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The ratios among the particle modes are from Knollenberg and Hunten (1980).
The optical thickness of each cloud layer shown in Fig. 2(h) is distributed to three particle modes (mode1, 2, and 3) and shown in Table 1.
In a plasma with a population of super-thermal particles generated by heating or fusion processes, kinetic effects can lead to the additional destabilisation of MHD modes or even to additional energetic particle modes.
Air quality is affected by natural and anthropogenic sources, and the emissions of particles <10 μm and <2.5 μm, respectively, have to be determined to quantify their contributions to the so-called coarse (10 2.5 μm) and fine (<2.5 μm) particle modes in ambient air.
These three particle modes have distinctly different chemical composition, sources, and lifetimes in the atmosphere.
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The ratios among each particle mode are taken from table 5 of Knollenberg and Hunten (1980).
In the premixed ethylene/air flame, nano-structured CeO2 partly evaporates forming a new particle mode.
The coagulation (γSD) model alone is unable to reproduce well the larger particle mode (mode II).
Thorium colloid analysis in water has been carried out by a single particle mode using inductively coupled plasma mass spectrometry (ICP-MS).
The apparent large particle mode observed with the USP inlet seem rather to be droplets from the same monomodal distribution that have not fully evaporated.
The corresponding monomodal distribution is observed to evolve to bimodal one at z > 5 mm, with the sub-primary particle mode being progressively depleted in favor of the growth of a mode corresponding to larger primary particles (10 12 nm size).
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