2010
DOI: 10.1016/j.geoderma.2009.11.007
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The relationship between diffuse spectral reflectance of the soil and its cation exchange capacity is scale-dependent

Abstract: 1Diffuse reflectance spectroscopy (DRS) is increasingly being used to predict nu-2 merous soil physical, chemical and biochemical properties. However, soil properties and 3 processes vary at different scales and, as a result, relationships between soil properties 4 often depend on scale. In this paper we report on how the relationship between one 5 such property (CEC) and the DRS of the soil depends on spatial scale. We show this 6 by means of a nested analysis of covariance of soils sampled on a balanced nest… Show more

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Cited by 31 publications
(12 citation statements)
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“…Overall, our results indicate that MBL and Cubist outperformed the global PLSR and RF models. In large and complex datasets, the relationship between soil properties and spectra can be highly nonlinear [14,86]. As a result, both MBL and Cubist were able to better predict soil physical and chemical properties.…”
Section: Best Model Performancementioning
confidence: 99%
“…Overall, our results indicate that MBL and Cubist outperformed the global PLSR and RF models. In large and complex datasets, the relationship between soil properties and spectra can be highly nonlinear [14,86]. As a result, both MBL and Cubist were able to better predict soil physical and chemical properties.…”
Section: Best Model Performancementioning
confidence: 99%
“…It is necessary to select characteristic bands that can not only eliminate irrelevant or nonlinear variables and reduce redundancy, but also simplify the model to obtain a model with better prediction ability and that is more robust. As an optimization algorithm, GA has been widely used in the field of spectral analysis (Savvides et al, 2010). In addition, PLSR was selected as the regression model for GA to obtain a more efficient and steadier model.…”
Section: Chemometric Analysesmentioning
confidence: 99%
“…In the last years, several studies have addressed the potential of soil spectroscopy, which typically is used at the laboratory scale, to provide predictors to estimate a large number of soil properties such as clay, sand, and silt contents (Ben‐Dor and Banin, 1995; Brown, 2007; Gomez et al, 2008a; Lagacherie et al, 2008; Janik et al, 2009; Ramirez‐Lopez et al, 2013), organic C content (Nocita et al, 2013; Cambule et al, 2012; Ramirez‐Lopez et al, 2013), soil moisture (Minasny et al, 2008; Rijal et al, 2013; Kodaira and Shibusawa, 2013), CaCO 3 content (Gomez et al, 2008a; Lagacherie et al, 2008), salt content (Wang et al, 2012), pH (Janik et al, 1998; Viscarra Rossel and Behrens, 2010), cation exchange capacity (Janik et al, 2009; Savvides et al, 2010; Kodaira and Shibusawa, 2013), and some macro‐ and micronutrients (Janik et al, 2009; Kodaira and Shibusawa, 2013).…”
mentioning
confidence: 99%