| Title: | A reactive transport model for mercury fate in soil--application to different anthropogenic pollution sources |
| Author(s): | Leterme B; Blanc P; Jacques D; |
| Address: | "Performance Assessments, Institute for Environment, Health, and Safety, Belgian Nuclear Research Centre (SCK*CEN), Boeretang 200, 2400, Mol, Belgium, bleterme@sckcen.be" |
| Journal Title: | Environ Sci Pollut Res Int |
| DOI: | 10.1007/s11356-014-3135-x |
| ISSN/ISBN: | 1614-7499 (Electronic) 0944-1344 (Linking) |
| Abstract: | "Soil systems are a common receptor of anthropogenic mercury (Hg) contamination. Soils play an important role in the containment or dispersion of pollution to surface water, groundwater or the atmosphere. A one-dimensional model for simulating Hg fate and transport for variably saturated and transient flow conditions is presented. The model is developed using the HP1 code, which couples HYDRUS-1D for the water flow and solute transport to PHREEQC for geochemical reactions. The main processes included are Hg aqueous speciation and complexation, sorption to soil organic matter, dissolution of cinnabar and liquid Hg, and Hg reduction and volatilization. Processes such as atmospheric wet and dry deposition, vegetation litter fall and uptake are neglected because they are less relevant in the case of high Hg concentrations resulting from anthropogenic activities. A test case is presented, assuming a hypothetical sandy soil profile and a simulation time frame of 50 years of daily atmospheric inputs. Mercury fate and transport are simulated for three different sources of Hg (cinnabar, residual liquid mercury or aqueous mercuric chloride), as well as for combinations of these sources. Results are presented and discussed with focus on Hg volatilization to the atmosphere, Hg leaching at the bottom of the soil profile and the remaining Hg in or below the initially contaminated soil layer. In the test case, Hg volatilization was negligible because the reduction of Hg(2+) to Hg(0) was inhibited by the low concentration of dissolved Hg. Hg leaching was mainly caused by complexation of Hg(2+) with thiol groups of dissolved organic matter, because in the geochemical model used, this reaction only had a higher equilibrium constant than the sorption reactions. Immobilization of Hg in the initially polluted horizon was enhanced by Hg(2+) sorption onto humic and fulvic acids (which are more abundant than thiols). Potential benefits of the model for risk management and remediation of contaminated sites are discussed" |
| Keywords: | "Environmental Monitoring/*methods *Environmental Pollution Mercuric Chloride Mercury/*analysis Mercury Compounds *Models, Chemical Soil/*chemistry Soil Pollutants/*analysis Thermodynamics;" |
| Notes: | "MedlineLeterme, Bertrand Blanc, Philippe Jacques, Diederik eng Research Support, Non-U.S. Gov't Germany 2014/06/15 Environ Sci Pollut Res Int. 2014 Nov; 21(21):12279-93. doi: 10.1007/s11356-014-3135-x. Epub 2014 Jun 15" |
