Articles | Volume 2, issue 1
Hydrol. Earth Syst. Sci., 2, 41–49, 1998
https://doi.org/10.5194/hess-2-41-1998
Hydrol. Earth Syst. Sci., 2, 41–49, 1998
https://doi.org/10.5194/hess-2-41-1998

  31 Mar 1998

31 Mar 1998

Soil moisture gradients and controls on a southern Appalachian hillslope from drought through recharge

J. A. Yeakley3,1,4, W. T. Swank2, L. W. Swift2, G. M. Hornberger1, and H. H. Shugart1 J. A. Yeakley et al.
  • 1Department of Environmental Sciences, University of Virginia, Charlottesville, Va 22903 USA.
  • 2Coweeta Hydrologic Laboratory, Southern Experiment Station, USDA-Forest Service, Otto, NC 28763 USA.
  • 3Present address: Environmental Sciences and Resources Program, Portland State University, Portland, Or 97207-0751 USA.
  • 4Corresponding author. Tel.:(1).503.7258040; fax:(1).503.7253888; email: yeakley@pdx.edu.

Abstract. Soil moisture gradients along hillslopes in humid watersheds, although indicated by vegetation gradients and by studies using models, have been difficult to confirm empirically. While soil properties and topographic features are the two general physio-graphic factors controlling soil moisture on hillslopes, studies have shown conflicting results regarding which factor is more important. The relative importance of topographic and soil property controls was examined in an upland forested watershed at the Coweeta Hydrologic Laboratory in the southern Appalachian mountains. Soil moisture was measured along a hillslope transect with a mesic-to-xeric forest vegetation gradient over a period spanning precipitation extremes. The hillslope was transect instrumented with a time domain reflectometry (TDR) network at two depths. Soil moisture was measured during a severe autumn drought and subsequent winter precipitation recharge. In the upper soil depth (0-30 cm), moisture gradients persisted throughout the measurement period, and topography exerted dominant control. For the entire root zone (0-90 cm), soil moisture gradients were found only during drought. Control on soil moisture was due to both topography and storage before drought. During and after recharge, variations in soil texture and horizon distribution exerted dominant control on soil moisture content in the root zone (0-90 cm). These results indicate that topographic factors assert more control over hillslope soil moisture during drier periods as drainage progresses, while variations in soil water storage properties are more important during wetter periods. Hillslope soil moisture gradients in southern Appalachian watersheds appear to be restricted to upper soil layers, with deeper hillslope soil moisture gradients occurring only with sufficient drought.

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