T299 Novel Approaches to Mine Remediation: Addressing the Legacy of Hardrock Mining through Innovative and Practical Methods
Wednesday, 25 October 2017
8:00 AM - 12:00 PM
Room 618/619/620
EFFECT OF ALUMINUM OXYHYDROXIDE COATINGS ON THE PERFORMANCE OF ANOXIC LIMESTONE DRAINS
Paper number: T299-13
Program: Technical Sessions
Time: 11:00 AM – 11:15 AM
Authors
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J. Donald RimstidtVirginia Tech, Blacksburg, VA
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Madeline SchreiberVirginia Tech, Blacksburg, VA
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John A. ChermakVirginia Tech, Blacksburg, VA
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Robert R. SealU.S. Geological Survey, Reston, VA
Abstract
Initially, batch experiments were used to evaluate what Al minerals form during the reaction of acidic Al-rich solutions with calcite. Aluminum concentrations ranged from 0.002 M to 0.01 M and the pH ranged from 3.6 to 3.8. Examination of the produced coatings with x-ray diffraction identified poorly crystalline gibbsite as the primary Al coating. Subsequent mixed flow reactor (MFR) experiments are being used to quantify the effect of the Al mineral coatings on the calcite dissolution rate. We are measuring pH to determine the rate of H+ consumption during the reaction of the acidic Al sulfate solutions with calcite. Initial MFR results show that the consumption of H+ declines after 4 to 6 hours, suggesting that the formation of a coating is limiting the diffusion of H+ to the calcite surface. Additional experiments using different Al concentrations are currently being conducted. Results from an initial experiment showed that the diffusion coefficient for H+ in the gibbsite layer (7.8x10-13 m2/sec) is four orders of magnitude smaller than that in water (9.3x10-9 m2/sec). Results of these experiments will be used to estimate the dissolution of limestone in ALDs under different pH conditions and Al concentrations similar to those found in discharges from pyrite-bearing materials.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-306073
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