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- W2034275026 endingPage "1894" @default.
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- W2034275026 abstract "Abstract Total organic P, humic and fulvic acid‐P associations and inositol phosphates in nine volcanic soils of southern Chile were determined. The concentration of organic P (Po) ranged from 654 to 1942 ppm accounting for 49% to 64% of total soil P. Phosphorus associated to humic (HA‐P) and fulvic acids (FA‐P) accounted for 51–68% and 32–49% of Po, respectively. Inositol penta‐ and hexaphosphates represented 42% to 67% of Po suggesting that significant amounts are associated with both humic and fulvic acids. Po content was significantly correlated to organic C, total soil P and HA‐P. HA‐P and FA‐P fractions obtained from the most representative soil were examined by dyalisis and gel filtration. While approximately 96% of HA‐P presented a molecular weight higher than 100,000 daltons, 53% of FA‐P had a molecular weight under 12,000 daltons. It is suggested that these more labile organic P forms would be more easily mineralized, thus increasing the available P pool." @default.
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- W2034275026 date "1989-11-01" @default.
- W2034275026 modified "2023-10-16" @default.
- W2034275026 title "Macromolecule‐P associations and inositol phosphates in some chilean volcanic soils of temperate regions" @default.
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- W2034275026 doi "https://doi.org/10.1080/00103628909368190" @default.
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