The dissolution and precipitation rates of boehmite, AlOOH, at 100.3°C and limited precipitation kinetics of gibbsite, Al(OH)3, at 50.0°C were measured in neutral to basic solutions at 0.1 molal ionic strength (NaCl+NaOH+NaAl(OH)4) near-equilibrium using a pH-jump technique with a hydrogen-electrode concentration cell. This approach allowed relatively rapid reactions to be studied from under- and over-saturation by continuous in situ pH monitoring after addition of basic or acidic titrant, respectively, to a pre-equilibrated, well-stirred suspension of the solid powder. The magnitude of each perturbation was kept small to maintain near-equilibrium conditions. For the case of boehmite, multiple pH-jumps at different starting pHs from over- and under-saturated solutions gave the same observed, first order rate constant consistent with the simple or elementary reaction: Al(OOH)(cr)+H2O(l)+OH-⇄Al(OH)4-.This relaxation technique allowed us to apply a steady-state approximation to the change in aluminum concentration within the overall principle of detailed balancing and gave a resulting mean rate constant, (2.2±0.3)×10−5kgm−2s−1, corresponding to a 1σ uncertainty of 15%, in good agreement with those obtained from the traditional approach of considering the rate of reaction as a function of saturation index. Using the more traditional treatment, all dissolution and precipitation data for boehmite at 100.3°C were found to follow closely the simple rate expression:Rnet,boehmite=10-5.485{mOH-}{1-exp(ΔGr/RT)}, with Rnet in units of molm−2s−1. This is consistent with Transition State Theory for a reversible elementary reaction that is first order in OH− concentration involving a single critical activated complex. The relationship applies over the experimental ΔGr range of 0.4–5.5kJmol−1 for precipitation and −0.1 to −1.9kJmol−1 for dissolution, and the pHm≡−log(mH+) range of 6–9.6. The gibbsite precipitation data at 50°C could also be treated adequately with the same model:Rnet,gibbsite=10-5.86{mOH-}{1-exp(ΔGr/RT)}, over a more limited experimental range of ΔGr (0.7–3.7kJmol−1) and pHm (8.2–9.7).