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Abstract

 

This article in JEQ

  1. Vol. 34 No. 1, p. 263-273
     
    Received: May 11, 2004


    * Corresponding author(s): e.burton@griffith.edu.au
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doi:10.2134/jeq2005.0263

Geochemical Partitioning of Copper, Lead, and Zinc in Benthic, Estuarine Sediment Profiles

  1. Edward D. Burton *ab,
  2. Ian R. Phillipsa and
  3. Darryl W. Hawkerc
  1. a School of Environmental Engineering, Faculty of Environmental Sciences, Griffith University, Nathan, QLD, 4111, Australia
    b CRC for Coastal Zone, Estuary and Waterway Management, Indooroopilly Sciences Centre, 80 Meiers Road, Indooroopilly, QLD, 4068, Australia
    c School of Australian Environmental Studies, Faculty of Environmental Sciences, Griffith University, Nathan, QLD, 111, Australia

Abstract

The geochemical partitioning of copper (Cu), lead (Pb), and zinc (Zn) was examined in benthic sediment profiles (0- to 20-cm depth interval) composed of relatively coarse (65–90% sand-sized particles), noncohesive, suboxic material (Eh +120 to +260 mV). Total Cu, Pb, and Zn concentrations ranged from 8.3 to 194, 16.3 to 74.8, and 30.1 to 220 mg/kg, respectively, and were related to vertical trends in sediment texture. The observed distribution coefficients describing solid–solution partitioning were in the range of 100 to 1000 L/kg. The geochemical partitioning of solid-phase Cu, Pb, and Zn between six operationally defined fractions was examined with a sequential extraction scheme. The association of Cu, Pb, and Zn with amorphous oxides, crystalline oxides, and organic matter was linearly dependent on the abundance of each respective phase. For retention by amorphous oxide minerals, the observed stoichiometry ranged from 5.2 to 23.7 mg/g for Cu, 12.8 to 21.5 mg/g for Pb, and 23.1 to 85.7 mg/g for Zn. Corresponding values for association with crystalline oxides were an order of magnitude less than those for amorphous oxides, indicating a lesser affinity of trace metals for crystalline oxides. The stoichiometric relationships describing association with organic matter ranged from 17.6 to 54.0 mg/g for Cu, 6.1 to 9.6 mg/g for Pb, and 6.4 to 16.4 mg/g for Zn. The results from this study provide an insight into processes controlling trace metal partitioning in coarse-textured, suboxic, estuarine sediments.

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