生物炭
泥炭
温室气体
环境科学
碳纤维
木炭
甲烷
斜线和字符
废物管理
二氧化碳
环境化学
化学
热解
生态学
材料科学
工程类
复合材料
有机化学
复合数
生物
作者
Peduruhewa H. Jeewani,Robert W. Brown,Chris Evans,Jack Cook,Benjamin P. Roberts,M. D. Fraser,David R. Chadwick,Davey L. Jones
标识
DOI:10.1016/j.soilbio.2025.109814
摘要
Peat soils store significant amounts of carbon (C) globally, and increased C sequestration into peatlands could play a role in offsetting anthropogenic greenhouse gas (GHG) emissions. As such, there is a need to find and assess optimal greenhouse gas removal (GGR) interventions to minimise GHG losses, protect current C stocks, and promote further C sequestration. This mesocosm study assessed the additional C storage potential of different C-rich substrates (Juncus straw or Juncus-derived biochar) and/or FeSO4 amendments, with a low water table (LW; −15 cm) and high-water table (HW; 0 cm) in intact soil columns (20 cm diam. x 25 cm deep) extracted from degraded upland peat. GHG fluxes, soluble nutrients, changes in microbial community structure and enzyme activity were measured over a one-year period to evaluate the net C storage and their overall GGR potential. HW reduced CO2 emissions by 28 % compared to LW, while CH4 emissions increased, ultimately contributing 61 % of the overall CO2 equivalent (CO2eq) GHG emissions in HW cores with no amendments. Organic amendments had a significant effect on CO2 and CH4 emissions with the highest cumulative emissions being from the Straw-HW (26.2 t CO2eq ha−1 yr−1) and the lowest cumulative emissions being from the Biochar + FeSO4+HW (7.9 t CO2eq ha−1 yr−1). Biochar + FeSO4+HW led to the strongest net gain in soil C, suppressing decomposition of the native peat-C as well as CH4 emissions. The application of FeSO4 significantly reduced CO2eq GHG emissions by preventing methanogenesis through alternative electron acceptors. The Biochar + HW treatment suppressed Ascomycota abundance by 22 %. The combination of a high-water level, biochar addition and availability of alternative electron acceptors (e.g., FeSO4) can increase net C accumulation and GGR via both abiotic and biotic mechanisms, including i) increased C input, ii) modulation of soil microbiome to reduce peat turnover; and iii) suppression of CH4 and N2O emissions.
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