The primary objectives of this study were to determine (1) the exchange characteristics of various soil amendments using a range of salt solutions, (2) the effect of selected soil amendments on heavy metal (Cu2+, Pb2+, and Zn2+) availability, and (3) the effect of selected soil amendments on NH4 + and P availability. The CEC of zeolite and red mud obtained using solutions of 0.1 M BaCl2 and 0.1 M BaCl2/NH4Cl were significantly lower than values obtained using 1 M KCl and 1 M NH4Cl. The higher CEC obtained with monovalent cations indicated that larger divalent cations could not enter the mineralogical framework of zeolite and red mud, and, consequently, a number of exchange sites were only accessible to the smaller monovalent cations. These findings suggest that 1 M KCl and 1 M NH4NO3 should be used as the extracting solutions to obtain the best estimation of CEC and ECEC of red mud and zeolite. The ability of red mud, zeolite, and calcium phosphate (Ca-P), mixed at rates of 0%, 5%, 10%, and 20% (w/w), to sorb Cu2+, Pb2+, and Zn2+ generally followed the order: red mud>zeolite>>Ca-P, while the affinity sequence for these metals followed the order: Pb2+≥Cu2+>>Zn2+. The higher affinity of the sand/amendment mixtures for Pb2+ and Cu2+ relative to Zn2+ was attributed to metal hydrolysis and subsequent specific adsorption as Pb(OH)+ and Cu(OH)+. Zinc was considered to have been primarily sorbed as the divalent cation species. Rates of 5% (w/w) adequately reduced the availability of heavy metals to concentrations below environmental guidelines based on the Toxicity Characteristic Leaching Procedure. Red mud and zeolite added at a rate of 10% (w/w) to the A and B horizon of a sandy soil significantly increased their ability to remove NH4 + from solution, but had negligible effect on P sorption compared with unamended soils. Increased NH4 + removal was attributed to the associated increase in CEC and the greater selectivity of the exchange sites for this cation relative to resident exchangeable Ca2+ and Na+. The absence of P sorption by these two amendments was attributed to the high pH and predominantly negative surface charge of the red mud and the lack of sorption sites in zeolite. Gypsum, on the other hand, tended to depress NH4 + retention but markedly increased P sorption. The depressive effect on NH4 + was due to increased competition between NH4 + and Ca2 + for a limited number of exchange sites, while formation of calcium phosphates of low solubility was the possible mechanism for increased P sorption.