草地学报 ›› 2019, Vol. 27 ›› Issue (1): 153-162.DOI: 10.11733/j.issn.1007-0435.2019.01.020

• 研究论文 • 上一篇    下一篇

δ13C值在羊草草原植物体中的差异和变化及其影响因素分析

耿元波1, 王子腾1,2, 李茹霞1,2   

  1. 1. 中国科学院地理科学与资源研究所, 北京 100101;
    2. 中国科学院大学, 北京 100049
  • 收稿日期:2018-05-03 修回日期:2019-01-02 出版日期:2019-02-15 发布日期:2019-04-13
  • 通讯作者: 耿元波,E-mail:gengyb@igsnrr.ac.cn
  • 作者简介:耿元波(1969-),男,新疆霍城县人,博士,副研究员,主要从事环境生物地球化学方面的研究,E-mail:gengyb@igsnrr.ac.cn
  • 基金资助:
    国家自然科学基金项目(41071138)资助

Analysis of Differences and Influencing Factors of Plant δ13C in Leymus chinensis Grassland in Inner-Mongolia,China

GENG Yuan-bo1, WANG Zi-teng1,2, LI Ru-xia1,2   

  1. 1. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2018-05-03 Revised:2019-01-02 Online:2019-02-15 Published:2019-04-13

摘要: 为了解稳定同位素13C在草原植物体中的分配和变化以及水分和温度对13C组成(δ13C)的影响,在内蒙古羊草草原的生长盛期(7-9月),应用13C脉冲标记技术,测定了13C脉冲标记处理和对照处理下羊草草原植物活体和活根中的δ13C,分析了土壤水分、气温和地温对植物体中δ13C的影响。结果表明:对照处理中羊草草原植物活根δ13C值比活体高1~2‰,标记处理中活体δ13C值显著高于活根,标记处理中活体和活根的δ13C均显著高于对照处理。生长盛期,标记和对照处理中植物活体和活根的δ13C值均表现为先减小再增加,随后再减小的趋势。对照处理中活体和活根以及标记处理中活根的δ13C与0~20 cm土壤水分含量之间线性负相关,而标记处理中活体δ13C与0~20 cm土壤水分之间存在二次函数关系。标记、对照两处理中羊草草原活体、活根δ13C与温度均呈线性正相关。

关键词: 羊草草原, δ13C, 13C脉冲标记, 土壤水分, 气温, 土壤温度

Abstract: In order to understand the distribution and change of stable carbon isotope13C in grassland plants and the effects of soil moisture and temperature on the stable carbon isotope13C composition (δ13C),we measured the δ13C of shoots and living roots which both had two treatments,13C pulse labeling treatment and control treatment,and analyzed the effect of soil moisture content,air temperature and ground temperature on the δ13C of plants body during the fast-growing stage (July-September) of the Leymus chinensis grassland in Inner Mongolia. The results showed that the δ13C of the living roots was 1~2‰ higher than the δ13C of the shoots in control treatments,and the δ13C of the shoots in13C pulse labeling treatment was significantly greater than the δ13C of the living roots. The variation trends of the δ13C value of shoots and living roots in labeling and control treatments were both in good consistency with time,which showed that the value of13C in shoots and living roots decreased at first,then increased,and then decreased during the growing season of plants. The δ13C of the shoots and living roots in control group and living roots in13C pulse labeling treatment had a linear negative correlation with soil moisture content in the layer of 0~20 cm,but the δ13C of shoots in13C pulse labeling treatment had Quadratic function relation with the soil moisture content in the layer of 0~20 cm,which indicated that the δ13C increased with increasing soil moisture content when it had a low soil moisture content,and the δ13C decreased when there was a high soil moisture content. In13C pulse labeling treatment and control treatment,there were significant positive correlation between temperature and the δ13C of the shoots and living roots,the δ13C of the shoots and living roots increased with increasing the temperature.

Key words: Leymus chinensis grassland, 13C pulse labeling, δ13C, Soil moisture content, Air temperature, Soil temperature

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