2009
DOI: 10.1016/j.jssc.2009.09.031
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Evidence of local defects in the oxygen excess apatite La9.67(SiO4)6O2.5 from high resolution neutron powder diffraction

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Cited by 45 publications
(38 citation statements)
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“…A vanadium sample holder was used. Since a few structural data had already been reported on Mg doped compound [18,41,42] and we recently published the structure of La 9.67 ❒ 0.33 Si 6 O 26.5 [6], neutron diffraction data were collected on La 9 Ba 1 Si 6 O 26.5 , La 9.67 ❒ 0.33 Si 5.5 Ge 0.5 O 26.5 , and La 9.83 ❒ 0.17 Si 5.5 Al 0.5 O 26.5 powders only. Experiments at high temperatures, 700°C, 800°C and 900°C, corresponding to the operating temperatures of the SOFCs were also carried out on La 9 Ba 1 Si 6 O 26.5 .…”
Section: Methodsmentioning
confidence: 99%
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“…A vanadium sample holder was used. Since a few structural data had already been reported on Mg doped compound [18,41,42] and we recently published the structure of La 9.67 ❒ 0.33 Si 6 O 26.5 [6], neutron diffraction data were collected on La 9 Ba 1 Si 6 O 26.5 , La 9.67 ❒ 0.33 Si 5.5 Ge 0.5 O 26.5 , and La 9.83 ❒ 0.17 Si 5.5 Al 0.5 O 26.5 powders only. Experiments at high temperatures, 700°C, 800°C and 900°C, corresponding to the operating temperatures of the SOFCs were also carried out on La 9 Ba 1 Si 6 O 26.5 .…”
Section: Methodsmentioning
confidence: 99%
“…Indeed, they are chemically stable and exhibit good ionic conduction properties [3][4][5]. With general formula La 10−x □ x (SiO 4 ) 6 O 2 + 3x/2 , they crystallised in the P6 3 /m space group [6] and their structure is built upon [SiO 4 ] tetrahedra spaced with La cations located in two sites: a 7-coordinated one, 4f, and a 9-coordinated one, 6h, and two extra oxide ions located in channels along the c-axis, bordered by the La(6h) cation. As calcium phosphate apatites, the structure of these lanthanum silicates is very flexible, and it can accept a wide range of partial substitutions on both the Si and La sites.…”
Section: Introductionmentioning
confidence: 99%
“…For the silicates it has been shown that oxygen excess in the range, 0 ≤ x ≤ 0.5 is possible, while higher oxygen content, 0 ≤ x ≤ 1.0 has been achieved for the germanates [13,18,20,21]. For the silicate series, the exact location of extrastoichiometric oxygen, x, has attracted some controversy, with reports of interstitial sites close to the SiO4 tetrahedra, while in other studies, mobile oxygen at the centre of the channels has been claimed [4,8,9,10,12,13,23,27,35,36]. For the germanates, the situation appears more clearcut, with computer modeling, neutron diffraction and Raman studies indicating occupancy by oxygen sites close to the GeO4 tetrahedra leading to the formation of five coordinate Ge [10, 20-22, 37, 40].…”
Section: Introductionmentioning
confidence: 99%
“…Guillot et al investigated the crystal structure of La 9.67 -(SiO 4 ) 6 O 2.5 using primarily Rietveld analysis of NPD patterns collected at 3, 100, and 300 K. 87) They refined the structure parameters on the basis of the model with space group P6 3 /m. They compared R wp values for the models with and without the O5(12i) site, and the structure model with the O5(12i) site was concluded to be promising.…”
Section: Crystal Structure Model After the Discovery Of Oxygen-ion Comentioning
confidence: 99%