Paramagnetic Defect Centers in Hydrothermal Kaolinite from an Altered Tuff in the Nopal Uranium Deposit, Chihuahua, Mexico

Jean-Pierre Muller1, 3, Philippe Ildefonse2, 3 and Georges Calas3
1 O.R.S.T.O.M., Département T.O.A., 75480 Paris Cedex 10, France
2 U.F.R. Sciences Physiques de la Terre, Université Paris 7 2 Place Jussieu, 75251 Paris Cedex 05, France
3 Laboratoire de Minéralogie-Cristallographie, UA CNRS 09, Universités Paris 6 et 7 4 Place Jussieu, 75252 Paris Cedex 05, France

Abstract: Point defect centers in hydrothermal kaolinite have been investigated using electron paramagnetic resonance (EPR). Kaolinite was sampled in petrographically well-defined materials coming from uranium-rich hydrothermally altered volcanic tufts (Nopal I uranium deposit, Chihuahua, Mexico), which show extensive kaolinization and an intense redistribution of uranium. Several kaolinite parageneses were defined according to their origin (fissure fillings and feldspar pseudomorphs); their location relative to the U6+ mineralization at the scale of the deposit (mineralized breccia pipe vs. barren surrounding rhyolitic tufts), and at the scale of mineral assemblages; and their crystal chemistry.

Two types of centers of axial symmetry were identified (A- and A′-centers) and represent positive holes trapped on apical oxygens (Si—O--centers). A-centers were stable to 400°C, whereas A′-centers annealed at 350°C. A relation between defect-center concentration and U content demonstrates that natural irradiation was responsible for these centers. On the other hand, defect-center concentration was not directly linked to the origin (fissural or feldspar pseudomorph) or the crystal chemistry (structural order and substitutional Fe3+ content) of the kaolinite, According to petrographic data, and with respect to the relative thermal stability of A- and A′-centers, two successive irradiations of kaolinite were evidenced: (1) originally during crystallization of kaolinite from radioactive hydrothermal solutions, and (2) permanently when kaolinite was in contact with secondary U-silicates, which led to the formation of A′-centers.

Because of the short half-life of U, these two radiation-induced centers were created by short-lived elements of the U-decay series. As a consequence, variations of defect-center concentration possibly reflect variations in radioactive disequilibrium during the history of the alteration system. This provides a unique tool for tracing the dynamics of the transfer of radionuclides in the geosphere: kaolinite may be used as a sensitive in situ dosimeter, which may be useful in the fields of weathering petrology and nuclear waste management.

Key Words: Defect centers • Electron paramagnetic resonance • Hydrothermal • Kaolinite • Natural radiation

Clays and Clay Minerals; December 1990 v. 38; no. 6; p. 600-608; DOI: 10.1346/CCMN.1990.0380605
© 1990, The Clay Minerals Society
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