Dehydration phase transitions in new aluminium arsenate minerals from the Penberthy Croft mine, Cornwall, UK
dc.contributor.author | Grey, IE | en_AU |
dc.contributor.author | Brand, HEA | en_AU |
dc.contributor.author | Betterton, J | en_AU |
dc.date.accessioned | 2021-12-07T03:52:00Z | en_AU |
dc.date.available | 2021-12-07T03:52:00Z | en_AU |
dc.date.issued | 2016-12 | en_AU |
dc.date.statistics | 2021-11-08 | en_AU |
dc.description.abstract | Bettertonite, [Al6(AsO4)3(OH)9(H2O)5]•11H2O and penberthycroftite, [Al6(AsO4)3(OH)9(H2O)5].8H2O, two new minerals from the Penberthy Croft mine, Cornwall, have flexible layer structures based on corner-connected heteropolyhedral columns. Their response to dehydration on heating was studied using in situ synchrotron powder X-ray diffraction at temperatures in the range -53 to 157°C. The bettertonite sample transforms to penberthycroftite in a narrow temperature range of 67 to 97°C with a large (8%) contraction of the layer separation and a 6 Å sliding of adjacent layers relative to each other. Above 100°C a second phase transition occurs to a DL (displaced layer) phase, involving another 8% inter-layer contraction combined with a rotation of the columns. On heating the penberthycroftite sample the phase transition to the DL phase occurs at a lower temperature of ∼80°C. The DL phase is stable to a temperature of ∼120°C. At higher temperatures, increased rotation of the columns is accompanied by a progressive amorphization of the sample. Bettertonite, penberthycroftite and the DL phase exhibit negative thermal expansion (NTE) along all three axes with large NTE coefficients, of the order of-100 x 10 -6 °C-1. © 2016 The Mineralogical Society of Great Britain and Ireland | en_AU |
dc.identifier.citation | Grey, I. E., Brand, H. E. A. & Betterton, J. (2016). Dehydration phase transitions in new aluminium arsenate minerals from the Penberthy Croft mine, Cornwall, UK. Mineralogical Magazine, 80(7), 1205-1217. doi:10.1180/minmag.2016.080.126 | en_AU |
dc.identifier.issn | 0026-461X | en_AU |
dc.identifier.issue | 7 | en_AU |
dc.identifier.journaltitle | Mineralogical Magazine | en_AU |
dc.identifier.pagination | 1205-1217 | en_AU |
dc.identifier.uri | https://doi.org/10.1180/minmag.2016.080.126 | en_AU |
dc.identifier.uri | https://apo.ansto.gov.au/dspace/handle/10238/12369 | en_AU |
dc.identifier.volume | 80 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | Cambridge University Press | en_AU |
dc.subject | Phase transformations | en_AU |
dc.subject | Dehydration | en_AU |
dc.subject | Synchrotrons | en_AU |
dc.subject | X-ray diffraction | en_AU |
dc.subject | Minerals | en_AU |
dc.subject | Aluminium | en_AU |
dc.subject | United Kingdom | en_AU |
dc.subject | Mines | en_AU |
dc.title | Dehydration phase transitions in new aluminium arsenate minerals from the Penberthy Croft mine, Cornwall, UK | en_AU |
dc.type | Journal Article | en_AU |
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