Deep-water pressure boosts reservoir carbon sequestration through microbial modulation
Biochar Editorial Office, Shenyang Agricultural UniversityThe global push for carbon neutrality necessitates a comprehensive understanding of natural carbon sinks, particularly within aquatic ecosystems such as lakes and reservoirs. These environments play a dual role, acting as both sources and sinks of carbon, with their sediment–water interface being a critical zone for carbon transformation and storage. A recent investigation addresses a longstanding question: how precisely does varying hydrostatic pressure, stemming from water level fluctuations in deep-water reservoirs, influence the microbially mediated processes central to carbon cycling and sequestration?
To unravel these complex dynamics, researchers conducted a meticulous microcosm simulation using sediment and water sourced from the Jinpen Reservoir in Shaanxi Province, China. This experimental setup rigorously simulated four distinct hydrostatic pressure levels, ranging from atmospheric pressure (0.1 MPa) to higher pressures (0.2 MPa, 0.5 MPa, and 0.7 MPa), corresponding to varying water depths. The team then employed advanced metagenomics and metabolomics techniques to comprehensively analyze changes in microbial community structure, the abundance of specific functional genes, and the activity of metabolic pathways associated with carbon cycling.
- Journal
- Carbon Research
- Funder
- Science Fund for Distinguished Young Scholars of Hebei Province, National Natural Science Foundation of China, Natural Science Foundation of Hebei Province