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Correlation of irradiation-induced yellow color with the O - hole center in tourmaline

Authors :
Krambrock, K.
Pinheiro, M. V. B.
Guedes, K.J.
Medeiros, S.M.
Schweizer, S.
Spaeth, J.-M.
Source :
Physics and Chemistry of Minerals; 20040401, Vol. 31 Issue: 3 p168-175, 8p
Publication Year :
2004

Abstract

Tourmaline with the general formula XY <subscript>3</subscript> Z <subscript>6</subscript>(BO <subscript>3</subscript>) <subscript>3</subscript>Si <subscript>6</subscript>O <subscript>18</subscript>(OH,O) <subscript>3</subscript>(OH,F) and the trigonal space group R3 m ( C <subscript>3</subscript> <subscript>v</subscript> <superscript>5</superscript>) is known as a gemstone with great variety of colors. Some color centers are related to transition metal ions, and others to electron or hole traps. In this paper we report on a combined study using electron paramagnetic resonance (EPR), electron nuclear double resonance (ENDOR), and the optical detection of EPR (ODEPR) on a yellow color center produced by ?-irradiation in colorless Li-bearing elbaite tourmaline from Brazil. The color center is an O <superscript>-</superscript> hole trap center, which is stabilized within the plane spanned by three Y sites, and is located in the structural channels formed by Si <subscript>6</subscript>O <subscript>18</subscript>. We suggest that two of the Y sites are substituted by <superscript>27</superscript>Al and the other by <superscript>6,7</superscript>Li. During the irradiation process atomic hydrogen H <superscript>0</superscript> is also produced, which shows the same thermal stability as the hole center (250 °C). Therefore, we assign H <superscript>0</superscript> to be the local charge compensator for the hole trap. From the ODEPR measurements we conclude that the yellow color is caused by the O <superscript>-</superscript> hole center. The large negative isotropic Al superhyperfine interaction of the O <superscript>-</superscript> hole trap center is consistent with a calculation of the transferred hyperfine interactions by exchange polarization supporting the proposed defect model of an O <superscript>-</superscript> at the O <subscript>1</subscript> sites, whereby the O <superscript>-</superscript> is relaxed into the plane formed by three Y ions.

Details

Language :
English
ISSN :
03421791 and 14322021
Volume :
31
Issue :
3
Database :
Supplemental Index
Journal :
Physics and Chemistry of Minerals
Publication Type :
Periodical
Accession number :
ejs5820946
Full Text :
https://doi.org/10.1007/s00269-003-0378-3