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Science 11 June 1999:
Vol. 284. no. 5421, pp. 1788 - 1789
DOI: 10.1126/science.284.5421.1788

Perspectives

Also see the archival list of Science's Compass: Enhanced Perspectives

MANTLE GEOCHEMISTRY:
Enhanced: A Lesson from Ceramics

Alexandra Navrotsky

Understanding the processes in Earth's lower mantle requires detailed knowledge of the composition, phase, and physical properties of the mantle minerals, chiefly magnesium silicates with a perovskite structure. Navrotsky (page 1788) argues that lessons can be learned from ceramic perovskites that have been studied in more detail than the silicate perovskites. A defect formation mechanism involving oxygen vacancy formation, coupled with facile hydration, may be operative in the mantle perovskites, with significant consequences for flow properties and water transport in the lower mantle.


The author is at the Thermochemistry Facility, Department of Chemical Engineering and Materials Science, University of California, Davis, CA 95616, USA. E-mail: anavrotsky{at}ucdavis.edu

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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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Water in Earth's Lower Mantle.
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