Uncertainty analysis for pedotransfer functions

By Budiman Minasny, A. B. M. Bratney. 2002

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A new model for the soil‐water retention curve that solves the problem of residual water contents (2004, background): “In most practical applications of Equation (1), however, it is assumed that M¼ 1 N 1, so much so that M is often no longer even mentioned (e.g. Minasny & McBratney, 2002).”
A conditioned Latin hypercube method for sampling in the presence of ancillary information (2006, methodology): “It has been used in soil science and environmental studies for assessing the uncertainty in a prediction model (Minasny and McBratney, 2002), and in geostatistics for simulation of Gaussian random fields (Pebesma and Heuvelink, 1999; Zhang and Pinder, 2004).”