Adsorption of mercury species on river sediments - effects of selected abiotic parameters
| Authors | |
|---|---|
| Year of publication | 2010 |
| Type | Article in Periodical |
| Magazine / Source | Central European Journal of Chemistry |
| MU Faculty or unit | |
| Citation | |
| Field | Analytic chemistry |
| Keywords | Mercury species; Adsorption; River sediments |
| Description | Abiotic parameters (pH, temperature, current velocity, mercury species concentration, and sediment and aqueous media composition) influence mercury species (MeHg+, EtHg+, PhHg+ and inorganic Hg2+) adsorption on river sediments. The highest amount of adsorbed MeHg+ and EtHg+ (82-93% and 85-91% for static and agitated system, respectively) occurred at pH 3-4. For PhHg+ the maximum adsorption (90% and 95% for static and agitated systems) was located over the broad 3-10 pH range, while for Hg2+ (94% and 97% for static and agitated systems) it was at pH similar to 3. Temperature (4.5-60 degrees C) influenced the adsorption rate but not the quantity. Both rate and quantity increased in the order: static < agitated <= stirred systems. The aqueous medium composition affected both rate and quantity. Sulfate caused the largest adsorption decrease for organomercury species (15-25% decrease); sulfide reduced Hg2+ adsorption about 67%. Cations at pH 5.2 reduced either the adsorption rate (Ca2+, Al3+) or the total adsorption (Zn2+, Fe3+). Positive correlations were found between sediment C, N, S content as well as cation exchange capacity (CEC) with mercury adsorption (R = 0.45-0.66, 0.56-0.89, 0.45-0.61 and 0.55-0.73, respectively) while negative correlations were observed with Fe and Al (R = -0.63 to -0.90 and -0.65 to -0.86, respectively) |
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