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ARS Home » Plains Area » Bushland, Texas » Conservation and Production Research Laboratory » Soil and Water Management Research » Research » Publications at this Location » Publication #197132


item Schwartz, Robert
item Baumhardt, Roland - Louis
item Evett, Steven - Steve

Submitted to: Annual Southern Conservation Tillage Conference for Sustainable Agriculture
Publication Type: Abstract Only
Publication Acceptance Date: 5/15/2006
Publication Date: 6/15/2006
Citation: Schwartz, R.C., Baumhardt, R.L., Evett, S.R. 2006. Monitoring tillage effects on soil water dynamics using automated time-domain reflectometry. In: Proceedings of the 28th Annual Southern Conservation Systems Conference, June 26-28, 2006, Amarillo, Texas. p. 284.

Interpretive Summary:

Technical Abstract: Tillage modifies soil physical properties near the surface, which can influence evaporation and how water is redistributed within the profile. The objective of this study was to evaluate the effects of sweep tillage soil water dynamics at a high temporal resolution. Plots were established in a fallow field under stubble-mulch tillage on a Pullman clay loam (Fine, mixed, superactive, thermic Torrertic Paleustolls). Half of the plots were periodically tilled to a depth of .08 m using a sweep plow. The remaining plots were not tilled throughout the duration of the study. Plots were kept weed free and devoid of residue throughout the study period. Soil water contents were monitored at half-hourly intervals using time-domain reflectometry at 0.05, 0.1, 0.15, 0.2, and 0.3 m. During a 123 day period from April to August, tillage decreased net water storage by 10 mm (P < 0.05) at 0 to 0.3 m as compared with no-tillage. Higher water contents at 0.05 and 0.1 m depths under no tillage persisted throughout the summer despite greater rainfall infiltration amounts under sweep tillage (21 mm) and the absence of residues in both treatments. Maximum daily net radiation of the tilled surface after DOY 203 ranged from 4 to 19% greater than that of the no tillage surface and these differences diminished with time after tillage. Increased soil water depletion under tillage was likely due to a change in soil hydraulic properties accompanied by enhanced vapor flow near the surface and greater absorption of radiation by a tilled surface with reduced albedo.