An assessment of heavy metal contamination in soils of fresh water aquifer system and evaluation of eco-toxicity by lithogenic implications

• Published in: Environmental monitoring and assessment 2013-04, Vol.185 (4), p.3503-3516
• Main Authors: Harichandan, R., Routroy, S., Mohanty, J. K., Panda, C. R.
• Format: Article
• Language: English
• Subjects: Animal, plant and microbial ecology; Applied ecology; Atmospheric Protection/Air Quality Control/Air Pollution; Biological and medical sciences; Cadmium; Contamination; Copper; Earth and Environmental Science; Ecology; Ecotoxicology; Ecotoxicology, biological effects of pollution; Environment; Environmental Management; Environmental Monitoring; Fresh Water - chemistry; Fundamental and applied biological sciences. Psychology; Geologic Sediments - chemistry; Groundwater - chemistry; India; Iron; Metals, Heavy - analysis; Metals, Heavy - toxicity; Monitoring/Environmental Analysis; Risk Assessment; Sediments; Soil Pollutants - analysis; Surface layer; Texture; Water Pollutants, Chemical - analysis; Water Pollutants, Chemical - toxicity; Water Pollution, Chemical - statistics & numerical data
• ISSN: 0167-6369; 1573-2959
• DOI: 10.1007/s10661-012-2806-7

The chemistry of heavy metals in sediments with respect to bio-availability and chemical reactivity is regulated by pH, texture, and organic matter contents of the sediments and specific binding form and coupled reactivity of the metals within. To focus on the metal distribution (Fe, Mn, Pb, Cd, Zn, Co, Cu, and Cr) and behavior in a fresh water aquifer system along with the ecological toxicity parameters, a four-step sequential extraction method was applied on 18 Eastern Ghats’ type sediments from fluorosis-hit Nayagarh district, India. Geo-accumulation index of metals in the sediments indicates that they are practically uncontaminated and/or less contaminated with and Fe, Mn, and Cu; contaminated to moderately contaminated with Pb, Zn, and Cr; and strongly contaminated with Cd. Rather, more than 80 % recovered Cd metal concentration in sediments constitute the labile fractions. Temporal clustering of metal fractions indicates transition metal fraction distribution claiming the sediment pH regulation. Similarly, base metal distribution accounts for organic carbon and soil conductivity due to their greater availability in exchangeable and sulfide fractions. Correlation analysis and factor analysis scores demonstrate lack of inter-relationship between transition group and base metal fractions. High fluoride concentration in ground water is associated with high sodium-bicarbonate-iron affinity with elevated pH values (i.e., >7.0) and high positive factor score with the total iron concentration in ground water.