Sodalite, Na 4 Si 3 Al 3 O 12 Cl: structure and ionic mobility at high temperatures by neutron diffraction

Crystal data: Na 4 Si 3 Al 3 O 12 Cl, cubic, space group P 43 n , Z = 2, F (000) = 233.06 fm, μ n = 0.06 cm −1 , lattice parameter a o  (Å) [ T ] (K) at eight temperatures: 8.882 (1) [295]; 8.902 (2) [500]; 8.912 (1) [600]; 8.923 (1) [700] 8.951 (2) [800]; 8.971(1) [900]; 8.988 (1) [1000]; 9.037 (1)...

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Veröffentlicht in:Acta crystallographica. Section B, Structural science Structural science, 1996-08, Vol.52 (4), p.616-627
Hauptverfasser: McMullan, R. K., Ghose, S., Haga, N., Schomaker, V.
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Ghose, S.
Haga, N.
Schomaker, V.
description Crystal data: Na 4 Si 3 Al 3 O 12 Cl, cubic, space group P 43 n , Z = 2, F (000) = 233.06 fm, μ n = 0.06 cm −1 , lattice parameter a o  (Å) [ T ] (K) at eight temperatures: 8.882 (1) [295]; 8.902 (2) [500]; 8.912 (1) [600]; 8.923 (1) [700] 8.951 (2) [800]; 8.971(1) [900]; 8.988 (1) [1000]; 9.037 (1) [1200]. The crystal structure has been determined at six temperatures (295 ≤ T ≤ 1200 K) based on neutron diffraction data with (sin θ/λ ) < 0.80 Å −1 . Besides conventional parameters, the least-squares refinement model included thermal tensor parameters up to fourth-order for sodium and chlorine (295 ≤ T ≤ 1200 K) and up to third-order for oxygen ( T ≥ 700 K), together with the 1:1 coupled site occupancy factors of sodium and chlorine ( T = 1200 K). The indices-of-fit, wR ( F 2 ), are in the range 0.015–0.028 with observation-to-parameter ratios from 7.0 to 8.6. Bond lengths and angles in the aluminosilicate framework have average e.s.d.'s less than 0.002 Å and 0.08°. Between 295 and 1200 K, the observed Si—O (Al—O) bond lengths differ by −0.015 Å (−0.012 Å); corrections for librating rigid SiO 4 (AlO 4 ) groups change the difference to +0.004 Å (+0.006 Å), compared with the 295 K value of 1.620 Å (1.741 Å). The unique Si—O—Al angle increases from 138.24° (295 K) to 146.87° (1200 K), while the Si and Al valence angles are virtually unchanged. Between 295 and 1200 K the [Na 4 Cl] clusters expand with increases in the Na—Cl bond lengths of 0.200 Å, with simultaneous increases in Na—O bond lengths of 0.145 Å and decreases in the shortest Na...O contact distances of 0.126 Å. The thermal expansion of sodalite is attributed to the increasing amplitudes of coupled translational motion of the Na + ions and the librational motion of the [Al/ SiO 4 ] tetrahedra, leading to the untwisting of the aluminosilicate framework. Maps of the probability density functions for Na + and Cl − indicate ionic diffusion paths along (111) directions. There is a finite probability of finding the Na + ion within the plane of the next-nearest O atoms, suggesting that Na + jumps from an occupied to an unoccupied site in the next-nearest cage through the six-membered ring of [Al/SiO 4 ] tetrahedra.
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The indices-of-fit, wR ( F 2 ), are in the range 0.015–0.028 with observation-to-parameter ratios from 7.0 to 8.6. Bond lengths and angles in the aluminosilicate framework have average e.s.d.'s less than 0.002 Å and 0.08°. Between 295 and 1200 K, the observed Si—O (Al—O) bond lengths differ by −0.015 Å (−0.012 Å); corrections for librating rigid SiO 4 (AlO 4 ) groups change the difference to +0.004 Å (+0.006 Å), compared with the 295 K value of 1.620 Å (1.741 Å). The unique Si—O—Al angle increases from 138.24° (295 K) to 146.87° (1200 K), while the Si and Al valence angles are virtually unchanged. Between 295 and 1200 K the [Na 4 Cl] clusters expand with increases in the Na—Cl bond lengths of 0.200 Å, with simultaneous increases in Na—O bond lengths of 0.145 Å and decreases in the shortest Na...O contact distances of 0.126 Å. 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Section B, Structural science</title><description>Crystal data: Na 4 Si 3 Al 3 O 12 Cl, cubic, space group P 43 n , Z = 2, F (000) = 233.06 fm, μ n = 0.06 cm −1 , lattice parameter a o  (Å) [ T ] (K) at eight temperatures: 8.882 (1) [295]; 8.902 (2) [500]; 8.912 (1) [600]; 8.923 (1) [700] 8.951 (2) [800]; 8.971(1) [900]; 8.988 (1) [1000]; 9.037 (1) [1200]. The crystal structure has been determined at six temperatures (295 ≤ T ≤ 1200 K) based on neutron diffraction data with (sin θ/λ ) &lt; 0.80 Å −1 . Besides conventional parameters, the least-squares refinement model included thermal tensor parameters up to fourth-order for sodium and chlorine (295 ≤ T ≤ 1200 K) and up to third-order for oxygen ( T ≥ 700 K), together with the 1:1 coupled site occupancy factors of sodium and chlorine ( T = 1200 K). The indices-of-fit, wR ( F 2 ), are in the range 0.015–0.028 with observation-to-parameter ratios from 7.0 to 8.6. Bond lengths and angles in the aluminosilicate framework have average e.s.d.'s less than 0.002 Å and 0.08°. Between 295 and 1200 K, the observed Si—O (Al—O) bond lengths differ by −0.015 Å (−0.012 Å); corrections for librating rigid SiO 4 (AlO 4 ) groups change the difference to +0.004 Å (+0.006 Å), compared with the 295 K value of 1.620 Å (1.741 Å). The unique Si—O—Al angle increases from 138.24° (295 K) to 146.87° (1200 K), while the Si and Al valence angles are virtually unchanged. Between 295 and 1200 K the [Na 4 Cl] clusters expand with increases in the Na—Cl bond lengths of 0.200 Å, with simultaneous increases in Na—O bond lengths of 0.145 Å and decreases in the shortest Na...O contact distances of 0.126 Å. The thermal expansion of sodalite is attributed to the increasing amplitudes of coupled translational motion of the Na + ions and the librational motion of the [Al/ SiO 4 ] tetrahedra, leading to the untwisting of the aluminosilicate framework. 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Section B, Structural science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>McMullan, R. K.</au><au>Ghose, S.</au><au>Haga, N.</au><au>Schomaker, V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Sodalite, Na 4 Si 3 Al 3 O 12 Cl: structure and ionic mobility at high temperatures by neutron diffraction</atitle><jtitle>Acta crystallographica. Section B, Structural science</jtitle><date>1996-08-01</date><risdate>1996</risdate><volume>52</volume><issue>4</issue><spage>616</spage><epage>627</epage><pages>616-627</pages><issn>0108-7681</issn><abstract>Crystal data: Na 4 Si 3 Al 3 O 12 Cl, cubic, space group P 43 n , Z = 2, F (000) = 233.06 fm, μ n = 0.06 cm −1 , lattice parameter a o  (Å) [ T ] (K) at eight temperatures: 8.882 (1) [295]; 8.902 (2) [500]; 8.912 (1) [600]; 8.923 (1) [700] 8.951 (2) [800]; 8.971(1) [900]; 8.988 (1) [1000]; 9.037 (1) [1200]. The crystal structure has been determined at six temperatures (295 ≤ T ≤ 1200 K) based on neutron diffraction data with (sin θ/λ ) &lt; 0.80 Å −1 . Besides conventional parameters, the least-squares refinement model included thermal tensor parameters up to fourth-order for sodium and chlorine (295 ≤ T ≤ 1200 K) and up to third-order for oxygen ( T ≥ 700 K), together with the 1:1 coupled site occupancy factors of sodium and chlorine ( T = 1200 K). The indices-of-fit, wR ( F 2 ), are in the range 0.015–0.028 with observation-to-parameter ratios from 7.0 to 8.6. Bond lengths and angles in the aluminosilicate framework have average e.s.d.'s less than 0.002 Å and 0.08°. Between 295 and 1200 K, the observed Si—O (Al—O) bond lengths differ by −0.015 Å (−0.012 Å); corrections for librating rigid SiO 4 (AlO 4 ) groups change the difference to +0.004 Å (+0.006 Å), compared with the 295 K value of 1.620 Å (1.741 Å). The unique Si—O—Al angle increases from 138.24° (295 K) to 146.87° (1200 K), while the Si and Al valence angles are virtually unchanged. Between 295 and 1200 K the [Na 4 Cl] clusters expand with increases in the Na—Cl bond lengths of 0.200 Å, with simultaneous increases in Na—O bond lengths of 0.145 Å and decreases in the shortest Na...O contact distances of 0.126 Å. The thermal expansion of sodalite is attributed to the increasing amplitudes of coupled translational motion of the Na + ions and the librational motion of the [Al/ SiO 4 ] tetrahedra, leading to the untwisting of the aluminosilicate framework. Maps of the probability density functions for Na + and Cl − indicate ionic diffusion paths along (111) directions. There is a finite probability of finding the Na + ion within the plane of the next-nearest O atoms, suggesting that Na + jumps from an occupied to an unoccupied site in the next-nearest cage through the six-membered ring of [Al/SiO 4 ] tetrahedra.</abstract><doi>10.1107/S0108768196004132</doi><tpages>12</tpages></addata></record>
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title Sodalite, Na 4 Si 3 Al 3 O 12 Cl: structure and ionic mobility at high temperatures by neutron diffraction
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