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Restructuring factors of soot particles. / Mikhailov, E. F.; Vlasenko, S. S.; Kiselev, A. A.; Ryshkevich, T. I.

In: Izvestiya - Atmospheric and Ocean Physics, Vol. 34, No. 3, 09.10.1998, p. 307-317.

Research output: Contribution to journal › Article › peer-review

Harvard

Mikhailov, EF, Vlasenko, SS, Kiselev, AA & Ryshkevich, TI 1998, 'Restructuring factors of soot particles', Izvestiya - Atmospheric and Ocean Physics, vol. 34, no. 3, pp. 307-317.

APA

Mikhailov, E. F., Vlasenko, S. S., Kiselev, A. A., & Ryshkevich, T. I. (1998). Restructuring factors of soot particles. Izvestiya - Atmospheric and Ocean Physics, 34(3), 307-317.

Vancouver

Mikhailov EF, Vlasenko SS, Kiselev AA, Ryshkevich TI. Restructuring factors of soot particles. Izvestiya - Atmospheric and Ocean Physics. 1998 Oct 9;34(3):307-317.

Author

Mikhailov, E. F. ; Vlasenko, S. S. ; Kiselev, A. A. ; Ryshkevich, T. I. / Restructuring factors of soot particles. In: Izvestiya - Atmospheric and Ocean Physics. 1998 ; Vol. 34, No. 3. pp. 307-317.

BibTeX

@article{57ac1335f6be41369b59a08494f8bf44,
title = "Restructuring factors of soot particles",
abstract = "Restructuring mechanisms of soot particles that are in an atmosphere of a condensed vapor are considered. It is found that the condensation of vapor on a surface of previously rarefied soot aggregates leads to the formation of compact fragments of close-packed particles-globules. The effect of water vapor is established to depend on the charge and chemical composition of the particles. It is shown that the effect of vapor manifests itself first and foremost in a fractal dimension change and in the shift of the particle size distribution to the range of small sizes. In the context of the theory of fractal systems, a model that accounts for the influence of capillary forces on restructuring processes of soot clusters is proposed.",
author = "Mikhailov, {E. F.} and Vlasenko, {S. S.} and Kiselev, {A. A.} and Ryshkevich, {T. I.}",
year = "1998",
month = oct,
day = "9",
language = "English",
volume = "34",
pages = "307--317",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Restructuring factors of soot particles

AU - Mikhailov, E. F.

AU - Vlasenko, S. S.

AU - Kiselev, A. A.

AU - Ryshkevich, T. I.

PY - 1998/10/9

Y1 - 1998/10/9

N2 - Restructuring mechanisms of soot particles that are in an atmosphere of a condensed vapor are considered. It is found that the condensation of vapor on a surface of previously rarefied soot aggregates leads to the formation of compact fragments of close-packed particles-globules. The effect of water vapor is established to depend on the charge and chemical composition of the particles. It is shown that the effect of vapor manifests itself first and foremost in a fractal dimension change and in the shift of the particle size distribution to the range of small sizes. In the context of the theory of fractal systems, a model that accounts for the influence of capillary forces on restructuring processes of soot clusters is proposed.

AB - Restructuring mechanisms of soot particles that are in an atmosphere of a condensed vapor are considered. It is found that the condensation of vapor on a surface of previously rarefied soot aggregates leads to the formation of compact fragments of close-packed particles-globules. The effect of water vapor is established to depend on the charge and chemical composition of the particles. It is shown that the effect of vapor manifests itself first and foremost in a fractal dimension change and in the shift of the particle size distribution to the range of small sizes. In the context of the theory of fractal systems, a model that accounts for the influence of capillary forces on restructuring processes of soot clusters is proposed.

UR - http://www.scopus.com/inward/record.url?scp=0031664767&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0031664767

VL - 34

SP - 307

EP - 317

JO - Izvestiya - Atmospheric and Oceanic Physics

JF - Izvestiya - Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 3

ER -

ID: 36009952