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生态学杂志 ›› 2024, Vol. 43 ›› Issue (11): 3433-3442.doi: 10.13292/j.1000-4890.202411.006

• 研究报告 • 上一篇    下一篇

江苏滨海盐沼湿地碳动态时空差异及其对气候变化的响应

万安娜1,韩其飞1,2*,李超凡1,王文彪3,崔正南3


  

  1. 1南京信息工程大学地理科学学院, 南京 210044; 2南京信息工程大学气象灾害预报预警与评估协同创新中心, 南京 210044; 3亿利资源集团有限公司, 北京 100020)

  • 出版日期:2024-11-10 发布日期:2024-11-12

Spatial-temporal variations of carbon dynamics and their responses to climate change in Jiangsu coastal salt marshes.

WAN Anna1, HAN Qifei1,2*, LI Chaofan1, WANG Wenbiao3, CUI Zhengnan3   

  1. (1School of Geographical Sciences, Nanjing University of Information Science & Technology, Nanjing 210044, China; 2Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology, Nanjing 210044, China; 3Elion Resources Group Co., Ltd, Beijing 100020, China).

  • Online:2024-11-10 Published:2024-11-12

摘要: 滨海盐沼湿地是重要的蓝色碳汇,同时也是气候变化的敏感区,评估滨海盐沼湿地的碳汇能力及对气候变化的响应,对我国制定增汇减排政策,实现“双碳”目标具有重要意义。本研究利用DNDC(Denitrification-Decomposition)模型模拟江苏省不同地区滨海盐沼湿地碳动态的时空变化,探讨芦苇、碱蓬和互花米草3种典型盐沼湿地对长期气候变化的响应。结果表明:1981—2020年江苏滨海盐沼湿地的碳汇总量为9.70 Tg C,总的全球增温潜势(global warming potential, GWP)为-19.24 Tg CO2eq,其中射阳的碳汇总量与对增温的负效应最大;在空间分布上,江苏南部的碳汇能力和GWP大于北部;不同盐沼湿地之间差异明显,碳汇能力从大到小依次是互花米草湿地、芦苇湿地和碱蓬湿地,GWP则表现为芦苇湿地<互花米草湿地<碱蓬湿地;在年际变化上,1981—2020年江苏各地3种盐沼湿地的净初级生产力与GWP均呈增加趋势,碳汇能力年际差异较大,但总体变化趋势不明显;气温升高,碱蓬和互花米草的净初级生产力增加,芦苇净初级生产力减小,CH4和N2O排放量的变化明显大于净初级生产力,除各地芦苇湿地N2O排放量表现出不同特征外,CH4和N2O排放量均有大幅增加;降雨与芦苇湿地和互花米草湿地的净初级生产力和CH4排放量呈正相关,碱蓬湿地则相反,降雨与三种盐沼湿地N2O排放量均呈正相关。


关键词: 盐沼湿地, 滨海蓝色碳汇, 碳动态, 气候变化, DNDC模型

Abstract: Coastal salt marshes are important blue carbon sink, which are sensitive to climate change. Assessing the carbon sink capacity of coastal salt marshes and their response to climate change is of great significance for China to achieving the carbon peaking and carbon neutrality goals. In this study, the DNDC (Denitrification-Decomposition) model was utilized to simulate the temporal and spatial variations of carbon sink in coastal salt marshes in different regions of Jiangsu Province, and to explore the responses of three typical salt marshes dominated by Phragmites australis, Suaeda salsa and Spartina alterniflora to long-term climate change. From 1981 to 2020, the total carbon sink of Jiangsu coastal salt marshes was 9.70 Tg C, and the total global warming potential (GWP) was -19.24 Tg CO2-eq, with the largest total carbon sink and the negative effect on warming of Sheyang. Spatially, the carbon sink capacity and GWP in southern Jiangsu were greater than those in the north, and varied among the three types of salt marshes. The carbon sink capacity was in a descending order of Spartina alterniflora, Phragmites australis, and Suaeda salsa, while GWP followed an order of Phragmites australis < Spartina alterniflora < Suaeda salsa. In terms of interannual variation, net primary productivity (NPP) and GWP of the three salt marshes in various sites showed an increasing trend from 1981 to 2020. The carbon sink capacity varied greatly across different years, but the changing trend was not obvious on the whole. With the increase of temperature, NPP of Suaeda salsa and Spartina alterniflora increased, while that of Phragmites australis decreased. The changes in CH4 and N2O emissions were significantly greater than those of NPP. CH4 and N2O emissions increased significantly except for the different trends of N2O emissions in Phragmites australis in different regions. Rainfall was positively correlated with NPP and CH4 emissions in Phragmites australis and Spartina alterniflora, while Suaeda salsa showed an opposite pattern. Rainfall was positively correlated with N2O emissions in three salt marshes.


Key words: salt marsh, coastal blue carbon, carbon dynamics, climate change, DNDC model