Theoretical and Experimental Study on the In-Plane SN2-Type Substitution Reaction of Haloalkenes with Inversion of Configuration at the sp2Carbon†

2004 ◽  
Vol 6 (14) ◽  
pp. 2461-2463 ◽  
Author(s):  
Kaori Ando ◽  
Mitsuru Kitamura ◽  
Kasei Miura ◽  
Koichi Narasaka
1991 ◽  
Vol 32 (34) ◽  
pp. 4317-4320 ◽  
Author(s):  
Akio Toshimitsu ◽  
Chitaru Hirosawa ◽  
Shigeo Tanimot

Molecules ◽  
2019 ◽  
Vol 24 (3) ◽  
pp. 642 ◽  
Author(s):  
Kento Ueta ◽  
Takayuki Tanaka ◽  
Atsuhiro Osuka

A corrole is a tetrapyrrolic macrocycle known as a ring-contracted porphyrinoid. Despite the progress of the synthetic chemistry of meso-aryl-substituted corroles since the early 2000s, meso-heteroatom-substituted corroles have been scarcely reported. Herein we report that the SNAr-type substitution reaction of a meso-chlorocorrole silver complex with diphenylamine or carbazole in the presence of NaH as a base produced meso-aminocorroles. The structures, ultraviolet–visible spectroscopy (UV/Vis), and emission spectra of these meso-aminocorroles were discussed. Furthermore, the oxidation reaction of a meso-diphenylaminocorrole was examined, which resulted in the formation of 10,10-diethoxyisocorrole.


1976 ◽  
Vol 40 (316) ◽  
pp. 875-886 ◽  
Author(s):  
Claude Triboulet

SummaryCompositions concerning sodic amphiboles (glaucophane) in the system Na2O-Al2O3-MgO-SiO2-H2O have been studied at PH2O ≤ 3 kb, 380 °C < T < 700 °C. The study attempts to establish the mineral parageneses under these physical conditions as they define the clay mineral (saponite-hectorite smectite) and greenschist (chlorite-albite) facies. The occurence of sodic amphiboles is defined by compositional parameters. Glaucophane does not appear in the present investigation.The method of ‘reaction reversal’, i.e. using precrystallized mineral assemblages to form new ones, has been used to establish the three reactions: albite + chlorite → paragonite + saponite, paragonite + chlorite → saponite + cordierite, and saponite + paragonite → albite + cordierite. In general, the clay mineral → greenschist transformation is favoured by an increase in pressure in the system studied. The amphibole present is a sodic richterite with the type substitution


2007 ◽  
Vol 2 (2) ◽  
pp. 290-300 ◽  
Author(s):  
Zhenshan Jia ◽  
Xiang Zhang ◽  
Gaihong Zhang ◽  
Shaohua Huang ◽  
Hao Fang ◽  
...  

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