Size distribution and element composition of dust aerosol in Chinese Otindag Sandland

被引:5
作者
Cheng, TT [1 ]
Lü, D
Chen, HB
Wang, GC
机构
[1] Fudan Univ, Dept Environm Sci & Engn, Shanghai 200433, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, Div Middle Atmosphere & Remote Sounding Theory &, Beijing 100029, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2005年 / 50卷 / 08期
基金
中国国家自然科学基金;
关键词
Otindag Sandland; dust aerosol; physical and chemical properties;
D O I
10.1360/04wd0169
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Part physical and chemical characteristics of dust aerosol were determined for samples collected from Otindag Sandland of China in spring, 2001. Number concentration, mass concentration, chemical element concentration and size distribution of aerosol particles with 0.5 mu m < D-p < 100.0 mu n were examined. The average number and mass concentrations of aerosols were 274.8 cm(-3) and 0.54 mg/m(3) for the field period respectively, and 31.4 cm(-3) and 0.07 mg/m(3) for the non-dusty days. PM10 played a dominant role in the aerosol mass concentrations. The particles with D-p < 8.0 mu m accounted for about 93.7% of total aerosol number loading in dusty days. The particle size distributions of aerosols were characterized by bi-modal logarithm normal function in heavy and moderate dusty days, and mono-modal in windblown and non-dusty days. Crustal elements such as Al, Fe, etc. in aerosols almost originated from soils. Pollutant elements of S, Pb, etc. associated with aerosols were affected by remote anthropogenic pollutant sources in upwind regions. Mo, V and Co in aerosols were possibly from other dust sources other than local soils. The aerosols over Otindag Sandland consisted of particles from local soils, upwind pollutant sources and other dust sources.
引用
收藏
页码:788 / 792
页数:5
相关论文
共 24 条
[1]  
[Anonymous], J DESERT RES
[2]   Relationships among aerosol constituents from Asia and the North Pacific during PEM-West A [J].
Arimoto, R ;
Duce, RA ;
Savoie, DL ;
Prospero, JM ;
Talbot, R ;
Cullen, JD ;
Tomza, U ;
Lewis, NF ;
Jay, BJ .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D1) :2011-2023
[3]   ATMOSPHERIC TRACE-ELEMENTS AT ENEWETAK-ATOLL .1. CONCENTRATIONS, SOURCES, AND TEMPORAL VARIABILITY [J].
DUCE, RA ;
ARIMOTO, R ;
RAY, BJ ;
UNNI, CK ;
HARDER, PJ .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1983, 88 (NC9) :5321-5342
[4]  
IPCC, 2001, CLIM CHANG 2001 SCI, P291
[5]  
Lei Wenfang, 1993, PLATEAU METEOROLOGY, V12, P170
[6]   Contributions of different land cover types in Otindag Sandy Land and Bashang area of Hebei Province to the material source of sand stormy weather in Beijing [J].
Liu, HY ;
Tian, YH ;
Ding, D .
CHINESE SCIENCE BULLETIN, 2003, 48 (17) :1853-1856
[7]   IRON-DEFICIENCY LIMITS PHYTOPLANKTON GROWTH IN THE NORTHEAST PACIFIC SUBARCTIC [J].
MARTIN, JH ;
FITZWATER, SE .
NATURE, 1988, 331 (6154) :341-343
[8]  
Niu S, 2000, J DESERT RES, V20, P264
[9]  
Niu S, 2001, CHINESE J ATMOSPHERI, V25, P243
[10]   COMMONALITIES IN MEASURED SIZE DISTRIBUTIONS FOR AEROSOLS HAVING A SOIL-DERIVED COMPONENT [J].
PATTERSON, EM ;
GILLETTE, DA .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS AND ATMOSPHERES, 1977, 82 (15) :2074-2082