Stoichiometric and catalytic degradation of SF6 with cobaltocene

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Abstract The controlled reduction of SF6 (25 °C, 1 bar) with cobaltocene results in the formation of the mixed salt [Cp2Co]2[SF5][F]. The salt can be characterized by solution and solid-state heteronuclear nuclear magnetic resonance and infrared spectroscopies and demonstrates a degree of mineralization of the S and F atoms when reacted with borosilicate glass. Although [Cp2Co]2[SF5][F] is highly reactive, the structure of the corresponding [Cp2Co][F] is also reported herein, thus providing structural evidence for the naked fluoride anion. The mild activation of SF6 by cobaltocene also permits its catalytic degradation using phosphines as terminal reductants.