Re-emission of legacy mercury from soil adjacent to closed point sources of Hg emission

Mercury (Hg) emissions from point sources to air may disperse over long distance depending on Hg speciation in the plume. A significant fraction of Hg, particularly in its divalent forms, deposits locally and causes pollution to surrounding biomes. The objective of this study was to investigate (1) the historic Hg deposition to the immediate vicinity of an industrial complex that had intentional use of Hg (i.e., chlor-alkali and polyvinyl chloride production) for 5 decades until 2011, and (2) the Hg⁰ re-emission from soil to air soon after the closure of the facility. The spatial distribution of near-ground Hg⁰ vapor in air, soil Hg concentration and stable isotope ratio, air-soil Hg⁰ flux and Hg⁰ concentration in soil pore-gas were measured. It was found that the surrounding soils are severely contaminated with Hg due to the Hg release of the industrial complex, displaying soil Hg content up to 4.8 μg g⁻¹. A spatial trend of Hg mass dependent isotope fractionation signature (δ²⁰²Hg = −2.11‰ to 0.72‰) with respect to the distance from the closed facility was identified, representing a mixing between regional background and industrial Hg sources. Hg release from the industrial operation enhanced surface soil Hg content within a 6.5-km radius from the facility. Inside the facility, residual Hg wastes (i.e., electrolysis sludge and consumed HgCl₂ catalyst) represent a strong localized emission source of atmospheric Hg⁰. Near-ground atmospheric Hg⁰ concentration and soil Hg⁰ efflux progressively elevated toward the facility with an increase by 2–3 orders of magnitude compared to the values observed in the off-site background. These results suggest that the natural soil surfaces surrounding the closed industrial facility act as a large nonpoint source emitting legacy deposited Hg as much as the release from naturally enriched mines.