干旱区研究 ›› 2012, Vol. 29 ›› Issue (6): 1014-1021.
高进长, 苏永红
收稿日期:2011-12-07
修回日期:2012-02-08
发布日期:2012-11-19
通讯作者:
苏永红. E-mail: syh@lzb.ac.cn
作者简介:高进长(1984-),男,河南安阳人,在读硕士,主要从事干旱区土壤呼吸方面的研究. E-mail: jzhgao@lzb.ac.cn
基金资助:GAO Jin-zhang, SU Yong-hong
Received:2011-12-07
Revised:2012-02-08
Online:2012-11-19
摘要: 土壤是陆地生态系统最大的碳源,也是最大的碳汇。土壤呼吸作为全球碳循环的一个重要组成部分,是调控全球碳循环和气候变化的关键过程,也是当前全球变化生态学研究的重要领域和碳循环中碳收支研究中的一个热点问题。水分是土壤呼吸的重要扰动因子,比较不同来源土壤水分对土壤呼吸的影响,对准确估算土壤呼吸具有重要意义,这在干旱和半干旱地区尤为明显。通过土壤水分的3种主要来源:降水、灌溉和地下水,比较分析了土壤呼吸对不同来源水分的响应过程和规律,为今后土壤呼吸方面的研究提供参考。
高进长, 苏永红. 土壤呼吸对不同来源水分响应的研究进展[J]. 干旱区研究, 2012, 29(6): 1014-1021.
GAO Jin-zhang, SU Yong-hong. Research Progress in Effect of Soil Moisture Content on Soil Respiration[J]. Arid Zone Research, 2012, 29(6): 1014-1021.
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