Paper No. 28
Presentation Time: 3:45 PM


ALI, Hendratta, Department of Geosciences, Fort Hays State University, 600 Park Street, Hays, KS 67601 and ATEKWANA, Eliot, Boone Pickens School of Geology, Oklahoma State University, 105 Noble Research Center, Stillwater, OK 74078,

The neutralization of carbonate-rich mine tailings releases high amounts of CO2 that may be trapped in groundwater systems, and released rapidly to the atmosphere when the groundwater discharges on the surface. In this study, we measured dissolved inorganic carbon (DIC), major ions, and stable carbon isotope ratios δ13C of DIC from carbonate-rich mine tailings, that produce neutral mine drainage. We investigated the temporal evolution of DIC and δ13CDIC released from the neutralized carbonate-rich tailings in a laboratory leaching experiment. The goal was to simulate DIC evolution and the resulting changes in stable carbon isotopes of DIC that arise when groundwater is released from the subsurface from neutral mine drainage in carbonate-rich environments. The objective was (1) to investigate DIC and δ13CDIC evolution during the outgassing of CO2(aq) from the neutral tailings discharge (2) temporal changes in δ13CDIC during CO2(g) outgassing. From the experimental data, rapid decreases in DIC and increasing pH and alkalinity was observed in the first 48 hours of leaching carbonate rich tailings waste with excess sulfuric acid. The DIC decrease is due to loss of excess CO2(aq) released from the leachate as reactor was opened to atmosphere. The DIC decrease from CO2(aq) loss, maybe analogous to CO2(aq) loss as groundwater charged with DIC is discharge to the surface at a seep or source point. We relate the temporal change in DIC from the reactor over time to decreases that would be observed in field settings in the DIC as groundwater discharge flows downstream. The mechanism of excess CO2(g) loss from the reactor is kinetic and this will lead to a kinetic δ13CDIC enrichment (from initial -1.9permil to final 2.5permil after 172 hours of sampling). the highest enrichment ~ 5.0 permil occurs between the first 100hours and then remains more or less constant to end of the experiment at 172 hours. The magnitude of the δ13CDIC enrichment depends on the initial concentration of excess CO2(aq) in the discharge water and the amount plus rate of CO2(g) loss from the discharge. Carbon evolution in neutral mine drainage has potential implications in our understanding of CO2(g) released from carbonate-rich mining tailings environments.