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Scott D. Wankel

Researcher at Woods Hole Oceanographic Institution

Publications -  94
Citations -  4827

Scott D. Wankel is an academic researcher from Woods Hole Oceanographic Institution. The author has contributed to research in topics: Nitrate & Chemistry. The author has an hindex of 32, co-authored 78 publications receiving 3895 citations. Previous affiliations of Scott D. Wankel include Stanford University & United States Geological Survey.

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Book ChapterDOI

Tracing Anthropogenic Inputs of Nitrogen to Ecosystems

TL;DR: For example, the World Health Organization and U.S. Environmental Protection Agency have set a limit of 10 mg L nitrate (as N) for drinking water because nitrate poses a health risk, especially for children, who can contract methemoglobinemia (blue-baby syndrome) as mentioned in this paper.
Journal ArticleDOI

Nitrogen Isotopes as Indicators of NOx Source Contributions to Atmospheric Nitrate Deposition Across the Midwestern and Northeastern United States

TL;DR: The results suggest that large areas of the landscape potentially receive atmospheric NO(y) deposition inputs in excess of what one would infer from existing monitoring data alone, and spatial patterns in delta15N values are a valuable complement to existing tools for assessing relationships between NO3- deposition, regional emission inventories, and for evaluating progress toward NO(x) reduction goals.
Journal ArticleDOI

Coupled biotic–abiotic Mn(II) oxidation pathway mediates the formation and structural evolution of biogenic Mn oxides

TL;DR: In this paper, the authors explore the reactivity of biogenic Mn oxides formed by a common marine bacterium (Roseobacter sp AzwK-3b), which has been previously shown to oxidize Mn(II) via the production of extracellular superoxide, resulting in the formation of highly reactive colloidal birnessite with hexagonal symmetry.
Journal ArticleDOI

Dominance of sulfur-fueled iron oxide reduction in low-sulfate freshwater sediments.

TL;DR: Sulfidization was a dominant pathway in iron reduction despite low sulfate concentrations and regardless of iron oxide substrate, indicating that sulfur (re)cycling is a dominant force in iron cycling even in low-sulfate systems and in a manner difficult to predict using the classical thermodynamic ladder.