Abstract
Kinetic studies have been carried out on the dissolution of 10µm beads of silica and of the siliceous tests of two species of diatoms (Thalassiosira fluviatus andSkeletonema costatum) in sea water at 10–50°C and over the pH range 6–9. At all temperatures dissolution of the biogenous silica occurred most rapidly at pH 8 and most slowly at pH 6. First order kinetics were closely followed when the silica was present in a considerable excess over that required for saturation, the rate being proportional to the area of the silica. Apparent deviation from this type of kinetics occurred when there was insufficient silica to bring about saturation. This was undoubtedly due to the progressive decrease in the surface area which takes place as the particle dissolves. Application of the rather simplistic model developed by Kamataniet al. (1980), which makes allowance for this decrease, gave a close correspondence with the data until ∼ 90% of the silica had dissolved.
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Hubbard, L.M.L., Riley, J.P. Kinetic studies of the rate of dissolution of silica and diatom tests in sea water. Journal of the Oceanographical Society of Japan 40, 148–154 (1984). https://doi.org/10.1007/BF02302495
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DOI: https://doi.org/10.1007/BF02302495