A controlled experiment to investigate the correlation between early-time signal attributes of ground-coupled radar and soil dielectric properties

被引:41
作者
Pettinelli, Elena [1 ]
Di Matteo, Andrea [2 ]
Beaubien, Stanley Eugene [3 ]
Mattei, Elisabetta [4 ]
Lauro, Sebastian Emanuel [1 ]
Galli, Alessandro [5 ]
Vannaroni, Giuliano [1 ]
机构
[1] Roma Tre Univ, Dept Math & Phys, I-00146 Rome, Italy
[2] Delft Univ Technol, Dept Geotechnol, NL-2628 Delft, Netherlands
[3] Univ Roma La Sapienza, Dept Earth Sci, I-00185 Rome, Italy
[4] Univ Tuscia, Dept Ind Engn, Largo Univ Snc, I-01100 Viterbo, Italy
[5] Univ Roma La Sapienza, Dept Informat Engn Elect & Telecommun, I-00184 Rome, Italy
关键词
Ground Penetrating Radar; Ground-coupled antennas; Subsoil electromagnetic parameters; Early-time signal attributes; Time Domain Reflectometry; PENETRATING RADAR; WATER-CONTENT; RADIATION-PATTERNS; TRANSIENT FIELDS; DIRECT WAVE; GPR; PERMITTIVITY; ANTENNA; PROPAGATION; EXPLORATION;
D O I
10.1016/j.jappgeo.2013.11.012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Ground-coupled radar has been used in the literature to estimate shallow subsoil permittivity using ground-wave velocity measurements. It has also been shown that the electromagnetic (EM) properties of the soil significantly affect antenna performance, modifying in particular the amplitude, shape, and duration of the 'early-time' Ground Penetrating Radar (GPR) signals. To quantitatively evaluate these effects we built a test site consisting of a 4 x 7 x 1.2 m volume filled primarily with sand; this volume is hydraulically isolated from the surroundings and contains buried pipes in which water can be introduced or removed to control the level of the water table. On a regular grid of 28 points we measured the soil dielectric properties at depth intervals of 0-10 and 0-20 cm using Time Domain Reflectometry (TDR) probes, and collected GPR data using both 250 and 500 MHz bistatic antennas. The measurements were performed with the water table at different depths to systematically change the shallow-soil dielectric properties. Relative permittivity and conductivity values were calculated from the TDR data, and the average envelopes of the first half cycle of the early-time GPR signals were computed. Data analysis shows a high degree of linear correlation (r >= 0.8) between the early-time signal attributes for both antenna frequencies and the EM properties obtained using both TDR probe lengths. The highest correlation (r = 0.9) was found between the 500 MHz data and the permittivity measured along the 0-20 cm depth interval; this relationship is explained in terms of ground wave penetration. The results of our investigation confirm previous field observations and are in full agreement with theoretical predictions and related numerical simulations, highlighting the potential for alternative convenient approaches to predict EM properties of the shallow subsoil. (C) 2013 Elsevier B.V. All rights reserved.
引用
收藏
页码:68 / 76
页数:9
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