An assessment of thermodynamic reaction constants for simulating aqueous environmental monomethylmercury speciation

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 0.4 M: 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. Schwart-zenbach and Schellenberg, 1965); CH₃Hg ⁺ + Br^-?CH₃HgBr, log₁₀K = 6.87 (20°C corr. Schwartzenbach and Schellenberg, 1965); CH₃Hg ⁺ +1^-?CH₃HgI, 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 ⁺ + S^2-?CH₃HgS ^-, log₁₀K = 21.1; CH³Hg ⁺+ SH ^-? CH3HgSH, log₁₀K = 14.5 (H ⁺ + SH^-?CH₂S, 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 ⁺+ CH₃HgS^{1 -}?(CH₃Hg)₂S, log₁₀K = 16.32 (Schwartzenbach and Schellenberg, 1965; Rabenstein et al., 1978; and Erni, 1981).