Characterization of African dust over southern Italy

被引:74
作者
Blanco, A
De Tomasi, F
Filippo, E
Manno, D
Perrone, MR [1 ]
Serra, A
Tafuro, AM
Tepore, A
机构
[1] Univ Lecce, Dipartimento Fis, Ist Nazl Fis Mat, I-73100 Lecce, Italy
[2] Univ Lecce, Dipartimento Sci Mat, Ist Nazl Fis Mat, I-73100 Lecce, Italy
关键词
D O I
10.5194/acp-3-2147-2003
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Dust samples from rainfall residues have been collected in southeast Italy (40degrees20' N, 18degrees6' E) during dust outbreaks occurred from April to June 2002 to characterize morphological and elemental particle composition by different techniques, and investigate the dependence of particle properties on source regions. Four-day analytical back trajectories and satellite images have been used to infer source regions of the investigated dust samples. It has been found that the TOMS absorbing aerosol index was in the range 0.7-2.2 over Southern Italy when samples have been collected. The particle-size and -shape analysis by a scanning electron microscope (SEM) has revealed either that the particle-diameter distribution was between 0.3 and 30 mum with median-diameter values between 1.7-2.4 mum, and that the particles were characterized by a roundness factor varying from 0.8 to 2.5. The infrared transmission spectra have allowed recognizing that all dust samples contained a significant amount of illite. The X-ray energy dispersive (EDX) measurements have revealed that the Al/Si ratio of the transported dust varies from 0.41 to 0.50, and that the Al/Si, Ca/Al, K/Ca, and Fe/Ca ratios differ according to source regions and therefore can be used as indicators of dust source regions. Indeed, it has been found that dust samples with larger Ca/Al and Si/Al ratios and lower Fe/Ca and K/Ca ratios, have been collected along dust events with a source region in northwestern Sahara. On the contrary, the samples collected along dust events with the origin mainly in Chad, Niger, Algeria and Lybia were characterized by larger Fe/Ca and K/Ca ratios.
引用
收藏
页码:2147 / 2159
页数:13
相关论文
共 44 条
[31]   Image processing for particle characterization [J].
Nazar, AM ;
Silva, FA ;
Ammann, JJ .
MATERIALS CHARACTERIZATION, 1996, 36 (4-5) :165-173
[32]   Physico-chemical characterisation of the inhalable particulate matter (PM10) in an urban area:: an analysis of the seasonal trend [J].
Paoletti, L ;
De Berardis, B ;
Diociaiuti, M .
SCIENCE OF THE TOTAL ENVIRONMENT, 2002, 292 (03) :265-275
[33]   Evaluation of a standardised procedure to assess the shape of pellets using image analysis [J].
Podczeck, F ;
Rahman, SR ;
Newton, JM .
INTERNATIONAL JOURNAL OF PHARMACEUTICS, 1999, 192 (02) :123-138
[34]   CASE OF TRANSPORT AND DEPOSITION OF SAHARAN DUST OVER THE ITALIAN PENINSULA AND SOUTHERN EUROPE [J].
PRODI, F ;
FEA, G .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1979, 84 (NC11) :6951-6960
[35]  
Prospero J. M., 1981, Special Papers-Geological Society of America, V186, P71, DOI [10.1130/SPE186-p71, DOI 10.1130/SPE186-P71]
[36]   Long-term measurements of the transport of African mineral dust to the southeastern United States: Implications for regional air quality [J].
Prospero, JM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D13) :15917-15927
[37]   Environmental characterization of global sources of atmospheric soil dust identified with the Nimbus 7 Total Ozone Mapping Spectrometer (TOMS) absorbing aerosol product [J].
Prospero, JM ;
Ginoux, P ;
Torres, O ;
Nicholson, SE ;
Gill, TE .
REVIEWS OF GEOPHYSICS, 2002, 40 (01) :2-1
[38]   Formation and cycling of aerosols in the global troposphere [J].
Raes, F ;
Van Dingenen, R ;
Vignati, E ;
Wilson, J ;
Putaud, JP ;
Seinfeld, JH ;
Adams, P .
ATMOSPHERIC ENVIRONMENT, 2000, 34 (25) :4215-4240
[39]   Chemical speciation of individual atmospheric particles using low-Z electron probe X-ray microanalysis:: characterizing "Asian Dust" deposited with rainwater in Seoul, Korea [J].
Ro, CU ;
Oh, KY ;
Kim, H ;
Chun, YS ;
Osán, J ;
de Hoog, J ;
Van Grieken, R .
ATMOSPHERIC ENVIRONMENT, 2001, 35 (29) :4995-5005
[40]  
SALISBURY JW, 1991, INFRARED SPECTRA MIN