T134 Chemical and Hydrological Interactions in the Evolution and Control of Coal and Metal Mine Drainage I
Tuesday, 24 October 2006
8:00 AM - 12:00 PM
GEOCHEMICAL LESSONS LEARNED FROM LABORATORY TESTING THROUGH OPERATION OF A WATERSHED-SCALE ACID ROCK DRAINAGE WATER TREATMENT SYSTEM
Paper number: T134-9
Program: Technical Sessions
Time: 10:05 AM – 10:20 AM
Authors
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E. Griff WyattNashville, TN
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Franklin MillerLexington, KY
Abstract
Water quality monitoring data that continues to be collected is quite extensive and includes daily field iron and pH measurements in North Potato Creek above the plant, just below the plant outfall, and at the discharge from the pit. The system to date has met or exceeded expectations in terms of downstream water quality improvements. Dissolved iron concentrations above the plant have been found to generally range between 6 mg/L and 10 mg/L and dissolved iron concentrations leaving the watershed are below 0.1 mg/L with associated pH values ranging from 7 to 9 and alkalinities generally ranging from 12 to 25 mg/L. Observations from the operating data that have a broader interest to other ARD-impacted watersheds are that iron nucleates in the water treatment facility much more readily than observed in the laboratory testing and manganese removal efficiencies from the operating system show a large variability ranging from 20 to 90%.