Published July 1979 | Version v1
Journal article

Mechanical hysteresis loops of an anelastic solid and the determination of rock attenuation properties

  • 1. U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025

Description

We demonstrate that mechanical hysteresis loop shapes for a linear anelastic solid satisfying Q-1approx. = constant over a wide frequency range are sensitive to the cycling stress waveform. Cusped or asymmetrical hysteresis loops are compatible with linear anelastic behavior for nonsinusoidal loading and do not necessarily imply a nonlinear attenuation mechanism. Because loop shape depends on the cycling stress waveform, we suggest that detailed observation of the stress time function, the hysteresis loop shapes, and experimental determination of the creep function over a time interval comparable to that of the cyclic loading experiment provide a direct and stringent test of the linearity of rock attenuation. Such detailed observation of hysteresis loop shapes during nonsinusoidal stress cycles can also provide a test in the linear range for theoretically constructed creep functions

Additional details

Publishing Information

Journal Title
Geophys. Res. Lett.
Journal Volume
6
Journal Issue
7
Series
Geophys. Res. Lett.
Journal Page Range
545-548

INIS

Country of Publication
United States
Country of Input or Organization
United States
INIS RN
11517154
Subject category
S58: GEOSCIENCES;
Descriptors DEI
ATTENUATION; CREEP; HYSTERESIS; REGOLITH; ROCK MECHANICS; SEISMIC WAVES; WAVE FORMS
Descriptors DEC
MECHANICAL PROPERTIES; MECHANICS