1. An assessment of thermodynamic reaction constants for simulating aqueous environmental monomethylmercury speciation.
- Author
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Loux, Nicholas T.
- Subjects
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METHYLMERCURY , *MERCURY , *LIGANDS (Chemistry) , *BICARBONATE ions , *ECOLOGY , *CARBONIC acid - Abstract
Monomethylmercury (CH3Hg+) is both the most ecologically significant and the least well characterized species of mercury in environmental settings. Our understanding of the environmental speciation behavior of this compound is limited both as the result of lesser available laboratory data (when compared to inorganic mercury) as well as the uncertainties associated with our understanding of the properties of environmental ligands. A careful examination and synthesis of data reported in the technical literature led to the following findings: (1) a 25°C, zero ionic strength bicarbonate ion complexation constant estimate is remarkably close to an earlier reported value at 0.4M: CH3Hg+ + HCO3- ...CH3HgHCO3, log10K = 2.6 (+0.22, 1 SD), (2) three 25°C zero ionic strength reaction constants reported by DeRobertis et al. (1998) were confirmed to within ~ +0.1 log10K units: CH3Hg+ +OH-...CH3HgOH, log10K = 9.47; 2CH3Hg+ +H2O...(CH3Hg)2OH+ +H+, log10K = -2.15; CH3Hg+ +Cl-...CH3HgCl, log10K = 5.45, (3) "best estimate" literature complexation constants corrected to zero ionic strength include: CH3Hg+ +F-...CH3HgF, log10K = 1.75 (20°C corr. Schwartzenbach and Schellenberg, 1965); CH3Hg+ +Br -...CH3HgBr, log10K = 6.87 (20°C corr. Schwartzenbach and Schellenberg, 1965); CH3Hg+ +l -...CH3Hgl, log10K = 8.85 (20°C corr. Schwartzenbach and Schellenberg, 1965); and CH3Hg+ +SO4 ²_...CH3HgSO4-, log10K = 2.64 (25°C, DeRobertis et al., 1998), (4) literature reported values for simulating monomethylmercury complexation with the carbonate ion may be too low: CH3Hg+ +CO3 ²-...CH3HgCO3-, log10K = 6.1 (Rabenstein et al., 1976; Erni, 1981), and (5) "best estimate" constants for simulating methyl mercury complexation with reduced environmental sulfur species include: CH3Hg+ +S² -...CH3HgS-, log10K = 21.1; CH3Hg+ +SH-...CH3HgSH, log10K = 14.5 (H+ +SH-..H2S, log10K = 6.88; Dyrssen and Wedborg, 1991); CH3Hg+ +RS-...CH3HgSR, log10K = 16.5 (H+ +RS-..RSH, log10K = 9.96; Qian et al., 2002); and CH3Hg+ +CH3HgS¹ -..(CH3Hg)2S, log10K = 16.32 (Schwartzenbach and Schellenberg, 1965; Rabenstein et al., 1978; and Erni, 1981). [ABSTRACT FROM AUTHOR]
- Published
- 2007
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