth, implicit smoothing being given in the model parameterization. It is implicit in both methods that the inversion accuracy is strictly related to the amplitude stability of the radar and plane wave approximation. Therefore, the system calibration and the compensation of some propagation effects (e.g., near field, losses due to conductivity and to scattering from particles distributed between layers and on interfaces, pulse distortion) become crucial aspects for each specific application.

[1]  B. Ursin,et al.  Comparison of some inverse methods for wave propagation in layered media , 1986, Proceedings of the IEEE.

[2]  Fawwaz T. Ulaby,et al.  Dielectric properties of soils in the 0.3-1.3-GHz range , 1995, IEEE Trans. Geosci. Remote. Sens..

[3]  Shechao Feng,et al.  Geometrical model of conductive and dielectric properties of partially saturated rocks , 1985 .

[4]  P. Beckmann,et al.  The scattering of electromagnetic waves from rough surfaces , 1963 .

[5]  Akira Ishimaru,et al.  Wave propagation and scattering in random media , 1997 .

[6]  David J. Daniels,et al.  Introduction to subsurface radar , 1988 .

[7]  M. A. Karam,et al.  PROPAGATION AND SCATTERING IN MULTI-LAYERED RANDOM MEDIA WITH ROUGH INTERFACES , 1982 .

[8]  Dmitry Shepelsky,et al.  Inverse scattering method in electromagnetic sounding theory , 1994 .

[9]  Umberto Spagnolini,et al.  Multi-layer detection/tracking for monostatic ground penetrating radar , 1996, IGARSS '96. 1996 International Geoscience and Remote Sensing Symposium.

[10]  K R Maser,et al.  MODELING THE ELECTROMAGNETIC PROPERTIES OF CONCRETE , 1993 .

[11]  A. Tarantola Inverse problem theory : methods for data fitting and model parameter estimation , 1987 .

[12]  A. P. Annan,et al.  Ground-penetrating radar for high-resolution mapping of soil and rock stratigraphy , 1989 .

[13]  T. Schmugge,et al.  An Empirical Model for the Complex Dielectric Permittivity of Soils as a Function of Water Content , 1980, IEEE Transactions on Geoscience and Remote Sensing.

[14]  Mati Wax,et al.  The estimate of time delay between two signals with random relative phase shift , 1981, ICASSP.

[15]  S. Coen,et al.  Inverse scattering of a layered and dispersionless dielectric half-space, part I: Reflection data from plane waves at normal incidence , 1981 .