Significance of oxides and particulate organic matter in controlling trace metal partitioning in a contaminated estuary

• Published in: Marine chemistry Vol. 88; no. 3; pp. 179 - 192
• Main Authors: Turner, Andrew, Millward, Geoffrey E., Le Roux, Sophie M.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01.09.2004; Elsevier Science
• Subjects: Brackish; Earth sciences; Earth, ocean, space; Exact sciences and technology; External geophysics; Fe–Mn oxides; Geochemistry; Mineralogy; Organic matter; Partitioning; Physical and chemical properties of sea water; Physics of the oceans; Salinity; Sediment; Silicates; Sorption; Trace metals; Water geochemistry; ANE, British Isles, England, Merseyside, Mersey Estuary; British Isles, England, Mersey Estuary; British Isles; Sorption; Organic matter; Sediment; Partitioning; Fe–Mn oxides; Trace metals; Salinity; sea water; models; salinity; trace metals; oxides; regression analysis; oxidation; metals; exhibits; sorption; hydrochemistry; chemical reduction; organic materials; estuaries; particles; energy
• ISSN: 0304-4203; 1872-7581
• DOI: 10.1016/j.marchem.2004.03.008

The sediment–water partitioning of radiolabelled Cd, Hg and Zn has been investigated along an estuarine salinity gradient using samples from the Mersey Estuary, UK. Partitioning was studied using untreated particles, and particles that had been extracted using either a reducing agent (NH 2OH.HCl–HOAc) or an oxidising agent (H 2O 2) in order to qualitatively evaluate the relative roles of Fe–Mn oxides and particulate organic matter (POM), respectively, on metal uptake. The extent of Cd partitioning between sediment and water, parameterised in terms of the distribution coefficient, K D, exhibited a reduction with increasing salinity, regardless of whether or not particles had been digested. However, the magnitude of K D decreased significantly following either chemical treatment, suggesting that both oxides and organic matter are important sorbents for Cd. The K D for Hg in the presence of untreated particles increased with increasing salinity, and chemical reduction of the particles enhanced the uptake of Hg and reinforced this trend. Particle oxidation led to a significant reduction in the K D for Hg, and uptake by the particles decreased with increasing salinity. These observations suggest that POM is considerably more important than Fe–Mn oxides in the removal of aqueous Hg, and that its presence is a prerequisite for enhanced sorption (or salting out) at elevated salinities. The salinity dependence of K D for Zn displayed characteristics of both Cd (below salinities of about 5) and Hg (at greater salinities). However, the magnitude of K D for Zn uptake was relatively insensitive to either chemical treatment, suggesting that oxides, POM, and residual phases contribute to the overall sorption of Zn by estuarine particles. Regression analyses of the metal partition data suggest that sorption to oxides and POM is nonadditive, and that the salinity dependence of metal partitioning results mainly from salinity-controlled interactions between metal and organic matter. Sequential extraction of metals bound to untreated and chemically treated particles in the partitioning experiments indicated that the exchangeability or lability of all metals increased on removal of either oxides or POM. This implies that sorption sites of relatively high energy are destroyed (or become less accessible), or sorption sites of relatively low energy are created (or become more accessible) on chemical treatment. These observations support a conceptual model for the particle surface whose integrity and binding properties are only maintained by the coexistence of and interaction between oxides and organic matter.