Diffuse reflectance spectroscopy for the characterization of calcareous glacial till soils from North Central Montana
Diffuse reflective spectroscopy (DRS) is a method of soil carbon (C) quantification. In this study, the Vis-NIR (350-2500 nm) and MIR (2500-25000 nm) regions were evaluated to determine respective predictive accuracies of soil organic and inorganic carbon (SOC and SIC, respectively). The dataset inc...
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| Language: | en |
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2006
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| Online Access: | http://etd.lib.montana.edu/etd/2006/steward/StewardG1206.pdf |