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中国沙漠 ›› 2005, Vol. 25 ›› Issue (3): 336-341.

• 研究论文 • 上一篇    下一篇

沙坡头地区沙尘气溶胶质量浓度的试验观测研究

刘立超1, 王涛1, 周茅先1, 李新荣1, 失吹贞代2, 柳泽文孝3   

  1. 1. 中国科学院寒区旱区环境与工程研究所沙坡头沙漠试验研究站, 甘肃兰州 730000;
    2. 物理化学研究所表面解析研究室, 日本和光市 351-0198;
    3. 山形大学地球环境系, 日本山形省 990-8560
  • 收稿日期:2004-03-20 修回日期:2004-06-23 出版日期:2005-06-20 发布日期:2005-06-20
  • 作者简介:刘立超(1969-),男(汉族),甘肃镇原县人,副研究员,主要从事沙区气象与干旱环境研究。E-mail:lichao@ns.lzb.ac.cn
  • 基金资助:
    国家重点基础研究发展规划项目(G2000048703);国家自然科学基金(40005002);中日合作项目"Studies on Origin and Transport of Aeolian Dust and its Impact on Climate(ADEC)"共同资助

Characteristics of Sandy Aerosols in Shapotou Region, Northeast Fringe of Tengger Desert, China

LIU Li-chao1, WANG Tao1, ZHOU Mao-xian1, LI Xin-rong1, Sadayo Yabuki2, Yanagisawa Fumitaka3   

  1. 1. Shapotou Desert Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. The Institute of Physical and Chemical Research(RIKEN), Wako 351-0198, Japan;
    3. Yamagata University, Yamagata 990-8560, Japan
  • Received:2004-03-20 Revised:2004-06-23 Online:2005-06-20 Published:2005-06-20

摘要: 中国北方沙尘气溶胶的理化特征及其气候效应受到了广泛关注,但现有的研究大都是基于较短时段和典型事件的试验观测。本项研究利用大流量采样器和安德森采样器,对沙坡头地区沙尘气溶胶的质量浓度特征进行了长达3a的监测,获得了该地区沙尘气溶胶的年变化特征,并与背景气象资料和降尘观测结果进行了对比分析;针对典型天气过程的观测结果表明,不同天气条件(背景大气、浮尘、扬沙和沙尘暴)下TSP浓度存在倍数关系和量级的差异,其质量浓度随粒径分布特征也明显不同;两种采样器观测结果的对比分析也表明,局地沙尘释放是沙坡头地区大气气溶胶的主要来源,但在沙尘暴过程中,远源沙尘输送的贡献也不容忽略。

关键词: 沙坡头, 沙尘气溶胶, 沙尘暴

Abstract: The physical and chemical characteristics of mineral aerosols originated from desert area of northern China attracted more and more attentions in recent year, whereas most of studies are based on the short-term observation or typical dust events. In last three years, a long-term study on mass concentration of mineral aerosols was conducted using high-volume sampler and Anderson sampler in Shapotou, northeast fringe of Tengger Desert, China. The mass concentration of total suspended particle (TSP) show similar seasonal variation with dust deposition and close correlation with meteorological data, such as precipitation, days with dust storm and strong wind. On the average, the amount of TSP mass concentration shows different quantitative level during different weather condition, which are 101 μg·m3 in clear atmosphere, 102 μg·m3 under dust-suspended condition and 103 μg·m3 during sand-blowing and dust-storm process. And it also be possible to reach 103 μg·m3 during extra-strong dust-storm. The mass concentration-size distributions of mineral aerosols are distinct between clean atmosphere and dust storm.

Key words: Shapotou, sandy dust, dust storm

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