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Mid-Infrared and Near-Infrared Diffuse Reflectance Spectroscopy for Soil Carbon Measurement

G. W. McCarty*,a, J. B. Reeves, IIIa,b, V. B. Reevesa,b, R. F. Follettc and J. M. Kimbled

a Environmental Quality Laboratory, Building 007 Room 201, BARC-West, Beltsville, MD 20705
b FDA, Rockville, MD
c USDA-ARS Fort Collins, CO
d USDA-NRCS Lincoln, NE



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Fig. 1. Geographic location of the 14 sampling sites within the west central United States.

 


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Fig. 2. Comparison of mid-infrared and near-infrared spectra of a highly calcareous soil before and after treatment with acid for removal of carbonates. The carbonate (i.e., CaCO3) spectrum in each spectral region is included for additional comparison.

 


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Fig. 3. Comparison of calibration for near-infrared and mid-infrared spectroscopy based on total and inorganic soil C measured by dry combustion (actual). Partial least squares (PLS) regression analysis for total C used 17 factors for mid-infrared spectroscopy (MIRS) and 16 factors for near- infrared spectroscopy (NIRS), and analysis for inorganic C used 16 factors for MIRS and 19 factors for NIRS. Residual Mean Squared Deviation is represented by RMSD.

 


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Fig. 4. Comparison of calibrations near- and mid-infrared spectroscopy based on organic C in untreated and acidified soils measured by dry combustion (actual). Partial Least Squares (PLS) regression analysis for organic C used 17 factors for mid-infrared spectroscopy (MIRS) and 18 factors for NIRS, and analysis for organic C (acid) used 19 factors for MIRS and 17 factors for NIRS. Residual Mean Squared Deviation is represented by RMSD.

 


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Fig. 5. Residual error distributions for mid-infrared spectroscopy (MIRS) and near-infrared spectroscopy (NIRS) calibrations. Dashed lines indicate two standard deviations (2{sigma}).

 





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