2014
DOI: 10.1016/b978-0-12-420225-2.00004-2
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Major Issues of Diffuse Reflectance NIR Spectroscopy in the Specific Context of Soil Carbon Content Estimation

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Cited by 39 publications
(22 citation statements)
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“…In addition, due to the scattering effect, the useful part of the absorption spectra (related to elemental concentration) is relatively small when compared to the scattering effect (Gobrecht et al, 2014). Multivariate calibration techniques are used to calibrate the spectra to known measured soil properties.…”
Section: Infrared Spectroscopy For Measuring Soil Contaminantsmentioning
confidence: 99%
See 1 more Smart Citation
“…In addition, due to the scattering effect, the useful part of the absorption spectra (related to elemental concentration) is relatively small when compared to the scattering effect (Gobrecht et al, 2014). Multivariate calibration techniques are used to calibrate the spectra to known measured soil properties.…”
Section: Infrared Spectroscopy For Measuring Soil Contaminantsmentioning
confidence: 99%
“…field condition and air dried condition respectively. The spectral influence of soil moisture is then removed from the total spectral space by orthogonal projection (Gobrecht et al, 2014). Minasny et al (2011) demonstrated an improved calibration and validation in soil carbon concentration using EPO-transformed spectra.…”
Section: Taking Ir and Pxrf To The Field And The Role Of Spectral Libmentioning
confidence: 99%
“…Near infrared (NIR) spectroscopy (NIRS, 800–2500 nm, vis‐NIRS, 400–2500 nm) is a promising approach for simultaneous estimations of a large number of physical and chemical soil properties [for reviews see Reeves III (), Bellon‐Maurel and McBratney (), Gobrecht et al (), and Soriano‐Disla et al ()]. In general, vis‐NIR estimations will not accurately reproduce physical and wet‐chemical laboratory analyses (where, depending on the analysis procedure, precision and accuracy may also vary), but accuracies of vis‐NIR estimations may still be sufficient for studies, which require large data sets, such as, e.g ., long‐term monitoring studies or large scale inventories.…”
Section: Introductionmentioning
confidence: 99%
“…Spectroscopy, covering the optical (reflected solar radiation) and thermal infrared (earth tsurface emitted radiation) regions across the 0.4-15 µm spectral range, can be used to determine a wide range of soil properties [1] such as organic carbon (OC) [2], texture [3], cationic exchange capacity (CEC) [4], total phosphorus (P) [5], exchangeable potassium (K) [6], electrical conductivity (EC) [7][8][9], total concentration of potential pollutant metals/metalloids [10] and mineral content [11,12]. Aside from the fundamental interaction of electromagnetic radiation with matter, indirect interaction can be found and provide additional quantitative information of the soil in question [13].…”
Section: Introductionmentioning
confidence: 99%