Get Aerosols: Science and Technology PDF

By Igor Agranovski

ISBN-10: 352732660X

ISBN-13: 9783527326600

This self-contained guide and prepared reference examines aerosol technological know-how and know-how intensive, offering an in depth perception into this innovative box. As such, it covers primary ideas, experimental tools, and a large choice of purposes, starting from aerosol filtration to organic aerosols, and from the synthesis of carbon nanotubes to aerosol reactors.Written by means of a number of across the world popular specialists within the box, this can be an important source for chemists and engineers within the chemical and fabrics disciplines throughout a number of industries, in addition to perfect supplementary studying in graduate point classes.

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3 Possible Sources of Fractal Particles The sources of FAs are subdivided into two groups: natural and anthropogenic ones. 1 Natural Sources Volcanos Volcanic eruptions produce a lot of volcanic ash, consisting of aggregated oxide particles of the size from fractions of a micrometer up to millimeters. In addition, extreme volcanic conditions produce a lot of smaller aggregates. Forest fires These produce a huge amount of ash flakes whose sizes vary from fractions of a micrometer up to centimeters.

065 µm), which means that the free-molecule regime of particle charging demands some special conditions and can be realized, for example, in the ionosphere. 23) that is, the flux is proportional to the ion density n∞ far away from the particle. The proportionality coefficient α(a) is known as the charging efficiency. The problem is to find α(a). 24) We can generalize Eq. 25) where nR is the ion concentration at a distance R from the particle center. It is important to emphasize that nR is (still) an arbitrary value introduced as a boundary condition at the distance R (also arbitrary) to a kinetic equation that is necessary to solve for defining α(a, R).

45) R3−D One immediately sees that the total volume occupied by the voids is exactly 4πR3 /3 once the shape factor γ defining the dependence of the average volume V(a) of a void on its characteristic size a is given as γ = 4π(6 − D)/3(3 − D) (V = γ a3 ). 9, indicating that these FAs are of coagulation origin. 2) Such low fractal dimensions are explained by non-isotropy of observed FAs, which are mostly aligned in one direction. This anisotropy probably arises due to Coulomb or dipole–dipole interaction of FAs.

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Aerosols: Science and Technology by Igor Agranovski

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