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Title: Epitaxial Growth of Gibbsite Sheets on the Basal Surface of Muscovite Mica

Abstract

The growth of aluminum (oxyhydr)oxide films on the basal surface of muscovite mica is an excellent model system for studying mineral nucleation, growth, and reactivity. Using off-specular crystal truncation rod X-ray scattering, we have determined the atomic-scale epitaxial relationships between muscovite and monolayer overgrowths of a gibbsite-like material. Here, we observe that dioctahedral sheets of aluminum (oxyhydr)oxide grow in three structurally distinct domains, separated by antiphase boundaries. Vacancies in the dioctahedral sheets overlie either the silicate tetrahedra or the ditrigonal cavities of the underlying muscovite surface. High-resolution atomic force microscopy indicates lateral island sizes of ~10 nm separated by 1–2 nm spaces. Together, the X-ray and microscopy data provide insights into the coordination chemistry and morphology of films formed by heterogeneous nucleation and growth.

Authors:
ORCiD logo [1];  [2]; ORCiD logo [3];  [4]; ORCiD logo [2]; ORCiD logo [3];  [5]
  1. Univ. of Chicago, Chicago, IL (United States). Center for Advanced Radiation Sources
  2. Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Univ. of Washington, Seattle, WA (United States)
  3. Argonne National Lab. (ANL), Argonne, IL (United States)
  4. Univ. of Hawai’i at Manoa, Honolulu, HI (United States)
  5. Univ. of Chicago, Chicago, IL (United States). Center for Advanced Radiation Sources, and James Franck Inst.
Publication Date:
Research Org.:
Univ. of Chicago, IL (United States); Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES). Chemical Sciences, Geosciences, and Biosciences Division; National Science Foundation (NSF); USDOE Office of Science (SC), Basic Energy Sciences (BES) (SC-22). Materials Sciences & Engineering Division
OSTI Identifier:
1580747
Alternate Identifier(s):
OSTI ID: 1596316; OSTI ID: 1608422
Grant/Contract Number:  
AC02-06CH11357; FG02-94ER14466; SC0019108; AC05-76RL01830; 1722969; 1541516
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Physical Chemistry. C
Additional Journal Information:
Journal Volume: 123; Journal Issue: 45; Journal ID: ISSN 1932-7447
Publisher:
American Chemical Society
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; antiphase; crystal truncation rod; epitaxy; gibbsite; heterogeneous nucleation and growth; muscovite

Citation Formats

Stubbs, Joanne E., Legg, Benjamin A., Lee, Sang Soo, Dera, Przemyslaw, De Yoreo, James J., Fenter, Paul, and Eng, Peter J. Epitaxial Growth of Gibbsite Sheets on the Basal Surface of Muscovite Mica. United States: N. p., 2019. Web. doi:10.1021/acs.jpcc.9b08219.
Stubbs, Joanne E., Legg, Benjamin A., Lee, Sang Soo, Dera, Przemyslaw, De Yoreo, James J., Fenter, Paul, & Eng, Peter J. Epitaxial Growth of Gibbsite Sheets on the Basal Surface of Muscovite Mica. United States. https://doi.org/10.1021/acs.jpcc.9b08219
Stubbs, Joanne E., Legg, Benjamin A., Lee, Sang Soo, Dera, Przemyslaw, De Yoreo, James J., Fenter, Paul, and Eng, Peter J. Mon . "Epitaxial Growth of Gibbsite Sheets on the Basal Surface of Muscovite Mica". United States. https://doi.org/10.1021/acs.jpcc.9b08219. https://www.osti.gov/servlets/purl/1580747.
@article{osti_1580747,
title = {Epitaxial Growth of Gibbsite Sheets on the Basal Surface of Muscovite Mica},
author = {Stubbs, Joanne E. and Legg, Benjamin A. and Lee, Sang Soo and Dera, Przemyslaw and De Yoreo, James J. and Fenter, Paul and Eng, Peter J.},
abstractNote = {The growth of aluminum (oxyhydr)oxide films on the basal surface of muscovite mica is an excellent model system for studying mineral nucleation, growth, and reactivity. Using off-specular crystal truncation rod X-ray scattering, we have determined the atomic-scale epitaxial relationships between muscovite and monolayer overgrowths of a gibbsite-like material. Here, we observe that dioctahedral sheets of aluminum (oxyhydr)oxide grow in three structurally distinct domains, separated by antiphase boundaries. Vacancies in the dioctahedral sheets overlie either the silicate tetrahedra or the ditrigonal cavities of the underlying muscovite surface. High-resolution atomic force microscopy indicates lateral island sizes of ~10 nm separated by 1–2 nm spaces. Together, the X-ray and microscopy data provide insights into the coordination chemistry and morphology of films formed by heterogeneous nucleation and growth.},
doi = {10.1021/acs.jpcc.9b08219},
journal = {Journal of Physical Chemistry. C},
number = 45,
volume = 123,
place = {United States},
year = {Mon Oct 14 00:00:00 EDT 2019},
month = {Mon Oct 14 00:00:00 EDT 2019}
}

Journal Article:
Free Publicly Available Full Text
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Cited by: 8 works
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Figures / Tables:

Figure 1 Figure 1: In-situ AFM images taken prior to, during, and after film growth. (a) High resolution image of a muscovite (001) surface in 10 mM HCl, showing the expected pseudo-hexagonal lattice. (b) Grown film imaged in-situ at 70 °C, showing ~57% coverage with islands. (c) Height profile of blue linemore » in (b), showing that the apparent film height is on the order of 6 Å. (d) Room temperature image of film after growth, with center region showing mechanical erosion to expose the underlying mica surface, demonstrating that the film is only one gibbsite layer thick. (e) High resolution imaging of a film after 90 hours aging, showing semi-crystalline linear features, but lacking perfect crystalline order.« less

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