Fractal radar scattering from soil.
A general technique is developed to retrieve the fractal dimension of self-similar soils through microwave (radar) scattering. The technique is based on a mathematical model relating the fractal dimensions of the georadargram to that of the scattering structure. Clear and different fractal signatures have been observed over four geosystems (soils and sediments) compared in this work.
Oleschko
Klaudia
K
Instituto de Geologia, Universidad Nacional Autónoma de México (UNAM), Ciudad Universitaria, Apartado Postal 70-296, CP 04510, Coyoacan, Distrito Federal, Mexico. olechko@servidor.unam.mx
Korvin
Gabor
G
Figueroa
Benjamin
B
Vuelvas
Marco Antonio
MA
Balankin
Alexander S
AS
Flores
Lourdes
L
Carreón
Dora
D