Cumulative Sulfate Loads Shift Porewater to Sulfidic Conditions in Freshwater Wetland Sediment.
Autor: | Johnson NW; Department of Civil Engineering, University of Minnesota Duluth, Duluth, Minnesota, USA., Pastor J; Department of Biology, University of Minnesota Duluth, Duluth, Minnesota, USA., Swain EB; Minnesota Pollution Control Agency, St. Paul, Minnesota, USA. |
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Jazyk: | angličtina |
Zdroj: | Environmental toxicology and chemistry [Environ Toxicol Chem] 2019 Jun; Vol. 38 (6), pp. 1231-1244. |
DOI: | 10.1002/etc.4410 |
Abstrakt: | It is well established that sulfide can be toxic to rooted aquatic plants. However, a detailed description of the effects of cumulative sulfate loads on sulfide and iron (Fe) porewater geochemistry, plant exposure, and ecological response is lacking. Over 4 yr, we experimentally manipulated sulfate loads to self-perpetuating wild rice (Zizania palustris) populations and monitored increases in the ratio of sulfur (S) to Fe in sediment across a range of sulfide loading rates driven by overlying water sulfate. Because natural settings are complicated by ongoing Fe and S loads from surface and groundwater, this experimental setting provides a tractable system to describe the impacts of increased S loading on Fe-S porewater geochemistry. In the experimental mesocosms, the rate of sulfide accumulation in bulk sediment increased linearly with overlying water sulfate concentration up to 300 µg-SO (© 2019 The Authors. Environmental Toxicology and Chemistry published by Wiley Periodicals, Inc. on behalf of SETAC.) |
Databáze: | MEDLINE |
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