Gaseous elemental mercury emissions and CO₂ respiration rates in terrestrial soils under controlled aerobic and anaerobic laboratory conditions

• Published in: The Science of the total environment Vol. 408; no. 7; pp. 1691 - 1700
• Main Authors: Obrist, Daniel, Faïn, Xavier, Berger, Carsen
• Format: Journal Article
• Language: English
• Published: Kidlington [Amsterdam; New York]: Elsevier Science 01-03-2010; Elsevier
• Subjects: Applied sciences; Atmospheric pollution; Dispersed sources and other; Exact sciences and technology; Pollution; Pollution sources. Measurement results; Microbial activity; Organic matter; Carbon dioxide; Microbial respiration; Environmental factor; Zerovalent metal; Forest soil; Pollutant emission; Anaerobe; Mineralization; Laboratory study; Redox conditions; Respirometry; Anaerobic conditions; Aerobe; Soil mercury volatilization; Heavy metal; Trace element; Edaphic factor; Carbon mineralization; Air pollution; Poison; Air ground interface; Mercury; Principal component analysis
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2009.12.008

Mercury (Hg) levels in terrestrial soils are linked to the presence of organic carbon (C). Carbon pools are highly dynamic and subject to mineralization processes, but little is known about the fate of Hg during decomposition. This study evaluated relationships between gaseous Hg emissions from soils and carbon dioxide (CO₂) respiration under controlled laboratory conditions to assess potential losses of Hg to the atmosphere during C mineralization. Results showed a linear correlation (r ² =0.49) between Hg and CO₂ emissions in 41 soil samples, an effect unlikely to be caused by temperature, radiation, different Hg contents, or soil moisture. Stoichiometric comparisons of Hg/C ratios of emissions and underlying soil substrates suggest that 3% of soil Hg was subject to evasion. Even minute emissions of Hg upon mineralization, however, may be important on a global scale given the large Hg pools sequestered in terrestrial soils and C stocks. We induced changes in CO₂ respiration rates and observed Hg flux responses, including inducement of anaerobic conditions by changing chamber air supply from N₂/O₂ (80% and 20%, respectively) to pure N₂. Unexpectedly, Hg emissions almost quadrupled after O₂ deprivation while oxidative mineralization (i.e., CO₂ emissions) was greatly reduced. This Hg flux response to anaerobic conditions was lacking when repeated with sterilized soils, possibly due to involvement of microbial reduction of Hg²⁺ by anaerobes or indirect abiotic effects such as alterations in soil redox conditions. This study provides experimental evidence that Hg volatilization, and possibly Hg²⁺ reduction, is related to O₂ availability in soils from two Sierra Nevada forests. If this result is confirmed in soils from other areas, the implication is that Hg volatilization from terrestrial soils is partially controlled by soil aeration and that low soil O₂ levels and possibly low soil redox potentials lead to increased Hg volatilization from soils.