The Geochemical Behavior of Aluminum in Acidified Surface Waters
Gibbsite
Solubility equilibrium
DOI:
10.1126/science.232.4746.54
Publication Date:
2006-10-05T20:28:52Z
AUTHORS (2)
ABSTRACT
Speciation calculations for aluminum, in water samples taken from a drainage basin containing acid mine waters, demonstrate distinct transition conservative behavior pH below 4.6 to nonconservative above 4.9. This corresponds the pK first hydrolysis constant of aqueous aluminum ion and appears be consistent phenomenon independent field location, ionic strength, sulfate concentration. Nonconservative is closely correlated with equilibrium solubility microcrystalline gibbsite or amorphous hydroxide.
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