Citation Information

  • Title : Soil profile sulfate in irrigated southern high plains cotton fields and Ogallala groundwater.
  • Source : Journal of Soil and Water Conservation
  • Publisher : Soil and Water Conservation Society
  • Volume : 66
  • Issue : 5
  • Pages : 287-294
  • Year : 2011
  • DOI : 10.2489/jswc.66.
  • ISBN : 10.2489/jswc.66.5.287
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Schubert, A. M.
    • Hudnall, W. H.
    • Booker, J. D.
    • Bronson, K. F.
    • Malapati, A.
  • Climates: Steppe (BSh, BSk).
  • Cropping Systems: Cotton. Irrigated cropping systems.
  • Countries: USA.

Summary

Sulfate (SO 4) is one of the most important anions in soils and groundwater in semiarid regions, including west Texas. Crops' sulfur (S) requirement is about 10% to 20% of the nitrogen requirements. However, there is far less information on soil test SO 4-S (S in the SO 4 form [sulfate-S]) for the western United States, compared to the humid eastern United States. The deposition of S from the atmosphere has declined nationwide, as coal-fired power plants have been scrubbing their emissions of S. This, combined with greater cotton yields and the lack of S fertilization on the Texas Southern High Plains (SHP) point to the need for a soil profile SO 4-S assessment. The first objective of this study was to assess residual soil profile SO 4-S content in irrigated cotton ( Gossypium hirsutum) fields across a range of soil types and counties of the Texas SHP. The second objective was to compile regional SO 4-S concentration data from the Texas Water Development Board irrigation well water quality database and analyze Ogallala groundwater SO 4-S levels by county, soil map unit, and well depth. Soil profile (0 to 0.9 m [0 to 36 in]) SO 4-S content ranged from 120 to 475 kg ha -1 (107 to 424 lb ac -1) among seven center-pivot fields sampled. About half of this S was in the 0.6 to 0.9 m (24 to 36 in) soil layer, which typically was sandy clay loam or clay loam in texture. Well water SO 4-S concentration ranged from 9 to 220 mg L -1 (ppm) in clayey soils with deep groundwater to sandy soils with shallow groundwater, respectively. Groundwater SO 4-S concentration was greater than the USEPA drinking water standard of 83 mg L -1 in 32% of the wells, especially in the southeastern corner of the study area. There was no consistent relationship between soil map unit and SO 4-S content in the soil profile (0 to 0.9 m). A significant negative relationship between well depth and well water SO 4-S concentration was observed in all the eleven-county study area of the SHP of West Texas. In conclusion, soil profile SO 4 content to 0.9 m is high in SHP irrigated cotton fields and in most cases should be adequate for crop S nutritional requirements.

Full Text Link