Home First principles study of water adsorption on the (100) surface of zircon: Implications for zircon dissolution
Article
Licensed
Unlicensed Requires Authentication

First principles study of water adsorption on the (100) surface of zircon: Implications for zircon dissolution

  • Etienne Balan EMAIL logo , Francesco Mauri , Jean-Pierre Muller and Georges Calas
Published/Copyright: March 26, 2015
Become an author with De Gruyter Brill

Abstract

We have studied the interaction of aqueous species with the (100) face of zircon using first-principles quantum mechanical calculations. Adsorption energy of molecular water on the Zr Lewis site is 1.27 eV per molecule, whereas the energy of dissociative adsorption is only 0.84 eV per molecule. Thus, the non-dissociative adsorption of water is strongly preferred with respect to the dissociative adsorption on the (100) face of zircon. Such behavior, which is related to the weak ability of the surface structure to relax, is changed by a 5% increase of the surface cell parameters. From our theoretical results, we propose that the exceptional resistance of zircon to dissolution may be related to the strong acidity of the Zr-O-Si bridging O atoms, which promotes the associative adsorption of water on the (100) surface of zircon.

Received: 2000-10-30
Accepted: 2001-3-5
Published Online: 2015-3-26
Published in Print: 2001-7-1

© 2015 by Walter de Gruyter Berlin/Boston

Articles in the same Issue

  1. Calcite inclusions in forsterite
  2. The induced thermoluminescence and thermal history of plagioclase feldspars
  3. Characterization and comparison of structural and compositional features of planetary quadrilateral pyroxenes by Raman spectroscopy
  4. A P21/c-C2/c high-pressure phase transition in Ca0.5Mg1.5Si2O6 clinopyroxene
  5. Energy-filtered transmission electron microscopy (EFTEM) of intergrown pyroxenes
  6. TEM analysis of microbial mediated sedimentation and lithification in modern marine stromatolites
  7. Mineralogy of a natural As-rich hydrous ferric oxide coprecipitate formed by mixing of hydrothermal fluid and seawater: Implications regarding surface complexation and color banding in ferrihydrite deposits
  8. A C/MoS2 mixed-layer phase (MoSC) occurring in metalliferous black shales from southern China, and new data on jordisite
  9. Step edges on galena (100): Probing the basis for defect driven surface reactivity at the atomic scale
  10. Solubility study of Ti,Zr-based ceramics designed to immobilize long-lived radionuclides
  11. Characterization of synthetic Cs-Li cancrinite grown in a butanediol-water system: An NMR spectroscopic and Rietveld refinement study
  12. Optical spectra of Co2+ in three synthetic silicate minerals
  13. Spectroscopic standards for four- and fivefold-coordinated Fe2+ in oxygen-based minerals
  14. Hydrous species in crystalline and metamict titanites
  15. First principles study of water adsorption on the (100) surface of zircon: Implications for zircon dissolution
  16. A molecular dynamics study of the glass transition in CaAl2Si2O8: Thermodynamics and tracer diffusion
  17. The crystal structure of aravaipaite
  18. Letter. Feldspar thermometry in ultrahigh-temperature metamorphic rocks: Evidence of crustal metamorphism attaining ~1100 °C in the Archean Napier Complex, East Antarctica
Downloaded on 16.9.2025 from https://www.degruyterbrill.com/document/doi/10.2138/am-2001-0715/html
Scroll to top button