The slow and steady salinization of Sparkling Lake, Wisconsin

The concentrations of conservative solutes in seepage lakes are determined by the relative inputs of precipitation vs. groundwater. In areas of road salt application, seepage lakes may be at high risk of salinization depending on groundwater flow. Here, we revisit a 1992 analysis on the salinization...

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Main Authors: Hilary A. Dugan, Linnea A. Rock
Format: Article
Language:English
Published: Wiley 2023-02-01
Series:Limnology and Oceanography Letters
Online Access:https://doi.org/10.1002/lol2.10191
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author Hilary A. Dugan
Linnea A. Rock
author_facet Hilary A. Dugan
Linnea A. Rock
author_sort Hilary A. Dugan
collection DOAJ
description The concentrations of conservative solutes in seepage lakes are determined by the relative inputs of precipitation vs. groundwater. In areas of road salt application, seepage lakes may be at high risk of salinization depending on groundwater flow. Here, we revisit a 1992 analysis on the salinization of Sparkling Lake, a deep seepage lake in Northern Wisconsin. The original analysis predicted a rapid increase in chloride concentrations before reaching a steady steady of 8 mg L−1 by 2020. Forty years of monitoring Sparkling Lake show that rather than reaching a dynamic equilibrium, chloride concentrations have steadily increased. We update the original box model approach by adding a soil reservoir component that shows the slow steady rise in chloride is the result of terrestrial retention. For freshwater rivers and lakes, chloride retention on the landscape will both delay chloride impairment and prolong recovery and must be considered when modeling future chloride contamination risk.
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spelling doaj.art-efdb3cb4148b48de9de9cd5b67cb0a822023-01-27T05:34:23ZengWileyLimnology and Oceanography Letters2378-22422023-02-0181748210.1002/lol2.10191The slow and steady salinization of Sparkling Lake, WisconsinHilary A. Dugan0Linnea A. Rock1Center for Limnology, University of Wisconsin‐Madison Madison, Wisconsin USACenter for Limnology, University of Wisconsin‐Madison Madison, Wisconsin USAThe concentrations of conservative solutes in seepage lakes are determined by the relative inputs of precipitation vs. groundwater. In areas of road salt application, seepage lakes may be at high risk of salinization depending on groundwater flow. Here, we revisit a 1992 analysis on the salinization of Sparkling Lake, a deep seepage lake in Northern Wisconsin. The original analysis predicted a rapid increase in chloride concentrations before reaching a steady steady of 8 mg L−1 by 2020. Forty years of monitoring Sparkling Lake show that rather than reaching a dynamic equilibrium, chloride concentrations have steadily increased. We update the original box model approach by adding a soil reservoir component that shows the slow steady rise in chloride is the result of terrestrial retention. For freshwater rivers and lakes, chloride retention on the landscape will both delay chloride impairment and prolong recovery and must be considered when modeling future chloride contamination risk.https://doi.org/10.1002/lol2.10191
spellingShingle Hilary A. Dugan
Linnea A. Rock
The slow and steady salinization of Sparkling Lake, Wisconsin
Limnology and Oceanography Letters
title The slow and steady salinization of Sparkling Lake, Wisconsin
title_full The slow and steady salinization of Sparkling Lake, Wisconsin
title_fullStr The slow and steady salinization of Sparkling Lake, Wisconsin
title_full_unstemmed The slow and steady salinization of Sparkling Lake, Wisconsin
title_short The slow and steady salinization of Sparkling Lake, Wisconsin
title_sort slow and steady salinization of sparkling lake wisconsin
url https://doi.org/10.1002/lol2.10191
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