Dynamic Coupling of Iron, Manganese, and Phosphorus Behavior in Water and Sediment of Shallow Ice-Covered Eutrophic Lakes

Decreasing duration and occurrence of northern hemisphere ice cover due to recent climate warming is well-documented; however, biogeochemical dynamics underneath the ice are poorly understood. We couple time-series analyses of water column and sediment water interface (SWI) geochemistry with hydrody...

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Published inEnvironmental science & technology Vol. 49; no. 16; pp. 9758 - 9767
Main Authors Schroth, Andrew W, Giles, Courtney D, Isles, Peter D. F, Xu, Yaoyang, Perzan, Zachary, Druschel, Gregory K
Format Journal Article
LanguageEnglish
Published United States American Chemical Society 18.08.2015
Subjects
Biogeochemistry
Climate
Eutrophication
Fluid mechanics
freshwater
geochemistry
Geography
Geologic Sediments - chemistry
Global warming
Hydrodynamics
hydroxides
Ice
Ice Cover
iron
Iron - analysis
Lakes
Lakes - chemistry
manganese
Manganese - analysis
oxygen
Oxygen - analysis
oxygen consumption
Phosphorus
Phosphorus - analysis
river water
sediments
Temperature
Time series
time series analysis
Trace Elements - analysis
Water - chemistry
Water Pollutants, Chemical - analysis
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Abstract Decreasing duration and occurrence of northern hemisphere ice cover due to recent climate warming is well-documented; however, biogeochemical dynamics underneath the ice are poorly understood. We couple time-series analyses of water column and sediment water interface (SWI) geochemistry with hydrodynamic data to develop a holistic model of iron (Fe), manganese (Mn), and phosphorus (P) behavior underneath the ice of a shallow eutrophic freshwater bay. During periods of persistent subfreezing temperatures, a highly reactive pool of dissolved and colloidal Fe, Mn, and P develops over time in surface sediments and bottom waters due to reductive dissolution of Fe/Mn­(oxy)­hydroxides below the SWI. Redox dynamics are driven by benthic O2 consumption, limited air–water exchange of oxygen due to ice cover, and minimal circulation. During thaw events, the concentration, distribution and size partitioning of all species changes, with the highest concentrations of P and “truly dissolved” Fe near the water column surface, and a relatively well-mixed “truly dissolved” Mn and “colloidal” Fe profile due to the influx of geochemically distinct river water and increased circulation. The partitioning and flux of trace metals and phosphorus beneath the ice is dynamic, and heavily influenced by climate-dependent physical processes that vary in both time and space.
AbstractList Decreasing duration and occurrence of northern hemisphere ice cover due to recent climate warming is well-documented; however, biogeochemical dynamics underneath the ice are poorly understood. We couple time-series analyses of water column and sediment water interface (SWI) geochemistry with hydrodynamic data to develop a holistic model of iron (Fe), manganese (Mn), and phosphorus (P) behavior underneath the ice of a shallow eutrophic freshwater bay. During periods of persistent subfreezing temperatures, a highly reactive pool of dissolved and colloidal Fe, Mn, and P develops over time in surface sediments and bottom waters due to reductive dissolution of Fe/Mn­(oxy)­hydroxides below the SWI. Redox dynamics are driven by benthic O2 consumption, limited air–water exchange of oxygen due to ice cover, and minimal circulation. During thaw events, the concentration, distribution and size partitioning of all species changes, with the highest concentrations of P and “truly dissolved” Fe near the water column surface, and a relatively well-mixed “truly dissolved” Mn and “colloidal” Fe profile due to the influx of geochemically distinct river water and increased circulation. The partitioning and flux of trace metals and phosphorus beneath the ice is dynamic, and heavily influenced by climate-dependent physical processes that vary in both time and space.
Decreasing duration and occurrence of northern hemisphere ice cover due to recent climate warming is well-documented; however, biogeochemical dynamics underneath the ice are poorly understood. We couple time-series analyses of water column and sediment water interface (SWI) geochemistry with hydrodynamic data to develop a holistic model of iron (Fe), manganese (Mn), and phosphorus (P) behavior underneath the ice of a shallow eutrophic freshwater bay. During periods of persistent subfreezing temperatures, a highly reactive pool of dissolved and colloidal Fe, Mn, and P develops over time in surface sediments and bottom waters due to reductive dissolution of Fe/Mn(oxy)hydroxides below the SWI. Redox dynamics are driven by benthic O2 consumption, limited air-water exchange of oxygen due to ice cover, and minimal circulation. During thaw events, the concentration, distribution and size partitioning of all species changes, with the highest concentrations of P and "truly dissolved" Fe near the water column surface, and a relatively well-mixed "truly dissolved" Mn and "colloidal" Fe profile due to the influx of geochemically distinct river water and increased circulation. The partitioning and flux of trace metals and phosphorus beneath the ice is dynamic, and heavily influenced by climate-dependent physical processes that vary in both time and space.
Decreasing duration and occurrence of northern hemisphere ice cover due to recent climate warming is well-documented; however, biogeochemical dynamics underneath the ice are poorly understood. We couple time-series analyses of water column and sediment water interface (SWI) geochemistry with hydrodynamic data to develop a holistic model of iron (Fe), manganese (Mn), and phosphorus (P) behavior underneath the ice of a shallow eutrophic freshwater bay. During periods of persistent subfreezing temperatures, a highly reactive pool of dissolved and colloidal Fe, Mn, and P develops over time in surface sediments and bottom waters due to reductive dissolution of Fe/Mn(oxy)hydroxides below the SWI. Redox dynamics are driven by benthic O₂ consumption, limited air–water exchange of oxygen due to ice cover, and minimal circulation. During thaw events, the concentration, distribution and size partitioning of all species changes, with the highest concentrations of P and “truly dissolved” Fe near the water column surface, and a relatively well-mixed “truly dissolved” Mn and “colloidal” Fe profile due to the influx of geochemically distinct river water and increased circulation. The partitioning and flux of trace metals and phosphorus beneath the ice is dynamic, and heavily influenced by climate-dependent physical processes that vary in both time and space.
Author Druschel, Gregory K
Perzan, Zachary
Xu, Yaoyang
Schroth, Andrew W
Giles, Courtney D
Isles, Peter D. F
AuthorAffiliation Rubenstein School of Environment and Natural Resources
Department of Geology
Vermont EPSCoR
University of Vermont
Department of Earth Sciences
Indiana University Purdue University
Middlebury College
AuthorAffiliation_xml – name: Indiana University Purdue University
– name: University of Vermont
– name: Department of Earth Sciences
– name: Rubenstein School of Environment and Natural Resources
– name: Middlebury College
– name: Vermont EPSCoR
– name: Department of Geology
Author_xml – sequence: 1
  givenname: Andrew W
  surname: Schroth
  fullname: Schroth, Andrew W
  email: aschroth@uvm.edu
– sequence: 2
  givenname: Courtney D
  surname: Giles
  fullname: Giles, Courtney D
– sequence: 3
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– sequence: 4
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  surname: Perzan
  fullname: Perzan, Zachary
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  fullname: Druschel, Gregory K
BackLink https://www.ncbi.nlm.nih.gov/pubmed/26206098$$D View this record in MEDLINE/PubMed
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acs
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Index Database
Enrichment Source
Publisher
StartPage 9758
SubjectTerms Biogeochemistry
Climate
Eutrophication
Fluid mechanics
freshwater
geochemistry
Geography
Geologic Sediments - chemistry
Global warming
Hydrodynamics
hydroxides
Ice
Ice Cover
iron
Iron - analysis
Lakes
Lakes - chemistry
manganese
Manganese - analysis
oxygen
Oxygen - analysis
oxygen consumption
Phosphorus
Phosphorus - analysis
river water
sediments
Temperature
Time series
time series analysis
Trace Elements - analysis
Water - chemistry
Water Pollutants, Chemical - analysis
Title Dynamic Coupling of Iron, Manganese, and Phosphorus Behavior in Water and Sediment of Shallow Ice-Covered Eutrophic Lakes
URI http://dx.doi.org/10.1021/acs.est.5b02057
https://www.ncbi.nlm.nih.gov/pubmed/26206098
https://www.proquest.com/docview/1706703457
https://www.proquest.com/docview/1712571956
https://www.proquest.com/docview/2000215632
Volume 49
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