Zobrazeno 1 - 8
of 8
pro vyhledávání: '"R. N. Sobolev"'
Autor:
R. N. Sobolev, A. V. Khnykin
Publikováno v:
Vestnik komp'iuternykh i informatsionnykh tekhnologii. :13-17
One of the risks of information security of companies is the risk of information leakage through the screen photography. Often this happens using a mobile device. In view of this, it is worth the task of automated detection of this fact of violation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a822d5fd0aaa6c4fa7307520c64a69a1
https://doi.org/10.14489/vkit.2022.05.pp.013-017
https://doi.org/10.14489/vkit.2022.05.pp.013-017
Publikováno v:
Russian Metallurgy (Metally). 2021:102-108
The melting of a mineral grain and a polymineral rock sample are analyzed. The melting is shown to be a long-term multistage process, which occurs in a certain temperature range and starts in the surface layer of grains. The melting of monomineral fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f872f202809633aaba85da92fc166c54
https://doi.org/10.1134/s0036029521020269
https://doi.org/10.1134/s0036029521020269
Autor:
R. N. Sobolev
Publikováno v:
Doklady Earth Sciences. 479:495-498
A crystal becomes melted in a few stages. The structure of the crystal surface differs from that of its interior. Therefore, as its interior is gradually involved in the melting process, the phase transition temperature becomes higher. The melting po
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b29fd159d5a0b3a72a21ad28802a79b1
https://doi.org/10.1134/s1028334x18040177
https://doi.org/10.1134/s1028334x18040177
Autor:
R. N. Sobolev
Publikováno v:
Doklady Earth Sciences. 473:367-370
The first-order phase transition is accompanied by an increase in disordering. Defects and dislocations of the crystal cell decrease the temperature of the phase transition. Atoms located on the crystal surface get higher internal free energy first.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de6e63baf77f3928e7ed4d82d082a1e4
https://doi.org/10.1134/s1028334x1703028x
https://doi.org/10.1134/s1028334x1703028x
Autor:
R. N. Sobolev
Publikováno v:
Doklady Earth Sciences. 472:40-43
Glass formation takes place under conditions of rapid cooling of a melt at a great temperature difference between the melt and the host rock, which must have high thermal conductivity. The most favorable conditions for glass formation exist when the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40b0996eb2b2f582fc5a73518b517fd3
https://doi.org/10.1134/s1028334x1701010x
https://doi.org/10.1134/s1028334x1701010x
Autor:
V. V. Mal’tsev, R. N. Sobolev
Publikováno v:
Doklady Earth Sciences. 438:830-833
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bffeec9d49eb9e4cea1ea1f996e06ba5
https://doi.org/10.1134/s1028334x11060250
https://doi.org/10.1134/s1028334x11060250
Autor:
R. N. Sobolev
Publikováno v:
Doklady Earth Sciences. 412:144-146
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75cc414b272a511b82571b046d86a6e6
https://doi.org/10.1134/s1028334x07010333
https://doi.org/10.1134/s1028334x07010333
Autor:
R. N. Sobolev
Publikováno v:
Mineralogical Magazine. :864-865
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4aa35edd9ed293668623e85f59c72f33
https://doi.org/10.1180/minmag.1994.58a.2.185
https://doi.org/10.1180/minmag.1994.58a.2.185