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Spatial Variation in the Optical Properties of Dissolved Organic Matter (DOM) in Lakes on the Canadian Precambrian Shield and Links to Watershed Characteristics

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Abstract

In the present study, we explored the use of various optical parameters to detect differences in the composition of the dissolved organic matter (DOM) in a set of lakes that are all located on the Canadian Precambrian Shield, but within which Cu and Ni speciation predictions were previously shown to diverge from measured values in some lakes but not in others. Water samples were collected with in situ diffusion samplers in 2007 (N = 18 lakes) and 2008 (N = 8 lakes). Significant differences in DOM quality were identified between the sampling regions (Rouyn-Noranda, Québec and Sudbury, Ontario) and among lakes, based on dissolved organic carbon concentrations ([DOC]), specific UV absorbance (SUVA254), fluorescence indices (FI), and excitation–emission matrix (EEM) fluorescence measurements. Parallel factor analysis (PARAFAC) of the EEM spectra revealed four components, two of which (C3, oxidized quinone fluorophore of allochthonous origin, and C4, tryptophan-like protein fluorescence of autochthonous origin) showed the greatest inter-regional variation. The inter-lake differences in DOM quality were consistent with the regional watershed characteristics as determined from satellite imagery (e.g., watershed-to-lake surface area ratios and relative percentages of surface water, rock outcrops vegetative cover and urban development). Source apportionment plots, built upon PARAFAC components ratios calculated for our lakes, were used to discriminate among DOM sources and to compare them to sources identified in the literature. These results have implications for other areas of research, such as quantifying lake-to-lake variations in the influence of organic matter on the speciation of trace elements in natural aquatic environments.

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Acknowledgments

The authors acknowledge the technical assistance provided by M.G. Bordeleau, S. Duval and J. Perreault in the laboratory and P. Girard and P. Marcoux in the field. We also thank M.-A. Robin for providing GIS data, as well as S. Smith and C. Stedmon for helpful discussions on PARAFAC modeling. I. Lavoie provided invaluable assistance with the multivariate statistical analyses. Sampling was greatly facilitated by the personnel of the Laurentian University Cooperative Freshwater Ecology Unit, led by J. Gunn, in the Sudbury area and by L. Jourdain of the Ministère des ressources naturelles et de la faune du Québec in the Rouyn-Noranda area. Comments provided by R.-M. Couture on earlier versions of the MS were greatly appreciated. Financial support was provided by the Natural Sciences and Engineering Research Council of Canada and by the Metals in the Human Environment Research Network (www.mithe-rn.org). P.G.C. Campbell and C. Fortin are supported by the Canada Research Chair Program. The constructive comments of two anonymous referees are gratefully acknowledged.

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Correspondence to Peter G. C. Campbell.

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Mueller, K.K., Fortin, C. & Campbell, P.G.C. Spatial Variation in the Optical Properties of Dissolved Organic Matter (DOM) in Lakes on the Canadian Precambrian Shield and Links to Watershed Characteristics. Aquat Geochem 18, 21–44 (2012). https://doi.org/10.1007/s10498-011-9147-y

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