Technical Papers
Nov 12, 2012

Curve Numbers for Low-Compaction Steep-Sloped Reclaimed Mine Lands in the Southern Appalachians

Publication: Journal of Hydrologic Engineering
Volume 18, Issue 12

Abstract

In the coal-mining region of the Appalachians, the Forestry Reclamation Approach (FRA) is currently promoted by the U.S. Dept. of Interior, Office of Surface Mining (OSM). FRA’s goal in establishing native forest cover on reclamation sites requires the use of loose spoils rather than traditionally compacted spoils during hillslope reconstruction. Loose spoils improve tree planting survival and enhance overall forest growth. Although FRA has been shown to be successful on low-gradient slopes without excessive runoff leading to erosion, rainfall-runoff relationships have not been studied on steep slopes (>20°) where most surface-mine reclamation typically occurs. A curve number (CN) range representing low-compaction steep-sloped conditions was needed for Appalachian FRA sites. Three active surface-mine sites in East Tennessee were monitored during a 1-year period (June 2009–July 2010) for rainfall (5-min intervals) and runoff hydrology (discharge volume, peak discharge) using a unique Pinson-type collection system. CNs were estimated by the traditional NEH-4 (Part 630) method and two asymptotic, frequency-matching techniques. It was found that an initial abstraction (λ) of 0.2 best fits the data. CNs generated by the NEH-4 method among all three mining sites were not significantly different suggesting common shale-based loose spoils on steep slopes have similar runoff behavior. The CN determined by the asymptotic method provided an estimate with a practical range between 58.5 and 60. This CN range is lower than one would expect from surface-mine sites, suggesting infiltration influenced the measured rainfall-runoff relationships. Further research is needed to investigate the influence of slope and infiltration on runoff behavior at surface-mine sites applying FRA.

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Acknowledgments

The authors gratefully acknowledge the funding support of the U.S. Department of Interior, Office of Surface Mining (OSM), Applied Science Program Grant CA No. S08AP12822. David Lane and Vic Davis of OSM were particularly helpful in obtaining permission to conduct these field experiments on private coal-mining property, and offering suggestions during the study design development. We greatly appreciate the support of the mine operators at the national, premium, and mountainside sites for the construction of the field plots and for allowing access to their property during the study. Field and laboratory assistance for data collection were aided by many University of Tennessee students, including Isaac Jeldes, Nathan Felosi, Samuel Mathews, Chris Dixon, and Chris Drinnon.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 18Issue 12December 2013
Pages: 1627 - 1638

History

Received: Dec 22, 2011
Accepted: Nov 9, 2012
Published online: Nov 12, 2012
Discussion open until: Apr 12, 2013
Published in print: Dec 1, 2013

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Authors

Affiliations

Siavash Hoomehr [email protected]
M.ASCE
Postdoctoral Research Associate, Dept. of Biological Systems Engineering, Virginia Polytechnic Institute and State Univ. (Virginia Tech), Blacksburg, VA 24061 (corresponding author). E-mail: [email protected]
John S. Schwartz
M.ASCE
Associate Professor, Dept. of Civil and Environmental Engineering, Univ. of Tennessee, Knoxville, TN 37996.
Daniel C. Yoder
M.ASCE
Professor, Dept. of Biosystems Engineering and Soil Science, Univ. of Tennessee, Knoxville, TN 37996.
Eric C. Drumm
M.ASCE
Professor, Dept. of Biosystems Engineering and Soil Science, Univ. of Tennessee, Knoxville, TN 37996.
Wesley Wright
Research Associate II, Dept. of Biosystems Engineering and Soil Science, Univ. of Tennessee, Knoxville, TN 37996.

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