2018
DOI: 10.1016/j.ejrs.2017.02.001
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Application of near-infrared reflectance for quantitative assessment of soil properties

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Cited by 94 publications
(65 citation statements)
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“…The soil heavy metals with low content are often difficult to directly estimate using soil spectral features. However, soil heavy metals, often absorbed or bounded, are characterized by spectrally active constituents depending on environmental conditions, which make it possible to estimate their contents and derive their spatial distributions using spectral variables from remote sensing data, especially hyperspectral data [49,50]. Previous studies have shown the availability for predicting soil heavy metal content by spectroscopic reflectance [49,50].…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The soil heavy metals with low content are often difficult to directly estimate using soil spectral features. However, soil heavy metals, often absorbed or bounded, are characterized by spectrally active constituents depending on environmental conditions, which make it possible to estimate their contents and derive their spatial distributions using spectral variables from remote sensing data, especially hyperspectral data [49,50]. Previous studies have shown the availability for predicting soil heavy metal content by spectroscopic reflectance [49,50].…”
Section: Discussionmentioning
confidence: 99%
“…However, soil heavy metals, often absorbed or bounded, are characterized by spectrally active constituents depending on environmental conditions, which make it possible to estimate their contents and derive their spatial distributions using spectral variables from remote sensing data, especially hyperspectral data [49,50]. Previous studies have shown the availability for predicting soil heavy metal content by spectroscopic reflectance [49,50]. However, how to select the spectral variables that significantly contribute to the reduction of model fitting errors and increase of estimation accuracy but are not correlated with each other is critically important [15].…”
Section: Discussionmentioning
confidence: 99%
“…This spectrum encodes information able to provide information to derive qualitative and quantitative information of soil properties [17]. VNIR-SWIR spectroscopy is based on characteristic vibrations of chemical bonds in molecules [18]. Particularly, in the visible region (400-700 nm) the electronic transitions generate wide absorption bands related to chromophores that affect soil colour, while in the NIR-SWIR (700-2500 nm) weak overtones and combinations of these vibrations occur due to stretching and bending of the N-H, O-H, and C-H bonds [19,20].…”
Section: Introductionmentioning
confidence: 99%
“…The spectroscopic test provides valuable information on the spectral responses associated with heavy metal contamination, and thus, the test results give a band combination and spectral signatures useful for remote sensing approaches. The visible-near infrared-shortwave infrared (VNIR-SWIR) spectral ranges (350 to 2500 nm) have been used to study the physicochemical properties of mineral objects and the associated environmental changes [12,[16][17][18][19][20][21][22][23][24][25][26][27][28][29].…”
Section: Introductionmentioning
confidence: 99%