Regioselective Reactions of 1,3-Diynes with the Titanocene Vinylidene Fragment [Cp*2Ti=C=CH2]. Crystal and Molecular Structure of Cp*2TiC(Cc="http://pubs.acs.or
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The titanocene vinylidene intermediate[Cp*2Ti=C=CH2] (6)(Cp*: C5(CH3)5), formedbyethene or methane elimination fromCp*2TiCH2CH2C=CH2(5) andCp*2Ti(CH=CH2)(CH3)(7), respectively, reacts with 1,3-diynes RCC-CCR (R= Me (13a), Ph (13b), SiMe3(13c),CMe3 (13d)) by a [2 + 2]-cycloaddition,giving metallacyclobutenesCp*2TiC(CCR)=CRC=CH2(9a-d). Using the unsymmetrical 1,3-diyneRCCCCR1 (R = CMe3, R1 =SiMe3 (13e)), a9:1 mixture of the metallacyclobutenesCp*2TiC(CCR)=CR1C=CH2(9e) and Cp*2TiC(CCR1)=CRC=CH2 (9e')is formed. In all cases, exclusive formation of oneregioisomerexhibiting the CCR substituent in the chars/alpha.gif" BORDER=0>-position of themetallacycle is observed. Theregioselectivity of the formation of 9 is attributed to thepolarity of the CC bond as well asthe stereochemical conditions, proven by ab initiocalculations at the Hartree-Fock (HF)level of theory with the 3-21G(*) standard basis set and molecularmodeling. The X-raystructure of 9c is presented. Subsequent reactions of9 with an excess of the titanoceneintermediate 6, to form binuclear metallacycles, are notobserved.

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