›› 2007, Vol. 15 ›› Issue (5): 449-453.DOI: 10.11733/j.issn.1007-0435.2007.05.009

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A Study on CO2 Emission Rate from Alpine Meadow in the Source Region of Yellow River in Guo-luo, Qing-hai Province

SUN Bu-gong1, LONG Rui-jun2,3, KONG Zheng1, FENG Rui-zhang1   

  1. 1. Pratacultural College, Gansu Agricultural University, Lanzhou, Gansu Province 730070, China
    2. Northwest Institute of Plateau Biology, CAS, Xining, Qinghai Province 810001, China;
    3. College of Grassland Science, Lanzhou University, Lanzhou, Gansu Province 730000, China
  • Received:2007-03-08 Revised:2007-07-25 Online:2007-10-15 Published:2007-10-15

青海果洛黄河源区高寒草甸CO2释放速率研究

孙步功1, 龙瑞军2,3, 孔郑1, 冯瑞章1   

  1. 1. 甘肃农业大学草业学院, 甘肃, 兰州, 730070;
    2. 中国科学院西北高原生物研究所, 青海, 西宁, 810001;
    3. 兰州大学草地学院, 甘肃, 兰州, 730000
  • 通讯作者: 龙瑞军,E-m ail:longr j@gsau.edu.cn
  • 作者简介:孙步功(1971- ),男,甘肃通渭人,副教授,博士研究生,从事草地生态研究,E-mail:sunbg@gsau.edu.cn
  • 基金资助:
    国家“十五”科技攻关计划项目(2001BA606A-02-03);中国科学院“百人计划”项目(30371021)

Abstract: The CO2 emission rate from degraded alpine meadow in the source region of Yellow River in Guo-luo, Qing-hai Province was studied using static chamber-GC method. The results indicate that CO2 emission rate from non-degraded meadow, minor degraded meadow, medium degraded meadow, and heavily degraded meadow showed evident characteristics of daily variations, e.g. peaked at 15:00-17:00 and minimized at 7:00-9:00, with higher CO2 emission rate at daytime than at night. Furthermore, the CO2 emission also showed a seasonal variation with higher emission rate during the plant growing seasons than at the wilting period. The fastigium of CO2 emission appeared in August and low in January and February. In addition, the daily variations of CO2 emission rate were restricted by soil temperature at 5cm depth and soil surface temperature, and a significant correlation was detected between the seasonal dynamics of CO2 emission rate and soil temperature at 5cm depth (P<0.01).

Key words: CO2 emission rate, Degraded alpine meadow ecosystem, Daily variation, Seasonal change

摘要: 以青海果洛黄河源区高寒退化草甸生态系统为对象,应用静态密闭箱-气相色谱法对高寒退化草甸生态系统CO2释放进行了初步研究。结果表明:所选4种不同退化程度高寒草甸,即未退化草甸(A)、轻度退化草甸(B)、中度退化草甸(C)和重度退化草甸(D),其CO2释放速率有明显的日变化特征,日最大排放速率在15:00-17:00左右出现,最低值出现于清晨7:00-9:00左右,释放白天大于夜晚;(2)CO2释放速率具有明显的季节性变化特征,生长期CO2释放速率明显高于枯黄期,8月为CO2释放高峰期,1月或2月为CO2释放低谷期;(3)CO2释放速率的日变化主要受地表温度和5cm地温制约,季节动态与5cm地温呈显著正相关关系(P<0.01),本研究为进一步进行高寒退化草甸生态系统源江效应的准确估测提供科学依据。

关键词: CO2释放速率, 高寒退化草甸系统, 日动态, 季节动态

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