JEQ Journal of Natural Resources and Life Sciences Education
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Journal of Environmental Quality 31:204-216 (2002)
© 2002 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America

TECHNICAL REPORT
Landscape and Watershed Processes

The Effects of Throughfall Manipulation on Soil Leaching in a Deciduous Forest

D.W. Johnson*,a, P.J. Hansonb and D.E. Todd, Jr.b

a Environmental and Resource Sciences, Fleischmann Agriculture Bldg/370, Univ. of Nevada, Reno, NV 89557
b Environmental Sciences Division, Oak Ridge National Lab., P.O. Box 2008, Building 1059, Oak Ridge, TN 37831-6422

* Corresponding author (dwj{at}unr.edu)

Received for publication February 19, 2001. The effects of changing precipitation on soil leaching in a deciduous forest were examined by experimentally manipulating throughfall fluxes in the field. In addition to an ambient treatment (AMB), throughfall fluxes were reduced by 33% (DRY treatment) and increased by 33% (WET treatment) using a system of rain gutters and sprinklers on Walker Branch Watershed, Tennessee. Soil leaching was measured with resin lysimeters in the O horizons and with ceramic cup lysimeters in the E (25 cm) and Bt (70 cm) horizons. Large and statistically significant treatment effects on N fluxes were found in the O horizons (lower N fluxes in the DRY and higher N fluxes in the WET treatment). Together with the greater O horizon N content observed in the DRY treatment, this suggested that N was being immobilized at a greater rate in the DRY treatment than in the AMB or WET treatments. No statistically significant treatment effects on soil solution were found in the E horizons with the exception of (Ca2+ + Mg2+) to K+ ratio. Statistically significant treatment effects on electrical conductivity (EC), pH, Ca2+, Mg2+, K+, Na+, SO2-4, and Cl- were found in the Bt horizons due to differences between the DRY and other treatments. Despite this, calculated fluxes of Ca2+, Mg2+, K+, Na+, SO2-4, and Cl- were lowest in the DRY treatment. These results suggest that lower precipitation will cause temporary N immobilization in litter and long-term enrichment in soil base cations whereas increased precipitation will cause long-term depletion of soil base cations.

Abbreviations: AMB, no treatment, ambient throughfall • DO, dry, open (location in the DRY treatment between troughs) • DRY, treatment where throughfall flux was decreased by 33% • DT, dry, treated (location in the DRY treatment under troughs) • EC, electrical conductivity • NuCM, Nutrient Cycling Model • ortho-P, ortho-phosphate • SWF, soil water flux • TDE, Throughfall Displacement Experiment • WET, treatment where throughfall flux was increased by 33% • WO, wet, open (location in the WET treatment removed from drip points) • WT, wet, treated (location in the WET treatment near drip points)




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