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Fig. 7 Evaluation of successive reaction kinetic model of Chou et al. (1989) based on dolomite dissolution near equilibrium. Rate of change in alkalinity in dolomite-seeded Ca–Mg–HCO3–CO3 solutions, pIAPdolomite ranging from 17.0 to 19.0, plotted against (H+)2/(Ca2+)(HCO-3)





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The SCI Journals Agronomy Journal Crop Science
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