By Topic

A high-temperature torsion apparatus for the high-resolution characterization of internal friction and creep in refractory metals and ceramics: Application to the seismic-frequency, dynamic response of Earth’s upper mantle

Sign In

Cookies must be enabled to login.After enabling cookies , please use refresh or reload or ctrl+f5 on the browser for the login options.

The purchase and pricing options are temporarily unavailable. Please try again later.
2 Author(s)
Gribb, Tye T. ; Department of Materials Science and Engineering, University of Wisconsin-Madison, Madison, Wisconsin 53706 ; Cooper, Reid F.

Your organization might have access to this article on the publisher's site. To check, click on this link:http://dx.doi.org/+10.1063/1.1148694 

The design and performance of a compact apparatus for the characterization of internal friction in simple shear at elevated temperature (≤1400 °C) and low frequencies (≤1 Hz) are described. High-temperature components are fabricated from a refractory molybdenum alloy that is straightforwardly machined. The apparatus has demonstrated, at high temperature, a torque resolution of 2×10-5 N m and an angular displacement resolution of 4×10-6 rad; for the specimen size we employ, these limits provide a shear stress and strain resolution of 2 kPa and 5×10-7, respectively. The apparatus, while applicable to dynamic and static mechanical analyses of any engineering material, was developed for the characterization of internal friction (attenuation) in synthetic silicate aggregates representative of Earth’s upper mantle; we discuss the constraints inherent in the required tests, as they affect apparatus design (including materials selection) and experimental protocol. Static and dynamic data at 1250 °C for a polycrystalline aggregate of ferromagnesian olivine of controlled, uniform (∼3 μm) grain size are presented and discussed.© 1998 American Institute of Physics.

Published in:

Review of Scientific Instruments  (Volume:69 ,  Issue: 2 )