Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.

Site Tools

  • AAAS
  • Subscribe
  • Feedback

Site Search

Search Advanced

Science 26 September 1997:
Vol. 277. no. 5334, pp. 1965 - 1967
DOI: 10.1126/science.277.5334.1965

Reports

Increased Compressibility of Pseudobrookite-Type MgTi2O5 Caused by Cation Disorder

Robert M. Hazen, * Hexiong Yang

Compressibilities were determined for four pseudobrookite-type magnesium titanate (MgTi2O5) samples with different degrees of Mg-Ti disorder. Compressibilities of a and c axes in disordered MgTi2O5 were 10% and 7% greater, respectively, than those of a relatively ordered sample. The estimated bulk moduli for fully ordered and disordered MgTi2O5 are 167 ± 1 and 158 ± 1 gigapascals, respectively. This difference is an order of magnitude greater than that predicted by bulk modulus-volume systematics. Cation order, in addition to composition and structure information, is thus important when documenting the elasticity of crystalline phases. Elastic constants of mantle silicates that are subject to pressure-induced cation ordering must be reevaluated.

Geophysical Laboratory and Center for High Pressure Research, Carnegie Institution of Washington, 5251 Broad Branch Road NW, Washington, DC 20015, USA.
*   To whom correspondence should be addressed. E-mail: hazen{at}gl.ciw.edu


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Cation distribution in MgFe2O4 vs. pressure and temperature: Experiments in a "piston-cylinder" apparatus.
A. I. Turkin and V. A. Drebushchak (2005)
American Mineralogist 90, 764-767
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)