Publication date: 1 May 2016
Source:Geoderma, Volume 269
Author(s): Oriol Ramírez-Guinart, Miquel Vidal, Anna Rigol
Americium (Am) solid–liquid distribution coefficients (Kd ) and desorption percentages were quantified in 20 soils with contrasting edaphic properties by means of batch tests aimed at elucidating the mechanisms and soil properties governing Am sorption. The Kd (Am) values ranged from 103 to 105 d (Am) prediction models. Univariate Linear Regressions (ULR) and Multiple Linear Regressions (MLR) based on the use of original soil variables and a Principal Component Analysis (PCA) and Partial Least Squares Regression (PLS) based on latent variables revealed that Am sorption was controlled by organic matter, pH, the carbonate and amorphous iron content and the soil specific surface area. The MLR and PLS models explained up to 73% and 70% of the Kd (Am) variability, respectively; thus, they can be used to estimate Kd (Am) values directly from soil properties.
Source:Geoderma, Volume 269
Author(s): Oriol Ramírez-Guinart, Miquel Vidal, Anna Rigol
