Effects of the transition zone above a water table on the reflection of GPR waves

被引:41
作者
Bano, Maksim [1 ]
机构
[1] Univ Strasbourg, EOST, UMR 7516, Lab Proche Surface, F-67084 Strasbourg, France
关键词
D O I
10.1029/2006GL026158
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We simulate two levels of water table ( at 72 and 48 cm depth) by injecting water in a sand box that also contains several buried objects. GPR profiles acquired with a 1200 MHz antenna at the top of the sand box do not show any clear reflections from the water table. This is because of the existence of a 'transition zone' in which the velocity is a continuously decreasing function of depth. The reflection coefficient in this case decreases with increasing frequency and even vanishes for a cut-off frequency f(0) which itself increases with decreasing transition zone thickness. By modeling in the frequency domain, we explain the absence of the high-frequency GPR reflections from the top of the saturated zone. When the wavelength is small ( high frequency) compared to the thickness of the transition layer, the reflection coefficient is negligible and hence no reflections from the water table will be observed.
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页数:5
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