Diffusion of a synthetic urban landfill leachate through compacted natural illitic clays and the role of reactive accessory minerals (carbonates and gypsum) in the geochemical behavior of major soluble ions are evaluated. The leachate is composed of NH þ 4 and Na + (0.25 M) balanced by Cl À (0.25 M), acetate (0.1 M) and HCO À 3 (0.15 M). The pH is 7.8 and it is typical of the mature stage of organic matter degradation within an urban landfill. Laboratory scale diffusion tests were performed over 4 months (long term experiment, LT) and 2 weeks (short term experiment, ST). The ST experiments were designed to allow the measurement of the Cl À gradient as a diffusion tracer in the compacted clay. In the LT experiments the chemical gradients were already at steady state, but geochemical reactions involving dissolution of gypsum and precipitation of calcite were observed. Evolution of pore-water chemistry, mineralogy, cation exchange properties, and the specific surface of clays were determined. Numerical simulations were carried out using the geochemical code RETRASO. Chloride transport, precipitation of carbonates, pH buffering, and Ca 2+ /NH þ 4 cation exchange reactions took place in the laboratory tests. Apparent Cl À diffusion coefficients were determined by direct modeling of the ST tests and validated with the LT experiments. These coefficients were considered in the simulation of transport coupled with experimentally calculated exchange constants and dissolution/precipitation reactions of gypsum and carbonates. Sulfate reduction coupled with acetate oxidation has been proven to be relevant in the sample with significant concentration of SO 2À 4 (Bailén). This process also includes significant precipitation of carbonates (mainly calcite) and causes a decrease of SO 2À 4 in the porewater.