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Discriminating Crop Residues from Soil by Shortwave Infrared Reflectance

Craig S.T. Daughtry

USDA-ARS, Remote Sensing and Modeling Lab., Bldg 007, Room 116, 10300 Baltimore Ave., Beltsville, MD 20705-2350



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Fig. 1 Reflectance spectra of corn, soybean, and wheat residues at a range of relative water contents (RWC) from oven dry to water saturated

 


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Fig. 2 Reflectance spectra of five soils at a range of relative water contents (RWC) from oven dry to water saturated

 


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Fig. 3 Reflectance of Othello soil and corn residues in selected wavelength bands as a function of the relative water content (RWC). TM3 = 630 to 690 nm; TM4 = 760 to 900 nm; TM5 = 1550 to 1750 nm; and TM7 = 2080 to 2350 nm

 


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Fig. 4 Reflectance of crop residues and soils in a visible (TM3, 630–690 nm) and near-infrared (TM4, 760–900 nm) band. The regression line was developed using all of the soil samples. RMSE is the root mean square error

 


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Fig. 5 Reflectance of crop residues and soils in two shortwave infrared bands (TM5, 1550–1750 nm; TM7, 2080–2350 nm). The regression line was developed using all of the soil samples. RMSE is the root mean square error

 


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Fig. 6 Cellulose absorption index (CAI) of crop residues and soils plotted as function of the relative water content (RWC). The dashed line is at . All soils are located below the line, and all crop residues are located above the line

 


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Fig. 7 Reflectance of corn, soybean, and wheat crop residues at 2019 nm plotted as function of the relative water content (RWC). RMSE is the root mean square error

 


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Fig. 8 Expected changes in the cellulose absorption index (CAI) for mixed scenes of crop residue and soil as a function of the relative water content (RWC). The fraction of residue cover ranged from 0 (100% Othello soil) to 1.0 (100% corn residue). Arrows indicate the

 





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The Plant Genome
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