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应用生态学报 ›› 2025, Vol. 36 ›› Issue (4): 1159-1170.doi: 10.13287/j.1001-9332.202504.024

• 研究论文 • 上一篇    下一篇

内蒙古呼伦湖流域生态系统碳储量时空变化与未来情景模拟

王琪1,3, 单楠2,3, 李楠楠1,3, 张兆勇1,3, 李泉1,3, 刁锐4, 王文林2,3, 曲玉冰2,3*   

  1. 1呼伦贝尔市北方寒冷干旱地区内陆湖泊研究院, 内蒙古呼伦贝尔 021000;
    2生态环境部南京环境科学研究所, 南京 210042;
    3生态质量综合监测站内蒙古呼伦湖站(湿地), 内蒙古呼伦贝尔 021000;
    4乌兰浩特生态环境监测站, 内蒙古兴安盟 137400
  • 收稿日期:2024-10-13 接受日期:2025-02-11 出版日期:2025-04-18 发布日期:2025-10-18
  • 通讯作者: *E-mail: Yubing_Qu@163.com
  • 作者简介:王 琪, 女, 1992年生, 硕士研究生。主要从事野生动植物保护和生态环境科学研究。E-mail: wang-qi907291797@163.com
  • 基金资助:
    呼伦湖保护区科学技术研究能力加强关键技术研究项目委托课题Ⅲ期(HSZCS-C-F-230005)和呼伦湖生态安全调查评估项目(2021—2025)

Spatiotemporal variation and future scenario simulation of ecosystem carbon storage in the Hulun Lake Basin, Inner Mongolia, China

WANG Qi1,3, SHAN Nan2,3, LI Nannan1,3, ZHANG Zhaoyong1,3, LI Quan1,3, DIAO Rui4, WANG Wenlin2,3, QU Yubing2,3*   

  1. 1Hulunbuir Inland Lake Research Institute of Northern Cold and Arid Areas, Hulunbuir 021000, Inner Mongolia, China;
    2Nanjing Institute of Environmental Sciences, Ministry of Ecology and Environment, Nanjing 210042, China;
    3Inner Mongolia Hulun Lake (Wetland) Comprehensive Moni-toring Station for Ecological Quality, Hulunbuir 021000, Inner Mongolia, China;
    4Ulanhot Ecological Environment Monitoring Station, Xing'an League 137400, Inner Mongolia, China
  • Received:2024-10-13 Accepted:2025-02-11 Online:2025-04-18 Published:2025-10-18

摘要: 陆地生态系统中的碳储存在气候变化和全球碳循环中发挥着关键作用。为了探究呼伦湖流域生态系统碳储量的时空变化,本研究将InVEST模型和PLUS模型相结合,系统分析1990—2020年土地利用变化对碳储量的影响,模拟预测2030年不同情景下的土地利用布局和碳储量空间格局。结果表明: 1990—2020年,呼伦湖流域土地利用空间分布发生显著变化,耕地、林地、裸地和建设用地面积增加,草地、水域和湿地面积减少。呼伦湖流域碳储量增加了1.48×107 t,增幅为1.0%。其中,林地和耕地的碳储量分别增加7.18×107和6.7×106 t,草地、水域和湿地的碳储量分别降低6.01×107、1.8×106和1.7×106 t。流域碳储量呈现明显的空间异质性特征,高值主要集中于流域东部山地丘陵区,低值主要分布于流域东北部和呼伦湖及其周边区域,其空间分异与土地利用格局呈高度耦合关系。2030年,呼伦湖流域在自然发展、城镇发展、耕地保护和生态保护情景下的碳储量均呈增加趋势。其中,生态保护情景下的增长最显著,增加6.19×106 t,增幅为0.4%。研究结果可为呼伦湖流域土地利用格局优化和碳储存能力提升提供重要参考。

关键词: 呼伦湖流域, PLUS模型, InVEST模型, 碳储量, 多情景模拟

Abstract: Carbon storage in terrestrial ecosystems plays a crucial role in climate change and the global carbon cycle. To investigate the spatiotemporal variations of carbon storage in the Hulun Lake Basin, we combined the InVEST and PLUS models to systematically analyze the impacts of land use changes from 1990 to 2020 on carbon storage, and simulate land use patterns and spatial distribution of carbon storage under different scenarios for 2030. The results indicated that the Hulun Lake Basin experienced significant changes in land use distribution during 1990-2020. The area of cultivated land, forest, bare land, and built-up land increased, while the area of grassland, water, and wetlands decreased. Total carbon storage in the basin increased by 1.48×107 t, with a growth rate of 1.0%. Carbon storage in forest and cultivated land increased by 7.18×107 and 6.7×106 t, while that in grassland, water, and wetlands decreased by 6.01×107, 1.8×106, and 1.7×106 t, respectively. Carbon storage in the basin exhibited significant spatial heterogeneity, with higher carbon storage areas mainly distributed in the eastern hilly areas of the basin and lower carbon storage areas mainly located in the northeastern part of the basin and around Hulun Lake. The spatial differentiation showed a strong coupling relationship with land use patterns. Under the four scenarios for 2030, including natural development, urban development, cropland protection, and ecological conservation,carbon storage in the Hulun Lake Basin showed an increasing trend, with the ecological conservation scena-rio demonstrating the most significant growth of 6.19×106 t and a growth rate of 0.4%. Our findings would provide important references for optimizing land use pattern and enhancing carbon storage capacity in the Hulun Lake Basin.

Key words: the Hulun Lake Basin, PLUS model, InVEST model, carbon storage, multi-scenario simulation