Citation Information

  • Title : Soil physical properties in crop rotation systems as affected by liming materials
  • Source : Pesquisa Agropecuária Brasileira
  • Publisher : Embrapa Informação Tecnológica Pesquisa Agropecuária Brasileira
  • Volume : 46
  • Issue : 12
  • Pages : 1690-1698
  • Year : 2011
  • DOI : 10.1590/S0100-20
  • ISBN : 10.1590/S0100-204X2011001200015
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Costa Crusciol, C. A.
    • Calonego, J. C.
    • Amaral Castro, G. S.
  • Climates: Temperate (C). Humid subtropical (Cwa, Cfa).
  • Cropping Systems: No-till cropping systems. Cereal crops. Maize. Crop-pasture rotations. Oats. Soybean.
  • Countries: Brazil.

Summary

The objective of this work was to evaluate the effects of crop rotation systems and liming materials on soil physical properties. The experiment was carried out from October 2006 to July 2008, in Botucatu, SP, Brazil, in a completely randomized block design in a split-plot arrangement with eight replicates. Main plots consisted of four crop rotation systems: soybean/fallow/maize/fallow, soybean/white-oat/maize/bean, soybean/millet/maize/pigeon pea and soybean/signal grass/maize/signal grass. Subplots consisted of the control treatment, without soil correction, and of the application of 3.8 Mg ha(-1) of dolomitic lime (ECC = 90%) or 4.1 Mg ha(-1) of calcium-magnesium silicate (ECC = 80%), on the surface of a clayed Rhodic Ferralsol. Aggregate stability, soil bulk density, total porosity, macro and microporosity, soil penetration resistance and moisture content were evaluated. Superficial application of the lime materials does not reduce soil aggregation and increases macroporosity down to 0.20 m, with calcium-magnesium silicate application, and to 0.10 m, when lime is applied. Soil under fallow in off-season decreases aggregate stability and increases soil penetration resistance in upper layers. The cultivation of Congo signal grass, between summer crops, increases aggregate stability down to 0.10-m depth.

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