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dc.contributor.authorFu, Yong, 1948-*
dc.creatorFu, Yong, 1948-en_US
dc.date.accessioned2013-03-28T10:14:59Zen
dc.date.available2013-03-28T10:14:59Zen
dc.date.issued1988en_US
dc.identifier.urihttp://hdl.handle.net/10150/276722en
dc.description.abstractThe data of 14 soils were used to compute the ion activity product (IAP), the ratio of the ion activity product and to the solubility product (Ksp) of the pure minerals (IAP/Ksp) and to estimate the solid activity coefficients (SAC) of the soil components. The value of IAP and SAC of AlPO4 differs from soil to soil and increases with increasing P added to soil in acid soils and for calcium phosphate in basic soils. Magnesium apparently did not cause P adsorption or precipitation in the soils studied. The SAC of aluminum phosphate ranged from 10 to 10000 in acid soils. The mole fraction of the total phosphate in soil seemed to be a more satisfactory basis for calculating the concentration of the solid phase than was measurements of the available phosphate.
dc.language.isoen_USen_US
dc.publisherThe University of Arizona.en_US
dc.rightsCopyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.en_US
dc.subjectSoil absorption and adsorption.en_US
dc.subjectPhosphatic fertilizers.en_US
dc.subjectPhosphates -- Absorption and adsorption.en_US
dc.titleSolid activity coefficients of phosphate adsorbed by soilen_US
dc.typetexten_US
dc.typeThesis-Reproduction (electronic)en_US
dc.identifier.oclc21493224en_US
thesis.degree.grantorUniversity of Arizonaen_US
thesis.degree.levelmastersen_US
dc.identifier.proquest1333593en_US
thesis.degree.disciplineGraduate Collegeen_US
thesis.degree.disciplineSoils and Water Scienceen_US
thesis.degree.nameM.S.en_US
dc.identifier.bibrecord.b17260668en_US
refterms.dateFOA2018-06-15T03:53:21Z
html.description.abstractThe data of 14 soils were used to compute the ion activity product (IAP), the ratio of the ion activity product and to the solubility product (Ksp) of the pure minerals (IAP/Ksp) and to estimate the solid activity coefficients (SAC) of the soil components. The value of IAP and SAC of AlPO4 differs from soil to soil and increases with increasing P added to soil in acid soils and for calcium phosphate in basic soils. Magnesium apparently did not cause P adsorption or precipitation in the soils studied. The SAC of aluminum phosphate ranged from 10 to 10000 in acid soils. The mole fraction of the total phosphate in soil seemed to be a more satisfactory basis for calculating the concentration of the solid phase than was measurements of the available phosphate.


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