Biogeochemical evolution of trace elements in a pristine watershed in the Brazilian southeastern coastal region

• Published in: Applied geochemistry Vol. 16; no. 9; pp. 1139 - 1151
• Main Authors: DePaula, Francisco C.F., Mozeto, Antonio A.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01-07-2001; Elsevier
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; Freshwater; Geochemistry; Hydrology; Hydrology. Hydrogeology; Mineralogy; Silicates; Water geochemistry; Brazil; Rio de Janeiro Brazil; Brazil, Rio de Janeiro, Capivari R; South America; Eh; accumulation; heavy metals; dissolution; concentration; baseline; transport; distribution; biogeochemistry; drainage basins; enrichment; remediation; trace-element analyses; burial; water quality; ecosystems; pH; sediments
• ISSN: 0883-2927; 1872-9134
• DOI: 10.1016/S0883-2927(00)00084-6

Establishing ‘
reference sites’ is a difficult task and a critical factor in determining the baseline functioning of ecosystems. The information thus obtained on nutrient and contaminant background concentrations in turn subsidizes the remediation of impacted landscapes. This paper reports a study on metal (Cr, Cu, Pb, Zn, Mn, Fe and Al) and nutrient (C) distribution in sediments from Capivari River watershed (Praia do Sul Biological Reserve, Ilha Grande, Rio de Janeiro State, Brazil), an area where typical SE Brazilian coastal ecosystems are located. Contrary to what one would expect from the high rate at which these ecosystems have been deteriorating in recent decades, the study site is surprisingly well preserved. The present study was developed to assess variations in heavy metal concentrations in river basin sediments, to identify the geochemical carriers of these elements, and determine the influence of water quality and organic matter on their distribution. Results showed that heavy metal distribution has been influenced by the natural biogeochemical properties of those ecosystems found in an upland-to-lowland sequence in the watershed. Minimum and maximum total concentration were: 5 and 23 mg/kg for Cr; 4 and 29 mg/kg for Cu; 13 and 53 mg/kg for Pb; 24 and 142 mg/kg for Zn; 54 and 342 mg/kg for Mn; 0.8 and 7.2% for Fe; 0.5 and 4.9% for Al; 6.3 and 25% for C. The pH and E
H are the key-parameters in explaining total metal concentration decrease in the swamp area, where dissolution processes and losses through metal transport seem important. The most important geochemical carriers are Al in the basin’s “continental” stretch and Fe in the estuarine portion. The data also provide evidence showing that organic matter is the key-parameter in Cu concentration control in the sediments through burial and accumulation processes especially in the swamp area. Heavy metal concentrations in sediments from the study area are generally lower than those found in similar regional ecosystems. Surface enrichment in heavy metal concentrations in collected sediment cores was not observed. The authors therefore conclude that this site is suitable as a ‘
reference site’ for studies on the biogeochemistry and ecotoxicology of SE Brazilian coastal ecosystems.