Rate of formation and dissolution of mercury sulfide nanoparticles: The dual role of natural organic matter

• Published in: Geochimica et cosmochimica acta 2010-08, Vol.74 (16), p.4693-4708
• Main Author: Slowey, Aaron J.
• Format: Article
• Language: English
• Subjects: Aggregates; Dissolution; Light scattering; Mercury; Microorganisms; Nanoparticles; Soils; Sulfides
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2010.05.012

Mercury is a global contaminant of concern due to its transformation by microorganisms to form methylmercury, a toxic species that accumulates in biological tissues. The effect of dissolved organic matter (DOM) isolated from natural waters on reactions between mercury(II) (Hg) and sulfide (S(-II)) to form HgS (s) nanoparticles across a range of Hg and S(-II) concentrations was investigated. Hg was equilibrated with DOM, after which S(-II) was added. Dissolved Hg (Hg aq) was periodically quantified using ultracentrifugation and chemical analysis following the addition of S(-II). Particle size and identity were determined using dynamic light scattering and X-ray absorption spectroscopy. S(-II) reacts with Hg to form 20 to 200 nm aggregates consisting of 1–2 nm HgS (s) subunits that are more structurally disordered than metacinnabar in the presence of 2 × 10 −9 to 8 × 10 −6 M Hg and 10 (mg C) L −1 DOM. Some of the HgS (s) nanoparticle aggregates are subsequently dissolved by DOM and (re)precipitated by S(-II) over periods of hours to days. At least three fractions of Hg–DOM species were observed with respect to reactivity toward S(-II): 0.3 μmol reactive Hg per mmol C (60 percent), 0.1 μmol per mmol C (20 percent) that are kinetically hindered, and another 0.1 μmol Hg per mmol C (20 percent) that are inert to reaction with S(-II). Following an initial S(-II)-driven precipitation of HgS (s), HgS (s) was dissolved by DOM or organic sulfur compounds. HgS (s) formation during this second phase was counterintuitively favored by lower S(-II) concentrations, suggesting surface association of DOM moieties that are less capable of dissolving HgS (s). DOM partially inhibits HgS (s) formation and mediates reactions between Hg and S(-II) such that HgS (s) is susceptible to dissolution. These findings indicate that Hg accessibility to microorganisms could be controlled by kinetic (intermediate) species in the presence of S(-II) and DOM, undermining the premise that equilibrium Hg species distributions should correlate to the extent or rate of Hg methylation in soils and sediments.