Journal
DALTON TRANSACTIONS
Volume 50, Issue 3, Pages -Publisher
ROYAL SOC CHEMISTRY
DOI: 10.1039/d0dt03125a
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Funding
- Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) under Germany's Excellence Strategy -Exzellenzcluster 2186 The Fuel Science Center [EXC 236, 390919832]
- Max Planck Society
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Sheet silicates, such as talc and pyrophyllite, contain parallel sheets of tetrahedral silicate, with the ferric analogue being rarely found in nature and synthetic protocols for purely iron-based pyrophyllite yet to be published. This study reports the first artificial synthesis of ferripyrophyllite under exceptional mild conditions, showing high thermostability and catalytic activity in ammonia synthesis.
Sheet silicates, also known as phyllosilicates, contain parallel sheets of tetrahedral silicate built up by [Si2O5](2-) entities connected through intermediate metal-oxygen octahedral layers. The well-known minerals talc and pyrophyllite are belonging to this group based on magnesium and aluminium, respectively. Surprisingly, the ferric analogue rarely occurs in nature and is found in mixtures and conglomerates with other materials only. While partial incorporation of iron into pyrophyllites has been achieved, no synthetic protocol for purely iron-based pyrophyllite has been published yet. Here we report about the first artificial synthesis of ferripyrophyllite under exceptional mild conditions. A similar ultrathin two-dimensional (2D) nanosheet morphology is obtained as in talc or pyrophyllite but with iron(iii) as a central metal. The high surface material exhibits a remarkably high thermostability. It shows some catalytic activity in ammonia synthesis and can serve as catalyst support material for noble metal nanoparticles.
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