中国农业科技导报 ›› 2016, Vol. 18 ›› Issue (5): 141-147.DOI: 10.13304/j.nykjdb.2016.034

• 资源环境 生物药物 生物质转化 • 上一篇    下一篇

内蒙古农牧交错带油松人工林碳汇效应研究

郭月峰1,祁伟1,2,姚云峰1*,张美丽1,温健1,韩兆敏1,刘龙1,尉迟文思1   

  1. 1.内蒙古农业大学沙漠治理学院, 呼和浩特 010011; 2.内蒙古自治区水利水电勘测设计院, 呼和浩特 010020
  • 收稿日期:2016-01-18 出版日期:2016-10-15 发布日期:2016-04-24
  • 通讯作者: 姚云峰,教授,博士,主要从事水土保持研究。E-mail:18904718855@163.com
  • 作者简介:郭月峰,讲师,博士,主要从事水土保持与荒漠化防治研究。E-mail:guoyuefeng0525@126.com。
  • 基金资助:
    国家自然科学基金项目(31500584);内蒙古应用研究与开发计划项目(20110732);高等学校科学研究项目(NJZZ16055);内蒙古自然科学基金项目(2016MS0407)资助。

Carbon Sink Effect in Pinus tabulaeformis Afforestation  Species of the Agro-pasture Zigzag Zone in Inner Mongolia

GUO Yue-feng1, QI Wei1,2, YAO Yun-feng1*, ZHANG Mei-li1, WEN Jian1, HAN Zhao-min1, LIU Long1, YUCHI Wen-si1#br#   

  1. 1.Desert Science and Engineering College, Inner Mongolia Agricultural University, Hohhot 010011;
    2.Inner Mongolia Water Resources and Hydropower Survey and Design Institute, Hohhot 010020, China
  • Received:2016-01-18 Online:2016-10-15 Published:2016-04-24

摘要: 造林工程对生态环境的恢复发挥着重要的作用,对全球的碳素循环有重要影响。以内蒙古农牧交错带退牧还林的油松(Pinus tabulaeformis)人工林为研究目标,以未退牧的天然草地作为参考,分析了造林工程对生态系统中的碳储量以及碳循环造成的影响。结果表明:造林工程使植被碳库碳储量快速提高,且随着油松林龄的增长,土壤碳库呈现先降低后逐渐升高的动态变化,凋落物碳库与生态系统的碳库随着林龄的增长而呈缓慢增长的趋势;油松林木平均碳汇速率由大到小表现为:中龄林>近熟林>幼龄林>成熟林;以成熟林(43 a)为参照,油松林林分植被碳库固碳潜力为3 695.28 g/m2,生态系统固碳潜力为4 384.99 g/m2。研究结果表明,从长远来看,研究区进行退牧还油松人工林后,生态系统固碳效果是可观的碳汇。

关键词: 油松人工林, 碳汇效应, 内蒙古农牧交错带

Abstract: Afforestation project plays an important role in ecosystem restoration and exerts significant influence on global carbon cycle. This study took the Pinus tabulaeformis man-made forests in the agro-pasture zigzag zone of Inner Mongolia as research target, and natural grasslands as a referance; analyzed the effects of “conversion from grazing land to forest” on carbon stock and carbon cycle in the ecosystem. The results indicated that afforestation activities had led to rapid increase of vegetation carbon stock. Along with the prolonging of forest age, a dynamic change occurred in slowly increase of litter carbon stock and ecosystem carbon stock, while soil carbon stock firstly dropped and then gradually rose. The average carbon sink rates changed with forest age as following: medium age forest > near-mature forest > young forest > mature forest. With mature forest (43 a) as reference, the vegetation layer carbon sequestration potential (CSP) was 3 695.28 g/m2, while the P. tabulaeformis ecosystem CSP was 4 384.99 g/m2. These results indicated that after conversion from grazing land into forest in the study area, the P. tabulaeformis ecosystem was a considerable carbon sink in the long term.

Key words: Pinus tabulaeformis man-made forest, carbon sink effect, agro-pasture zigzag zone in Inner Mongolia