J4

• 水文·工程·环境 • 上一篇    下一篇

松嫩平原西部碱尘气溶胶的元素特征分析

胡克1,陈兵2,Hiroyuki Kitagawa3,介冬梅4,赵奎涛2   

  1. 1.中国地质大学 海洋学院,北京 100083;2.吉林大学 地球科学学院,长春 130061;3.名古屋大学 环境科学研究所,日本 名古屋 464-8601;4.东北师范大学 城市与环境科学学院,长春 130024
  • 收稿日期:2005-08-30 修回日期:1900-01-01 出版日期:2006-05-26 发布日期:2006-05-26
  • 通讯作者: 胡克

Study on Element Compositions of Alkaline Dust Aerosols in Western Songnen Plain, China

HU Ke1, CHEN Bing2, Hiroyuki Kitagawa3, JIE Dong-mei4, ZHAO Kui-tao2   

  1. 1.School of Marine Sciences, China University of Geosciences, Beijing 100083, China;2. College of Earth Sciences, Jilin University, Changchun 130061, China;3. Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan;4. College of Urban and Environment Sciences, North-East Normal University, Changchun 130024, China
  • Received:2005-08-30 Revised:1900-01-01 Online:2006-05-26 Published:2006-05-26
  • Contact: HU Ke

摘要: 碱尘暴期间松嫩平原西部碱尘气溶胶的主要元素质量浓度排序为Na、Al、Fe、Ca、Mg、K、Ti、Ba、Zn,与当地盐碱化土壤的元素组成吻合,而与沙尘、城市气溶胶的元素组成有差别。风力对碱尘气溶胶元素组成有明显的影响,当风速在8.0~17.1 m/s时,元素组成的质量浓度排序为Na、Ca、Al、Fe、Mg、K、Ba、Ti、Zn。Na元素质量浓度的激增是碱尘暴元素组分的一大特征,明显富集元素为Na和B;相对于当地背景大气气溶胶的富集情况,Zn、Cu、Ba、B的富集因子值在碱尘暴期间明显降低;在各种天气情况下,B、Cu均具有较高的富集因子。碱尘中Ti元素的富集因子值均小于1,而Ca、Fe、K、Mg、Mn、Sr、V的富集因子值为1~4。两个采样点的Ca、Na、Al、Fe、Mg、Ti、Zn的富集因子近似,表明该区碱尘的主要元素具有特定的一致性;而B、Ba、Cu、V的富集因子相差较大,可以作为区分不同碱尘源的标志性元素。

关键词: 松嫩平原, 碱尘, 气溶胶, 元素组成, 富集因子

Abstract: The concentration of the main elements of the alkaline dust storm from Western Songnen Plain follows the decreasing order of Na, Al, Fe, Ca, Mg, K, Ti, Ba and Zn, which is compatible with the element composition of local saline soil but quite different from the normal sand dust and municipal aerosols. The relationship between wind and aerosol composition suggests that at the critical wind speed of alkaline dust storm (ADS) of 8.0~17.1 m/s,the concentration of the main elements follows the decreasing order of Na,Ca,Al,Fe,Mg,K,Ba,Ti and Zn.Enrichment factor (EF) values of element Na increase sharply during ADS, in contrast to the decrease of Zn, B, Cu etc., which indicates that EF values of most hazardous metals are smaller during ADS periods than no ADS periods. The lower EF values of these hazardous metals during ADS periods can be ascribed to the excessive input of saline components, such as Na, Ca. EF value of Ca, Fe, K, Mg, Mn, Sr, V is around 1~4. As EF values of major elements are almost the same between two sampling sites, while the trace elements, such as B, Ba, Cu and V can be used to distinguish the dust sources because of the considerable differences between the two sampling sites.

Key words: Songnen Plain, alkaline dusts, aerosol, element compositions, enrichment factor

中图分类号: 

  • X131.1
[1] 代杰瑞, 喻超, 张明杰, 董建, 胡雪平. 淄博市区大气颗粒物重金属元素分布特征及其来源分析[J]. 吉林大学学报(地球科学版), 2018, 48(4): 1201-1211.
[2] 房春生, 孟赫, 田雷, 钟宇红, 王菊. 吉林省典型城市大气颗粒物主要排放源成分谱对比研究[J]. J4, 2010, 40(5): 1149-1156.
[3] 殷汉琴, 周涛发, 张鑫, 袁峰, 李湘凌, 陈永宁, 陈兴仁, 陈富荣, 贾十军. 铜陵市大气降尘中铜元素的污染特征[J]. J4, 2009, 39(4): 734-738.
[4] 夏锦霞,李方林,杨东. 长江宜昌段水系沉积物镉高值带成因[J]. J4, 2009, 39(2): 305-0311.
[5] 李绪谦,潘晓峰,孙大志,商书波,李红艳,付向明,林景玉. 辽宁张士灌区细河流域地下水污染物空间分布特征及污染源判别分析[J]. J4, 2007, 37(4): 767-0772.
[6] 方 樟,肖长来,梁秀娟,冯 波. 松嫩平原地下水脆弱性模糊综合评价[J]. J4, 2007, 37(3): 546-0550.
[7] 孙平安, 林年丰, 李昭阳, 汤洁, 汪雪格. 松嫩平原水土保持价值复合计算模型的建立及应用[J]. J4, 2006, 36(03): 433-442.
[8] 李昭阳,汤 洁,孙平安,林年丰. 松嫩平原西南部土地利用动态变化的分形研究[J]. J4, 2006, 36(02): 250-0258.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!