Concentrations and Distributions of Metals Associated with Dissolved Organic Matter from the Suwannee River (GA, USA)

    Publications: Contribution to journalArticlePeer Reviewed

    Abstract

    Concentrations and distributions of metals in Suwannee River (SR) raw filtered surface water (RFSW) and dissolved organic matter (DOM) processed by reverse osmosis (RO), XAD-8 resin (for humic and fulvic acids [FA]), and XAD-4 resin (for "transphilic" acids) were analyzed by asymmetrical flow field-flow fractionation (AsFlFFF). SR samples were compared with DOM samples from Nelson's Creek (NLC), a wetland-draining stream in northern Michigan; previous International Humic Substances Society (IHSS) FA and RO samples from the SR; and an XAD-8 sample from Lake Fryxell (LF), Antarctica. Despite application of cation exchange during sample processing, all XAD and RO samples contained substantial metal concentrations. AsFlFFF fractograms allowed metal distributions to be characterized as a function of DOM component molecular weight (MW). In SR RFSW, Fe, Al, and Cu were primarily associated with intermediate to higher than average MW DOM components. SR RO, XAD-8, and XAD-4 samples from May 2012 showed similar MW trends for Fe and Al but Cu tended to associate more with lower MW DOM. LF DOM had abundant Cu and Zn, perhaps due to amine groups that should be present due to its primarily algal origins. None of the fractograms showed obvious evidence for mineral nanoparticles, although some very small mineral nanoparticles might have been present at trace concentrations. This research suggests that AsFlFFF is important for understanding how metals are distributed in different DOM samples (including IHSS samples), which may be key to metal reactivity and bioavailability.
    Original languageEnglish
    Pages (from-to)54-65
    Number of pages12
    JournalEnvironmental Engineering Science
    Volume32
    Issue number1
    DOIs
    Publication statusPublished - 1 Jan 2015

    Funding

    We thank the Center for Environmental Science and Technology (CEST) at Notre Dame for use of analytical equipment and personnel support. K. Kuhn was supported by an NSF Graduate Research Fellowship and a Pathfinder Fellowship from the Consortium of Universities for the Advancement of Hydrologic Science, Inc (CUAHSI). We thank the Department of Environmental Geosciences at the Univ. of Vienna for use of the AsFlFFF system, and financial, laboratory, and personnel support. D. McKnight kindly provided the LF sample. Collection of the SR samples was partially funded by the IHSS. We thank E.M. Perdue (Ball State Univ.) for overseeing 2012 sample collection at the SR, D. McInnis (Notre Dame) for valuable discussion, and K. Butler (U.S.G.S) for analytical expertise. We thank C.H. Conaway and two anonymous reviewers for many helpful comments. Any use of trade, firm, or product name is for descriptive purposes only and does not imply endorsement by the U.S. Government.

    Austrian Fields of Science 2012

    • 105302 Hydrochemistry
    • 105303 Hydrogeology
    • 104002 Analytical chemistry
    • 105904 Environmental research

    Keywords

    • reverse osmosis
    • XAD
    • Suwannee River
    • DOM
    • metals
    • field-flow fractionation
    • FIELD-FLOW FRACTIONATION
    • RARE-EARTH-ELEMENTS
    • SIZE-EXCLUSION CHROMATOGRAPHY
    • AQUATIC HUMIC SUBSTANCES
    • FULVIC-ACID
    • FLUORESCENCE SPECTROSCOPY
    • SYNCHRONOUS FLUORESCENCE
    • TEMPORAL VARIATIONS
    • MOLECULAR-WEIGHT
    • REVERSE-OSMOSIS

    Cite this