G. Mairesse
Centre national de la recherche scientifique
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Featured researches published by G. Mairesse.
Solid State Ionics | 1990
Francis Abraham; J. C. Boivin; G. Mairesse; Guy Nowogrocki
Abstract A new family of oxygen anionic conductors, exhibiting high performances at low temperature, has been prepared and characterized. They derive from Bi4V2O11 by partial substitution of vanadium by other metallic ions (BIMEVOX). Results dealing with the copper substituant (BICUVOX) are detailed.
Solid State Ionics | 1991
T. Iharada; A. Hammouche; J. Fouletier; M. Kleitz; J. C. Boivin; G. Mairesse
Partial substitution of metals such as Cu or Zn for vanadium in Bi4V2O11 leads to materials exhibiting high anionic conductivities at temperatures as low as 500 K. These materials have been characterized electrochemically for use as potential solid electrolytes in potentiometric and amperometric oxygen sensors. Their electronic conductivities are significant.
Journal of Materials Chemistry | 1998
M. Saiful Islam; Sylvie Lazure; Rose-Noëlle Vannier; Guy Nowogrocki; G. Mairesse
A combination of neutron powder diffraction and computer simulation techniques was performed on undoped and doped Bi2WO6 Aurivillius type compounds to clarify some of the factors controlling oxygen transport in these materials. Oxygen vacancies in doped compounds are randomly distributed within the perovskite-like slab. The most favourable dopants are predicted to be NbVand TaV on WVI and LaIII on BiIII in accordance with the experimental results. The calculated migration energy of 0.63 eV is in agreement with the values deduced from impedance spectroscopy data for Ta and Nb doped Bi2WO6 at T>550 °C. At lower temperatures, pair clusters are predicted to form with a 0.25 eV mean binding energy, leading to a 0.88 eV activation energy for oxygen vacancy migration, in good correlation with experimental values. Finally, consideration of possible oxygen ion migration pathways in the structure showed that energy barriers to migration are lowest between adjacent apical and equatorial sites of WO6 oxygen octahedra.
Solid State Ionics | 1996
S. Lazure; Ch. Vernochet; R.N. Vannier; Guy Nowogrocki; G. Mairesse
Abstract Partial substitution for vanadium in Bi 4 V 2 O 11 can lead to the stabilization at room temperature of one of the three polymorphs α, β, γ exhibited by the mother compound. A tentative classification of the BIMEVOX phases based on these structural polytypes is carried out, and a review of the different identified ways to stabilize the γ-type phases, the most performant ones in term of oxide anion conduction, is proposed. The experimental results clearly indicate that the predominant parameter is not the size or the valence state of the dopant, but rather the structural parameter correlated with the ability for the dopant to regularize the diffusion slab between the Bi 2 O 2 sheets in these layered materials.
Solid State Ionics | 1994
E. Pernot; M. Anne; M. Bacmann; P. Strobel; J. Fouletier; R.N. Vannier; G. Mairesse; Francis Abraham; Guy Nowogrocki
The partially Cu- or Ni-substituted compounds (Bi4V2(1−x)M2xO11−3x;M=Cu, Ni) are highly oxygen-conducting. Three phases (α, β, γ) are observed in the unsubstituted compound; α is the low-conducting room temperature phase and γ the high-conducting phase at high temperature. Structure and conductivity are studied as a function of the substitution on the vanadium sites. Between 0 and 6% at room temperature, the Cu compound remains in the orthorhombic α phase and its ionic conductivity increases. A strong anisotropic conductivity is observed. For 0.07≤x≤0.12, the average structure is tetragonal (γ-type) at room temperature. The conductivity is very high and does not vary very much over this substitution range. Impedance spectroscopy measurements have also been carried out on the x=0.07 Ni-substituted compound. Commensurate or incommensurate superstructures are observed for all of these compounds.
Solid State Sciences | 2003
G. Mairesse; Pascal Roussel; R.N. Vannier; M. Anne; Caroline Pirovano; Guy Nowogrocki
Abstract Using combined X-ray single crystal and neutron powder thermodiffraction data, the crystal structure of the high temperature γ -form of Bi 4 V 2 O 11 was confirmed and accurately refined in the I4/mmm space group and that of the β -form was entirely determined in the centrosymmetric Amam space group. The two-fold superlattice characterising the β structure is the result of an ordering process involving corner-sharing V–O tetrahedra and disordered trigonal bipyramids. A possible scheme for the γ ↔ β phase transition is proposed.
Solid State Ionics | 2001
Caroline Pirovano; M. Saiful Islam; Rose-Noëlle Vannier; Guy Nowogrocki; G. Mairesse
Abstract Computer simulation techniques are used to model the structures of several Aurivillius phases (with the general formula (Bi 2 O 2 )[A m −1 (B) m O 3 m +1 ]) and related compounds. The methods are based upon interatomic potentials and efficient energy minimisation procedures. The results indicate general agreement between the simulated and experimental structures. From recent diffraction data of the Bi 2 GeO 5 system, a new refinement of the crystal structure has been obtained. A discussion of trends related to the Bi lone-pair parameters of these Aurivillius phases is also presented.
Solid State Sciences | 2003
G. Mairesse; Pascal Roussel; R.N. Vannier; M. Anne; Guy Nowogrocki
The crystal structure of α-Bi 4 V 2 O 11 was solved in the A2 space group and refined using combined X-ray single crystal and neutron powder diffraction data in the following unit cell a = 16.5949(3) A (3 x a m = 5.5316 A), b = 5.6106(1) A, c = 15.2707(3) A, γ = 90.260(2)°. It is built upon [Bi 2 O 2 ] 2+ layers spaced with vanadium-oxygen slabs where the vanadium atoms exhibit three different oxygen environments. The main characteristic of these V-O slabs is a well defined dimeric unit with two trigonal bipyramids sharing one edge and connected to two VO tetrahedra. These rigid blocks extend along [100] and are spaced with a disordered area where different V-O trigonal bipyramids are interconnected. A possible scheme to explain the actual 6a m superlattice is proposed. It also accounts for the diffusion lines systematically observed along [100] by SAED. A relationship between the crystal structures of the three Bi 4 V 2 O 11 polymorphs and their corresponding conductivity is tentatively suggested.
Journal of Materials Chemistry | 1996
Marielle Huvé; Rose-Noëlle Vannier; Guy Nowogrocki; G. Mairesse; Gustaaf Van Tendeloo
Bi4V2O11, the parent compound of the BIMEVOX family, has been studied by TEM and HREM, at room temperature and at high temperatures. Under the experimental conditions, Bi4V2O11 undergoes a VV–VIV reduction, ultimately leading to the formation of Bi6V3O16(Bi4V2O10.66) with VIV/VV= 1/2. This transformation is confirmed by in situ X-ray diffraction studies of Bi4V2O11 under reducing atmospheres up to 330 °C. The symmetry of the α-Bi4V2O11 polymorph, stable at ambient temperature, is dependent on the chemical purity of V2O5 used for the synthesis.
Solid State Ionics | 1995
R.N. Vannier; G. Mairesse; Francis Abraham; Guy Nowogrocki; E. Pernot; M. Anne; M. Bacmann; P. Strobel; J. Fouletier
Abstract Bi 4 V 2 O 11 powdered samples and single crystals were studied by high temperature X-ray diffraction and impedance spectroscopy to characterize the phase transitions. From high temperature X-ray diffraction on powders and single crystals, the α ⇆ β and β ⇆ γ reversible phase transitions were observed. The β ⇆ γ one is ferroelastic ⇆ paraelastic but surprisingly the α ⇆ β transition also exhibits a ferroelastic character, with a 90 ° switching of the a and b axis on cooling and/or, more scarcely, on heating. Impedance spectroscopy measurements were carried out using platelet shaped single crystals with well developed (001) faces. The corresponding σ ∥ (001 plane) and σ ⊥ ( c direction) bulk conductivities were obtained and compared with values from ceramic pellets, σ ∥ values are close to those characterizing the pellets, and the anisotropy of the conductivity is evidenced by σ ∥ values about 2 orders of magnitude larger than σ ⊥ ones. Slope changes observed in Arrhenius plots are in agreement with the phase transitions.