淇澳岛红树林分布格局变化及对地上碳储量和碳排放量的影响(2003—2023年)

Impacts of land use change on aboveground carbon storage and carbon emission in Qi’ao Island

  • 摘要: 在经济高速发展和人口迅速增长的推动下,滨海地区土地利用发生了显著变化,直接或间接影响生态系统碳循环及气候变化进程.作为滨海地区的碳汇代表之一,红树林具有巨大、可持续的固碳潜力,在缓解气候变化中具有重要地位.随着土地利用的变化,红树林的分布面积及树种组成均发生了显著变化,进而影响了其碳汇功能.因此,本文以中国红树植物种类最为丰富的淇澳岛为研究对象,结合样方调查和Landsat-5、Landsat-8、Landsat-9卫星遥感影像数据,分析了淇澳岛2002年至2023年土地利用动态演变规律,并利用碳排放核算方法,阐释了土地利用变化对该区域地上碳储量和碳排放量的影响.结果表明:1)2003—2023年间,淇澳岛养殖池面积由2003年的303.21 hm2逐步减少至2023年的140.31 hm2,呈下降趋势;而红树林面积则由196.11 hm2增加至645.75 hm2,反映出生态保护政策的有效实施及生态修复举措对生态系统的恢复具有积极作用,尤其是在红树林的保护和恢复方面.2)建设用地与非建设用地的碳动态展示了不同土地利用类型对碳平衡的不同贡献.3)遥感反演模型结果表明红树林区域固碳量由1379.59 t增长至97613.53 t,这不仅与红树林面积的扩大和林龄的增加有关,也得益于单位面积地上碳储量的提升.作为淇澳岛的主要碳汇,红树林的保护对于实现区域和国家的碳中和目标至关重要.该研究有助于进一步量化红树林修复对滨海区域固碳能力提升的贡献,并为滨海区域固碳潜力核算提供理论支撑.

     

    Abstract: Coastal areas have undergone substantial land use changes due to rapid economic development and population growth, directly or indirectly affecting the carbon cycle and climate change processes. As one of the primary carbon sinks in coastal areas, mangroves possess substantial and sustainable carbon sequestration potential and play an important role in mitigating climate change. However, mangroves have been notably impacted by the land use conversion, altering not only the composition and area of mangrove species but also the function of the ecosystems, thereby influencing their overall carbon sink capacity. This study focused on Qi’ao Island, known for its rich diversity of mangrove species in China. By integrating field investigations of mangrove species composition with Landsat-5, Landsat-8 and Landsat-9 satellite remote sensing imagery from 2002 to 2023, the study explored the dynamic evolution of land use patterns on Qi’ao Island. Using a carbon emission accounting method, the impact of land use change on aboveground carbon storage and emission was assessed. The results revealed that: (1) From 2003 to 2023, the area of aquaculture ponds on Qi’ao Island decreased from 303.21 hm2 in 2003 to 140.31 hm2 in 2023, indicating a decreasing trend. Conversely, the mangrove area increased from 196.11 hm2 to 645.75 hm2, demonstrating the positive effects of effective ecological protection policies and restoration measures, particularly in the preservation and restoration of mangroves. (2) The remote sensing inversion model showed that carbon sequestration in the mangrove area increased from 1,379.59 t to 97,613.53 t, which was attributed not only to the expansion of the mangrove area but also to an increase in aboveground carbon storage per unit area. (3) The carbon dynamics of construction land and non-construction land illustrated the different contributions of various land use types to the carbon balance. As the primary carbon sink on Qi’ao Island, the protection of mangroves is essential for achieving regional and national carbon neutrality goals. This study provides valuable insights into the role of mangrove restoration in enhancing carbon sequestration capacity in coastal areas and offers theoretical support for estimating the carbon sequestration potential of coastal ecosystems.

     

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