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Determination of Clay and Other Soil Properties by Near Infrared Spectroscopy

L. K. Sørensen* and S. Dalsgaard

Steins Laboratorium, Ladelundvej 85, 6650 Brørup, Denmark



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Fig. 1. Geographic distribution of samples in sample Set 1. The number of samples within each county is shown.

 


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Fig. 2. Clay results obtained by cross validation on sample Set 2. Calibration was performed in the wavelength range 408 to 2492 nm after first derivative treatment of spectra.

 


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Fig. 3. Clay results obtained by cross validation on samples containing <26% clay from sample Sets 1 and 2. Calibration was performed in the wavelength range 408 to 2492 nm after first derivative treatment of spectra.

 


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Fig. 4. Spectral profiles of samples in sample Set 1 after first derivative treatment together with the correlation plot showing the correlation between wavelengths and clay content. The y axis shows the correlation coefficient.

 


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Fig. 5. Results obtained for total C by cross validation on combined sample Sets 1 and 2. Calibration was performed in the wavelength range 408 to 2492 nm after first derivative treatment of spectra.

 


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Fig. 6. Validation results obtained for total C on the independent sample Set 4 using calibration model developed on combined samples Set 1 and 2 (wavelength range 408 to 2492 nm, first derivative treatment of spectra). T-outliers were not removed.

 


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Fig. 7. Silt results obtained by cross validation on sample Set 1. Calibration was performed in the wavelength range 408 to 2492 nm after first derivative treatment of spectra.

 


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Fig. 8. Sand results obtained by cross validation on sample Set 1. Calibration was performed in the wavelength range 408 to 2492 nm after first derivative treatment of spectra.

 





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