CoutureHouleGagnon2012

Référence

Couture, S., Houle, D., Gagnon, C. (2012) Increases of dissolved organic carbon in temperate and boreal lakes in Quebec, Canada. Environmental Science and Pollution Research, 19(2):361-371. (Scopus )

Résumé

Purpose: Increases in dissolved organic carbon (DOC) concentrations have been reported in surface waters worldwide in the last 10 to 20 years. The causes behind these increases have been attributed to many factors, including climate change and decreasing depositions of atmospheric sulphate (SO4 2-). Trends in DOC concentrations and their potential causal factors were examined in a network of 30 lakes lying in undisturbed temperate and boreal catchments in the province of Quebec, Canada. Methods: Temporal trends in lake DOC concentrations were analysed with the seasonal Kendall test. For each lake, the variation in DOC concentration over time was assessed in light of the variation in SO4 2- concentration in precipitation, air temperature, precipitation and solar radiation using the forward stepwise multiple regression. Results: Between 1989 and 2006, significant increases in DOC were observed in most of the lakes, the mean rate of change being 0. 05 mg L-1 year-1. Lake DOC concentrations were significantly explained by different models that yielded a variance explanation ranging from 13% to 77%. The models included long-term temperature variables (i. e. averaged over intervals of 10 years), short-term precipitation variables (i. e. summed over intervals 6 months), radiation (i. e. ice-free period prior to the DOC observation) and precipitation SO4 2- concentration as explanatory variables. Conclusion: Temporal changes in DOC concentrations seem more consistent with the evolution of climate parameters rather than SO4 2- concentrations despite the fact that most lakes were in the process of recovery, showing increases in pH. © 2011 Her Majesty the Queen in Right of Canada.

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@ARTICLE { CoutureHouleGagnon2012,
    AUTHOR = { Couture, S. and Houle, D. and Gagnon, C. },
    TITLE = { Increases of dissolved organic carbon in temperate and boreal lakes in Quebec, Canada },
    JOURNAL = { Environmental Science and Pollution Research },
    YEAR = { 2012 },
    VOLUME = { 19 },
    PAGES = { 361-371 },
    NUMBER = { 2 },
    NOTE = { cited By 26 },
    ABSTRACT = { Purpose: Increases in dissolved organic carbon (DOC) concentrations have been reported in surface waters worldwide in the last 10 to 20 years. The causes behind these increases have been attributed to many factors, including climate change and decreasing depositions of atmospheric sulphate (SO4 2-). Trends in DOC concentrations and their potential causal factors were examined in a network of 30 lakes lying in undisturbed temperate and boreal catchments in the province of Quebec, Canada. Methods: Temporal trends in lake DOC concentrations were analysed with the seasonal Kendall test. For each lake, the variation in DOC concentration over time was assessed in light of the variation in SO4 2- concentration in precipitation, air temperature, precipitation and solar radiation using the forward stepwise multiple regression. Results: Between 1989 and 2006, significant increases in DOC were observed in most of the lakes, the mean rate of change being 0. 05 mg L-1 year-1. Lake DOC concentrations were significantly explained by different models that yielded a variance explanation ranging from 13% to 77%. The models included long-term temperature variables (i. e. averaged over intervals of 10 years), short-term precipitation variables (i. e. summed over intervals 6 months), radiation (i. e. ice-free period prior to the DOC observation) and precipitation SO4 2- concentration as explanatory variables. Conclusion: Temporal changes in DOC concentrations seem more consistent with the evolution of climate parameters rather than SO4 2- concentrations despite the fact that most lakes were in the process of recovery, showing increases in pH. © 2011 Her Majesty the Queen in Right of Canada. },
    AUTHOR_KEYWORDS = { Climate; Dissolved organic carbon; Lakes; Quebec Canada; Sulphate deposition },
    DOCUMENT_TYPE = { Article },
    DOI = { 10.1007/s11356-011-0565-6 },
    KEYWORDS = { carbon; sulfate, air temperature; atmospheric deposition; catchment; climate change; concentration (composition); dissolved organic carbon; lake pollution; precipitation (climatology); solar radiation; sulfate; surface water; temperate environment; temporal variation, article; Canada; chemistry; climate change; environmental monitoring; lake; methodology; precipitation; regression analysis; temperature; theoretical model; water pollutant, Carbon; Chemical Precipitation; Climate Change; Environmental Monitoring; Lakes; Models, Theoretical; Quebec; Regression Analysis; Sulfates; Temperature; Water Pollutants, Chemical, Canada; Quebec [Canada] },
    SOURCE = { Scopus },
    URL = { https://www.scopus.com/inward/record.uri?eid=2-s2.0-84856005938&partnerID=40&md5=f40ec914950b440670ef5d50b647a55e },
}

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