(2017) 'New apatite-type oxide ion conductor, Bi2La8[(GeO4)6]O3 : structure, properties, and direct imaging of low-level interstitial oxygen atoms using aberration-corrected scanning transmission electron microscopy.', Advanced functional materials., 27 (8). p.
1605625.Further information on publisher's website:
Use policyThe full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-pro t purposes provided that:• a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders.Please consult the full DRO policy for further details. The new solid electrolyte Bi2La8[(GeO4)6]O3 has been prepared and characterized by variabletemperature synchrotron X-ray and neutron diffraction, aberration-corrected scanning transmission electron microscopy and physical property measurements (impedance spectroscopy and second harmonic generation). The material is a triclinic variant of the apatite structure type and owes its ionic conductivity to the presence of oxide ion interstitials. A combination of annular bright-field scanning transmission electron microscopy experiments and frozen-phonon multi-slice simulations enabled direct imaging of the crucial interstitial oxygen atoms present at a level of 8 out of 1030 electrons per formula unit of the material, and crystallographically disordered, in the unit cell. Scanning transmission electron microscopy also led to a direct observation of the local departures from the centrosymmetric average structure determined by diffraction. As no second harmonic generation signal was observed, these displacements are non-cooperative on the longer length scales probed by optical methods.2