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云贵高原草地生态系统CO2通量变化特征
引用本文:孙思思,吴战平,肖启涛,于飞,古书鸿,方荻,李浪,赵兴炳.云贵高原草地生态系统CO2通量变化特征[J].草业学报,2020,29(4):184-191.
作者姓名:孙思思  吴战平  肖启涛  于飞  古书鸿  方荻  李浪  赵兴炳
作者单位:1.贵州省山地环境气候研究所,贵州省山地气候与资源重点实验室,贵州 贵阳 550002; 2.中国科学院南京地理与湖泊研究所,中国科学院流域地理学重点实验室,江苏 南京210008; 3.贵州省遵义市气象局,贵州 遵义 563099; 4.中国气象局成都高原气象研究所,四川 成都 610072
基金项目:中国气象局气候变化专项(CCSF201915),国家自然科学基金(41801093)和成都高原气象研究所科研项目资助
摘    要:草地是云贵高原的重要植被类型,与其他地区研究相比,该地区草地生态系统的CO2交换过程和驱动机理的研究较为薄弱。基于涡度相关系统对云贵高原草地生态系统观测的连续高频数据(2017年10月-2018年8月),分析了该生态系统CO2通量的时间变化特征及其环境影响因素。结果表明:日尺度上CO2通量具有显著的变化特征,为明显的单峰型变化,白天净吸收,夜晚净排放。季节尺度上,每月均为碳吸收,吸收速率呈春夏高,秋冬低的特征,吸收峰值出现在6月,最低值在1月,且生长季的碳吸收变化幅度比非生长季大。影响CO2通量变化的主要环境因子有太阳辐射、气温、土壤温度和风速,综上,云贵高原草地生态系统CO2通量对温度较为敏感,温度升高可提高其固碳能力。总的来看,该生态系统是一个明显的碳汇,研究时段内净碳吸收量为425.14 g CO2·m-2

关 键 词:云贵高原  草地生态系统  CO2通量  环境因子  
收稿时间:2019-09-18
修稿时间:2019-11-11

Factors influencing CO2 fluxes of a grassland ecosystem on the Yunnan-Guizhou Plateau,China
SUN Si-si,WU Zhan-ping,XIAO Qi-tao,YU Fei,GU Shu-hong,FANG Di,LI Lang,ZHAO Xing-bing.Factors influencing CO2 fluxes of a grassland ecosystem on the Yunnan-Guizhou Plateau,China[J].Acta Prataculturae Sinica,2020,29(4):184-191.
Authors:SUN Si-si  WU Zhan-ping  XIAO Qi-tao  YU Fei  GU Shu-hong  FANG Di  LI Lang  ZHAO Xing-bing
Institution:1.Guizhou Institute of Mountainous Environment and Climate, Guizhou Key Laboratory of Mountainous Climate and Resources, Guiyang 550002, China; 2.Key Laboratory of Watershed Geographic Science, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; 3.Meteorological Administration in Zunyi City, Zunyi 563099, China; 4.Institute of Plateau Meteorology, CMA, Chengdu 610072, China
Abstract:Grassland is a dominant vegetation type on the Yunnan-Guizhou Plateau, and comparatively little is known about the CO2 flux and its diurnal and seasonal variation. Based on in-situ measurement using eddy covariance methodology from October 2017 to August 2018, the diurnal cycle and seasonal variations of CO2 flux for a grassland ecosystem of Yunnan-Guizhou Plateau were analyzed, and key factors determining CO2 flux were determined. The CO2 flux had obvious diurnal variation, with net uptake during the day and net emission at night, and the diurnal cycle being more significant in growing season than in the non-growing season. Overall, the grassland ecosystem was a sink of atmospheric CO2, which also varied seasonally with high uptake rate in spring and summer and low rate in autumn and winter. Specifically, the peak CO2 uptake rate occurred in June and lowest was observed in January. The diurnal and seasonal variation in the CO2 flux were associated with solar radiation, air temperature, soil temperature and wind speed fluctuations. Global warming would enhance the carbon sequestration capacity of the grassland ecosystem, given the CO2 flux was sensitive to temperature. Our results suggested that the grassland ecosystem acted as carbon sink and absorbed 425.14 g CO2·m-2 from the atmosphere during the study period.
Keywords:Yunnan-Guizhou Plateau  grassland ecosystem  CO2 flux  environmental factors  
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