SSSAJ Journal of Natural Resources and Life Sciences Education
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Published in Soil Sci Soc Am J 57:1341-1347 (1993)
© 1993 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Erosion Processes on Arid Minespoil Slopes

Roy C. Sidle*, R. W. Brown and B. D. Williams

USDA Forest Service, Intermountain Research Station, 860 North 1200 East, Logan, UT 84321

*Corresponding author.

ABSTRACT

Surface wash and dry ravel erosion rates from minespoil were measured for 4.7 yr after initial reclamation at a site in western Nevada. Average annual total erosion from all 15 plots ranged from 0.48 to 1.10 Mg ha–1. Neither mulching treatment nor slope gradient (3:1 vs. 2:1) significantly affected surface wash from reclaimed minespoils. About 70% of the total wash load from the entire study period occurred during two midsummer to autumn periods (1989 and 1990) in which the most intense storms occurred. Southwest-facing slopes (windward) had significantly higher surface erosion compared with northeast-facing slopes (leeward). The higher surface roughness encountered on 2:1 slopes appeared to more effectively control surface wash than gentler (3:1) slope gradients or early-stage vegetative cover. Straw mulch significantly reduced ravel erosion from the relatively smooth 3:1 slopes. Mulch treatment was not effective in reducing ravel erosion from rougher, 2:1 slopes. Windward (southwest-facing) slopes had significantly higher ravel erosion than northeast-facing slopes. Ravel rates were not as directly affected by rainfall intensity as were surface wash rates. Regressions of surface wash with EI (rainfall energy-intensity factor) were best with short-term intensities (i.e., EI5, R2 = 0.94); regressions of ravel with EI were best using longer term intensities (EI30; R2 = 0.83). Except for very dry collection periods (including autumn to spring), surface wash exceeded ravel.

Received for publication February 8, 1993.





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