MICROBIAL-GROWTH AND SULFUR IMMOBILIZATION FOLLOWING THE INCORPORATION OF PLANT RESIDUES INTO SOIL

J Wu, A.G. O'Donnell, JK Syers

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    49 Citations (Scopus)

    Abstract

    The interaction between microbial growth and S immobilization was investigated in an arable soil amended with oil-seed rape (young leaves) and barley straw (1% w/w). Initially, the rape decomposed more rapidly (40 vs 10% by day 5) and produced a larger microbial biomass (990 mug C g-1 soil) than the straw (710 mug C g-1 soil). The biomass in both of the amended soils then decreased to amounts 30-50% higher than those in the unamended soil by day 35 and was maintained at these levels throughout the 195 day incubation.Most of the rape-S (>80%) and straw-S (>60%) added to the soil was released as SO42--S or converted to biomass-S in 5 days. By this time, the amount of S assimilated by the biomass in the rape-amended soil was three times that found using straw. Biomass-S in both soils then decreased but remained twice as high in the rape-amended soil over the period of 15 195 days. The biomass in the straw amended soil had a similar C:S (85-120:1) to that of the unamended soil but was narrower (40-50:1) in the rape-amended soil.By day 5, SO4-S in both of the amended soils had increased significantly. The increase in SO42--S in the rape-amended soil was maintained over the 195 day incubation, suggesting that this S was available for plant uptake. However, by day 15, a net immobilization of soil S by the biomass (25% of soil inorganic S) was found using straw. This immobilized S was retained by the biomass throughout the 195 day incubation and was, therefore, unavailable for plant growth. This suggests that the incorporation of plant residues such as straw which contain low amounts of S may decrease the plant availability of soil S.
    Original languageEnglish
    Pages (from-to)1567-1573
    JournalSoil Biology & Biochemistry
    Volume25
    DOIs
    Publication statusPublished - 1993

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