何咏梅, 李伟, 杨丹荔, 等. 海螺沟冰川退缩区不同演替阶段植被碳贮量与分配格局[J]. 西南林业大学学报(自然科学), 2019, 39(5): 84–91 . DOI: 10.11929/j.swfu.201811044
引用本文: 何咏梅, 李伟, 杨丹荔, 等. 海螺沟冰川退缩区不同演替阶段植被碳贮量与分配格局[J]. 西南林业大学学报(自然科学), 2019, 39(5): 84–91 . DOI: 10.11929/j.swfu.201811044
Yongmei He, Wei Li, Danli Yang, Ji Luo. Vegetation Carbon Storage and Distribution Pattern in Different Succession Stages of Hailuogou Glacial Retreat[J]. Journal of Southwest Forestry University, 2019, 39(5): 84-91. DOI: 10.11929/j.swfu.201811044
Citation: Yongmei He, Wei Li, Danli Yang, Ji Luo. Vegetation Carbon Storage and Distribution Pattern in Different Succession Stages of Hailuogou Glacial Retreat[J]. Journal of Southwest Forestry University, 2019, 39(5): 84-91. DOI: 10.11929/j.swfu.201811044

海螺沟冰川退缩区不同演替阶段植被碳贮量与分配格局

Vegetation Carbon Storage and Distribution Pattern in Different Succession Stages of Hailuogou Glacial Retreat

  • 摘要: 在贡嘎山海螺沟冰川退缩区的植被演替序列典型地段依次设置8块样地,通过调查生物量,测定含碳率,计算碳贮量,分析演替过程不同阶段各个碳库变化过程,探索原生演替序列碳的动态变化。结果表明:原生演替序列8个样地的碳贮量分别为4.36、51.29、122.08、145.86、169.08、226.55、321.02、346.10 t/hm2,其中乔木层和土壤层碳贮量在整个演替序列上所占比例均超过85%。土壤所占比例随演替进行持续增加,由S1的21.20%增加到S8的41.86%;乔木所占比例则呈现先增加后减小的趋势,由S1的66.37%下降到S8的52.16%;其余各层在各个阶段所占比例较小。通过对海螺沟冰川退缩区植被演替序列各个阶段植被含碳率和碳贮量的测定,构建了原生演替不同阶段的碳分配和碳贮量格局,对研究原生演替过程中的碳循环以及植被恢复都有积极意义。

     

    Abstract: Eight sample plots were set in the glacier retreated area of Hailuogou. By investigating biomass, determining the carbon content, calculating carbon storage and analyzing the changes of carbon pools, the carbon dynamic changes of the primary succession sequence was explored. Results show that the carbon storage of 8 plots are 4.36, 51.29, 122.08, 145.86, 169.08, 226.55, 321.02, 346.10 t/hm2, respectively. Carbon storage in arbor and soil layers account for more than 85% of the whole succession sequence, in which the proportion of soil continue to increase from 21.20% of S1 to 41.86% of S8, while the proportion of arbor increases first and then decreases, from 66.37% of S1 to 52.16% of S8, the proportion of other layers in each stage is small. Through the determination of vegetation carbon content and carbon storage in each stage, the carbon distribution and carbon storage pattern of different stages of primary succession are constructed. This has positive implications for studying the carbon cycle and vegetation restoration in the process of primary succession.

     

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