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Fig. 1 Solubility of Al relative to gibbsite (Al(OH)3) in fresh, frozen, and dried soils; logAl is log10 activity of dissolved Al3+. Broken lines indicate theoretical equilibrium with respect to crystalline gibbsite
and microcrystalline gibbsite
. Arrows indicate no addition of acid or base. Al solubility increased as a result of drying the soils
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