“…Exactly for these reasons, TFs of 137 Cs relate only poorly to single soil properties such as percent clay, pH, or organic matter. For example, increased percent clay in soil does not have a clear effect on 137 Cs uptake in crops (Smolders et al 1997; Keum et al 2007), because it increases the 137 Cs binding potential, but conversely, it also increases K retention which stimulates 137 Cs uptake by roots. The TFs of 137 Cs can, however, be modeled from 3 input parameters: percent clay, the exchangeable K in soil, and the time after contamination (Absalom et al 1999).…”