Assessment of heavy metal enrichment in the offshore fine-grained sediments of the Caspian Sea

• Published in: Environmental monitoring and assessment 2016-05, Vol.188 (5), p.303-303, Article 303
• Main Authors: Pakzad, Hamid Reza, Pasandi, Mehrdad, Yeganeh, Siavash, Alizadeh Ketek Lahijani, Hamid
• Format: Article
• Language: English
• Subjects: Atmospheric Protection/Air Quality Control/Air Pollution; Cadmium; calcium carbonate; carbon; clay; Clay minerals; cobalt; copper; Earth and Environmental Science; Ecology; Ecotoxicology; Environment; Environmental impact; Environmental Management; Environmental Monitoring; Geologic Sediments - chemistry; Grain size; gravity; Heavy metals; Investigations; Lead; manganese; Metal concentrations; Metals; Metals, Heavy - analysis; Minerals; Monitoring/Environmental Analysis; nickel; Ocean floor; Oceans and Seas; Organic carbon; physicochemical properties; provenance; Sediments; silver; strontium; Water Pollutants, Chemical - analysis; Zinc
• ISSN: 0167-6369; 1573-2959
• DOI: 10.1007/s10661-016-5302-7

Sampling of the offshore seabed sediments of southwestern part of the Caspian Sea was carried out by gravity corer in order to study heavy metal concentration and the physicochemical factors controlling their distribution in the fine-grained fraction. The grain size distribution, amount, and type of clay minerals, total organic carbon (TOC) content, and Eh–pH of the sediments were determined. The average concentrations of the heavy metals in ppm are Mn (563), Cu (207.5), Sr (187), Zn (94), Pb (26.3), Ni (14.5), Co (11.5), Cd (2.56), and Ag (1.04) in their order of abundances. Co and Zn mostly indicate increase in silt-size fraction of the sediments suggesting their probable detrital provenance but the Mn, Ni, Cu, Sr, Pb, Cd, and Ag concentrations show a similar trend to distribution of the clay-size fraction. The concentrations of Mn, Co, and Cd increase with increase in the TOC content but the Cu, Pb, Ni, Ag, and Sr concentrations decrease with increase of the TOC content. The amounts of Zn, Cu, Sr, Pb, Cd, and Ag increase with increase in the CaCO₃ content. The calculated enrichment factor indicates that the sediments are very strong to extremely enriched in Ag, significantly enriched in Cu and Cd, and depleted to mineral for Pb, Sr, Co, Ni, and Zn. Variations of the Cu, Sr, Cd, Ag, and Pb concentrations are similar to the clay and CaCO₃ distributions.