Zobrazeno 1 - 7
of 7
pro vyhledávání: '"T. A. Vysokikh"'
Autor:
T. S. Vysokikh, M. V. Olonova
Publikováno v:
Проблемы ботаники южной сибири и монголии. 19:243-248
The study of the formation and spatial distribution of biodiversity is currently one of the most importantproblems of biology. The use of modern GIS-technologies open up the great opportunities for research in the fieldof biogeography and ecology, bu
Publikováno v:
Contemporary Problems of Ecology. 11:604-613
In addition to a specific morphotype, each species has a unique ecologo-climatic niche and a geographical area. The study of ecologo-climatic and geographical divergence may significantly contribute to the comprehension of species genesis and amount.
Publikováno v:
International Journal of Environmental Studies. 74:715-723
Research into the basic qualitative characteristics (phens), their distribution and combinations (morphotypes) was undertaken in order to reveal the genetic diversity with respect to section Stenopoa in Asian Russia. About one and half thousands occu
Publikováno v:
Russian Journal of Physical Chemistry A. 81:1836-1839
The interaction of ozone with chlorinated methanes adsorbed on a thin ice film was studied over the temperature range 77–292 K. Ozone was shown to oxidize chlorinated methanes starting with 210 K to produce chlorine oxides of various compositions.
Publikováno v:
Russian Journal of Physical Chemistry A. 81:878-882
The reaction of ozone with chlorobenzene was studied over the temperature range 77–305 K. Ozone was found to oxidize chlorobenzene starting with 77 K to produce a complex mixture of ozonides and peroxides of various compositions. The products of th
Publikováno v:
SPIE Proceedings.
Reactions of ozone with CH3Cl, CH2Cl2, CHCl3, CCL4, adsorbed on ice surface, have been investigated under temperatures 77 - 292 K. Ozonation reaction takes place only when temperature is above 210 K with formation of different chlorine oxides. The pr
Publikováno v:
Scopus-Elsevier
The possible formation of ozone hydrates and their interaction with hydrogen chloride under near-stratospheric conditions were investigated. The low-temperature IR spectroscopic technique was used to demonstrate the in situ formation of ozone hydrate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::638d3e38428bf54a73546f2a8faf46e5
http://www.scopus.com/inward/record.url?eid=2-s2.0-42149183768&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-42149183768&partnerID=MN8TOARS