Heavy metal fluxes at the sediment–water interface of three coastal ecosystems from south-west of the Iberian Peninsula

• Published in: Science of the total environment Vol. 247; no. 2; pp. 189 - 199
• Main Authors: Blasco, J., Sáenz, V., Gómez-Parra, A.
• Format: Journal Article Conference Proceeding
• Language: English
• Published: Shannon Elsevier B.V 20.03.2000; Elsevier Science
• Subjects: Applied sciences; Background levels; Brackish; Coastal ecosystems; Diffusive fluxes; Earth sciences; Earth, ocean, space; Engineering and environment geology. Geothermics; Europe, Iberian Peninsula; Exact sciences and technology; Heavy metals; Marine; Pollution; Pollution sources. Measurement results; Pollution, environment geology; Porewater; Sediment; Soil and sediments pollution; Spain, Cadiz Bay; Spain, Odiel R; Europe; Spain; ANE, Spain; Background levels; Porewater; Sediment; Heavy metals; Coastal ecosystems; Diffusive fluxes; Littoral zone; Iron; Sediments; Interstitial water; Heavy metal; Salt marsh; Pollution; Medium effect; Content; Chromium; Pollution source inventory; Redox potential; Copper; Manganese
• ISSN: 0048-9697; 1879-1026; 1879-1026
• DOI: 10.1016/S0048-9697(99)00490-8

Concentrations of the heavy metals Cr, Cu, Fe and Mn were measured in sediments and porewater samples collected in three coastal ecosystems southwest of the Iberian Peninsula: the Odiel and Barbate River Salt Marshes and the Bay of Cádiz. Both the sediment and the porewater metal concentrations in the Odiel River Salt Marshes are higher than the values found in the Bay of Cádiz and Barbate River Salt Marsh, particularly for copper, a metal associated with mining activity. In porewater, the profiles were not the same as those in the solid phase and reflect the different behaviours of the elements in relation to the redox conditions. The heavy metals Cr and Cu show a typical enrichment in the porewater of the oxic zone. The heavy metals Mn and Fe show an increase in the porewater at the depths where the maximum nitrate and phosphate concentrations occur, respectively. Significant differences between background levels for each heavy metal in the various studied zones exist. Iron and Cu showed larger background levels in the Odiel River Salt Marshes than those in the Cádiz Bay and the Barbate River Salt Marshes. In the Bay of Cádiz the background levels are also high, particularly for Cr. At the Odiel River Salt Marshes the diffusive flux of Cu is high (1.3–230.1 μg cm −2 year −1), which suggests that the Odiel River Salt Marshes are subject to strong contamination by Cu, which is presumably introduced to the sediment in particulate form. In the Bay of Cádiz, Cr is the only metal with positive diffusive flux (2.15 μg cm −2 year −1). It is higher than those obtained in other coastal ecosystems including the Odiel River Salt Marshes. The positive diffusive flux of Cr has been associated with the input of this metal by the naval industry and the manufacturing of car and aircraft components.