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Comparison of GPR and unilateral NMR for water content measurements in a laboratory scale experiment
- Source :
- Near surface geophysics, 11 (2013): 143–153. doi:10.3997/1873-0604.2012051, info:cnr-pdr/source/autori:C.Ferrara, V. Di Tullio, P.M.Barone, E.Mattei, S.E.Lauro, N. Proietti, D.Capitani, E.Pettinelli/titolo:Comparison of GPR and Unilateral NMR For Water Content Measurements in a Laboratory Scale Experiment/doi:10.3997%2F1873-0604.2012051/rivista:Near surface geophysics (Print)/anno:2013/pagina_da:143/pagina_a:153/intervallo_pagine:143–153/volume:11
- Publication Year :
- 2012
- Publisher :
- Wiley, 2012.
-
Abstract
- "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, lithology 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."
- Subjects :
- Mineralogy
Signal
law.invention
Waves and shallow water
Geophysics
Amplitude
law
Ground-penetrating radar
GROUND-PENETRATING RADAR
NUCLEAR-MAGNETIC-RESONANCE
SEISMIC TRACE ANALYSIS
MOUSE
PERMITTIVITY
BUILDINGS
ROME
WAVE
Surface roughness
Geotechnical engineering
Radar
Porosity
Water content
Physics::Atmospheric and Oceanic Physics
Geology
Subjects
Details
- ISSN :
- 18730604 and 15694445
- Volume :
- 11
- Database :
- OpenAIRE
- Journal :
- Near Surface Geophysics
- Accession number :
- edsair.doi.dedup.....10faf0e9b56b4b2739555bd272b2d4ec