A Dinuclear Molecular Iron(II) Silicate with Two High‐Spin Square‐Planar FeO 4  Units | Zendy

Pinkert Denise | Zendy; Demeshko Serhiy | Zendy; Schax Fabian | Zendy; Braun Beatrice | Zendy; Meyer Franc | Zendy; Limberg Christian | Zendy

AI Assistant Blog Pricing

Home ZAIA Blog

Premium

A Dinuclear Molecular Iron(II) Silicate with Two High‐Spin Square‐Planar FeO 4 Units

Author(s) -

Pinkert Denise,

Demeshko Serhiy,

Schax Fabian,

Braun Beatrice,

Meyer Franc,

Limberg Christian

Publication year - 2013

Publication title -

angewandte chemie international edition

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 5.831

H-Index - 550

eISSN - 1521-3773

pISSN - 1433-7851

DOI - 10.1002/anie.201209650

Subject(s) - silicate , ferrous , square (algebra) , ion , planar , crystallography , chemistry , enhanced data rates for gsm evolution , inorganic chemistry , materials science , mineralogy , organic chemistry , mathematics , geometry , engineering , computer science , computer graphics (images) , telecommunications

Ferrous flatland : Two flattened Fe II O 4 units that share an edge are found in the title compound (see structure). They are spanned by tripodal silanolate ligands, which form in situ from a trisilanol if iron ions are available for complexation. The compound approaches the situation in the natural iron silicate gillespite or in certain ceramics where square planar FeO 4 units have also been found.

This content is not available in your region!

Continue researching here.

Having issues? You can contact us here

Accelerating Research