F.T. MacKenzie O.P. Bricker A. Lerman 1975 <p>Dissolution of eight clay minerals, four zeolites, and quartz in seawater has been monitored for 8 1 2 years. For most of the minerals, dissolution can be described as a first-order reaction in which dissolved silica approaches from undersaturation steady concentration values with time. Characteristic reaction rate constants (k₁) are of the order of 10^-7<span>&nbsp;</span>sec^-1. One of the zeolites, clinoptilolite, shows a different dissolution behavior: SiO₂<span>&nbsp;</span>concentration in solution reaches a high value within one year, followed by a decline to a lower value, suggestive of precipitation of another silicate phase (possibly sepiolite). A mathematical solution is given for a kinetic equation combining the parabolic-rate and first-order rate processes. It is shown that in a wide range of silicate dissolution reactions taking place over long periods of time, the presence of the parabolic-rate dissolution processes cannot be detected, thereby making its inclusion in the kinetic equations unnecessary. The experimental rates of dissolution are comparable to the SiO₂^-<span>&nbsp;</span>dissolution rates in oceanic sediments near the sediment/water interface. But deeper in the sediment, the calculated dissolution rates are significantly lower than the near-interface and experimental values. © 1975.</p> application/pdf 10.1016/0012-821X(75)90213-7 en Rates of dissolution of aluminosilicates in seawater article