2015
DOI: 10.1016/j.jappgeo.2015.06.006
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Application of the Ground Penetrating Radar ARMA power spectrum estimation method to detect moisture content and compactness values in sandy loam

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Cited by 23 publications
(15 citation statements)
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“…Different media and their physical properties can cause the distribution of frequency-domain signals in energy, amplitude, amplitude envelope, and other information (Zhang, 1999) to achieve the purpose of inversion of media moisture content. Auto regressive and moving average (ARMA) is a frequency-domain spectral analysis method that can extract signal features at low signal-to-noise ratios and has the characteristics of high resolution (Cui et al, 2014).…”
Section: Water Content Inversion Methodsmentioning
confidence: 99%
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“…Different media and their physical properties can cause the distribution of frequency-domain signals in energy, amplitude, amplitude envelope, and other information (Zhang, 1999) to achieve the purpose of inversion of media moisture content. Auto regressive and moving average (ARMA) is a frequency-domain spectral analysis method that can extract signal features at low signal-to-noise ratios and has the characteristics of high resolution (Cui et al, 2014).…”
Section: Water Content Inversion Methodsmentioning
confidence: 99%
“…ARMA spectrum analysis is based on a stationary linear signal process to estimate power spectrum density (Khanshan et al, 2010;Cui et al, 2015). The spectral density is obtained by performing ARMA spectral analysis on the stationary digital radar signal (Li et al, 1997), and then calculated by Cadzow spectral analysis method (Cadzow, 1980), which reduces the estimation of spectral density parameters and uses logarithm to express the spectral density.…”
Section: Water Content Inversion Methodsmentioning
confidence: 99%
“…Some studies focused on the detection of changes in water content in concrete determine also that the center frequency and the bandwidth decreases as water content increases [66,67], even though the main objective was the analysis of the wave amplitude, analyzing in some cases the spectra amplitude attenuation depending on the water content [68]. The analysis of the spectrum behavior combined with backscattering was also applied in the study of shallow geology to detect seasonal subterranean streams, differentiating between active and non-active streams [69] and in the study of compaction and moisture in sandy loam [70]. Further evaluations studied the propagation of GPR signals in unsaturated ground using the Rayleigh dispersion and confirmed that the frequency of the waves changed depending on the moisture content: the maximum amplitude observed moved to lower frequency values as the water content increased [61].…”
Section: The Frequency Spectrummentioning
confidence: 99%
“…Soil is a loose, porous, dielectric material composed of water, air, and soil particles (Schaap, et al, 1997). The compactness and moisture content are important soil parameters that affect the plant growth, water movement, seedling emergence, and root penetration (Cui et al, 2015;Goutal et al, 2013;Ogée and Brunet, 2002). In early days, soil compactness was measured primarily by destructive sampling (Ronai and Shmulevich, 1995); later, instruments based on pressure-based soil cone-index measurement ( ASABE Standards, 2009;Erbach et al, 1991;Pillinger et al, 2018;Perumpral, 1987), microwave reflection measurement (Luo and Perumpral, 1995;Zoughi et al,1994), and volume and porosity measurement were used (Ronai and Shmulevich, 1995).…”
Section: Introductionmentioning
confidence: 99%