Comparison of GPR and unilateral NMR for water content measurements in a laboratory scale experiment

被引:13
作者
Ferrara, C. [1 ]
Di Tullio, V. [2 ,3 ]
Barone, P. M. [1 ]
Mattei, E. [1 ]
Lauro, S. E. [1 ]
Proietti, N. [2 ]
Capitani, D. [2 ]
Pettinelli, E. [1 ]
机构
[1] Univ Roma Tre, Dept Phys E Amaldi, I-00146 Rome, Italy
[2] CNR, Inst Chem Methodol, Res Area Rome, Magnet Resonance Lab Annalaura Segre, I-00015 Rome, Italy
[3] Univ Roma La Sapienza, Dept Earth Sci, I-00185 Rome, Italy
关键词
NUCLEAR-MAGNETIC-RESONANCE; GROUND-PENETRATING RADAR; PERMITTIVITY; BUILDINGS; MOUSE; WAVE;
D O I
10.3997/1873-0604.2012051
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Several factors affect antenna-soil coupling in a Ground Penetrating Radar (GPR) survey, like surface roughness, lithology, lateral heterogeneities, vegetation, antenna height from the surface and water content. Among them, Ethology and water content have a direct effect on the bulk electromagnetic properties of the material under investigation. It has been recently pointed out that the wavelet of the early-time portion of a radar signal is correlated to the shallow subsurface dielectric properties of a material. This result indicates that some information on such properties can be directly extracted from the analysis of GPR early-time traces. In the present paper, we use the early-time GPR signal, in terms of average envelope amplitude computed on the first half-cycle, to map the near-surface (few centimetres) lateral distribution of dielectric parameters, induced by changing the shallow water content on a concrete slab. This controlled experiment was specifically designed to study the effect of water content variations on antenna-material coupling, minimizing the influence of both surface roughness and heterogeneity. The quantitative control of the water in the shallow portion of the slab is performed by using a portable unilateral Nuclear Magnetic Resonance (NMR) sensor, which is able to determine the water content in the material on the basis of the measured proton density. The results show a matching pattern of the physical parameters measured with the two different techniques and a very high degree of linear correlation (r = 0.97) between the radar early-time signal average amplitude and the intensity of the NMR signal, which is proportional to the proton density, i.e., to the water content. This experiment suggests that the early-time approach could be used as a fast and high- spatial resolution tool for qualitatively mapping water content lateral variations in a porous material at shallow depth, using a ground-coupled single-offset antenna configuration and that a quantitative evaluation of the moisture content would require a calibration procedure.
引用
收藏
页码:143 / 153
页数:11
相关论文
共 50 条
[1]  
Annan A.P, 2003, VADOSE ZONE J, V2
[2]  
Annan A.P., 2005, HYDROGEOPHYSICS
[3]  
Annan A.P., 1996, Journal of Environmental Engineering Geophysics, P125, DOI [10.4133/jeeg1.b.125, DOI 10.4133/JEEG1.B.125]
[4]  
[Anonymous], 1999, THESIS TU MUNCHEN MU
[5]  
[Anonymous], 1997, INTRO APPL ENV GEOPH
[6]  
[Anonymous], 1997, CRC Handbook of Chemistry and Physics, V78th, P6
[7]  
[Anonymous], 2001, SEISMIC DATA ANAL, DOI DOI 10.1190/1.9781560801580
[8]  
[Anonymous], THESIS LUDWIG MAXIMI
[9]  
[Anonymous], 1971, Pulse and Fourier Transform NMR: Introduction to Theory and Methods
[10]   Nuclear magnetic resonance in inhomogeneous magnetic fields [J].
Balibanu, F ;
Hailu, K ;
Eymael, R ;
Demco, DE ;
Blümich, B .
JOURNAL OF MAGNETIC RESONANCE, 2000, 145 (02) :246-258