Characterization and Copper Binding of Humic and Nonhumic Organic Matter Isolated from the South Platte River:  Evidence for the Presence of Nitrogenous Binding Site

J.-P. Croué,* M. F. Benedetti, D. Violleau,§ and J. A. Leenheer
UMR 6008 CNRS Laboratoire de Chimie de l'Eau et de l'Environnement, ESIP, Universit de Poitiers, 40 Avenue du Recteur Pineau, 86022 Poitiers Cedex, France, UMR 7047 CNRS Laboratoire de Gochimie et Mtallognie, UPMC Case 124, Universit Pierre et Marie Curie, 4 Place Jussieu 75252 Paris Cedex 05, France, and United States Geological Survey, Denver Federal Center, P.O. Box 25046, Mail Stop 408, Building 95, Denver, Colorado 80225-0046
Environ. Sci. Technol., 2003, 37 (2), pp 328–336
DOI: 10.1021/es020676p
Publication Date (Web): December 6, 2002
Copyright © 2003 American Chemical Society
*

 Corresponding author phone:  33-549-45-3915; fax:  33-549-45-3768; e-mail:  Jean.Philippe.Croue@univ-poitiers.fr.

,

 Université de Poitiers.

,

 Université Pierre et Marie Curie.

,
§

 Actual address:  Laboratoire des Sciences de l'Environnement et de l'Aménagement, Université d'Angers, 2 Bld Lavoisier, 49045 Angers Cedex, France.

,

 United States Geological Survey.

Abstract

Humic substances typically constitute 40−60% of the dissolved organic matter (DOM) in surface waters. However, little information is available regarding the metal binding properties of the nonhumic hydrophilic portion of the DOM. In this study, humic and nonhumic DOM samples were isolated from the South Platte River (Colorado, DOC = 2.6 mg·L-1, SUVA254 = 2.4 L/mg·m) using a two-column array of XAD-8 and XAD-4 resins. The three major isolated fractions of DOM, which accounted for 57% of the bulk DOM, were characterized using a variety of analytical tools. Proton and copper binding properties were studied for each fraction. The main objective of this work was to compare the structural and chemical characteristics of the isolated fractions and test models describing DOM reactivity toward metal ions. The characterization work showed significant structural differences between the three isolated fractions of DOM. The hydrophobic acid fraction (i.e., humic substances isolated from the XAD-8 resin) gave the largest C/H, C/O, and C/N ratios and aromatic carbon content among the three isolated fractions. The transphilic acid (TPHA) fraction (“transphilic” meaning fraction of intermediate polarity isolated from the XAD-4 resin) was found to incorporate the highest proportion of polysaccharides, whereas the transphilic neutral (TPHN) fraction was almost entirely proteinaceous. The gradual increase of the charge with pH for the three DOM fractions is most likely caused by a large distribution of proton affinity constants for the carboxylic groups, as well as a second type of group more generally considered to be phenolic. In the case of the DOM fraction enriched in proteinaceous material (i.e., TPHN fraction), the results showed that the amino groups are responsible for the charge reversal. For low copper concentrations, nitrogen-containing functional groups similar to those of amino acids are likely to be involved in complexation, in agreement with previously published data.

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History

  • Published In Issue January 15, 2003
  • Received for review April 5, 2002
    Revised manuscript received October 10, 2002
    Accepted October 16, 2002

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