Particulate Carbon 1981
DOI: 10.1007/978-1-4757-6137-5_2
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Morphology and Internal Structure of Soot and Carbon Blacks

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Cited by 61 publications
(39 citation statements)
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“…The density of black carbon (elemental carbon, graphitic carbon and other optically absorbing carbon compounds) is believed to be smaller than 2 g cm −3 (Wagner, 1981) and often a value of 1 g cm −3 is used if the black carbon consists of chains of individual spherules (Schultz, 1993;Hitzenberger et al, 1999). Establishing a representative density is not straightforward if the carbonaceous material consists of spheres or agglomerates (Lahaye & Prado, 1981;Ishiguro, Takatori, & Akihama, 1997). Particle densities below 1 g cm −3 are assumed if non-spherical particles are in the form of a u y material (Zier & Goetz, 1982;Samson, Mulholland, & Gentry, 1987).…”
Section: Aerosol Volatility In a Moderately Polluted Environmentmentioning
confidence: 99%
“…The density of black carbon (elemental carbon, graphitic carbon and other optically absorbing carbon compounds) is believed to be smaller than 2 g cm −3 (Wagner, 1981) and often a value of 1 g cm −3 is used if the black carbon consists of chains of individual spherules (Schultz, 1993;Hitzenberger et al, 1999). Establishing a representative density is not straightforward if the carbonaceous material consists of spheres or agglomerates (Lahaye & Prado, 1981;Ishiguro, Takatori, & Akihama, 1997). Particle densities below 1 g cm −3 are assumed if non-spherical particles are in the form of a u y material (Zier & Goetz, 1982;Samson, Mulholland, & Gentry, 1987).…”
Section: Aerosol Volatility In a Moderately Polluted Environmentmentioning
confidence: 99%
“…Key physical parameters for soot are its size and morphology which fundamentally govern all the situations above. The current view of soot formation and growth in flames involves a series of steps including fuel thermal decomposition to small radicals (Palmer & Cullis, 1965;Glassman, 1988) that react to form polyaromatic hydrocarbons (D'Anna, D'Alesso, & Minutolo, 1994;Dobbins & Subramaniasivam, 1994;Dobbins, Fletcher, & Chang, 1998;Frenklach, 2002) that subsequently nucleate, coalesce and dehydrogenate to yield roughly spherical, graphitic, primary particles of soot with diameters in the few tens of nanometer range (Lahaye & Prado, 1981). After this, the physical process of three-dimensional diffusion limited cluster aggregation (DLCA) (Meakin, 1999;Oh & Sorensen, 1997) proceeds to make noncoalesced clusters which have a fractal morphology with a universal fractal dimension of D 1.8 (Samson, Mulholland, & Gentry, 1987;Dobbins & Megaridis, 1987;Zhang, Sorensen, Ramer, Olivier, & Merklin, 1988;Sorensen, Cai, & Lu, 1992;Koylu & Faeth, 1992).…”
Section: Introductionmentioning
confidence: 99%
“…Samson et al [ll] found that Df2 < Df3 for computer-generated clusters even when Df3 < 2. Other simulations have shown that the area-size relations of Table 1 are accurate only for clusters containing more than several thousand primary particles [12]. Thus, substantial corrections to the ideal fractal scaling laws may be required for such small clusters.…”
Section: Fractalsmentioning
confidence: 97%