creators_name: Oehl, Fritz creators_name: Oberson, Astrid creators_name: Probst, Mirijam creators_name: Fliessbach, Andreas creators_name: Roth, Hans-Rudolf creators_name: Frossard, Emmanuel type: journalp datestamp: 2004-06-26 lastmod: 2009-08-20 14:23:18 metadata_visibility: show title: Kinetics of microbial phosphorus uptake in cultivated soils ispublished: pub subjects: 4nutrient subjects: 2soilbiol subjects: 1soilqual full_text_status: restricted keywords: Microbial phosphorus uptake, Microbial phosphorus turnover, Organic farming, Conventional farming, Isotopic dilution techniques, Bodenfruchtbarkeit abstract: Knowledge about the role of microorganisms in P cycling at conditions of constant soil respiration rates and constant size of microbially bound P is lacking. To study the kinetics of microbial P uptake and cycling under such conditions, soils differing in biological activity were 33PO4 labelled by introducing a carrier-free tracer solution and incubated for 56 days. The 33PO4 incorporation into the fraction of microbial P releasable by chloroform treatment (Pchl) was assessed and the isotopic composition [=specific activity (SA); SA=33PO4/31PO4] of Pchl and soil solution P compared. Soils were taken from a 20-year-old field experiment including a nonfertilised control (NON), a minerally fertilised conventional (MIN) and two organic farming systems [bioorganic (ORG); bio-dynamic (DYN)]. Tracer P incorporation continuously increased during incubation in DYN, ORG and MIN soils. It decreased in the order DYN> ORG>MIN, with differences in 33PO4 uptake between the farming systems being higher than suggested by the differences in the amount of Pchl. In the P-deficient NON soil, the highest initial incorporation of tracer P was found, but no additional uptake could be detected thereafter. In all soils, the SA of Pchl converged to the SA of the soil solution with increasing time. 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