Abstract
Understanding multi-component nucleation is of great importance for atmospheric and environmental sciences. Vivid examples are: polar stratospheric clouds, acid rains and air pollution. All these phenomena occur because Earth’s atmosphere is a multi-component gaseous system in which nucleation leads to formation of droplets of complex composition. A rich field of applications of multi-component nucleation is associated with the natural gas industry since nucleation is the primary mechanism responsible for formation of mist during the expansion of natural gas [1]. This is the key process of the non-equilibrium gas-liquid separation technology[2].
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Similar content being viewed by others
References
M.J. Muitjens, V.I. Kalikmanov, M.E.H. van Dongen, A. Hirschberg, P. Derks, Revue de l’Institut Français du Pétrole 49, 63 (1994)
V. Kalikmanov, J. Bruining, M. Betting, D. Smeulders, in 2007 SPE Annual Technical Conference and Exhibition, (Anaheim, California, USA, 2007), pp. 11–14. Paper No: SPE 110736
O. Hirschfelder, J. Chem. Phys. 61, 2690 (1974)
H. Trinkaus, Phys. Rev. B 27, 7372 (1983)
K.F. Riley, M.P. Hobson, S.J. Bence, Mathematical Methods for Physics and Engineering (Cambridge University Press, Cambridge, 2007)
D. Wu, J. Chem. Phys. 99, 1990 (1993)
B. Wyslouzil, G. Wilemski, J. Chem. Phys. 103, 1137 (1995)
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2013 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Kalikmanov, V.I. (2013). Multi-Component Nucleation. In: Nucleation Theory. Lecture Notes in Physics, vol 860. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3643-8_14
Download citation
DOI: https://doi.org/10.1007/978-90-481-3643-8_14
Published:
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-3642-1
Online ISBN: 978-90-481-3643-8
eBook Packages: Physics and AstronomyPhysics and Astronomy (R0)