2005
DOI: 10.1016/j.atmosenv.2005.08.008
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Deposition velocities and washout ratios on a coastal site (southeastern Spain) calculated from 7Be and 210Pb measurements

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Cited by 45 publications
(32 citation statements)
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“…A similar, but less pronounced seasonal variation was also measured at Opme. Similar seasonal variation was observed in Europe (Dueñas et al, 2004(Dueñas et al, , 2005Daish et al, 2005;Todorovic et al, 2005). However, the majority of studies reported a maximum in the winter and a minimum in the summer: in Germany (Winkler et al, 1998), Estonia (Realo et al, 2007), Finland (Paatero et al, 1998), the Ivory Coast (Nho et al, 1996), and in Italy (Vecchi et al, 2005).…”
Section: Resultssupporting
confidence: 63%
“…A similar, but less pronounced seasonal variation was also measured at Opme. Similar seasonal variation was observed in Europe (Dueñas et al, 2004(Dueñas et al, , 2005Daish et al, 2005;Todorovic et al, 2005). However, the majority of studies reported a maximum in the winter and a minimum in the summer: in Germany (Winkler et al, 1998), Estonia (Realo et al, 2007), Finland (Paatero et al, 1998), the Ivory Coast (Nho et al, 1996), and in Italy (Vecchi et al, 2005).…”
Section: Resultssupporting
confidence: 63%
“…A large variations in the deposition velocity based on 210 Pb, between 0.1 cm s À1 to 5.0 cm s À1 have been reported, although the average values agree within a factor of w3 (0.6 to 1.9 cm s À1 ; Turekian et al, 1983;Graustein and Turekian, 1986;Todd et al, 1989;Anand and Rengarajan, 1990;Beks et al, 1998;Hussain et al, 1998;Winkler and Rosner, 2000;McNeary andBaskaran, 2003, 2007;Dueñas et al, 2005). There was no significant correlation between the total deposition velocities derived from either 210 Pb or 210 Po and the total particulate matter collected onto the filter which suggests that the aerosol mass does not control the amount of 210 Pb scavenged by aerosols (McNeary and Baskaran, 2003;Dueñas et al, 2005). McNeary and Baskaran (2003) proposed that only a small portion of the aerosols scavenges effectively 210 Pb from the atmosphere and a major portion of the aerosols do not actively Table 1.…”
Section: Depositional Velocities Of Aerosolsmentioning
confidence: 90%
“…Based on 30-year (1967e1996) long series of daily 210 Pb measurements in Finland, Paatero et al (1998) observed that daily variations are due to synoptic-scale weather situations while the seasonal variations are attributed to the efficiency of vertical mixing of the lower atmosphere. However, there are sites where higher 210 Pb in the summer months have also been reported (e.g., in Spain, Garcia-Talavera et al, 2001;Azahra et al, 2004a;Dueñas et al, 2005Dueñas et al, , 2009). …”
Section: Concentrations Of 210 Po and 210 Pb In Surface Air And Uppermentioning
confidence: 93%
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“…Validation of this assumption remains a difficult task since the existing knowledge on the speciation of these radioisotopes in the atmosphere is mainly based on the aerosol samples (e.g., Marley et al, 2000;Gaffney et al, 2004;Dueñ as et al, 2005;Lozano et al, 2011). There are reports that these radioisotopes occur mainly in fine aerosols of the particle sizes ranging from 0.1 to 1 lm (e.g., Gaffney et al, 2004).…”
Section: Introductionmentioning
confidence: 95%