Citation Information

  • Title : Use of gypsum for crop grain production under a subtropical no-till cropping system.
  • Source : Agronomy Journal
  • Publisher : American Society of Agronomy
  • Volume : 103
  • Issue : 6
  • Pages : 1804-1814
  • Year : 2011
  • DOI : 10.2134/agronj20
  • ISBN : 10.2134/agronj2011.0192
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Caires, E. F.
    • Garbuio, F. J.
    • Churka, S.
    • Joris, H. A. W.
  • Climates: Humid subtropical (Cwa, Cfa).
  • Cropping Systems: Maize. No-till cropping systems. Sorghum. Wheat.
  • Countries: Brazil.

Summary

Gypsum has been used in tropical and subtropical agriculture when subsoil acidity is an important yield-limiting factor. However, the conditions that promote increased crop yield as a result of gypsum addition in no-till (NT) systems still remain unclear. A field trial examined the effects of newly and previously surface-applied gypsum in a long-term NT system on the soil chemical properties and nutrition and yield of corn ( Zea mays L.), wheat ( Triticum aestivum L.), and soybean [ Glycine max (L.) Merr.] on a clayey Rhodic Hapludox in Parana State, Brazil. Gypsum was surface-applied at 0 and 6 Mg ha -1 in 2004 on plots that had received gypsum previously at 0, 3, 6, and 9 Mg ha -1 in 1998. Surface-applied gypsum newly and previously improved exchangeable Ca and SO 4-S availability throughout the soil profile, and increased the cumulative grain yield of the crops. Exchangeable K losses through leaching caused by gypsum application were low, and a larger mobility of exchangeable Mg as compared with exchangeable K in soil was found as a result of gypsum addition. An increase in Ca content in the corn, wheat, and soybean leaves, and in S content in the corn and wheat leaves occurred following the gypsum application. The use of gypsum showed economic viability to maximize crop grain production in a long-term NT soil with a sufficient level of exchangeable Ca (?8 mmol c dm -3) and low levels of exchangeable Al (?4 mmol c dm -3) and Al saturation (?15%) in the subsoil layers (20-60 cm).

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