A study was undertaken to quantify the rates of aluminum release in an acid soil (pH 4.40) which was known to produce differential growth responses to Al in Al-resistant and sensitive wheat cultivars which are characterized by differences in root organic acid exudation. Soil columns were leached with artificial soil solutions containing no Al in the presence or absence of citrate for periods of up to 12 days. The Al release rates could be resolved into two dissolution phases: A fast release phase for Al was attributed to the cation exchangeable pool while a second slower phase was attributable to the dissolution of readily weatherable minerals. Citrate increased the dissolution rates two fold in comparison to experiments performed without citrate. It was concluded that for rhizosphere considerations, the total releasable Al pool was finite in size and constituted approximately 2% of the soil's total Al reserves. This pool was not increased markedly in the presence of citrate. It was concluded that citrate not only complexed Al in solution but also complexed Al directly from the mineral phase. From experimental Al release rates, it was deduced that only the soil solution and exchangeable Al pools were responsible for Al rhizotoxicity and that organic acids exuded from the root probably provide an efficient mechanism for excluding Al from the root. Empirical equations were also constructed to describe Al dissolution from the two release pools for use in soil Al flux models.