By Pramod Kulkarni, Paul A. Baron, Klaus Willeke
Aerosol dimension: rules, recommendations, and functions 3rd version is the main specific remedy to be had of the newest aerosol size equipment. Drawing at the knowledge of diverse specialist participants; it offers a high-quality seize of size basics and practices a wide selection of aerosol applications.
This new version is up-to-date to handle new and constructing purposes of aerosol size, together with purposes in environmental future health, atmospheric technological know-how, weather swap, pollution, public overall healthiness, nanotechnology, particle and powder know-how, pharmaceutical study and improvement, fresh room know-how (integrated circuit manufacture), and nuclear waste management.
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Extra resources for Aerosol Measurement: Principles, Techniques, and Applications
5000 V 1 stat V E¼ ¼ 8:33 statV=cm 2 cm 300 statV Using Equation 2-43 Felec ¼ neE ¼ 18(1:6 Â 10À19 C)(2:5 Â 105 V=m) ¼ 7:2 Â 10À13 N [Felec ¼ neE ¼ 18(4:8 Â 10À10 statC)(8:33statV=cm) ¼ 7:2 Â 10À8 dyne] One newton (N) in SI units equals 105 dyne in the cgs system of units. Using Equation 2-30: p 3 p d r g ¼ (0:5 Â 10À6 m)3 (1000 kg=m3 ) (9:80 m=s2 ) 6 p p 6 h i p Fgrav ¼ (0:5 Â 10À4 cm)3 (1 g=cm3 ) (980 cm=s2 ) 6 (Eq. 2-45) or, including the electric charge, the particle electrical mobility, Z ¼ neB, Velec ¼ ZE (Eq.
S. Srivastava. 1968. Motion of a fluid in a curved tube. Proc. Roy. Soc. A. 307: 37 –53. 30 FUNDAMENTALS OF SINGLE PARTICLE TRANSPORT Mercer, T. T. 1973. Aerosol Technology in Hazard Evaluation. New York: Academic. Rader, D. J. 1990. Momentum slip correction factor for small particles in nine common gases. J. Aerosol Sci. 21: 161– 168. Sartor, J. , and C. E. Abbott. 1975. Prediction and measurement of the accelerated motion of water drops in air. J. Appl. Meteor. 14(2): 232 –239. Schlichting, H.
Published 2011 by John Wiley & Sons, Inc. 31 32 PHYSICAL AND CHEMICAL PROCESSES IN AEROSOL SYSTEMS particle approach for much of the analysis that follows will be adopted. We rely on the concepts of mean free path and diffusion coefficient, defined in Chapter 2. 1 Definitions The partial pressure of a vapor is a way of expressing the concentration of that vapor in a volume of a gas mixture. It is the pressure the vapor would exert if it were the only component present. This pressure, expressed as a fraction of the ambient pressure, is the fractional concentration of the vapor.