High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites

Structural refinements have been completed using data recorded for a Mg-rich cordierite at 24°C, 375°C, 775°C and 24°C (after heating to 775°C) and for an Fe-rich cordierite at 24°C and 375°C. The mean T-0 bond lengths in both cordierites remain unchanged but the mean octahedral bonds (M-0) lengthen...

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Main Author: Hochella, Michael F. Jr.
Other Authors: Geological Sciences
Format: Others
Language:en
Published: Virginia Tech 2014
Subjects:
Online Access:http://hdl.handle.net/10919/43955
http://scholar.lib.vt.edu/theses/available/etd-07282010-020312/
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spelling ndltd-VTETD-oai-vtechworks.lib.vt.edu-10919-439552021-10-09T05:25:58Z High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites Hochella, Michael F. Jr. Geological Sciences Gibbs, Gerald V. Ribbe, Paul H. Ross, F. K. Bloss, F. Donald anisotropic expansion LD5655.V855 1977.H62 Structural refinements have been completed using data recorded for a Mg-rich cordierite at 24°C, 375°C, 775°C and 24°C (after heating to 775°C) and for an Fe-rich cordierite at 24°C and 375°C. The mean T-0 bond lengths in both cordierites remain unchanged but the mean octahedral bonds (M-0) lengthen upon heating. The unusually low thermal expansion of the Mg-cordierite is the result of its relatively "rigid" tetrahedral framework and the anisotropic expansion of octahedra isolated from each other. This anisotropic expansion leads to a slight rotation of the six-membered rings, a concomitant collapse of the structure parallel to c, and an expansion parallel to a and b. In the Fe-cordierite, the Fe-octahedron is more flattened, resulting in c being smaller and a and b being larger than the cell dimensions in the Mg-cordierite. Upon heating Fe-cordierite, there is no evidence for a rotation of the rings and a, b and c increase as the M-O bonds expand. A re-examination of the water orientation in the cavities of the Mg-cordierite using neutron and X-ray Δp maps confirms the orientation obtained previously by spectroscopic methods for type I water, i.e., H-O-H near (100) with the H-H vector nearly parallel to e. However, no evidence was found in the Δp maps for type II water. A peak ascribed to the alkali atoms that centers the six-membered ring becomes elongated parallel to a upon heating through 375°C, while the peak ascribed to the oxygen associated with H2O is absent in the Mg-cordierite at 775°C and in the Fe-cordierite at 375°C. After heating the Mg-cordierite to 775°C the peak reappeared in the Δp maps computed from data recorded at 24°C, but it no longer showed an elongation parallel to a as it did before heating. Master of Science 2014-03-14T21:41:28Z 2014-03-14T21:41:28Z 1977-07-05 2010-07-28 2010-07-28 2010-07-28 Thesis Text etd-07282010-020312 http://hdl.handle.net/10919/43955 http://scholar.lib.vt.edu/theses/available/etd-07282010-020312/ en OCLC# 06828424 LD5655.V855_1977.H62.pdf In Copyright http://rightsstatements.org/vocab/InC/1.0/ 110 leaves BTD application/pdf application/pdf Virginia Tech
collection NDLTD
language en
format Others
sources NDLTD
topic anisotropic expansion
LD5655.V855 1977.H62
spellingShingle anisotropic expansion
LD5655.V855 1977.H62
Hochella, Michael F. Jr.
High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
description Structural refinements have been completed using data recorded for a Mg-rich cordierite at 24°C, 375°C, 775°C and 24°C (after heating to 775°C) and for an Fe-rich cordierite at 24°C and 375°C. The mean T-0 bond lengths in both cordierites remain unchanged but the mean octahedral bonds (M-0) lengthen upon heating. The unusually low thermal expansion of the Mg-cordierite is the result of its relatively "rigid" tetrahedral framework and the anisotropic expansion of octahedra isolated from each other. This anisotropic expansion leads to a slight rotation of the six-membered rings, a concomitant collapse of the structure parallel to c, and an expansion parallel to a and b. In the Fe-cordierite, the Fe-octahedron is more flattened, resulting in c being smaller and a and b being larger than the cell dimensions in the Mg-cordierite. Upon heating Fe-cordierite, there is no evidence for a rotation of the rings and a, b and c increase as the M-O bonds expand. A re-examination of the water orientation in the cavities of the Mg-cordierite using neutron and X-ray Δp maps confirms the orientation obtained previously by spectroscopic methods for type I water, i.e., H-O-H near (100) with the H-H vector nearly parallel to e. However, no evidence was found in the Δp maps for type II water. A peak ascribed to the alkali atoms that centers the six-membered ring becomes elongated parallel to a upon heating through 375°C, while the peak ascribed to the oxygen associated with H2O is absent in the Mg-cordierite at 775°C and in the Fe-cordierite at 375°C. After heating the Mg-cordierite to 775°C the peak reappeared in the Δp maps computed from data recorded at 24°C, but it no longer showed an elongation parallel to a as it did before heating. === Master of Science
author2 Geological Sciences
author_facet Geological Sciences
Hochella, Michael F. Jr.
author Hochella, Michael F. Jr.
author_sort Hochella, Michael F. Jr.
title High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
title_short High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
title_full High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
title_fullStr High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
title_full_unstemmed High temperature crystal chemistry of hydrous Mg- and Fe-rich cordierites
title_sort high temperature crystal chemistry of hydrous mg- and fe-rich cordierites
publisher Virginia Tech
publishDate 2014
url http://hdl.handle.net/10919/43955
http://scholar.lib.vt.edu/theses/available/etd-07282010-020312/
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