2002
DOI: 10.2136/sssaj2002.0640
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Mid-Infrared and Near-Infrared Diffuse Reflectance Spectroscopy for Soil Carbon Measurement

Abstract: Diffuse reflectance spectroscopy offers a nondestructive means for measurement of C in soils based on the The ability to inventory soil C on landscapes is limited by the reflectance spectra of illuminated soil. Both the NIR ability to rapidly measure soil C. Diffuse reflectance spectroscopic (400-2500 nm) and MIR (2500-25 000 nm) region have analysis in the near-infrared (NIR, 400-2500 nm) and mid-infrared been investigated for utility in quantifying soil C (Dalal (MIR, 2500-25 000 nm) regions provides means f… Show more

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Cited by 205 publications
(218 citation statements)
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“…The region of most interest for chemical analysis is the mid-infrared region (also called intermediate infrared) with the wavenumber range of 4000 to 400 cm -1 ; however recently there raising interest in near-infrared (14290-4000 cm -1 ) and far-infrared (400-100 cm -1 ) was seen [7][8][9]. The entire spectrum of electromagnetic radiation is divided into several bands and the boundaries between them are designated by limits of corresponding experimental methods of producing and detecting radiation.…”
Section: Infrared Spectroscopymentioning
confidence: 99%
“…The region of most interest for chemical analysis is the mid-infrared region (also called intermediate infrared) with the wavenumber range of 4000 to 400 cm -1 ; however recently there raising interest in near-infrared (14290-4000 cm -1 ) and far-infrared (400-100 cm -1 ) was seen [7][8][9]. The entire spectrum of electromagnetic radiation is divided into several bands and the boundaries between them are designated by limits of corresponding experimental methods of producing and detecting radiation.…”
Section: Infrared Spectroscopymentioning
confidence: 99%
“…Hence, the interest of pursuing research in spectroscopy was to implement more accurate and reproducible model estimation of soil properties. For the exploration of these spectral data, pre-processing functions were carried out to determine the most relevant spectral wavelengths for estimating soil properties [18]. The applications of statistical model associated with other processing functions have given good results in the analysis of soil properties through spectroscopy [2] [5].…”
Section: Introductionmentioning
confidence: 99%
“…[7][8][9][10][11] Among these studies, special attention has been given to those employing mid-infrared (DRIFTS) [12][13][14] and near-infrared (NIRRS) reflectance. [15][16] This is a non-invasive method of analysis that allows for the quantification of the main components in the mix of generated products in one measurement, with a high degree of reliability.…”
Section: Introductionmentioning
confidence: 99%