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中国科学院大学学报 ›› 2017, Vol. 34 ›› Issue (4): 462-470.DOI: 10.7523/j.issn.2095-6134.2017.04.008

• “全球变化生态学”专栏 • 上一篇    下一篇

极端干旱对若尔盖高原泥炭地生态系统CO2通量的影响

张远1, 郝彦宾1, 崔丽娟2,3, 李伟2,3, 张骁栋2,3, 张曼胤2,3, 李林峰1, 杨思2,3, 康晓明2,3   

  1. 1. 中国科学院大学生命科学学院, 北京 100049;
    2. 中国林业科学研究院湿地研究所湿地生态功能与恢复北京市 重点实验室, 北京 100091;
    3. 四川若尔盖高寒湿地生态系统定位观测研究站, 四川 阿坝藏族自治州 624500
  • 收稿日期:2016-06-12 修回日期:2016-09-15 发布日期:2017-07-15
  • 通讯作者: 康晓明,E-mail:xmkang@ucas.ac.cn
  • 基金资助:
    中国林业科学研究院林业新技术研究所基本科研业务费专项(CAFINT2014K06)、国家重点研发计划项目(2016YFC0501804)、国家自然科学基金(31300417)和中央级公益性科研院所基本科研业务费专项(CAFYBB2014QB026)资助

Effects of extreme drought on CO2 fluxes of Zoige alpine peatland

ZHANG Yuan1, HAO Yanbin1, CUI Lijuan2,3, LI Wei2,3, ZHANG Xiaodong2,3, ZHANG Manyin2,3, LI Linfeng1, YANG Si2,3, KANG Xiaoming2,3   

  1. 1. College of Life Sciences, University of Chinese Academy of Sciences, Beijing 100049, China;
    2. Beijing Key Laboratory of Wetland Services and Restoration, Institute of Wetland Research, Chinese Academy of Forestry, Beijing 100091, China;
    3. Sichuan Zoige Wetland Ecosystem Research Station, Tibetan Autonomous Prefecture of Aba 624500, Sichuan, China
  • Received:2016-06-12 Revised:2016-09-15 Published:2017-07-15

摘要: 采用野外控制试验和静态箱法,研究极端干旱事件对若尔盖高原泥炭地净生态系统二氧化碳交换(net ecosystem CO2 exchange, NEE)、生态系统呼吸(ecosystem respiration, Re)和总初级生产力(gross primary productivity, GPP)的影响及其响应机制。研究结果表明:极端干旱显著降低若尔盖高原泥炭地生态系统的NEE、Re和GPP(P<0.05),导致生态系统固碳能力减弱,而温度(空气温度和土壤温度)和土壤含水量(SWC)是若尔盖高原泥炭地碳收支变化的主要驱动因子。在对照处理(CK)和极端干旱处理(D)中,NEE、Re和GPP与空气温度呈显著正相关关系(P<0.05),极端干旱减弱NEE、Re和GPP对空气温度变化的敏感性。表层土壤温度与NEE、Re和GPP的相关性高于深层土壤温度与NEE、Re和GPP的相关性。分析5 cm土壤温度与NEE和Re的相关关系。极端干旱减弱NEE对5 cm土壤温度的敏感性,增强Re对5 cm土壤温度的敏感性。若尔盖高原泥炭地生态系统NEE、Re和GPP与土壤含水量显著正相关(P<0.05),而极端干旱对土壤全碳、全氮和有机碳的含量无显著影响(P > 0.05)。

关键词: 极端干旱, 泥炭地, 碳通量, 温度, 土壤含水量

Abstract: To study the effects of extreme drought on net ecosystem CO2 exchange (NEE), ecosystem respiration (Re), and gross primary productivity (GPP) of Zoige alpine peatland, the carbon fluxes in both extreme drought treatment (D) and control treatment (CK) were monitored by using static enclosed chamber technique in a control platform of extreme climate event. The results showed that extreme drought significantly decreased NEE, Re, and GPP (P<0.05) of Zoige alpine peatland and hence reduced the carbon fixation capacity of targeted ecosystem. We also found that temperatures (air temperature (Ta) and soil temperature (Ts)) and soil water content (SWC) were the main driving factors of carbon budget dynamics in Zoige alpine peatland. NEE, Re, and GPP were significantly positively correlated with air temperature (P < 0.05), and their sensitivity to the Ta change was weakened by extreme drought. The correlations of NEE, Re, and GPP with topsoil temperature were much stronger than those with subsoil temperature. Besides, we found that extreme drought reduced the sensitivity of NEE to soil temperature at depth of 5 cm, but strengthened the sensitivity of Re. Furthermore, NEE, Re, and GPP were significantly positively correlated with soil water content (P<0.05). However, extreme drought had no significant effect on soil total carbon, nitrogen, and soil organic carbon contents (P>0.05).

Key words: extreme drought, peatland, carbon fluxes, temperature, soil water content

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