Citation Information

  • Title : Effect of crop rotations and cultural practices on soil organic matter, microbial biomass and respiration in a thin Black Chernozem
  • Source : Canadian Journal of Soil Science
  • Publisher : Canadian Society of Soil Science/Agricultural Institute of Canada
  • Volume : 71
  • Issue : 3
  • Pages : 363-376
  • Year : 1991
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Lafond, G. P.
    • Zentner, R. P.
    • Biederbeck, V. O.
    • Campbell, C. A.
  • Climates: Continental (D). Warm summer continental/Hemiboreal (Dsb, Dfb, Dwb).
  • Cropping Systems: Continuous cropping. Legumes. Wheat.
  • Countries: Canada.

Summary

The effects of crop rotations and various cultural practices on soil organic matter quantity and quality in a Rego, Black Chernozem with a thin A horizon were determined in a long-term study at Indian Head, Saskatchewan. Variables examined included: fertilization, cropping frequency, green manuring, and inclusion of grass Jegume hay crop in predominantly spring wheat (Triticum aestiyum L.) production systems. Generally, fertilizer increased soil organic C and microbial biomass in continuous wheat cropping but not in fallow-wheat or fallow-wheat-wheat rotations. Soil organic C, C mineralization (respiration) and microbial biomass C and N increased (especially in the 7.5- to l5-cm depth) with increasing frequency of cropping and with the inclusion of legumes as green manure or hay crop in the rotation. The influence of treatments on soil microbial biomass C (BC) was less pronounced than on microbial biomass N. Carbon mineralization was a good index for delineating treatment effects. Analysis of the microbial biomass C/N ratio indicated that the microbial suite may have been modified by the treatments that increased soil organic matter significantly. The treatments had no effect on specific respiratory activity (CO2-C/BC). However, it appeared that the microbial activity, in terms of respiration, was greater for systems with smaller microbial biomass. Changes in amount and quality of the soil organic matter were associated with estimated amount and C and N content of plant residues returned to the soil.

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