圈围对海岸带湿地土壤有机碳及活性碳组分的影响
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国家重点研发计划资助(2023YFC3208500);国家自然科学基金(42141016,U2243207);上海市科委项目(22DZ1202700)


The influence of enclosure history on the change of soil active organic carbon components in coastal wetland
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    摘要:

    受海岸圈围的影响,海岸带湿地土壤理化环境发生剧烈改变,进而影响湿地生态系统土壤有机碳(Soil Organic Carbon,SOC)含量及其固碳功能。为了揭示海岸圈围及圈围历史对海岸带湿地土壤有机碳的影响,以上海崇明岛东部海岸带区域为典型研究区,比较了海岸带区域受潮汐影响的滨海湿地及不同圈围历史内陆湿地土壤理化因子、SOC含量及溶解性有机碳(Dissolved Organic Carbon,DOC)、微生物生物量碳(Microbial Biomass Carbon,MBC)、易氧化有机碳(Easily Oxidized Organic Carbon,EOC)的含量变化,分析了海岸圈围及圈围历史对海岸带湿地SOC及其活性组分变化的影响规律,并提出基于陆海统筹的海岸带湿地保护与管理建议。研究结果显示:(1)海岸圈围后,土壤电导率(Electrical Conductivity,EC)、总氮(Total Nitrogen,TN)含量、黏粒等理化因子均降低,随着圈围年限的增加,EC逐渐降低,而TN含量和黏粒则先下降再上升;(2)海岸圈围后,湿地SOC、DOC含量降低,且随圈围年限增加呈先下降再上升的趋势,MBC和EOC随圈围年限增加呈先上升后下降再上升的趋势,SOC、DOC、MBC和EOC之间呈显著正相关关系;(3)海岸带内陆湿地土壤的MBC/SOC、DOC/SOC和EOC/SOC均显著高于滨海湿地,且随圈围年限的增加均呈先上升再下降的趋势。研究结果有助于了解圈围对海岸带生态系统土壤有机碳的影响,为陆海统筹下的海岸带湿地碳汇功能提升和保护管理提供科学依据,服务我国的"双碳"目标。

    Abstract:

    Under coastal reclamation, the physicochemical environment of wetland soil in the coastal zone experiences significant alterations, impacting the soil organic carbon (SOC) content and the carbon sequestration capacity of the wetland ecosystem. In order to reveal the influence of coastal reclamation and its history on the carbon sink function of coastal wetlands, this study focuses on the eastern coastal zone of Chongming Island in Shanghai as a representative research area. This study compares changes in soil physicochemical factors, SOC contents, Dissolved Organic Carbon (DOC), Microbial Biomass Carbon (MBC), and Easily Oxidized Organic Carbon (EOC) are analyzed to understand how coastal perimeter and its history influence SOC and active carbon components in coastal wetlands. Based on these findings, suggestions for protecting and managing coastal wetlands through coordinated land-sea approaches are proposed. The results showed that: (1) After coastal reclamation, the soil Electrical Conductivity (EC), Total Nitrogen (TN) content, clay decreased, with EC progressively lowering as reclamation duration increased, while TN content and clay first decreased and then increased. (2) After coastal reclamation, the contents of SOC and DOC initially declined and subsequently exhibited an increasing trend as the years since reclamation progressed, while MBC and EOC initially surged post-reclamation, then decreased, and eventually increased with the passage of fencing years, correlating positively and significantly among SOC, DOC, MBC, and EOC.(3) The ratios MBC/SOC, DOC/SOC, and EOC/SOC in the coastal zone were significantly higher than those in the inland wetland, showing an initial increase and subsequent decrease with reclamation years, suggesting that SOC stability decreased initially after reclamation and then improved over time. The findings of this study are valuable for comprehending the impact of enclosure on soil organic carbon in coastal ecosystems, and provide a scientific foundation for enhancing the carbon sink function and implementing effective management strategies for coastal wetland protection under integrated land-sea planning. This aligns with China's objective of achieving "double carbon" goals.

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刘君恬,邹维娜,袁琳,王栋,王崚力,褚向乾.圈围对海岸带湿地土壤有机碳及活性碳组分的影响.生态学报,2025,45(9):4213~4222

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