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生态学杂志 ›› 2026, Vol. 45 ›› Issue (7): 2185-2194.doi: 10.13292/j.1000-4890.202607.023

• 研究报告 • 上一篇    下一篇

1975—2020年浑善达克沙地天然沙地云杉林地上碳储量时空变化特征

夏建新4,宋立宁1,2,3*,陈振举4,孙一荣1,2,3,于栋阁5,王凯泽1,2,3,郑青山6,郑晓1,2,3   

  1. 1中国科学院沈阳应用生态研究所, 森林生态与保育重点实验室(中国科学院), 沈阳 110016; 2辽宁清原森林生态系统国家野外科学观测研究站, 沈阳 110016; 3辽宁省公益林经营管理重点实验室, 沈阳 110016; 4沈阳农业大学, 沈阳 110866; 5赤峰市气象局, 内蒙古赤峰 024000; 6内蒙古白音敖包国家级自然保护区管理局, 内蒙古赤峰 025300)
  • 出版日期:2026-07-10 发布日期:2026-07-10

The spatiotemporal variations of aboveground carbon storage of natural sandy Picea mongolica forests in the Hunshandake Sandy Land from 1975 to 2020.

XIA Jianxin4, SONG Lining1,2,3*, CHEN Zhenju4, SUN Yirong1,2,3, YU Dongge5, WANG Kaize1,2,3, ZHENG Qingshan6, ZHENG Xiao1,2,3   

  1. (1CAS Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 2Qingyuan Forest CERN, National Observation and Research Station, Liaoning Province, Shenyang 110016, China; 3Key Laboratory for Management of Non-commercial Forests, Liaoning Province, Shenyang 110016, China; 4Shenyang Agricultural University, Shenyang 110866, China; 5Chifeng Meteorological Bureau, Chifeng 024000, Inner Mongolia, China; 6Baiyinaobao National Nature Reserve Management Administration, Chifeng 025300, Inner Mongolia, China).

  • Online:2026-07-10 Published:2026-07-10

摘要: 利用1975、1981、1990、2000、2013和2020 Landsat TM/ETM+卫星遥感数据,结合实地调查和室内实验的方法,量化了不同时期浑善达克沙地东缘白音敖包国家自然保护区沙地云杉天然林面积,建立了生物量遥感估算模型,反演了不同时期沙地云杉天然林生物量,结合测定的沙地云杉天然林不同径级各器官(干、枝和叶)碳含量,明确了不同时期沙地云杉天然林的地上碳储量及时空变化特征。结果表明:(1)1975、1981、1990、2000、2013和2020年沙地云杉天然林的面积分别为1573.66、1684.31、1775.21、1937.16、1968.27和1999.69 hm2,表明沙地云杉天然林面积在过去45年间持续增长。空间分布上,沙地云杉天然林呈现“西多东少”的空间分布特征,95.1%沙地云杉分布在研究区西部。(2)沙地云杉天然林生物量遥感估算模型为:y=7.556(1/b5)2-6.9174(1/b5)-20.917(b5为近红外波段,R2=0.73)。不同时期沙地云杉生物量分别为7.53×104、7.82×104、8.36×104、9.17×104、9.70×104和10.14×104 t。(3)不同径级和器官碳含量介于501.10~545.09 g·kg-1,基于各器官生物量加权平均法得到单株沙地云杉地上部分平均碳含量为524.16 g·kg-1。1975、1981、1990、2000、2013和2020年沙地云杉天然林地上碳储量分别为3.92×104、4.07×104、4.35×104、4.77×104、5.06×104和5.27×104 t。45年间,沙地云杉天然林地上碳储量增加了1.35×104 t,增长率为34.4%,表明沙地云杉林在固碳增汇方面效果显著,同时也反映了区域内生态系统碳汇能力逐步增强。空间上,碳储量呈现显著异质性(2.14~181.94 t·hm-2),以中低碳储量等级(20~40 t·hm-2)为主,但高碳储量等级(≥40 t·hm-2)成熟林的面积随时间显著增加,表明区域碳积累正趋向稳定增长阶段。沙地云杉天然林面积扩张与碳储量增长显著提升了区域碳汇能力,其碳储量动态与空间分布特征为天然林保护和管理以及我国碳中和目标的实现提供基础和数据支撑。


关键词: 沙地云杉, 径级, 碳含量, 碳储量, 分配格局

Abstract: The area of natural Picea mongolica forests in Baiyinaobao National Nature Reserve, the eastern edge of Hunshandake Sandy Land, was quantified based on the Landsat TM/ETM+ satellite remote sensing data from 1975, 1981, 1990, 2000, 2013 and 2020 combined with field investigation and laboratory experiments. A remote sensing estimation model for biomass was established, and then the biomass and carbon of natural Picea mongolica forests across different periods were inverted. Combined with the measured carbon content of organs (stem, branch, and leaf) of trees with different diameter classes, aboveground carbon storage and its spatiotemporal variation in the natural Picea mongolica forests across different periods were clarified. The results showed that: (1) The area of natural Picea mongolica forest in 1975, 1981, 1990, 2000, 2013 and 2020 was 1573.66, 1684.31, 1775.21, 1937.16, 1968.27, and 1999.69 hm2, respectively, indicating that the area had continuously increased over the past 45 years. The natural Picea mongolica forest showed a spatial distribution pattern with more in the west and less in the east, with 95.1% being distributed in the western part of the study area. (2) The remote sensing estimation model for biomass of natural Picea mongolica forest is: y=7.556(1/b5)2-6.9174(1/b5)-20.917 (b5 is the near-infrared band, R2=0.73). The biomass of the natural Picea mongolica forest was 7.53×104, 7.82×104, 8.36×104, 9.17×104, 9.70×104 and 10.14×104 t in  1975, 1981, 1990, 2000, 2013 and 2020, respectively. (3) The carbon content of different diameter classes and organs ranged from 501.10 g·kg-1 to 545.09 g·kg-1. The average carbon content of the aboveground part of Picea mongolica tree was 524.16 g·kg-1 based on the weighted average method of the biomass of each organ. The carbon storage of natural Picea mongolica forest in 1975, 1981, 1990, 2000, 2013 and 2020 was 3.92×104, 4.07×104, 4.35×104, 4.77×104, 5.06×104 and 5.27×104 t, respectively. During 1975-2020, aboveground carbon storage of natural Picea mongolica forest increased by 1.35×104 t, with a growth rate of 34.4%, indicating that Picea mongolica forest had a significant effect on carbon sequestration and sink enhancement, and also reflecting the gradual improvement of carbon sink capacity in the region. Spatially, the carbon storage showed significant heterogeneity (2.14-181.94 t·hm-2), with the medium and low carbon storage grades (20-40 t·hm-2) being the main ones (with the largest proportion), but the area of mature forests with high carbon storage grades (≥40 t·hm-2) increased significantly over time, indicating that the regional carbon accumulation was tending towards a stable growth stage. The area expansion of natural Picea mongolica forest and the increases in carbon storage have significantly enhanced the regional carbon sink capacity. The dynamics and spatial distribution characteristics of its carbon storage provide a scientific basis and data support for the protection and management of natural forests as well as for the achievement of China’s carbon neutrality goals.


Key words: Picea mongolica, diameter class, carbon content, carbon storage, allocation pattern