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Identifying environmental and geochemical variables governing metal concentrations in a stream draining headwaters in NW Spain
Institution:1. Ohio Environmental Protection Agency, P.O. Box 1049, Columbus, OH 43216-1049, United States of America;2. Kieser & Associates, LLC, 536 E. Michigan Ave., Suite 300, Kalamazoo, MI 49007, United States of America;1. Large Lakes Research Station, 9311 Groh Road, Grosse Ile, MI 48138, USA;2. Z-Tech Corporation, ICF Company, Large Lakes Research Station, 9311 Groh Road, Grosse Ile, MI 48138, USA;3. United States Environmental Protection Agency, Office of Research and Development, National Health and Environmental Effects Research Laboratory, Mid-Continent Ecology Division, Duluth, Large Lakes and Rivers Forecasting Research Branch, Large Lakes Research Station, 9311 Groh Road, Grosse Ile, MI 48138, USA
Abstract:Headwater stream, draining from a rural catchment in NW Spain, was sampled during baseflow and storm-event conditions to investigate the temporal variability in dissolved and particulate Al, Fe, Mn, Cu and Zn concentrations and the role of discharge (Q), pH, dissolved organic carbon (DOC) and suspended sediment (SS) in the transport of dissolved and particulate metals. Under baseflow and storm-event conditions, concentrations of the five metals were highly variable. The results of this study reveal that all metal concentrations are correlated with SS. DOC and SS appeared to influence both the metal concentrations and the partitioning of metals between dissolved and particulate. The SS was a good predictor of particulate metal levels. Distribution coefficients (KD) were similar between metals (4.72–6.55) and did not change significantly as a function of discharge regime. Stepwise multiple linear regression analysis reveals that the most important variable to explain storm-event KD for Al and Fe is DOC. The positive relationships found between metals, in each fraction, indicate that these elements mainly come from the same source. Metal concentrations in the stream were relatively low.
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