大气氧化沉降过氧化氢对湿地土壤有机碳转化和温室气体排放的影响
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1.华南农业大学;2.中国21世纪议程管理中心

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国家自然科学基金资助项目(42177396)


The impact of atmospheric oxidative deposition of hydrogen peroxide on organic carbon transformation and greenhouse gas emissions in mangrove wetland soils
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1.Guangdong Laboratory for Lingnan Modern Agriculture,Guangdong ProvincialKey Laboratory of Agricultural Rural Pollution Abatement and Environmental Safety,College of Natural Resources and Environment,South China Agricultural University;2.Administrative Center for China&3.amp;4.#39;5.&6.s Agenda

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    摘要:

    过氧化氢(H2O2)作为自然大气湿沉降的主要氧化性物质,输入湿地系统后会发生原位Fenton反应,其产生的强氧化自由基对湿地“碳汇”功能影响却较少受到关注。本研究利用室内模拟实验,探究了自然大气氧化性沉降过氧化氢输入对碳含量差异湿地土壤有机碳转化和温室气体排放的影响,揭示其引发的原位Fenton反应对湿地“碳汇”功能的潜在影响。结果表明,外源H2O2的输入显著促进了湿地土壤有机碳的转化降解,土壤颗粒有机碳(POC)、易氧化有机碳(EOC)和可溶性有机碳(DOC)含量显著降低(p<0.05),尤其在湿地土壤碳含量较高时效果更显著。与此同时,通过连续3个月的温室气体监测发现,自然H2O2沉降处理组中显著促进了湿地系统中CH4、N2O累积排放总量(p<0.05),而CO2累积排放总量略有上升,但差异不显著(p>0.05)。这表明自然大气氧化性沉降H2O2的输入不仅促进湿地土壤有机碳的分解,还导致了温室气体的释放,特别是CH4和N2O的增加。总体而言,自然大气氧化沉降H2O2的输入对湿地土壤中有机碳的分解起到催化作用,增加了土壤中碳循环的速率,对湿地生态系统的碳动态产生了影响。这一过程的理解有助于更全面地把握湿地土壤碳循环的机制,对于湿地生态系统的管理和保护具有重要的科学意义。

    Abstract:

    Hydrogen peroxide (H2O2), as the primary oxidative substance in natural atmospheric wet deposition, undergoes in situ Fenton reactions upon introduction into wetland systems. The impact of the resulting generation of powerful oxidative free radicals on the "carbon sink" function of wetlands has been relatively understudied. In this research, indoor simulated experiments were conducted to explore the influence of inputting natural oxidative precipitation of hydrogen peroxide on soil organic carbon transformation and greenhouse gas emissions in wetlands. The study aimed to reveal the potential effects of in situ Fenton reactions triggered by hydrogen peroxide on the "carbon sink" function of wetlands. The results indicated that the external input of H2O2 significantly promoted the transformation and degradation of soil organic carbon in wetlands. The content of particulate organic carbon (POC), easily oxidizable organic carbon (EOC), and soluble organic carbon (DOC) in the H2O2-treated group decreased significantly (p <0.05), particularly in wetland soils with higher carbon content. Meanwhile, continuous greenhouse gas monitoring over three months revealed that the natural H2O2 deposition treatment significantly enhanced the cumulative emissions of CH4 and N2O in the wetland system (p<0.05), while the cumulative emission of CO2 was slightly higher than that of the control group but not statistically significant (p>0.05). This suggests that the input of natural oxidative precipitation of H2O2 not only plays a promoting role in the transformation of soil organic carbon in wetlands but also triggers the release of greenhouse gases, especially with a more significant increase in CH4 and N2O. This process accelerates the decomposition of organic carbon, ultimately producing low-molecular-weight compounds and gas products such as CO2 and CH4. In summary, the input of hydrogen peroxide from natural atmospheric oxidative deposition catalyzes the decomposition of organic carbon in wetland soils, increasing the rate of carbon cycling in the soil and influencing the carbon dynamics of wetland ecosystems. Understanding this process contributes to a more comprehensive understanding of the mechanisms of soil carbon cycling in wetlands, with significant scientific implications for the management and conservation of wetland ecosystems.

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秦俊豪,王希,范凯青,王运基,何霄嘉.大气氧化沉降过氧化氢对湿地土壤有机碳转化和温室气体排放的影响.生态学报,,(). http://dx. doi. org/[doi]

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