This paper investigates mercury contamination in recent marine sediment of the Tyrrhenian continental shelf near the mouths of three rivers draining an area with cinnabar deposits (M. Amiata, Italy). By means of chemical leaching, two fractions of the total mercury were distinguished: a 'non-leachable' fraction, consisting of mercury held in relatively stable forms and a 'leachable' fraction, composed of forms that are more weakly bound to the sediments. The two Hg fractions are correlated to the organic matter content, the distribution of which is strictly dependent on the sediment surface area. In order to eliminate the effects of grain size variations among the samples, the Hg concentrations were normalized to the unit of surface area (ng/m2). Following this procedure, the 'non-leachable' Hg was found to be concentrated mostly in a belt along the coast, while the 'leachable' Hg fraction was shown to accumulate largely in the zones with high depositional dynamics near the mouths of the rivers. Hypotheses to account for the discrepancy between the low concentrations of 'leachable' Hg in the sediment of the outer continental shelf and the high concentrations in the fauna of the same area, reported in previous papers, are presented. © 1982.
Baldi, F., Bargagli, R. (1982). Chemical elaching and specific surface area measurements of marine sediments in the evaluation of mercury contamination near cinnabar deposits. MARINE ENVIRONMENTAL RESEARCH, 6(1), 69-82 [10.1016/0141-1136(82)90008-3].
Chemical elaching and specific surface area measurements of marine sediments in the evaluation of mercury contamination near cinnabar deposits
Baldi, F.;Bargagli, R.
1982-01-01
Abstract
This paper investigates mercury contamination in recent marine sediment of the Tyrrhenian continental shelf near the mouths of three rivers draining an area with cinnabar deposits (M. Amiata, Italy). By means of chemical leaching, two fractions of the total mercury were distinguished: a 'non-leachable' fraction, consisting of mercury held in relatively stable forms and a 'leachable' fraction, composed of forms that are more weakly bound to the sediments. The two Hg fractions are correlated to the organic matter content, the distribution of which is strictly dependent on the sediment surface area. In order to eliminate the effects of grain size variations among the samples, the Hg concentrations were normalized to the unit of surface area (ng/m2). Following this procedure, the 'non-leachable' Hg was found to be concentrated mostly in a belt along the coast, while the 'leachable' Hg fraction was shown to accumulate largely in the zones with high depositional dynamics near the mouths of the rivers. Hypotheses to account for the discrepancy between the low concentrations of 'leachable' Hg in the sediment of the outer continental shelf and the high concentrations in the fauna of the same area, reported in previous papers, are presented. © 1982.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
https://hdl.handle.net/11365/29421
Attenzione
Attenzione! I dati visualizzati non sono stati sottoposti a validazione da parte dell'ateneo