Contamination by mercury affects methane oxidation capacity of aerobic arable soils

Effects of long term Hg contamination and addition of Hg2 + on soil CH4 oxidation were investigated in laboratory incubation experiments. Non‐contaminated soils had CH4 oxidation rate constants (k) between 5.2 and 24.5 × 10− 3 h− 1, whereas Hg contaminated soils had rates ranging from 2.4 to 8.0 × 10− 3 h− 1. Specific oxidation rates (qK = k / Cbio), normalized with respect to soil microbial biomass C (Cbio), allowed the complete separation between the two groups and ranged between 32.6 and 56.2 × 10− 6 h− 1 μg− 1 Cbio in non‐contaminated soils and between 6.5 and 14.3 × 10− 6 h− 1 μg− 1 Cbio in long-term Hg contaminated soils. To test short-term toxicity effects and eventual adaptation of methane oxidizers, Hg2 + was added at two levels, 50 and 100 μg g− 1, to two soils, one non‐contaminated and the other contaminated for centuries by Hg, having about the same Cbio. Methane oxidation capacity and Cbio of the soil exposed for centuries to high levels of Hg, were not affected by Hg2 + additions. In the non‐contaminated soil Cbio was not affected, but methane oxidation rate decreased from 21.4 to 9.8 × 10− 3 h− 1. Our results show that Hg contamination, either long-term or short term, may negatively impair the CH4 oxidizing capacity of aerobic arable soils.

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► Long-term Hg contamination reduced CH4 oxidation in aerobic arable soils.
► Hg2+ addition up to 100 mg g–1 did not affect soil microbial biomass.
► Hg2+ addition to a non-contaminated soil significantly reduced CH4 oxidation.
► Hg2+ addition to a long-term Hg contaminated soil had no effect on CH4 oxidation.