长江流域资源与环境 >> 2012, Vol. 21 >> Issue (02): 204-.

• 生态环境 • 上一篇    下一篇

临安区域本底站大气甲烷浓度变化特征

徐宏辉|浦静姣|顾骏强|俞向明   

  1. (1.浙江省气象科学研究所|浙江 杭州 310017;2.临安区域大气本底站|浙江 临安 311307)
  • 出版日期:2012-02-20

VARIATION CHARACTERISTICS OF ATMOSPHERIC CH4 CONCENTRATION AT LIN’AN REGIONAL BACKGROUND STATION

XU Honghui1|PU Jingjiao1|GU Junqiang1|YU Xiangming2   

  1. (1.Zhejiang Institute of Meteorological Sciences,Hangzhou 310017,China|2.Lin’an Regional Background Station,Lin’an 311307,China
  • Online:2012-02-20

摘要:

通过分析2006年8月~2009年7月临安区域大气本底站Flask瓶采样获得的CH4浓度特征,结合地面风向、后向轨迹、排放清单,研究了CH4浓度变化特征和长三角地区排放源对CH4浓度的影响作用。结果表明,临安区域大气本底站的CH4浓度分布在1 7584×10-9~1 9700×10-9,具有较明显的季节波动变化特征,浓度季节变化幅度为737×10-9;CH4浓度平均年增幅达176×10-9,增速较快。东北风和东南风时,CH4浓度较高;西南风时CH4浓度较低。导致CH4高浓度分布的气团主要来自临安站的东北、偏东方向;导致CH4低浓度分布的气团集中在西南偏南

Abstract:

Characteristics of atmospheric CH4 concentration obtained by Flask measurements were analyzed at Lin'an regional background station from August 2006 to July 2009.According to the wind direction,backward trajectories and emission inventory,the variation characteristics of CH4 concentration was studied and the impact of emission sources on CH4 concentration was evaluated in Yangtze River Delta.The results revealed that atmospheric CH4 concentrations at Lin'an regional background station were between 1 7584×10-9 and 19700×10-9.The CH4 concentration varied as seasons change and the annual difference was about 737×10-9.The longterm trend of CH4 concentration showed rapid growth year by year;the average growth rate was about 176×10-9/a.The CH4 concentrations were high when the winds were from the northeast and southeast,and the CH4 concentrations were low when the winds were from southwest.The air mass contained high CH4 concentrations mainly came from the northeast and east sector while the air mass contained low CH4 concentrations almost came from the southwest and south sector

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 宋玉芝,秦伯强, 高光. 附着生物对富营养化水体氮磷的去除效果[J]. 长江流域资源与环境, 2009, 18(2): 180 .
[2] 刘滨谊,刘 琴. 服务于城市旅游形象的景观规划——以南京市为例[J]. 长江流域资源与环境, 2006, 15(2): 164 -168 .
[3] 梁常德,龙天渝,李继承,刘腊美. 三峡库区非点源氮磷负荷研究[J]. 长江流域资源与环境, 2007, 16(1): 26 -30 .
[4] 吴丰林,周德民,胡金明. 基于景观格局演变的城市湿地景观生态规划途径[J]. 长江流域资源与环境, 2007, 16(3): 368 .
[5] 屈 璠,刘 敏,侯立军,许世远,刘巧梅,欧冬妮. 潮汐循环影响下上覆水环境因子和氮营养盐的变化及其相关关系[J]. 长江流域资源与环境, 2007, 16(3): 345 .
[6] 一之濑俊明 大坪国顺 景元书. 依据经济水平建立的华中—华南粮食运输模型[J]. 长江流域资源与环境, 2009, 18(3): 217 -221 .
[7] 刘小丽, 沈 芳, 朱伟健, 刘 曦. MERIS卫星数据定量反演长江河口的悬沙浓度[J]. 长江流域资源与环境, 2009, 18(11): 1026 .
[8] 刘扬扬, 张行南, 徐双全, 倪斐. 长江口滩涂地形冲淤分析研究[J]. 长江流域资源与环境, 2010, 19(11): 1314 .
[9] 赵 爽| 王慧敏| 仇 蕾. 工业水环境监管契约研究[J]. 长江流域资源与环境, 2011, 20(10): 1279 .
[10] 王小冬|秦伯强|刘丽贞|赵林林|丁艳青|朱广伟|高 光|刘兴国. 底泥悬浮对营养盐释放和水华生长影响的模拟[J]. 长江流域资源与环境, 2011, 20(12): 1481 .