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Residual phosphorus solubility for an acid, clayey, forested soil in the presence of oxalate and citrate
A highly weathered, clayey soil was sampled 14 yr after a Pinus radiata stand was broadcast fertilized with 0, 50 and 200 kg P ha −1 as ordinary superphosphate. Incremental loadings of oxalate and citrate anions from 10 to 100 μmol of anion g −1 soil were evaluated for increased soluble, reactive P...
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Published in: | Canadian journal of soil science 1989-02, Vol.69 (1), p.111-117 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that cite this one |
Online Access: | Get full text |
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Summary: | A highly weathered, clayey soil was sampled 14 yr after a Pinus radiata stand was broadcast fertilized with 0, 50 and 200 kg P ha
−1
as ordinary superphosphate. Incremental loadings of oxalate and citrate anions from 10 to 100 μmol of anion g
−1
soil were evaluated for increased soluble, reactive P (SRP) and soluble, nonreactive (SNP) P. Sorption isotherms were compared to evaluate the effect of the previous fertilization on P sorption by the soil material sampled, and also to measure SNP displacement by orthophosphate-P. A portion of the SNP pool was more readily released than SRP and orthophosphate displaced a significant amount of SNP. After 14 yr the effect of fertilization was still obvious in the sampled soil material. Much of the organic anion-soluble P was in the SRP form. Key words: Citrate, organic P, orthophosphate, oxalate, Pinus radiata, residual P |
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ISSN: | 0008-4271 1918-1841 |
DOI: | 10.4141/cjss89-010 |