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ABSTRACT
The reaction of variscite with H+ and OH- in water solutions was investigated and the [OH-] exponent in the variscite solubility product expression was found to be dependent upon solution pH, being proportional to [OH-]2 only at pH 4. An increase from 1 to 10 g. of kaolinite to 0.5 g. of variscite in 50-ml. volume increased the aluminum concentration in solution from 2.3 x 10-5 to 4.8 x 10-5 molar and diminished the phosphate concentration in solution from 2.5 x 10-4 to 0.7 x 10-4 molar in accord with solubility product principles.
1 This work was supported in part by the University Research Committee through a grant of funds from the Wisconsin Alumni Research Foundation. Presented before Div. II, Soil Science Society of America, Aug. 17, 1955.
2 Assistant Professor of Soils, State College of Washington, and Professor of Soils, Univ. of Wisconsin, respectively.
Received for publication February 21, 1955.
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