Microbially-mediated P fluxes in calcareous soils as a function of water-extractable phosphate
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文摘
Gross organic P mineralization and immobilization were determined in calcareous soils. Microbial 33P uptake was greatest in soils with the lowest available inorganic P. A faster rate of microbial P turnover when available inorganic P is low is indicated. Microbial processes make a significant contribution to P cycling in forage field soils.

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