Ultra-flexible framework breathing in response to dehydration in liskeardite, [(Al,Fe)16(AsO4)9(OH)21(H2O)11]·26H2O, a natural open-framework compound
dc.contributor.author | Grey, IE | en_AU |
dc.contributor.author | Brand, HEA | en_AU |
dc.contributor.author | Rumsey, MS | en_AU |
dc.contributor.author | Gozukara, Y | en_AU |
dc.date.accessioned | 2021-12-07T22:17:10Z | en_AU |
dc.date.available | 2021-12-07T22:17:10Z | en_AU |
dc.date.issued | 2015-05-02 | en_AU |
dc.date.statistics | 2021-11-12 | en_AU |
dc.description.abstract | Dehydration of the natural open-framework compound, liskeardite, [(Al,Fe)16(AsO4)9(OH)21(H2O)11]·26H2O, is accompanied by a change in the sign of the thermal expansion from positive to negative above room temperature, and at ~100 °C the structure undergoes a dramatic 2D contraction by co-operative rotation of heteropolyhedral columns that constitute the framework walls. Monoclinic liskeardite, I112 with a≈b≈24.7 Å, c ≈7.8 Å and β≈90° is transformed to a tetragonal phase, I-4 with a≈20.6 Å, c ≈7.7 Å. The associated 30% decrease in volume is unprecedented in inorganic microporous compounds. The flexibility of the contraction is related to the double-hinged nature of the column rotations about [001]. Octahedra in adjacent columns are interconnected by corner-sharing with the two pairs of anions forming opposing edges of AsO4 tetrahedra, so a double-hinged rotation mechanism operates. Thermal analysis and mass spectroscopic results for liskeardite show that the phase transition at ~100 °C is related to removal of the channel water. The tetragonal phase shows exceptionally large NTE behaviour. Over the temperature range 148–178 the NTE along a and b is close to linear with a magnitude of the order of −900×10−6 °C−1. The contraction along the channel direction is smaller but still appreciable at −200×10−6 °C−1. © 2015 Elsevier Inc. | en_AU |
dc.identifier.citation | Grey, I. E., Brand, H. E.A., Rumsey, M. S., & Gozukara, Y. (2015). Ultra-flexible framework breathing in response to dehydration in liskeardite, [(Al,Fe)16(AsO4)9(OH)21(H2O)11]·26H2O, a natural open-framework compound. Journal of Solid State Chemistry, 228, 146-152. doi:10.1016/j.jssc.2015.04.035 | en_AU |
dc.identifier.issn | 0022-4596 | en_AU |
dc.identifier.journaltitle | Journal of Solid State Chemistry | en_AU |
dc.identifier.pagination | 146-152 | en_AU |
dc.identifier.uri | https://doi.org/10.1016/j.jssc.2015.04.035 | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/dspace/handle/10238/12382 | en_AU |
dc.identifier.volume | 228 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Elsevier | en_AU |
dc.subject | X-ray diffraction | en_AU |
dc.subject | Volume | en_AU |
dc.subject | Structural models | en_AU |
dc.subject | Dehydration | en_AU |
dc.subject | Thermal expansion | en_AU |
dc.subject | Phase transformations | en_AU |
dc.subject | Inorganic compounds | en_AU |
dc.subject | Rotation | en_AU |
dc.title | Ultra-flexible framework breathing in response to dehydration in liskeardite, [(Al,Fe)16(AsO4)9(OH)21(H2O)11]·26H2O, a natural open-framework compound | en_AU |
dc.type | Journal Article | en_AU |
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