2016
DOI: 10.1016/j.apgeochem.2016.10.004
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Physicochemical gradients, diffusive flux, and sediment oxygen demand within oil sands tailings materials from Alberta, Canada

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Cited by 7 publications
(3 citation statements)
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“…Although no increase in H 2 S was observed in the water cap of these experiments, it suggests that the observed decrease of measurable sulfide flux may in part be due to secondary processes (e.g., sulfide precipitation or a decrease in sulfur reducing bacteria). This result is similar to those found in Reid et al [21] and was suggested to be related to the formation of sulfides causing an increase in porosity. Sulfides, such as FeS 2 have a defined crystalline cubic structure.…”
Section: Chemical Componentsupporting
confidence: 92%
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“…Although no increase in H 2 S was observed in the water cap of these experiments, it suggests that the observed decrease of measurable sulfide flux may in part be due to secondary processes (e.g., sulfide precipitation or a decrease in sulfur reducing bacteria). This result is similar to those found in Reid et al [21] and was suggested to be related to the formation of sulfides causing an increase in porosity. Sulfides, such as FeS 2 have a defined crystalline cubic structure.…”
Section: Chemical Componentsupporting
confidence: 92%
“…A 2 × 2 experimental design (with replicates) allowed two environmental conditions (anoxic and oxic) to be tested, and determined the microbial impact (biotic vs. abiotic) on the sludge. This study design has been used in numerous past studies to address environmental impacts of various materials [20][21][22]. The four experimental conditions discussed in this study are biotic anoxic, abiotic anoxic, biotic oxic, and abiotic oxic.…”
Section: Site Description and Laboratory Incubationsmentioning
confidence: 99%
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