2016
DOI: 10.1007/s12524-016-0587-0
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Visible-Near Infrared Reflectance Spectroscopy for Rapid Characterization of Salt-Affected Soil in the Indo-Gangetic Plains of Haryana, India

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Cited by 31 publications
(17 citation statements)
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“…The three notable absorption peaks were identified at 1417-, 1914-, and 2209-nm bands by reflectance spectra as well as FDT-SG methods along with clay concentrations at 2200-2329 nm (Ben-Dor and Banin 1994;Islam et al 2003). The absorption peaks at 1400 and 1900 nm are related to water (moisture and hydroxyl ions) and clay lattice OH features at 1400 and 2200 nm (Bilgili et al 2010;Srivastava et al 2017). The water absorption peaks were usually enhanced in the FDT with SG smoothing method ( Fig.…”
Section: Spectral Reflectance Characteristics Of Soil and Its Relatiomentioning
confidence: 99%
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“…The three notable absorption peaks were identified at 1417-, 1914-, and 2209-nm bands by reflectance spectra as well as FDT-SG methods along with clay concentrations at 2200-2329 nm (Ben-Dor and Banin 1994;Islam et al 2003). The absorption peaks at 1400 and 1900 nm are related to water (moisture and hydroxyl ions) and clay lattice OH features at 1400 and 2200 nm (Bilgili et al 2010;Srivastava et al 2017). The water absorption peaks were usually enhanced in the FDT with SG smoothing method ( Fig.…”
Section: Spectral Reflectance Characteristics Of Soil and Its Relatiomentioning
confidence: 99%
“…The FDT and SG smoothing was used to process all the spectral data to smooth the spectra and to eliminate the particle size effects and noise produced by illumination variations (Bilgili et al 2010;Tsai and Philpot 1998). It is found to be an optimal spectral pre-treatment in alike studies (Awiti et al 2008;Bilgili et al 2010;Srivastava et al 2017). The SPAs were detected by the first derivative transferred spectra which generally augment the absorption features.…”
Section: Spectral Pre-treatment and Renovationmentioning
confidence: 99%
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