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 EARTHSUPPER-MANTLE
Tt. Gribb et Rf. Cooper, 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 EARTHSUPPER-MANTLE, Review of scientific instruments, 69(2), 1998, pp. 559-564
The design and performance of a compact apparatus for the characteriza
tion of internal friction in simple shear at elevated temperature (les
s than or equal to 1400 degrees C) and low frequencies (less than or e
qual to 1 Hz) are described. High-temperature components are fabricate
d from a refractory molybdenum alloy that is straightforwardly machine
d. The apparatus has demonstrated, at high temperature, a torque resol
ution of 2x10(-5) Nm and an angular displacement resolution of 4x10(-6
) rad; for the specimen size we employ, these limits provide a shear s
tress and strain resolution of 2 kPa and 5x10(-7), respectively. The a
pparatus, while applicable to dynamic and static mechanical analyses o
f any engineering material, was developed for the characterization of
internal friction (attenuation) in synthetic silicate aggregates repre
sentative of Earth's upper mantle; we discuss the constraints inherent
in the required tests, as they affect apparatus design (including mat
erials selection) and experimental protocol. Static and dynamic data a
t 1250 degrees C for a polycrystalline aggregate of ferromagnesian oli
vine of controlled, uniform (similar to 3 mu m) grain size are present
ed and discussed. (C) 1998 American Institute of Physics.