STABLE ISOTOPE AND MICROBIAL INDICATORS OF SULFUR CYCLE PATHWAYS IN AN AMD TREATMENT SYSTEM
We report small temporal variations in the sulfur isotope values of dissolved sulfate (δ34SSO4) in the effluent from the mine’s main seeps and observation wells. In contrast, significant δ34SSO4 differences between the passive bioreactor inflow and outflow were recorded. In the bioreactor outflow, a general temporal decrease in δ34SSO4was observed at the same time as increased sulfate & metal concentrations and decreases in pH were measured. Compared to δ34SSO4 in the bioreactor outflow, contrasting δ34SSO4 trends were measured in the post-treatment oxidation pond, with increasing δ34SSO4 values during 2007 and decreasing δ34SSO4 values afterwards.
To investigate microbial contributions to the sulfur cycle in the system, molecular techniques targeting the 16S rRNA and dsrAB gene sequences were employed. Phylogenetic analysis of the 16S rRNA gene sequences in the post-treated waters indicated the presence of a sulfur-oxidizing bacterium most closely related to Sulfuricurvum kujiense as the predominant phylotype. In conjunction with this finding, there was a low diversity of sulfate-reducing bacteria detected in the post-treatment waters with sequences most similar to the slow-growing Desulfobacca acetoxidans being the most prevalent.
The significance of these trends is likely related to the declining ability of the treatment system to produce alkalinity which affected both bacterial sulfate reduction processes in the bioreactor and oxidation pond and the sulfate mineral precipitation throughout the treatment system. Our results are being used to optimize the bioremediation strategies of the Tab-Simco treatment system.