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应用生态学报 ›› 2025, Vol. 36 ›› Issue (11): 3501-3511.doi: 10.13287/j.1001-9332.202511.010

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洞庭湖流域陆地生态系统碳汇研究现状及展望

陈名1, 李忠武1*, 聂小东1, 王诗兰1, 冉凤维2, 陈玥1   

  1. 1湖南师范大学地理科学学院, 洞庭湖流域生态环境变化与固碳增汇湖南省重点实验室, 长沙 410081;
    2长沙理工大学水利与海洋工程学院, 长沙 410114
  • 收稿日期:2025-09-01 接受日期:2025-09-30 出版日期:2025-11-18 发布日期:2026-06-18
  • 通讯作者: * E-mail: lzw17002@hunnu.edu.cn
  • 作者简介:陈 名, 男, 1999年生, 博士研究生。主要从事区域生态环境变化与碳循环研究。E-mail: chenmingy@hunnu.edu.cn
  • 基金资助:
    国家自然科学基金项目(42277335)和湖南省自然科学基金项目(2023JJ20030,2025JJ60248)

Current status and prospects of terrestrial ecosystem carbon sink in the Dongting Lake Basin, China

CHEN Ming1, LI Zhongwu1*, NIE Xiaodong1, WANG Shilan1, RAN Fengwei2, CHEN Yue1   

  1. 1Hunan Provincial Key Laboratory for Eco-environmental Changes and Carbon Sequestration of the Dongting Lake Basin, School of Geographical Sciences, Hunan Normal University, Changsha 410081, China;
    2School of Hydraulic and Ocean Engineering, Changsha University of Science & Technology, Changsha 410114, China
  • Received:2025-09-01 Accepted:2025-09-30 Online:2025-11-18 Published:2026-06-18

摘要: 陆地生态系统固碳增汇被认为是抵消全球碳排放、减缓气候变化最有效的措施之一。与区域陆地生态系统相比,流域陆地生态系统通常具有更为复杂的水文过程、高强度的人类活动干扰以及独立完整的生态系统。作为我国最典型的流域陆地生态系统之一,洞庭湖流域陆地生态系统碳汇的不稳定性高,同时碳汇潜力巨大。本文围绕洞庭湖流域陆地生态系统碳汇的时空格局、碳储量、增汇潜力及其固碳稳定性等方面,综述了其研究现状并提出未来研究展望。目前,该流域陆地生态系统碳汇的计量与监测主要依赖传统模型,存在验证标准不统一、精度较低以及忽视人为干扰等局限性;数据来源多限于土地利用与遥感影像数据,普遍存在分辨率不足、数据更新不及时等问题,导致碳汇计量结果差异很大。总体上,森林生态系统是流域内最主要的碳汇贡献者,而农田和湿地生态系统则呈现出较大的增汇潜力。未来研究应重点关注流域内复杂的水文情势和区域特色,开发耦合流域水文过程与生物地球化学循环过程的碳循环模型,系统评估和量化流域内人类活动对生态系统碳汇的影响机制,以更准确评估洞庭湖流域陆地生态系统的碳汇功能、增汇潜力及其多尺度驱动机制,为我国“双碳”目标的实现提供科学支撑。

关键词: 陆地生态系统, 碳汇估算, 碳储量, 增汇潜力, 洞庭湖流域

Abstract: The enhancement of carbon sequestration in terrestrial ecosystems is regarded as one of the most effective measures for mitigating global carbon emissions and climate change. Compared to that at the local scale, watershed terrestrial ecosystems at the watershed scale typically exhibit the characteristics of more complex hydrological processes, intense anthropogenic disturbance, independence and intact. The Dongting Lake basin, as one of the most representative watershed in China, exhibits low carbon sink stability but significant carbon sequestration potential. We reviewed current research on the spatiotemporal patterns, carbon storage, sequestration potential, and carbon storage stability along the Dongting Lake basin, and proposed future research prospects. Currently, the mea-surement and monitoring of terrestrial ecosystem carbon sinks primarily rely on conventional models, with the limitations of inconsistent validation standards, relatively low precision, and neglecting anthropogenic disturbances. Data sources are predominantly confined to land use and remote sensing imagery, which often suffer from insufficient spatial resolution and untimely updates, leading to considerable uncertainties in carbon sink estimation. Overall, forest ecosystems are the primary contributors to carbon sequestration across the basin, while farmland and wetland ecosystems exhibit substantial carbon sequestration potential. Further attention should also be directed toward the complex hydrological conditions and regional characteristics. There is a critical need to develop carbon cycle models that couple watershed hydrological processes with biogeochemical cycles. Additionally, we require a systematic assessment and quantification of the mechanisms underlying the influences of human activities on ecosystem carbon sequestration. Such efforts are essential for more accurately evaluating the carbon sequestration function, potential, and multi-scale drivers of the terrestrial ecosystem in the Dongting Lake basin, thereby offering scientific support for achieving China's “Dual Carbon” goals.

Key words: terrestrial ecosystem, carbon sink estimation, carbon storage, carbon sink potential, Dongting Lake Basin