Thesis (M.S.)--University of Nevada, Reno, 2005. / "December, 2005." Includes bibliographical references (leaves 80-85). Online version available on the World Wide Web.

Mining for silver, lead, zinc, and copper in Zimapan, Hidalgo State, Mexico has been ongoing since 1576. Unsecured tailings heaps and associated acid mine drainage have presented problems related to soil quality, water quality, and dust emission control in the Zimapan area. Objectives of the study of the mine tailings are (1) to determine mineralogy of the tailings in order to identify acid-producing minerals and heavy metals at risk for release in acidic conditions, and (2) to quantify carbonate minerals and (3) to determine heavy metal content that may be released by the products of sulfide mineral weathering. Representative mine tailings have been sampled from a site located north of Zimapan. Mineralogical characterization has been conducted with X-ray diffraction (XRD), and scanning and transmission electron microscopes (SEM and TEM). Total carbonates have been determined the Chittick procedure. X-Ray Fluorescence (XRF) has been utilized to determine total elemental composition. XRD and SEM analyses have confirmed the presence of pyrite and arsenopyrite indicating a potential for acid mine drainage. Calcite has been confirmed to have a significant presence in the unweathered samples by XRD and the Chittick procedure, with some samples containing an average of 19.4% calcite. NAA and XRF have revealed significant concentrations of toxic elements such as As, Pb and Zn in both the oxidized and unoxidized samples.

Water quality degradation is the foremost environmental issue faced by the mining industry. Negative impacts on water quality are commonly associated with unmitigated drainage emanating from sulfide-bearing mine waste deposits. These impacts stem from the liberation of acidity, sulfate, metals (e.g. Fe, Ni, Cu, Zn and Pb), and trace elements (e.g. Co, As, Cd, Sb and Tl) during the oxidation of sulfide minerals. Drainage at operational mines is commonly treated using techniques such as chemical oxidation and acid neutralization, which can succeed in achieving regulatory discharge guidelines. However, active treatment techniques are commonly burdened by high capital and operating costs. The development of passive technologies for treatment of mine drainage, which promote sulfate reduction, metal-sulfide precipitation and alkalinity production, therefore present a cost-effective alternative for managing mine drainage quality. This thesis describes laboratory and field evaluations of techniques for passive in situ treatment of acidic and neutral mine waters. Laboratory batch experiments evaluated the treatment of acid mine drainage (AMD) with mixtures of organic carbon and zero-valent iron (ZVI) for use in permeable reactive barriers (PRBs). Modest increases in sulfate-reduction rates up to 15 % were achieved by amending organic carbon mixtures with 5 to 10 % (dry wt.) ZVI. Reactive mixtures containing organic carbon supported growth of sulfate-reducing bacteria (SRB) and facilitated removal of Fe, Zn, Cd, Ni, Co and Pb. However, organic carbon was necessary to support SRB growth and sulfate reduction. Removal of Zn, Cd, Ni, Co and Pb in the absence of organic carbon is attributed to sorption and (co)precipitation reactions at the ZVI surface. Scanning electron microscopy (SEM) and X-ray absorption near-edge structure (XANES) spectroscopy confirmed the presence of secondary Fe-sulfides in mixtures containing organic carbon. The dominant reaction product in these mixtures was identified as disordered mackinawite [Fe1+xS]. The addition of ZVI to organic carbon enhanced AMD treatment over the duration of this experiment; however, long-term evaluation is required to identify optimal reactive mixtures. Field-based investigations into passive management of near-neutral pH tailings pore-water were carried out at the Greens Creek mine, located near Juneau, Alaska, USA. These studies focused on delineation of mechanisms controlling tailings pore-water chemistry, and a evaluation of the effectiveness of organic carbon amendment of tailings for passive in situ management of pore-water quality. Results demonstrate that sulfide-mineral oxidation and carbonate dissolution are the primary influences on tailings pore-water composition. Pyrite [FeS2] accounted for < 20 to > 35 wt. % of the tailings mineral assemblage, whereas dolomite [CaMg(CO3)2] and calcite [CaCO3] were present at ≤ 30 and 3 wt. %, respectively. The sulfide-mineral assemblage was dominated by pyrite; however, sphalerite [(Zn,Fe)S] and galena [PbS] were commonly observed, and tetrahedrite [(Fe,Zn,Cu,Ag)12Sb4S13], arsenopyrite [FeAsS], and chalcopyrite [CuFeS2] were present in lesser amounts. Geochemical analysis of tailings core samples generally agreed with mineralogical data. The occurrence of Cd, Cr, Co, Mo, Ni, Se, and Tl is attributed to their occurrence as impurities in primary sulfide phases. Most probable number (MPN) populations of neutrophilic sulfur-oxidizing bacteria (nSOB) and SRB were elevated at several locations within the tailings deposit. Near-neutral pH conditions dominated; however, elevated concentrations of dissolved SO4, S2O3, Fe, Zn, As, Sb, and Tl were observed within and below the oxidation zone. Field-scale experiments conducted over four years evaluated passive in situ treatment of pore-water by amending unoxidized tailings with 5 and 10 vol. % organic carbon. Field-scale cells were constructed to evaluate amendments containing differing mixtures of peat, dried spent brewing grain (SBG), and municipal biosolids (MB). Organic carbon amendment of the tailings supported the development of conditions favorable to sulfate reduction. Decreases in aqueous SO4 concentrations were observed in three cells amended with mixtures of peat, SBG, and MB. Removal of SO4 was generally accompanied by H2S production, enrichment in 34S-SO4, and increased SRB populations. Undersaturation of pore-water with respect to gypsum was observed. Sulfate reduction was sustained for the duration of the experiment in cells amended with 5 vol. % peat + SBG and 10 vol. % peat + SBG + MB. The addition of organic carbon also supported reductive dissolution of Fe(III) (oxy)hydroxides and mobilization of Fe and As. The largest increases in aqueous Fe and As concentrations were observed in cells amended with MB. Subsequent decreases in Fe and As concentrations were observed under sulfate-reducing conditions. Attenuation of Zn, Sb, and Tl accompanied SO4 removal. Mineralogical examination by SEM revealed the presence of secondary Zn-S and Fe-S precipitates on surfaces of organic carbon particles, and carbonate and aluminosilicate grains. This study demonstrates that amendment of tailings with a small and dispersed mass of organic carbon has potential to improve the quality of tailings pore water.

Water quality degradation is the foremost environmental issue faced by the mining industry. Negative impacts on water quality are commonly associated with unmitigated drainage emanating from sulfide-bearing mine waste deposits. These impacts stem from the liberation of acidity, sulfate, metals (e.g. Fe, Ni, Cu, Zn and Pb), and trace elements (e.g. Co, As, Cd, Sb and Tl) during the oxidation of sulfide minerals. Drainage at operational mines is commonly treated using techniques such as chemical oxidation and acid neutralization, which can succeed in achieving regulatory discharge guidelines. However, active treatment techniques are commonly burdened by high capital and operating costs. The development of passive technologies for treatment of mine drainage, which promote sulfate reduction, metal-sulfide precipitation and alkalinity production, therefore present a cost-effective alternative for managing mine drainage quality. This thesis describes laboratory and field evaluations of techniques for passive in situ treatment of acidic and neutral mine waters. Laboratory batch experiments evaluated the treatment of acid mine drainage (AMD) with mixtures of organic carbon and zero-valent iron (ZVI) for use in permeable reactive barriers (PRBs). Modest increases in sulfate-reduction rates up to 15 % were achieved by amending organic carbon mixtures with 5 to 10 % (dry wt.) ZVI. Reactive mixtures containing organic carbon supported growth of sulfate-reducing bacteria (SRB) and facilitated removal of Fe, Zn, Cd, Ni, Co and Pb. However, organic carbon was necessary to support SRB growth and sulfate reduction. Removal of Zn, Cd, Ni, Co and Pb in the absence of organic carbon is attributed to sorption and (co)precipitation reactions at the ZVI surface. Scanning electron microscopy (SEM) and X-ray absorption near-edge structure (XANES) spectroscopy confirmed the presence of secondary Fe-sulfides in mixtures containing organic carbon. The dominant reaction product in these mixtures was identified as disordered mackinawite [Fe1+xS]. The addition of ZVI to organic carbon enhanced AMD treatment over the duration of this experiment; however, long-term evaluation is required to identify optimal reactive mixtures. Field-based investigations into passive management of near-neutral pH tailings pore-water were carried out at the Greens Creek mine, located near Juneau, Alaska, USA. These studies focused on delineation of mechanisms controlling tailings pore-water chemistry, and a evaluation of the effectiveness of organic carbon amendment of tailings for passive in situ management of pore-water quality. Results demonstrate that sulfide-mineral oxidation and carbonate dissolution are the primary influences on tailings pore-water composition. Pyrite [FeS2] accounted for < 20 to > 35 wt. % of the tailings mineral assemblage, whereas dolomite [CaMg(CO3)2] and calcite [CaCO3] were present at ≤ 30 and 3 wt. %, respectively. The sulfide-mineral assemblage was dominated by pyrite; however, sphalerite [(Zn,Fe)S] and galena [PbS] were commonly observed, and tetrahedrite [(Fe,Zn,Cu,Ag)12Sb4S13], arsenopyrite [FeAsS], and chalcopyrite [CuFeS2] were present in lesser amounts. Geochemical analysis of tailings core samples generally agreed with mineralogical data. The occurrence of Cd, Cr, Co, Mo, Ni, Se, and Tl is attributed to their occurrence as impurities in primary sulfide phases. Most probable number (MPN) populations of neutrophilic sulfur-oxidizing bacteria (nSOB) and SRB were elevated at several locations within the tailings deposit. Near-neutral pH conditions dominated; however, elevated concentrations of dissolved SO4, S2O3, Fe, Zn, As, Sb, and Tl were observed within and below the oxidation zone. Field-scale experiments conducted over four years evaluated passive in situ treatment of pore-water by amending unoxidized tailings with 5 and 10 vol. % organic carbon. Field-scale cells were constructed to evaluate amendments containing differing mixtures of peat, dried spent brewing grain (SBG), and municipal biosolids (MB). Organic carbon amendment of the tailings supported the development of conditions favorable to sulfate reduction. Decreases in aqueous SO4 concentrations were observed in three cells amended with mixtures of peat, SBG, and MB. Removal of SO4 was generally accompanied by H2S production, enrichment in 34S-SO4, and increased SRB populations. Undersaturation of pore-water with respect to gypsum was observed. Sulfate reduction was sustained for the duration of the experiment in cells amended with 5 vol. % peat + SBG and 10 vol. % peat + SBG + MB. The addition of organic carbon also supported reductive dissolution of Fe(III) (oxy)hydroxides and mobilization of Fe and As. The largest increases in aqueous Fe and As concentrations were observed in cells amended with MB. Subsequent decreases in Fe and As concentrations were observed under sulfate-reducing conditions. Attenuation of Zn, Sb, and Tl accompanied SO4 removal. Mineralogical examination by SEM revealed the presence of secondary Zn-S and Fe-S precipitates on surfaces of organic carbon particles, and carbonate and aluminosilicate grains. This study demonstrates that amendment of tailings with a small and dispersed mass of organic carbon has potential to improve the quality of tailings pore water.

Colloid-borne Heavy Metals in the Drainage Gallery of an Abandoned Zn-Pb-Ag Mine (in German). The colloid inventories and the colloid-borne heavy metals in the Rothschönberger Stolln adit, the main drainage gallery of the Freiberg, Germany, mining district, were investigated. This adit runs from Freiberg to the village of Rothschönberg, where it flows into the river Triebisch, a tributary of the river Elbe. The water of the adit is a typical mine water from a flooded ore mine. The main reason for choosing the Rothschönberger Stolln adit for colloid investigations was that ample knowledge concerning the origin of the water and the geology of its catchment area exists. The aim was to characterize the colloids at the mouth of the adit and to elucidate if important contaminants occur in a colloid-borne form. A colloid concentration of about 1 mg/L was found. The particles have a size of 50 to 150 nm. They primarily consist of iron and aluminum oxyhydroxide and carry trace elements such as Pb, As, Cu, Y, La. The contaminants Pb and As are almost entirely colloid-borne. Colloids can have both a retarding and a stimulating influence on the transport of contaminants. The existence of colloids should be taken into account if mine waters flow to the biosphere or if mine waters are to be purified by permeable reactive barriers.

Thesis (M.S.)--West Virginia University, 2009. / Title from document title page. Document formatted into pages; contains xi, 66 p. : ill. (some col.). Vita. Includes abstract. Includes bibliographical references.

Thesis (Ph. D.)--West Virginia University, 2002. / Title from document title page. Document formatted into pages; contains xiv, 210 p. : ill. (some col.). Includes abstract. Includes bibliographical references.

Thesis (M.S.)--West Virginia University, 2003. / Title from document title page. Document formatted into pages; contains vi, 131 p. : ill. (some col.), col. map. Vita. Includes abstract. Includes bibliographical references (p. 69-74).

Acid Mine Drainage (AMD) is characterized by high metal concentrations and an extremely low pH, primarily generated by the microbial oxidation of iron sulfides from mine tailings. Research on the microbial AMD community has largely focused on Bacteria, while little information is known about the Archaeal and Eukaryote members or the seasonal patterns within the communities. Here I examined the Bacterial, Archaeal, and eukaryotic AMD seasonal microbial community, using direct sequencing techniques on AMD samples from the Copper Cliff Tailings AMD site in Sudbury, Ontario, Canada. I found large variation in the community profile and species composition between sampling times of both the Bacterial and Eukaryote communities, suggesting a dynamic community, both between and within seasons. Bacterial diversity was highest during the winter, with Acidithiobacillus dominating, while during the summer, Acidiphilium was the dominant genus. The winter Eukaryote community was dominated by classes of algae and fungi, while the majority of summer sequencing could not be classified to the class level. Few reads were obtained for the Archaeal domain, with low and similar biodiversity between seasons. Overall, the AMD community variation and abundance were found to largely correlate with drainage water and seasonal temperature.

Numerous streams on the West Coast drain catchments impacted by active or abandoned coal mining areas. Acid mine drainage (AMD) from coal mining can have significant negative effects on stream communities. Changing environmental ethics and regulations mean that mining companies are now encouraged to treat acid mine drainage to enable streams communities to recover. However, remediation efforts have not always been ecologically successful, and mining companies are seeking methods to enhance macroinvertebrate community recovery. Initially, I conducted an extensive survey of 45 streams draining the Stockton Plateau, which is the site of the largest opencast coal mine in New Zealand. I assessed physical and chemical conditions at each site as well as sampling benthic communities. This spatial survey showed streams impacted by acid mine drainage were comprised of chironomids and AMD-tolerant caddisflies such as Psilochorema and stoneflies such as Spaniocercoides. Un-impacted streams typically had a pH of ~5 and were dominated by mayflies (Deleatidium or Zephlebia). Analysis revealed that stream location within the landscape also had a significant influence on macroinvertebrate community composition. Another aspect of stream recovery is the ability of species to recolonise a stream. Therefore, I investigated the flight direction of adult aquatic insects in order to determine longitudinal and lateral flight preferences. No significant differences in flight direction were observed. I also investigated the influence of riparian habitat on lateral dispersal and found that a number of patterns were evident. Scrub vegetation supported higher densities of adult aquatic insects dispersing further from the stream, in contrast to the rapid decline in open bedrock and forest. Furthermore, a comparison between downstream drift and aerial flight showed significantly more individuals where drifting downstream, and this method is liable to provide rapid recolonisation of macroinvertebrates within connected stream networks. At the local scale, organic matter (comprising leaves bags and timber) and artificial moss cover were added to six streams to determine if organic matter and habitat availability would improve macroinvertebrate communities in manipulated streams. A series of floods during the experiment reduced taxonomic richness and density in manipulated streams. Overall, this study has shown that after AMD has been treated, the geographic position of streams within the landscape and lateral dispersal barriers may prevent streams being rapidly re-colonised. Therefore, to promote rapid re-colonisation of macroinvertebrates, stream remediation projects should be targeted at streams that either have un-impacted headwaters or tributaries. This will allow macroinvertebrates to drift in and re-colonise faster. In my experiment I did not find that organic matter significantly enhanced the macroinvertebrate community, but moss additions did provide additional habitat for macroinvertebrates. These results highlight the importance that disturbance events can have on remediation projects.