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Laboratory investigation of aluminum solubility and solid-phase properties following alum treatment of lake waters

Water samples from two southern California lakes adversely affected by internal nutrient loading were treated with a 20 mg/L dose of Al 3+ in laboratory studies to examine Al solubility and solid-phase speciation over time. Alum [Al 2(SO 4) 3·18 H 2O] applications to water samples from Big Bear Lake...

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Bibliographic Details
Published in:Water research (Oxford) 2005-10, Vol.39 (16), p.3918-3928
Main Authors: Berkowitz, Jacob, Anderson, Michael A., Graham, Robert C.
Format: Article
Language:English
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Summary:Water samples from two southern California lakes adversely affected by internal nutrient loading were treated with a 20 mg/L dose of Al 3+ in laboratory studies to examine Al solubility and solid-phase speciation over time. Alum [Al 2(SO 4) 3·18 H 2O] applications to water samples from Big Bear Lake and Lake Elsinore resulted in a rapid initial decrease in pH and alkalinity followed by a gradual recovery in pH over several weeks. Dissolved Al concentrations increased following treatment, reaching a maximum of 2.54 mg/L after 17 days in Lake Elsinore water and 0.91 mg/L after 48 days in Big Bear Lake water; concentrations in both waters then decreased to 45% gibbsite. These results were supported by geochemical modeling using Visual MINTEQ, with Al solubility putatively controlled by amorphous Al(OH) 3 shortly after treatment and approaching that of microcrystalline gibbsite after about 150 days. These findings indicate that Al(OH) 3 formed after alum treatment undergoes significant chemical and mineralogical changes that may alter its effectiveness as a reactive barrier to phosphorus release from lake sediments.
ISSN:0043-1354
1879-2448
DOI:10.1016/j.watres.2005.06.025