Microbiological and geochemical characterization of As-bearing tailings and underlying sediments

Over the past 100 years, extensive oxidation of As-bearing sulfide-rich tailings from the abandoned Long Lake Gold Mine (Canada) has resulted in the formation of acid mine drainage (pH 2.0-3.9) containing high concentrations of dissolved As (∼400 mg L-1), SO42-, Fe and other metals. Dissolved As is predominantly present as As(III), with increased As(V) near the tailings surface. Pore-gas O2 is depleted to < 1 vol% in the upper 30-80 cm of the tailings profile. The primary sulfides, pyrite and arsenopyrite, are highly oxidized in the upper portions of the tailings. Elevated proportions of sulfide-oxidizing prokaryotes are present in this zone (mean 32.3% of total reads). The tailings are underlain by sediments rich in organic C. Enrichment in δ34S-SO4 in pore-water samples in the organic C-rich zone is consistent with dissimilatory sulfate reduction. Synchrotron-based spectroscopy indicates an abundance of ferric arsenate phases near the impoundment surface and the presence of secondary arsenic sulfides in the organic-C beneath the tailings. The persistence of elevated As concentrations beneath the tailings indicates precipitation of secondary As sulfides is not sufficient to completely remove dissolved As. The oxidation of sulfides and release of As is expected to continue for decades. The findings will inform future remediation efforts and provide a foundation for the long-term monitoring of the effectiveness of the remediation program.

Removal of arsenic and metals from groundwater impacted by mine waste using zero-valent iron and organic carbon: Laboratory column experiments

Acid mine drainage and the associated contaminants, including As and metals, are ongoing environmental issues. Passive remediation technologies have the potential to remove As from mine waste effluents. A series of laboratory column experiments was conducted to evaluate the effectiveness of varying mixtures of organic carbon (OC), zero-valent iron (ZVI), and limestone for the treatment of As, metals, SO₄^2-, and acidity in groundwater from an abandoned gold mine. The onset of bacterially-mediated SO₄^2- reduction was indicated by a decrease in Eh, a decline in aqueous SO₄^2- concentrations coupled with enrichment of δ³⁴S, and the presence of sulfate-reducing bacteria and H₂S. Removal of As was observed within the first 3 cm of reactive material, to values below 10 µg L^-1, representing > 99.9% removal. An increase in pH from 3.5 to circumneutral values and removal of metals including Al, Cu, and Zn was also observed. Synchrotron results suggest As was removed through precipitation of As-crystalline phases such as realgar and orpiment, or through adsorption as As(V) on ferrihydrite. The results indicate the potential for a mixture of OC and ZVI to remove As from acidic, mine-impacted water.

Modelling the closure-related geochemical evolution of groundwater at a former uranium mine

A newly developed reactive transport model was used to evaluate the potential effects of mine closure on the geochemical evolution in the aquifer downgradient from a mine site. The simulations were conducted for the Königstein uranium mine located in Saxony, Germany. During decades of operation, uranium at the former mine site had been extracted by in situ acid leaching of the ore underground, while the mine was maintained in a dewatered condition. One option for decommissioning is to allow the groundwater level to rise to its natural level, flooding the mine workings. As a result, pore water containing high concentrations of dissolved metals, radionuclides, and sulfate may be released. Additional contamination may arise due to the dissolution of minerals contained in the aquifer downgradient of the mine. On the other hand, dissolved metals may be attenuated by reactions within the aquifer. The geochemical processes and interactions involved are highly non-linear and their impact on the quality of the groundwater and surface water downstream of the mine is not always intuitive. The multicomponent reactive transport model MIN3P, which can describe mineral dissolution-precipitation reactions, aqueous complexation, and oxidation-reduction reactions, is shown to be a powerful tool for investigating these processes. The predictive capabilities of the model are, however, limited by the availability of key geochemical parameters such as the presence and quantities of primary and secondary mineral phases. Under these conditions, the model can provide valuable insight by means of sensitivity analyses.

Genetic screening in Western Australia

The wider application of genetic screening is described in four Western Australian populations. Counselling with prenatal diagnosis of Down's syndrome was offered to 57 women over the age of 35 years and less than 16 weeks' gestation who attended an antenatal outpatients department. Forty-four women consented to amniocentesis and two affected fetuses were found. Both public and private patients can be screened to detect fetuses with Down's syndrome. In a population of 200 pregnant girls whose infants were intended for adoption, a specially designed family history form aided identification of genetic disorders in 32 families. Counselling was offered to the biological parents, to the adoptive parents, and, prospectively, to the child in later years. The effectiveness of the family history as a screening device is illustrated in this adoption sample. Counselling of parents of 20 decreased malformed infants initiated the genetic counselling clinic in Western Australia and led to subsequent referral of 92 similar cases by the family doctors. It was found that parents who gave birth to malformed infants welcome information and risk figures. Diagnostic screening in a population of 6000 intellectually handicapped individuals yielded 1372 cases (23%) with Mendelian, multifactorial, or chromosomal modes of inheritance. This screening enabled patients with inherited causes for their intellectual handicap to be identified and placed on a register for health planning.