2001
DOI: 10.1016/s0021-8502(00)00076-8
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Alternative analytical solution to condensational growth of polydisperse aerosols in the continuum regime

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Cited by 23 publications
(33 citation statements)
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“…Many previous modeling studies have attempted to understand the effects of these different processes on the aerosol distribution (see e.g. Pich et al, 1970;Lee, 1983;Barrett and Clement, 1988;Kulmala et al, 1989;Williams, 1995;Jacobson, 1999;Park and Lee, 2000;Park et al, 2001;Kulmala, 2003;Kulmala et al, 2004a). Some studies estimate that the transfer of organic carbon from hydrophobic to hygroscopic occurrs in the order of 2-3 days (Reddy and Boucher, 2004;Cooke et al, 2002), and in general, the residence time of black carbon and organic matter in the atmosphere is a function of its hygroscopicity (Cooke et al, 2002), indicating that the hygroscopicity of particles in the atmosphere depends on the chemical nature of the organic aerosol component.…”
Section: Introductionmentioning
confidence: 99%
“…Many previous modeling studies have attempted to understand the effects of these different processes on the aerosol distribution (see e.g. Pich et al, 1970;Lee, 1983;Barrett and Clement, 1988;Kulmala et al, 1989;Williams, 1995;Jacobson, 1999;Park and Lee, 2000;Park et al, 2001;Kulmala, 2003;Kulmala et al, 2004a). Some studies estimate that the transfer of organic carbon from hydrophobic to hygroscopic occurrs in the order of 2-3 days (Reddy and Boucher, 2004;Cooke et al, 2002), and in general, the residence time of black carbon and organic matter in the atmosphere is a function of its hygroscopicity (Cooke et al, 2002), indicating that the hygroscopicity of particles in the atmosphere depends on the chemical nature of the organic aerosol component.…”
Section: Introductionmentioning
confidence: 99%
“…The second term indicates the rate of disappearance of particles of volume v as a result of collisions with any other particle. Generally speaking, there are two classes methods suitable for addressing above PBE: (1) The deterministic methods such as sectional methods (Landgrebe and Pratsinis, 1990;Wu and Biswas, 1998;Jeong and Choi, 2001;Mitrakos et al, 2007), methods of moment (Park et al, 2001;Terry et al, 2001;Yamamoto, 2004;Yu et al, 2008;Yamamoto, 2012); (2) The non-deterministic methods such as Monte Carlo (MC) methods (Garcia et al, 1987;Liffman, 1992;Smith and Matsoukas, 1998;Kruis et al, 2000;Efendiev and Zachariah, 2002;Maisels et al, 2004;Zhao et al, 2009). Among all these methods, MC methods are particularly suitable and effective due to several reasons: (1) MC methods are essentially a statistical method, making them suitable for describing the inherently discrete processes such as coagulation; (2) MC methods exhibit great flexibility and scalability when new characteristic of particles needs to be incorporated, because they treat each simulation particle as an individual object having some properties such as sizes, positions, charges, etc.…”
Section: T V U U N U T N V U T Du T N V T V U N U T Dumentioning
confidence: 99%
“…Different methods are available at this point to solve above integro-differential equation, including sectional methods (Landgrebe and Pratsinis, 1990;Wu and Biswas, 1998;Jeong and Choi, 2001;Mitrakos et al, 2007;Yamamoto, 2012), methods of moment (Park and Lee, 2001;Terry et al, 2001;Yamamoto, 2004;Yu et al, 2008) and Monte Carlo methods (Garcia et al, 1987;Liffman, 1990;Simith and Matsoukas, 1998;Kruis et al, 2000;Lee and Matsoukas, 2000;Efendiev and Zachariah, 2002;Maisels et al, 2004;Zhao and Kruis, 2008). All these methods have different precision, algorithm complexity and computational efficiency.…”
Section: U U N U T N V U T Du T N V T V U N U T Dumentioning
confidence: 99%