2025/03/28 by Yongqiang Zhou, Ting Zhang, Lei Zhou +9 · 1 voice
Environmental Science · Engineering · #Atmospheric and Environmental Gas Dynamics #Methane Hydrates and Related Phenomena #Hydrocarbon exploration and reservoir analysis
paper · doi:10.1021/acs.est.4c13190
openalex publication_date 2025/03/28 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/01
Reservoirs are hotspots for methane (CH 4 ) emissions. However, to date, the effects of terrestrial organic matter (OM) input and degradation on CH 4 emissions from large reservoirs remain largely unknown. From May 2020 to April 2021, we conducted monthly sampling campaigns at 100 sites in Lake Qiandao (580 km 2 ), a mega-reservoir in China, and made monthly vertical profile observations from March to September 2023. We estimated an annual mean F CH 4 flux of 0.26 g C m –2 yr –1 (1.51 × 10 8 g C yr –1 ). Elevated F CH 4 and enriched δ 13 C-CH 4 coincided with low dissolved oxygen (DO) concentrations, high levels of organic suspended solids, terrestrial organic matter, nutrients, depleted δ 18 O-H 2 O, and low carbon isotope fractionation (α C ) in the inflowing lake regions. Dissolved CH 4 ( c CH 4 ) correlated positively to the relative abundance of aliphatic compounds. Anoxic bioincubation experiments revealed rapid degradation of riverine organic matter, accompanied by a 56-fold increase in c CH 4, δ 13 C-CH 4 enrichment (to −32.25‰), and a significant decrease in α C to 1.02. These findings indicate that acetoclastic CH 4 production makes a substantial contribution to c CH 4 and thus F CH 4 . Based on multiple lines of evidence, we conclude that input of terrestrial organic matter and its subsequent degradation lead to DO depletion, and their OM degradation byproducts serve as carbon substrates that promote CH 4 emissions.