Weathering of Sulfidic Shale and Copper Mine Waste: Secondary Minerals and Metal Cycling in Great Smoky Mountains National Park, Tennessee, and North Carolina, USA

Authors

Jane M. Hammarstrom, US Geological Survey, 954 National Center, Reston, VAFollow
Robert R. Seal II, U.S. Geological Survey, 954 National Center, Reston, Virginia 20192, USAFollow
Allen L. Meier, US Geological Survey, Denver, CO 80225, USA
John C. Jackson, US Geological Survey, 954 National Center, Reston, VA

Date of this Version

2003

Comments

Published in Environmental Geology (2003) 45:35–57.

Abstract

Metal cycling via physical and chemical weathering of discrete sources (copper mines) and regional (non-point) sources (sulfide-rich shale) is evaluated by examining the mineralogy and chemistry of weathering products in Great Smoky Mountains National Park, Tennessee, and North Carolina, USA. The elements in copper mine waste, secondary minerals, stream sediments, and waters that are most likely to have negative impacts on aquatic ecosystems are aluminum, copper, zinc, and arsenic because these elements locally exceed toxicity guidelines for surface waters or for stream sediments. Acid-mine drainage has not developed in streams draining inactive copper mines. Acid-rock drainage and chemical weathering processes that accompany debris flows or human disturbances of sulfidic rocks are comparable to processes that develop acid-mine drainage elsewhere. Despite the high rainfall in the mountain range, sheltered areas and intermittent dry spells provide local venues for development of secondary weathering products that can impact aquatic ecosystems.