Prehnite at the Atomic Scale: Al/Si Ordering, Hydrogen Environment, and High-Pressure Behavior
dc.contributor.author | Detrie, Theresa A. | en |
dc.contributor.committeechair | Ross, Nancy L. | en |
dc.contributor.committeemember | Angel, Ross J. | en |
dc.contributor.committeemember | Ballaran, Tiziana Boffa | en |
dc.contributor.department | Geosciences | en |
dc.date.accessioned | 2014-03-14T20:47:53Z | en |
dc.date.adate | 2008-12-10 | en |
dc.date.available | 2014-03-14T20:47:53Z | en |
dc.date.issued | 2008-11-03 | en |
dc.date.rdate | 2008-12-10 | en |
dc.date.sdate | 2008-11-14 | en |
dc.description.abstract | The mineral prehnite, Ca2(Al,Fe,Mn)(AlSi3O10)(OH)2, is a layered structure consisting of double-sheets of (Al,Si)O4 and SiO4 tetrahedra alternating with single sheets of AlO4(OH)2 octahedra. To understand the ordering in the structure and differences between various samples of prehnite, single-crystal X-ray diffraction data at ambient conditions were collected on four single crystals of prehnite from different localities. The positions of the H atoms have been determined for the first time, from a combination of X-ray and neutron diffraction data. The equation of state and high-pressure behavior of prehnite have been investigated using single-crystal X-ray diffraction up to 9.75(3) GPa. A second-order Birch–Murnaghan equation of state fit to the isothermal P-V data to 8.7 GPa yields a bulk modulus, K = 109.29(18) GPa. Structural data collected at high pressures indicate that the structure compresses uniformly. Above 8.7 GPa there is additional softening of the volume and the b-axis related to polyhedral tilting. However, the average structure is maintained across the transition. Ambient and high-pressure Raman and synchrotron infrared spectra were collected from 1 bar to 20 GPa. Raman spectra measured at ambient conditions of four prehnite crystals with different compositions confirmed that there are no structural changes with different compositions. High-pressure results showed the majority of modes shift to higher frequencies (in a smooth, linear fashion) with increasing pressure. The greatest change in the spectra is the softening of the modes in the OH-stretching region above 9 GPa, thought to be related to the polyhedral tilting around the H environment. | en |
dc.description.degree | Master of Science | en |
dc.identifier.other | etd-11142008-092001 | en |
dc.identifier.sourceurl | http://scholar.lib.vt.edu/theses/available/etd-11142008-092001/ | en |
dc.identifier.uri | http://hdl.handle.net/10919/35702 | en |
dc.publisher | Virginia Tech | en |
dc.relation.haspart | ETD_t.detrie_MSv6.pdf | en |
dc.rights | In Copyright | en |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en |
dc.subject | prehnite | en |
dc.subject | high-pressure | en |
dc.subject | X-ray diffraction | en |
dc.subject | neutron diffraction | en |
dc.subject | spectroscopy | en |
dc.subject | hydrogen | en |
dc.title | Prehnite at the Atomic Scale: Al/Si Ordering, Hydrogen Environment, and High-Pressure Behavior | en |
dc.type | Thesis | en |
thesis.degree.discipline | Geosciences | en |
thesis.degree.grantor | Virginia Polytechnic Institute and State University | en |
thesis.degree.level | masters | en |
thesis.degree.name | Master of Science | en |
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