Component additivity (CA) and generalised composite (GC) approaches to deri
ving a suitable surface complexation model for description of U(VI) adsorpt
ion to natural mineral assemblages are pursued in this paper with good succ
ess. A single, ferrihydrite-like component is found to reasonably describe
uranyl uptake to a number of kaolinitic iron-rich natural substrates at pH
> 4 in the CA approach with previously published information on nature of s
urface complexes, acid-base properties of surface sites and electrostatic e
ffects used in the model. The GC approach, in which little pre-knowledge ab
out generic surface sites is assumed, gives even better fits and would appe
ar to be a method of particular strength for application in areas such as p
erformance assessment provided the model is developed in a careful, stepwis
e manner with simplicity and goodness of fit as the major criteria for acce
ptance.