2002
DOI: 10.1023/a:1013322103518
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Cited by 26 publications
(1 citation statement)
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“…These methods differ in the assumptions about the form of relationships between primary and ancillary variables, and how the secondary information is used to estimate the primary variable at unsampled locations (Goovaerts 1997;McBratney et al 2003). Several ancillary variables are available at the field scale, for example digitized soil surveys, digital elevation models (DEM) and derived terrain indices, remotely sensed images of soil surface reflectance, apparent electrical conductivity (EC a ) and measurements of soil properties obtained with on-the-go sensors (Adamchuk et al 2004;Bishop and McBratney 2002;Hengl et al 2004;McBratney et al 2003). One of the most valuable sources of secondary information could be remote sensing because of the strong association between reflectances and SOC, and the low cost and real-time availability of imagery.…”
Section: Geostatistical Techniquesmentioning
confidence: 99%
“…These methods differ in the assumptions about the form of relationships between primary and ancillary variables, and how the secondary information is used to estimate the primary variable at unsampled locations (Goovaerts 1997;McBratney et al 2003). Several ancillary variables are available at the field scale, for example digitized soil surveys, digital elevation models (DEM) and derived terrain indices, remotely sensed images of soil surface reflectance, apparent electrical conductivity (EC a ) and measurements of soil properties obtained with on-the-go sensors (Adamchuk et al 2004;Bishop and McBratney 2002;Hengl et al 2004;McBratney et al 2003). One of the most valuable sources of secondary information could be remote sensing because of the strong association between reflectances and SOC, and the low cost and real-time availability of imagery.…”
Section: Geostatistical Techniquesmentioning
confidence: 99%