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Volume 36, Issue 5 p. 1495-1502
Surface Water Quality

Variable Rainfall Intensity and Tillage Effects on Runoff, Sediment, and Carbon Losses from a Loamy Sand under Simulated Rainfall

C.C. Truman

Corresponding Author

C.C. Truman

USDA-ARS, Southeast Watershed Research Lab., Tifton, GA, 31793

Corresponding author ([email protected]).Search for more papers by this author
T.C. Strickland

T.C. Strickland

USDA-ARS, Southeast Watershed Research Lab., Tifton, GA, 31793

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T.L. Potter

T.L. Potter

USDA-ARS, Southeast Watershed Research Lab., Tifton, GA, 31793

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D.H. Franklin

D.H. Franklin

USDA-ARS, J. Phil Campbell Sr., Natural Resource Conservation Center, Watkinsville, GA, 30677

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D.D. Bosch

D.D. Bosch

USDA-ARS, Southeast Watershed Research Lab., Tifton, GA, 31793

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C.W. Bednarz

C.W. Bednarz

Univ. of Georgia, Coastal Plain Experiment Station, Tifton, GA, 31793

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First published: 01 September 2007
Citations: 57

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Abstract

The low-carbon, intensively cropped Coastal Plain soils of Georgia are susceptible to runoff, soil loss, and drought. Reduced tillage systems offer the best management tool for sustained row crop production. Understanding runoff, sediment, and chemical losses from conventional and reduced tillage systems is expected to improve if the effect of a variable rainfall intensity storm was quantified. Our objective was to quantify and compare effects of a constant (Ic) intensity pattern and a more realistic, observed, variable (Iv) rainfall intensity pattern on runoff (R), sediment (E), and carbon losses (C) from a Tifton loamy sand cropped to conventional-till (CT) and strip-till (ST) cotton (Gossypium hirsutum L.). Four treatments were evaluated: CT-Ic, CT-Iv, ST-Ic, and ST-Iv, each replicated three times. Field plots (n = 12), each 2 by 3 m, were established on each treatment. Each 6-m2 field plot received simulated rainfall at a constant (57 mm h−1) or variable rainfall intensity pattern for 70 min (12-run ave. = 1402 mL; CV = 3%). The Iv pattern represented the most frequent occurring intensity pattern for spring storms in the region. Compared with CT, ST decreased R by 2.5-fold, E by 3.5-fold, and C by 7-fold. Maximum runoff values for Iv events were 1.6-fold higher than those for Ic events and occurred 38 min earlier. Values for Etot and Ctot for Iv events were 19–36% and 1.5-fold higher than corresponding values for Ic events. Values for Emax and Cmax for Iv events were 3-fold and 4-fold higher than corresponding values for Ic events. Carbon enrichment ratios (CER) were ≤1.0 for ST plots and ≥1.0 for CT plots (except for first 20 min). Maximum CER for CT-Ic, CT-Iv, ST-Ic, and ST-Iv were 2.0, 2.2, 1.0, and 1.2, respectively. Transport of sediment, carbon, and agrichemicals would be better understood if variable rainfall intensity patterns derived from natural rainfall were used in rainfall simulations to evaluate their fate and transport from CT and ST systems.