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    Primary and secondary origin of "non-extractable" soil inorganic phosphorus

    Syers, J. K.; Williams, J. D. H.; Tyner, E. H.; Walker, T. W.
    Abstract
    "Nonextractable" soil inorganic phosphorus can have both a primary and a secondary origin. Apatite included within other minerals and phosphorus distributed throughout mineral lattices constitute the primary sources. "Nonextractable" secondary phosphorus accumulates during soil development and is associated with hydrated sesquioxides.
    Keywords
    phosphorus; soil chemistry; apatite inclusions; lattice phosphorus; hydrated sesquioxides
    Date
    1969-07
    Type
    Journal Article
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    • Department of Soil and Physical Sciences [416]
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    Copyright © 1969 Soil Science Society of America
    Citation
    Syers, J. K., Williams, J. D. H., Tyner, E. H., & Walker, T. W. (1969). Primary and secondary origin of "non-extractable" soil inorganic phosphorus. Soil Science Society of America Proceedings, 33(4), 635-637.
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