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Carbon storage in evergreen broad-leaf forests in mid-subtropical re-gion of China at four succession stages

机译:中国亚热带地区常绿阔叶林的四个演替阶段碳储量

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摘要

To better understand the effect of forest succession on carbon sequestration, we investigated carbon stock and allocation of evergreen broadleaf forest, a major zonal forest in subtropical China. We sought to quantify the carbon sequestration potential. We sampled four forest types, shrub (SR), pine (Pinus massoniana) forest (PF), pine and broadleaf mixed forest (MF) and evergreen broadleaf forest (BF). A regression equation was constructed using tree height and diameter at breast height (DBH) and elements of total tree biomass. The equation was subse-quently utilized to estimate tree carbon storage. The carbon storage of understory, litter, and soil was also estimated. Carbon storage in biomass increased significantly from the early succession stage SR (6.21 t⋅ha-1) to the late stage BF (134.87 t⋅ha-1). The biomass carbon stock of forest layers generally increased with succession except for the understory. The soil organic carbon storage for the total profile increased with forest succession, from 51.16 to 90.49 t⋅ha-1, but the contribution of SOC to the carbon stock of the forest ecosystem declined from 89.18% to 40.15%. The carbon stock at ecosystem scale increased significantly with succes-sion from SR (57.37 t⋅ha-1), to PF (154.20 t⋅ha-1), to MF (170.96 t⋅ha-1) and to BF (225.36 t⋅ha-1), with carbon stock of BF 3.93 times that of SR. The forests in our study have great potential for increasing carbon se-questration, and large areas of secondary or degraded evergreen broad-leaf forests in the subtropical zone of China could be a great carbon sink in future.
机译:为了更好地了解森林演替对固碳的影响,我们调查了常绿阔叶林的碳储量和分配,常绿阔叶林是中国亚热带的主要地带性森林。我们试图量化碳固存潜力。我们对四种森林类型进行了采样,分别是灌木(SR),松树(Pinus massoniana)森林(PF),松木和阔叶混交林(MF)和常绿阔叶林(BF)。使用树木的高度和胸高的直径(DBH)以及树木总生物量的元素来构建回归方程。随后,利用该方程式估算树木的碳储量。还估算了林下,垃圾和土壤的碳储量。生物质中的碳储量从SR的早期演替阶段(6.21 t·ha-1)到BF的晚期阶段(134.87 t·ha-1)显着增加。除林下层外,森林层的生物量碳储量通常随着演替而增加。土壤总有机碳储量随森林演替而增加,从51.16增加到90.49 t·ha-1,但是SOC对森林生态系统碳储量的贡献从89.18%下降到40.15%。随着SR(57.37t⋅ha-1),PF(154.20t⋅ha-1),MF(170.96t⋅ha-1)和BF(225.36 t)的成功,生态系统规模的碳库显着增加。 ⋅ha-1),高炉的碳储量为SR的3.93倍。我们研究的森林具有增加碳固存的巨大潜力,而中国亚热带地区的大片次生或退化的常绿阔叶林将来可能成为重要的碳汇。

著录项

  • 来源
    《林业研究(英文版)》 |2013年第4期|677-682|共6页
  • 作者单位

    Huitong Experimental Station of Forest Ecology, State Key Laboratory of Forest and Soil Ecology, Institute of Applied Ecology, Chinese Academy of Sciences, 72 Wenhua Rd, Shenyang 110016, P. R. China;

    Huitong Experimental Station of Forest Ecology, State Key Laboratory of Forest and Soil Ecology, Institute of Applied Ecology, Chinese Academy of Sciences, 72 Wenhua Rd, Shenyang 110016, P. R. China;

    Hunan Academy of Forestry, Hengshan Station of Forest Ecology, Changsha 410004, P. R. China;

    Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun 130012, P. R. China;

    Huitong Experimental Station of Forest Ecology, State Key Laboratory of Forest and Soil Ecology, Institute of Applied Ecology, Chinese Academy of Sciences, 72 Wenhua Rd, Shenyang 110016, P. R. China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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