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中国沙漠 ›› 2016, Vol. 36 ›› Issue (3): 726-733.DOI: 10.7522/j.issn.1000-694X.2015.00037

• 生物与土壤 • 上一篇    下一篇

古尔班通古特沙漠南缘梭梭(Haloxylon ammodendron)群落土壤呼吸对生态系统呼吸的贡献

杨洁1,2, 刘冉1, 马杰1, 唐立松1, 李彦1   

  1. 1. 中国科学院新疆生态与地理研究所 荒漠与绿洲国家重点实验室/阜康荒漠生态系统国家站, 新疆 乌鲁木齐 830011;
    2. 中国科学院大学, 北京 100049
  • 收稿日期:2015-01-08 修回日期:2015-03-04 出版日期:2016-05-20 发布日期:2016-05-20
  • 通讯作者: 唐立松(E-mail:tangls@ms.xjb.ac.cn)
  • 作者简介:杨洁(1990-),女,河南人,硕士研究生,主要从事干旱区CO2通量及碳循环的研究。E-mail:yangjie_com@126.com
  • 基金资助:

    国家自然科学基金项目(41301279,41201041,41171049);"西部之光"西部博士项目(XBBS201204)

The Contribution of Soil Respiration to Ecosystem Respiration of Haloxylon ammodendron Community in the South of Gurbantunggut Desert

Yang Jie1,2, Liu Ran1, Ma Jie1, Tang Lisong1, Li Yan1   

  1. 1. State Key Laboratory of Desert and Oasis Ecology/Fukang Station of Desert Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2015-01-08 Revised:2015-03-04 Online:2016-05-20 Published:2016-05-20

摘要:

土壤呼吸作为生态系统呼吸的主要贡献者,其贡献率往往超过50%,而干旱区土壤呼吸与生态系统呼吸的比值在季节上的变化尚不明确。利用涡度相关技术与多通道土壤呼吸观测技术,对古尔班通古特沙漠南缘的梭梭(Haloxylon ammodendron)群落生长季CO2通量进行连续观测,探讨了土壤呼吸对生态系统呼吸的贡献及其在生长季变化特征。结果表明:(1)在整个生长季,生态系统呼吸呈单峰式变化,峰值出现在7月,为0.75 g·m-2·d-1;最小值出现在3月,为0.09 g·m-2·d-1;土壤呼吸在5-7月变化不大(0.34~0.51 g·m-2·d-1),7月底以后呈逐渐减小的趋势;(2)土壤呼吸与生态系统呼吸的比值(Rsoil/Reco)在整个生长季为0.38~0.98,平均0.67;季节变化上总体呈"U"型,即生长季初期和末期较高,而生长季中期较低;(3)Rsoil/Reco与梭梭同化枝生物量显著负相关(R2=0.458,P<0.05),说明随着梭梭同化枝生物量的增加,其对生态系统呼吸的贡献升高,导致了植物生长季中期Rsoil/Reco的下降。

关键词: 土壤呼吸, 生态系统呼吸, 二氧化碳通量, 涡度相关

Abstract:

Soil respiration (Rsoil) typically performs as the main contributors to the annual total ecosystem respiration (Reco) in ecosystem, but the seasonal variation of the Rsoil/Reco has not been investigated. The objective of this study was to investigate the characteristics of soil respiration and ecosystem respiration in a Haloxylon ammodendron community, located in the southern margin of Gurbantunggut Desert in western China. Special attention was paid on the seasonal variation of the Rsoil/Reco. The results showed that: (1) The Reco was unimodal distribution during the whole growing season, the maximum Reco was 0.75 g·m-2·d-1 and the minimum was 0.09 g·m-2·d-1. The Rsoil was little changed during May to July (0.34-0.51 g·m-2·d-1), and began decreasing since the end of July. (2) The Rsoil/Reco ranged from 0.38 to 0.98, with an average of 0.67 across the whole growing season. On a seasonal basis, Rsoil/Reco presented an obvious "U" pattern: the value of Rsoil/Reco was 0.71 at the beginning of growing season; in the middle of growing season, the value of Rsoil/Reco reduced (about 0.43) as the plants into rapid growth period because of plants senesced; at the end of growing season, the Rsoil/Reco increased. (3) There was a significant linear correlation between the Rsoil/Reco and biomass of H.ammodendron assimilating twigs (R2=0.458, P<0.05), indicated that as the H.ammodendron growth, the contribution of H.ammodendron aboveground respiration (especially with leaf respiration) to Reco also increased.

Key words: soil respiration, ecosystem respiration, carbon dioxide flux, eddy covariance

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