Data

Great Lakes Restoration Initiative Project 49 Fox River Basin 2016 and 2017 Data

University of New England, Australia
Kreiling, Rebecca ; Bartsch, Lynn ; Thoms, Martin
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.5066/P93RTNVY&rft.title=Great Lakes Restoration Initiative Project 49 Fox River Basin 2016 and 2017 Data&rft.identifier=10.5066/P93RTNVY&rft.publisher=University of New England, Australia&rft.description=The Fox River transports elevated loads of nitrogen and phosphorus to Lake Michigan. The increased concentration of N and P causes eutrophication of the lake, creating hypoxic zones and damaging the lake ecosystem.To decrease loading, best management practices (BMPs) have been implemented in the uplands of the basin. Little work has been done, however, to reduce nutrient concentrations in the river. Rivers are capable of removing nutrients through biotic uptake and sediment burial and are able to remove N through denitrification. Identifying and managing these locations of increased nutrient cycling known as “hot spots” may be another mechanism for nutrient mitigation.Our objective was to identify hot spots of N and P cycling in the Fox River basin. We measured rates of specific biogeochemical processes (e.g. ambient and potential denitrification, and sediment phosphorus uptake and release) at sites that had varying mixed land use. We also measured variables that are known to affect nitrogen and phosphorus cycling. Models were created to estimate how land use type and BMP coverage can effect the capacity of the Fox River and its tributaries to retain and cycle N and P.&rft.creator=Kreiling, Rebecca &rft.creator=Bartsch, Lynn &rft.creator=Thoms, Martin &rft.date=2019&rft.coverage=Upper Midwest Environmental Sciences Center (UMESC)&rft_rights=Rights holder: Martin Thoms&rft_rights=Rights holder: Martin Thoms&rft_subject=Freshwater Ecology&rft_subject=BIOLOGICAL SCIENCES&rft_subject=ECOLOGY&rft_subject=Environmental Management&rft_subject=ENVIRONMENTAL SCIENCES&rft_subject=ENVIRONMENTAL SCIENCE AND MANAGEMENT&rft_subject=Soil Chemistry (excl. Carbon Sequestration Science)&rft_subject=SOIL SCIENCES&rft_subject=Ecosystem Assessment and Management of Fresh, Ground and Surface Water Environments&rft_subject=ENVIRONMENT&rft_subject=ECOSYSTEM ASSESSMENT AND MANAGEMENT&rft_subject=Land and Water Management of environments not elsewhere classified&rft_subject=LAND AND WATER MANAGEMENT&rft.type=dataset&rft.language=English Access the data

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Rights holder: Martin Thoms

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The Fox River transports elevated loads of nitrogen and phosphorus to Lake Michigan. The increased concentration of N and P causes eutrophication of the lake, creating hypoxic zones and damaging the lake ecosystem.To decrease loading, best management practices (BMPs) have been implemented in the uplands of the basin. Little work has been done, however, to reduce nutrient concentrations in the river. Rivers are capable of removing nutrients through biotic uptake and sediment burial and are able to remove N through denitrification. Identifying and managing these locations of increased nutrient cycling known as “hot spots” may be another mechanism for nutrient mitigation.Our objective was to identify hot spots of N and P cycling in the Fox River basin. We measured rates of specific biogeochemical processes (e.g. ambient and potential denitrification, and sediment phosphorus uptake and release) at sites that had varying mixed land use. We also measured variables that are known to affect nitrogen and phosphorus cycling. Models were created to estimate how land use type and BMP coverage can effect the capacity of the Fox River and its tributaries to retain and cycle N and P.

Issued: 2019-05-17

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text: Upper Midwest Environmental Sciences Center (UMESC)

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