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ABSTRACT
Zinc and copper systems were titrated with NaOH in the presence of varying amounts of KH2PO4. The data indicated zinc formed the orthophosphate, Zn3(PO4)2 · 4H2O while copper precipitated as the basic phosphate, Cu5(H2PO4)2(OH)8. The pKsp calculated from the dissociation of these phosphates at their respective isoelectric pH values were 47.9 and 92.5 for zinc and copper phosphate, respectively. Basic copper phosphate was less soluble than zinc orthophosphate at all pH levels studied.
1 Contribution from the Department of Soils and Plant Nutrition, University of California, Davis.
2 Assistant Soil Chemist and Principal Laboratory Technician, respectively.
Received for publication April 23, 1961. Accepted for publication July 7, 1961.
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