Viktor P. Afanas’ev

Dr. Viktor P. Afanas’ev


Research Focus & Metrics

Academic Career Length

45Years (1982-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 October 1991 in Zeitschrift für Physik B Condensed Matter
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VAViktor P. Afanas’ev
Viktor P. Afanas’ev
DND. Naujoks
D. Naujoks

1 June 1994 in Zeitschrift für Physik B Condensed Matter
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VAViktor P. Afanas’ev
Viktor P. Afanas’ev
SFS. D. Fedorovich
S. D. Fedorovich
ALAlexander Lubenchenko
Alexander Lubenchenko
ARA. A. Ryjov
A. A. Ryjov
MEM. S. Esimov
M. S. Esimov

1 January 2003 in The European Physical Journal B
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VAViktor P. Afanas’ev
Viktor P. Afanas’ev
ALAlexander Lubenchenko
Alexander Lubenchenko
MGM. Gubkin
M. Gubkin

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VAViktor P. Afanas’ev
Viktor P. Afanas’ev
ABAlexander Yu. Basov
Alexander Yu. Basov
VBVladimir Budak
Vladimir Budak
Dmitry EfremenkoDmitry Efremenko
Dmitry Efremenko
Alexander KokhanovskyAlexander Kokhanovsky
Alexander Kokhanovsky
In this paper, we analyze the current state of the discrete theory of radiative transfer. One-dimensional, three-dimensional and stochastic radiative transfer models are considered. It is shown that the discrete theory provides a unique solution to the one-dimensional radiative transfer equation. All approximate solution techniques based on the discrete ordinate formalism can be derived based on the synthetic iterations, the small-angle approximation, and the matrix operator method. The possible directions for the perspective development of radiative transfer are outlined.

1 May 2019 in Russian Geology and Geophysics
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NPN.P. Pokhilenko
N.P. Pokhilenko
TSTatyana Shumilova
Tatyana Shumilova
VAViktor P. Afanas’ev
Viktor P. Afanas’ev
KLKonstantin Litasov
Konstantin Litasov
—Lavas of the Kamchatka volcanoes store cubic-octahedral diamonds identical in morphology and structure to synthetic crystals, and their natural origin is doubted. Judging by published data, the diamonds discovered in the Tolbachik lavas are similar to synthetic diamonds made by different producers, and the analyzed samples rather result from contamination with synthetic material. Ophiolite-hosted diamonds reported from Europe, China, Mongolia, and Polar Urals look like the Tolbachik diamonds and are of the same type. The similarity between crystals coming from geologically dissimilar objects indicates that contamination may occur in those cases as well. Thus, diamonds found in unusual hosts or geologic settings require careful checking. These findings have to be reproduced repeatedly in other in situ samples and approved by independent experts; with all respect to the priority of the first finders, the sampling sites should be open to many researchers, especially the respective specialists. The inevitable disproval of false diamond findings is discouraging and discredits the true discoveries. Possible contamination with synthetic or natural material from cutting tools has to be excluded in all newly found diamonds before claiming their natural origin.

1 February 2010 in Bulletin of the Russian Academy of Sciences: Physics
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VAViktor P. Afanas’ev
Viktor P. Afanas’ev
Dmitry EfremenkoDmitry Efremenko
Dmitry Efremenko
ALAlexander Lubenchenko
Alexander Lubenchenko
MVMaarten Vos
Maarten Vos
MWMichael R. Went
Michael R. Went
REELS spectra of the electrons reflected off niobium are measured with energy resolution <0.5 eV within the 5–40 eV energy range of the probing beam. The measurements were performed for the scattering angles θ = 45° and θ = 120° by means of two electron guns. The process of energy losses is described within the framework of a model with three different energy loss laws: surface, intermediate, and bulk layers are considered. Differential cross-sections of inelastic scattering are represented in the form of simple equations.