Biochar is widely used due to its potential in direct or indirect soil carbon sequestration. However, there is a lack of comprehensive studies on the changes in the physicochemical properties of biochar after long-term application in different types of soils and the effects on CO emissions. In this study, paddy soil and fluvisol were selected as typical acidic and alkaline soils. Rice biochar (RB) and maize biochar (MB) were incorporated into paddy soil and fluvisol for one year, and characterizations (e.g., SEM-EDS, FTIR, 3D-EEM, and TG-DTG) of pristine and aged biochars were analyzed. Incubation experiments were conducted to assess the impact of aged biochar on CO emissions from paddy soil and fluvisol. Results indicated consistent trends in the physicochemical properties of biochar after one year of aging in both acidic and alkaline soils. Aged biochars exhibited significant structural degradation, increased specific surface area, and increased oxygen-containing functional groups. The DOM fluorescence intensity of biochar decreased and the thermal stability increased after aging. Compared to pristine biochar, aged biochar promoted soil carbon sequestration, resulting in varied reductions in cumulative CO emissions from paddy soil and fluvisol in the short term. Spearman's correlation coefficient analysis and PCA loading plot revealed that field-aged biochar primarily influenced CO emissions from soil and carbon sequestration by reducing biochar DOC release and bioavailability of DOM, while enhancing the humification of biochar DOM. These findings suggest that aged biochar favors soil carbon sequestration in the short term, both in acidic and alkaline soils.
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http://dx.doi.org/10.1016/j.jenvman.2024.122811 | DOI Listing |
Plant Cell Environ
January 2025
Dipartimento di Scienze della Vita, Università di Trieste, Trieste, Italia.
Drought impacts trees in varied temporal and spatial patterns, suggesting that heterogeneity of below-ground water stores influences the fate of trees under water stress. Karst ecosystems rely on shallow soil overlying bedrock that can store available water in primary pores. A contribution of rock moisture to tree water status has been previously demonstrated, but actual mechanisms and rates of rock-to-root water delivery remain unknown.
View Article and Find Full Text PDFGlob Chang Biol
January 2025
CAS Key Laboratory of Coastal Environmental Processes and Ecological Remediation, Yantai Institute of Coastal Zone Research (YIC), Chinese Academy of Sciences (CAS), Shandong Key Laboratory of Coastal Environmental Processes, YICCAS, Yantai, China.
Coastal wetlands contain very large carbon (C) stocks-termed as blue C-and their management has emerged as a promising nature-based solution for climate adaptation and mitigation. The interactions among sources, pools, and molecular compositions of soil organic C (SOC) within blue C ecosystems (BCEs) remain elusive. Here, we explore these interactions along an 18,000 km long coastal line of salt marshes, mangroves, and seagrasses in China.
View Article and Find Full Text PDFFEMS Microbiol Ecol
January 2025
Department of Forest Sciences, University of Helsinki, PO Box 27, 00014 Helsinki, Finland.
J Environ Qual
January 2025
Agricultural and Ecological Research Unit, Indian Statistical Institute, Giridih, Jharkhand, India.
Biodegradation
January 2025
Centre of Advanced Study in Marine Biology, Faculty of Marine Sciences, Annamalai University, Parangipettai, Tamilnadu, 608502, India.
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