4.7 Article

The first example of a mixed valence ternary compound of silver with random distribution of Ag(I) and Ag(II) cations

Journal

DALTON TRANSACTIONS
Volume 44, Issue 24, Pages 10957-10968

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c5dt00740b

Keywords

-

Funding

  1. Slovenian Research Agency (ARRS) [P1-0045, P1-0112, P2-0348]
  2. Polish National Science Centre (NCN) [UMO-2011/01/B/ST5/06673]
  3. EU European Regional Development Fund within the Operational Programme Innovative economy [POIG.02.02.00-14-024/08-00]
  4. ICM supercomputers [G29-3]
  5. European Synchrotron Radiation Facility [LS 2209, BM23]

Ask authors/readers for more resources

The reaction between colourless AgSbF6 and sky-blue Ag(SbF6)(2) (molar ratio 2 : 1) in gaseous HF at 323 K yields green Ag-3(SbF6)(4), a new mixed-valence ternary fluoride of silver. Unlike in all other Ag(I)/Ag(II) systems known to date, the Ag+ and Ag2+ cations are randomly distributed on a single 12b Wyckoff position at the (4) over bar axis of the I (4) over bar 3d cell. Each silver forms four short (4 x 2.316(7)angstrom)and four long (4 x 2.764(6) angstrom) contacts with the neighbouring fluorine atoms. The valence bond sum analysis suggests that such coordination would correspond to a severely overbonded Ag(I) and strongly underbonded Ag(II). Thorough inspection of thermal ellipsoids of the fluorine atoms closest to Ag centres reveals their unusual shape, indicating that silver atoms must in fact have different local coordination spheres; this is not immediately apparent from the crystal structure due to static disorder of fluorine atoms. The Ag K-edge XANES analysis confirmed that the average oxidation state of silver is indeed close to +11/3. The optical absorption spectra lack features typical of a metal thus pointing out to the semiconducting nature of Ag-3(SbF6)(4). Ag-3(SbF6)(4) is magnetically diluted and paramagnetic (mu(eff) = 1.9 mu(B)) down to 20 K with a very weak temperature independent paramagnetism. Below 20 K weak antiferromagnetism is observed (Theta = -4.1 K). Replacement of Ag(I) with potassium gives K(I)(2)Ag(II)(SbF6)(4) which is isostructural to Ag(I)(2)Ag(II)(SbF6)(4). Ag-3(SbF6)(4) is a genuine mixed-valence Ag(I)/Ag(II) compound, i.e. Robin and Day Class I system (localized valences), despite Ag(I) and Ag(II) adopting the same crystallographic position.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available