Using mercury stable isotopes to quantify directional soil‒ atmosphere Hg(0) exchanges in rice paddy ecosystems: Implications for Hg(0) emissions to the atmosphere from land surfaces

Abstract

Gaseous elemental mercury (Hg(0)) emissions from soils constitute a large fraction of global total Hg(0) emissions. Existing studies do not distinguish biotic- and abiotic-mediated emissions and focus only on photoreduction mediated emissions, resulting in an underestimation of soil Hg(0) emissions into the atmosphere. In this study, directional mercury (Hg) reduction pathways in paddy soils were identified using Hg isotopes. Results showed significantly different isotopic compositions of Hg(0) between those produced from photoreduction (δ²⁰²Hg = −0.80 ± 0.67‰, Δ¹⁹⁹Hg = −0.38 ± 0.18‰), microbial reduction (δ²⁰²Hg = −2.18 ± 0.25‰, Δ¹⁹⁹Hg = 0.29 ± 0.38‰), and abiotic dark reduction (δ²⁰²Hg = −2.31 ± 0.25‰, Δ¹⁹⁹Hg = 0.50 ± 0.22‰). Hg(0) exchange fluxes between the atmosphere and the paddy soils were dominated by emissions, with the average flux ranging from 2.2 ± 5.7 to 16.8 ± 21.7 ng m⁻² h⁻¹ during different sampling periods. Using an isotopic signature-based, ternary mixing model, we revealed that photoreduction is the most important contributor to Hg(0) emissions from paddy soils. Albeit lower, microbial and abiotic dark reduction contributed up to 36 ± 22% and 25 ± 15%, respectively, to Hg(0) emissions on the 110th day. These novel findings can help improve future estimation of soil Hg(0) emissions from rice paddy ecosystems, which involve complex biotic-, abiotic-, and photo-reduction processes.