圈围对海岸带湿地土壤有机碳及其活性碳组分的影响
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1.华东师范大学/河口海岸学国家重点实验室/崇明生态研究院/蓝碳科学与技术研究中心;2.上海应用技术大学生态技术与工程学院;3.华东师范大学/

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The influence of enclosure history on the change of soil active organic carbon components in coastal wetland
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East China Normal University

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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碳汇功能的影响,本文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以及圈围历史<10年、圈围10—20年、圈围20—30年和圈围>30年的内陆湿地土壤理化因子、SOC含量及其活性组分溶解性有机碳(Dissolved Organic Carbon,DOC)、微生物生物量碳(Microbial Biomass Organic Carbon,MBC)、易氧化有机碳(Easily Oxidized Organic Carbon,EOC)的含量变化,活性有机碳分配比例和相关性,进而分析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,湿地土壤理化环境显著改变(P<0.05),土壤电导率(Electrical Conductivity,EC)、总氮(Total Nitrogen,TN)含量、黏粒百分比等理化因子均降低,且EC随着圈围年限的增加而逐渐降低,TN含量和黏粒百分比随着圈围年限的增加呈先下降再上升的趋势;(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于圈围30年后上升的趋势;(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(P<0.05),且随圈围年限的增加均呈先上升再下降的趋势,表明圈围后SOC稳定性先下降后随圈围年限的增加而上升;(4)SOC、DOC、MBC和EOC各有机碳组分之间呈显著正相关关系(P<0.05),土壤有机碳组分与土壤理化特征之间也具有显著相关性(P<0.05)。本研究结果有助于了解海岸圈围对海岸带生态系统固碳能力的影响,为陆海统筹下的海岸带湿地固碳增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 the influence of coastal perimeter, the physical and chemical environment of coastal wetland soil changes dramatically, which affects the SOC content and carbon sequestration function of wetland ecosystem. In order to reveal the influence of coastal perimeter and its history on the carbon sink function of coastal wetlands, this study focuses on the eastern coastal zone of Chongming Island in Shanghai. It compares changes in soil physical and chemical environment, organic carbon content, and active components such as Dissolved Organic Carbon (DOC), Microbial Biomass Organic Carbon (MBC), and Easily Oxidized Organic Carbon (EOC) in coastal wetlands affected by reclamation history of <10 years, 10—20 years, 20—30 years, and >30 years. The study also examines the allocation ratio and correlation of active organic carbon to analyze the impact of coastal enclosure and enclosure history on changes in SOC and its active components in coastal zone wetlands. Recommendations for the protection and management of coastal zone wetlands based on land-sea coordination are proposed. The results showed that: (1) After coastal reclamation, the soil physical and chemical environment of wetlands significantly changed (P<0.05), with decreases in soil Electrical Conductivity (EC), Total Nitrogen (TN) content, and clay. EC decreased gradually with the increase in reclamation years, while TN content and clay showed a trend of initially decreasing and then increasing with reclamation age. (2) SOC and DOC contents decreased after coastal reclamation, with a pattern of first decreasing and then increasing with reclamation years. MBC and EOC exhibited a trend of initial increase, subsequent decrease, and then increase after 30 years of reclamation. (3) The ratios MBC/SOC, DOC/SOC, and EOC/SOC in the coastal zone were significantly higher than those in the inland wetland (P<0.05), showing an initial increase and subsequent decrease with reclamation years, suggesting that SOC stability decreased initially after reclamation and then increased with time. (4) There was also a positive correlation (P<0.05) between SOC, DOC, MBC, and EOC, and significant correlations between organic carbon components and soil physicochemical characteristics. The findings contribute to understanding the impact of coastal enclosures on the carbon sequestration capacity of coastal ecosystems and provide a scientific basis for enhancing carbon sequestration and the function of coastal wetlands under integrated land and sea planning. The study also offers insights for the protection and management of China"s "double carbon" goal

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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其活性碳组分的影响 .生态学报,,(). http://dx. doi. org/[doi]

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