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Dep. Agronomy. Kansas State Univ., Manhattan, KS 66506
*Corresponding author.
ABSTRACT
The chemistry of Mn and P is often complicated by apparent undersaturation with respect to mineral phases. The role of Mn phosphates in controlling the solubility of Mn and PO4 was studied in acid soils which had been fertilized annually for 40 yr with NH4NO3 and superphosphate. Soil pH ranged from 4.1 to 6.8 and available P varied greatly. Fresh, field-moist soil samples were equilibrated with 0.01 M CaCl2 for 25 d and then analyzed for Mn and PO4 activities. A method was developed to measure redox potential reliably with a Pt electrode to allow calculation of Mn3+ activities. In previous studies, activities of PO4 in these soils were less than the solubilities of strengite (FePO4) and variscite (AlPO4), and Mn activities were less than Mn oxide solubilities. The measured activities of Mn3+ and PO3-4 were consistent with the presence of MnPO4·1.5H2O but were undersaturated with respect to Mn(II) phosphates.
Contribution no. 89-391-J from the Kansas Agric. Exp. Stn.
Received for publication April 3, 1989.
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