TY - JOUR
T1 - Soil Organic Carbon mapping of partially vegetated agricultural fields with imaging spectroscopy
AU - Bartholomeus, Harm
AU - Kooistra, Lammert
AU - Stevens, Antoine
AU - van Leeuwen, Martin
AU - van Wesemael, Bas
AU - Ben-Dor, Eyal
AU - Tychon, Bernard
N1 - Funding Information:
The authors wish to thank the Belgian Scientific Policy (BELSPO) for the funding of the project (contract number: SR\00\71) and the Vlaamse Instelling voor Technologisch Onderzoek (VITO) for the organization of the flight campaign as well as the geographic and atmospheric correction of the image. We are grateful to M. Bravin, E. Goidts, J. Verrelst and M. Cors for their collaboration during the fieldwork.
PY - 2011/2
Y1 - 2011/2
N2 - Soil Organic Carbon (SOC)isone of the key soil properties, but the large spatial variation makes continuous mapping a complex task. Imaging spectroscopy has proven to be an useful technique for mapping of soil properties, but the applicability decreases rapidly when fields are partially covered with vegetation. In this paper we show that with only a few percent fractional maize cover the accuracy of a Partial Least Square Regression (PLSR) based SOC prediction model drops dramatically. However, this problem can be solved with the use of spectral unmixing techniques. First, the fractional maize cover is determined with linear spectral unmixing, taking the illumination and observation angles into account. In a next step the influence of maize is filtered out from the spectral signal by a new procedure termed Residual Spectral Unmixing (RSU). The residual soil spectra resulting from this procedure are used for mapping of SOC using PLSR, which could be done with accuracies comparable to studies performed on bare soil surfaces (Root Mean Standard Error of Calibration=1.34 g/kg and Root Mean Standard Error of Prediction=1.65 g/kg). With the presented RSU approach it is possible to filter out the influence of maize from the mixed spectra, and the residual soil spectra contain enough information for mapping of the SOC distribution within agricultural fields. This can improve the applicability of airborne imaging spectroscopy for soil studies in temperate climates, since the use of the RSU approach can extend the flight-window which is often constrained by the presence of vegetation.
AB - Soil Organic Carbon (SOC)isone of the key soil properties, but the large spatial variation makes continuous mapping a complex task. Imaging spectroscopy has proven to be an useful technique for mapping of soil properties, but the applicability decreases rapidly when fields are partially covered with vegetation. In this paper we show that with only a few percent fractional maize cover the accuracy of a Partial Least Square Regression (PLSR) based SOC prediction model drops dramatically. However, this problem can be solved with the use of spectral unmixing techniques. First, the fractional maize cover is determined with linear spectral unmixing, taking the illumination and observation angles into account. In a next step the influence of maize is filtered out from the spectral signal by a new procedure termed Residual Spectral Unmixing (RSU). The residual soil spectra resulting from this procedure are used for mapping of SOC using PLSR, which could be done with accuracies comparable to studies performed on bare soil surfaces (Root Mean Standard Error of Calibration=1.34 g/kg and Root Mean Standard Error of Prediction=1.65 g/kg). With the presented RSU approach it is possible to filter out the influence of maize from the mixed spectra, and the residual soil spectra contain enough information for mapping of the SOC distribution within agricultural fields. This can improve the applicability of airborne imaging spectroscopy for soil studies in temperate climates, since the use of the RSU approach can extend the flight-window which is often constrained by the presence of vegetation.
KW - Imaging spectroscopy
KW - Residual spectral unmixing
KW - Soil Organic Carbon
UR - http://www.scopus.com/inward/record.url?scp=79952767694&partnerID=8YFLogxK
U2 - 10.1016/j.jag.2010.06.009
DO - 10.1016/j.jag.2010.06.009
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AN - SCOPUS:79952767694
SN - 1569-8432
VL - 13
SP - 81
EP - 88
JO - International Journal of Applied Earth Observation and Geoinformation
JF - International Journal of Applied Earth Observation and Geoinformation
IS - 1
ER -