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气相色谱法观测本底大气中的甲烷和二氧化碳 |
作者:周凌 NFDA1 汤洁… 文章来源:本站原创 点击数 更新时间:2006/4/12 17:41:32 文章录入:anny 责任编辑:anny |
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6 小 结 1.在AES?5个月的组装调试结果表明,GC系统具有良好的线性、灵敏度、精度和准确度. 2.在瓦里关本底台一年多时间的业务运行和标定情况表明,系统具有高自动化的操作性能和严格的质量控制,其设计符合WMO全球大气本底测量的要求. 3.GC法观测数据与FLASK法和NDIR法结果的对比表明,用这3种方法在瓦里关本底台获得的CH4和CO2数据都有较高的质量,且具有国际可比性. 4.瓦里关山大气CH4月平均浓度基本上在1780—1840ppb的范围内波动,随季节变化幅度不大. 5.瓦里关山大气CO2浓度的月平均值在355—365ppm范围内,其季节变化比较明显,夏末秋初降至最低,冬春季达最高值,浓度变化范围约10ppm. 参考文献 1 Ramanathan V, Cicerone R J et al. Trace gas trends and their potential role in climate change. J Geophys Res, 1985, 90:5547—5566 2 Keeling C D, Bacastow R B et al. Atmospheric carbon dioxide variations at Mauna Loa observatory, Hawaii. Tellus, 1976,28:538—551 3 Wen Yupu et al. Observation and investigation of variabilities of baseline CO2 concentration over Waliguan Mountain in Qinghai Province of China. Acta Meteorologica Sinica, 1995, 8(3):255—262 4 WMO/Geneva. International Operations Handbook for Measurement of Background Atmospheric Pollution. WMO—No. 49,1978,:2 5 WMO/Geneva.Greenhouse gases. Global Atmosphere Watch, 1990, (77):15—35 6 WMO/Geneva. Greenhouse gases. Global Atmosphere Watch, 1993,(86):1—19 7 Pearman G, Further I. Studies of the comparability of baseline atmospheric CO2 measurements. Tellus. 1977,29:171—181 8 NOAA/USA. Climate Monitoring and Diagnostic Laboratory, Summary Report, 1992,(21):16—29 9 NOAA/USA. Climate Monitoring and Diagnostic Laboratory, Summary Report,1993,(22):18—30 10 Australia Bureau of Meteorology /Melbourne, Baseline Atmospheric Program, 1996, (1993):71—89 11 Steele et al. The global distrabutin of methane in the troposphere. J Atmos Chem, 1987,5:125—171 12 王明星,刘卫卫等.我国西北部沙漠地区大气甲烷浓度的季节变化和长期变化趋势.科学通报,1989(9):684—686 |
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