“…Typically soil reflectance decreases with increasing SOC in the wavelength range 0.4-2.5 μm (Baumgardner et al, 1985) and different modelling techniques are used to predict SOC from continuous reflectance spectra or derivatives Banin, 1994, 1995;Reeves et al, 2002;Udelhoven et al, 2003;van Waes et al, 2005;Brown et al, 2006;Viscarra Rossel et al, 2006). The transfer of prediction models to airborne or satellite remote sensing data has only rarely been conducted (Hill and Schütt, 2000;Gomez et al, 2008;Jarmer et al, 2010), although the approach has promise to obtain area-wide estimates of SOC distribution and support regional carbon inventories.…”