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The salts of chloronium ions R-Cl+-R (R = CH3 or (CHCl)-Cl-2): formation, thermal stability, and interaction with chloromethanes Full article

Journal Physical Chemistry Chemical Physics
ISSN: 1463-9076 , E-ISSN: 1463-9084
Output data Year: 2016, Volume: 18, Number: 18, Pages: 12896-12904 Pages count : 9 DOI: 10.1039/c6cp00946h
Authors Stoyanov Evgenii S. 1,2
Affiliations
1 (Данные Web of science) Russian Acad Sci SB RAS, Siberian Branch, Vorozhtsov Inst Organ Chem, Novosibirsk 630090, Russia
2 (Данные Web of science) Novosibirsk State Univ, Dept Nat Sci, Natl Res Univ, Novosibirsk 630090, Russia

Abstract: The interaction of CH3Cl/CD3Cl or CH2Cl2/CD2Cl2 with the carborane acid H(CHB11Cl11) (abbreviated as H{Cl-11}) generates the salts of CH3-{Cl-11} and CH2Cl-{Cl-11} and their deuterio analogs, respectively, which are analogs of the salts of asymmetric chloronium cations. Next, salts of chloronium cations CH3-Cl+-CH3, ClCH2-Cl+-CH2Cl, and ClCH2-Cl+-CH3 and their deuterio analogs were obtained from the above compounds. The asymmetric ClCH2-Cl+-CH3 cation was found to be unstable, and at ambient temperature, slowly disproportionated into symmetric cations (CH3)(2)Cl+ and (CH2Cl)(2)Cl+. At a high temperature (150 degrees C), disproportionation was completed within 5 minutes, and the resulting cations further decomposed into CH3-{Cl-11} and CH2Cl-{Cl-11}. The molecular fragment ClCH2-(X) of the compounds (X = {Cl-11}, -Cl+-CH2Cl, or -Cl+-CH3) is involved in exchange reactions with CH2Cl2 and CHCl3, converting into CH3-(X) with the formation of chloroform and CCl4, respectively.
Cite: Stoyanov E.S.
The salts of chloronium ions R-Cl+-R (R = CH3 or (CHCl)-Cl-2): formation, thermal stability, and interaction with chloromethanes
Physical Chemistry Chemical Physics. 2016. V.18. N18. P.12896-12904. DOI: 10.1039/c6cp00946h WOS Scopus OpenAlex
Files: Full text from publisher
Identifiers:
Web of science: WOS:000375689200056
Scopus: 2-s2.0-84973570960
OpenAlex: W2330197922
Citing:
DB Citing
Web of science 9
Scopus 9
OpenAlex 10
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