Origin and variability of particulate matter (PM10) mass concentrations over the Eastern Mediterranean

被引:177
作者
Gerasopoulos, E.
Kouvarakis, G.
Babasakalis, P.
Vrekoussis, M.
Putaud, J. -P.
Mihalopoulos, N.
机构
[1] Univ Crete, Environm Chem Proc Lab, Dept Chem, Iraklion 70113, Greece
[2] Commiss European Communities, Joint Res Ctr, Inst Environm & Sustainabil, I-21020 Ispra, VA, Italy
关键词
particulate matter (PM10); chemical mass balance; Eastern Mediterranean;
D O I
10.1016/j.atmosenv.2006.04.020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Five-year PM10 concentrations (2000-05) at Heraklion (urban), Crete, and concurrent measurements of TSP and PM10 (2001-02 and 2004-05, respectively) at Finokalia (background) have been used to discriminate between the various sources of PM over the area and investigate the factors that control their levels. PM10 concentrations at Heraklion (51 +/- 33 mu g m(-3)) and Finokalia (28 +/- 30 mu g m(-3)) lie within the range found for urban and background-rural sites in the Eastern Mediterranean, respectively. Special focus has been given to the influence of transported dust from N. Africa, which is found to be more frequent during spring and fall. The additional effect from local sources has been also calculated at Heraklion (about 20 mu g m(-3)). The EU limit of 50 mu g m(-3) is exceeded at Heraklion, one in 4 days, during winter and spring (50% due to transported dust) and half of the days during summer and fall (pollution). At Finokalia exceedances are observed in winter and spring during one in 5 days, 80-100% of which are associated with dust events. The mass balance estimation for periods with no influence from dust shows that ions dominate the PM10 mass (40-60%) with dust and particulate carbonaceous matter (PCM) comprising the rest. During the identified dust outbreaks, the contribution of dust rises to 60-65%, while the contribution of ions declines to 30% and only 10% is PCM. (c) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:4679 / 4690
页数:12
相关论文
共 29 条
[1]   Chemical composition of size-resolved atmospheric aerosols in the eastern Mediterranean during summer and winter [J].
Bardouki, H ;
Liakakou, H ;
Economou, C ;
Sciare, J ;
Smolík, J ;
Zdímal, V ;
Eleftheriadis, K ;
Lazaridis, M ;
Dye, C ;
Mihalopoulos, N .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (02) :195-208
[2]   Muscle flap reconstruction for the treatment of major sternal wound infections after cardiac surgery:: A 10-year analysis [J].
Castelló, JR ;
Centella, T ;
Garro, L ;
Barros, J ;
Oliva, E ;
Sánchez-Olaso, A ;
Epeldegui, A .
SCANDINAVIAN JOURNAL OF PLASTIC AND RECONSTRUCTIVE SURGERY AND HAND SURGERY, 1999, 33 (01) :17-24
[3]   Measurements of PM10 and PM2.5 particle concentrations in Athens, Greece [J].
Chaloulakou, A ;
Kassomenos, P ;
Spyrellis, N ;
Demokritou, P ;
Koutrakis, P .
ATMOSPHERIC ENVIRONMENT, 2003, 37 (05) :649-660
[4]   Origins of African dust transported over the northeastern tropical Atlantic [J].
Chiapello, I ;
Bergametti, G ;
Chatenet, B ;
Bousquet, P ;
Dulac, F ;
Soares, ES .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D12) :13701-13709
[5]   The influence of meteorological conditions and atmospheric circulation types on PM10 and visibility in Tel Aviv [J].
Dayan, U ;
Levy, I .
JOURNAL OF APPLIED METEOROLOGY, 2005, 44 (05) :606-619
[6]  
Dockery D., 1996, PARTICLES OUR AIR CO, P123
[7]  
Draxler RR, 1998, AUST METEOROL MAG, V47, P295
[8]   Mineral dust concentrations, deposition fluxes and deposition velocities in dust episodes over Israel [J].
Ganor, E ;
Foner, HA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2001, 106 (D16) :18431-18437
[9]   Ozone variability in the marine boundary layer of the eastern Mediterranean based on 7-year observations [J].
Gerasopoulos, E ;
Kouvarakis, G ;
Vrekoussis, M ;
Kanakidou, M ;
Mihalopoulos, N .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2005, 110 (D15) :1-12
[10]  
GERASOPOULOS E, 2006, IN PRESS ATMOSPHERIC