Chemical Geology, Journal Year: 2024, Volume and Issue: unknown, P. 122577 - 122577
Published: Dec. 1, 2024
Language: Английский
Chemical Geology, Journal Year: 2024, Volume and Issue: unknown, P. 122577 - 122577
Published: Dec. 1, 2024
Language: Английский
Environmental Science & Technology, Journal Year: 2025, Volume and Issue: unknown
Published: Jan. 23, 2025
Charosphere, a highly active zone between biochar and surrounding soil, is widely present in agricultural wildfire-affected soils, yet whether reactive oxygen species (ROS) are produced within the charosphere remains unclear. Herein, production spatiotemporal evolution of ROS were explored. In situ capture visualized gradual decrease with increasing distance from biochar/soil interface. Temporally, O2•- H2O2 contents initially increased then declined incubation time, peaking at 3.04 5.40 μmol kg-1, respectively, while •OH content decreased continuously. High-throughput sequencing revealed that dissolved (DBC) facilitated by promoting growth bacteria electron-releasing capacity, such as Bacteroidetes, Acidobacteria, Actinobacteria, Chloroflexi. Additionally, adding electron transfer-weakened DBC significantly (ANOVA, P < 0.05), demonstrating also served shuttle electron-storing materials to promote accelerating transfer. This was further confirmed via fluorescence imaging, which visually showed stronger transfer ability near soil/biochar surface. Inhibition isotope experiments critical role CO2 emissions, primarily soil organic carbon. study highlights prevalent overlooked hotspot, advancing our understanding carbon turnover soils.
Language: Английский
Citations
1Wetlands Ecology and Management, Journal Year: 2025, Volume and Issue: 33(2)
Published: March 7, 2025
Language: Английский
Citations
1Critical Reviews in Environmental Science and Technology, Journal Year: 2025, Volume and Issue: unknown, P. 1 - 24
Published: March 14, 2025
Language: Английский
Citations
1Journal of Hazardous Materials, Journal Year: 2025, Volume and Issue: 492, P. 138207 - 138207
Published: April 9, 2025
Language: Английский
Citations
1Journal of Earth Science, Journal Year: 2025, Volume and Issue: unknown
Published: March 3, 2025
Language: Английский
Citations
0Environmental Science & Technology, Journal Year: 2025, Volume and Issue: unknown
Published: March 6, 2025
Detritusphere is a hotspot of carbon cycling in terrestrial ecosystems, yet the mineralization soil organic (SOC) within this microregion associated with reactive oxygen species (ROS) remains unclear. Herein, we investigated ROS production and distribution detritusphere six representative soils evaluated their contributions to SOC mineralization. We found that was significantly correlated several chemical biological factors, including pH, water-soluble phenols, water-extractable carbon, phenol oxidase activity, surface-bound or complexed Fe(II) low-crystalline minerals, highly crystalline Fe(II)-bearing SOC. These factors collectively contributed 99.6% variation production, as revealed by redundancy analyses. Among ROS, hydroxyl radicals (•OH) were key contributors mineralization, responsible for 10.4%-38.7% CO2 emissions quenching experiments. Inhibiting •OH decreased C-degrading enzyme activities, indicating stimulates increasing activity. Structural equation modeling further demonstrated promotes activities degrading phenols unlock "enzyme latch" availability upregulate gene expression. pathways equally exceeded its direct effect. findings provide detailed insight into mechanistic •OH-mediated dynamics detritusphere.
Language: Английский
Citations
0Critical Reviews in Environmental Science and Technology, Journal Year: 2025, Volume and Issue: unknown, P. 1 - 26
Published: April 26, 2025
Language: Английский
Citations
0Geoderma, Journal Year: 2025, Volume and Issue: 457, P. 117301 - 117301
Published: April 22, 2025
Language: Английский
Citations
0Environmental Science & Technology, Journal Year: 2025, Volume and Issue: unknown
Published: May 2, 2025
•OH-based oxidation plays a crucial role in dissolved organic matter (DOM) transformation and carbon flux, whereas quantifying the contribution of this pathway remains challenging. Here we combined concentration with isotope analysis DOM its generated CO2 to quantify oxidation. Results showed that 13C enrichment factors (ε values) were -8.1‰ -8.9‰ for benzene ring aromatic compounds, -4.2‰ -28.9‰ lower-molecular-weight acids, -13.0‰ from sediment. The fractionation sediment reflects average ε value humic substances acids. These values more negative than those photochemical microbial processes, enabling identification mechanisms. Using an end-member mix model, found proportion mineralization total emission ranged 20.9% 39.8% 100 g/L by 5-20 mM H2O2 under pH-neutral condition within 2 h was only 2% air same conditions. We also inorganic degassing contributed greatly during This study presents new isotope-based tool quantitatively assess DOM.
Language: Английский
Citations
0Water Research, Journal Year: 2025, Volume and Issue: 282, P. 123776 - 123776
Published: May 3, 2025
Language: Английский
Citations
0