USGS · 70012386
Driving- stress waveform and the determination of rock internal friction by the stress-strain curve method.
Abstract
Harmonic distortion in the stress-time function applied to rock specimens affects the measurement of rock internal friction in the seismic wave periods by the stress-strain hysteresis loop method. If neglected, the harmonic distortion can cause measurements of rock internal friction to be in error by 3O% in the linear range. The stress-time function therefore must be recorded and Fourier analysed for correct interpretation of the experimental data. Such a procedure would also yield a value for internal friction at the higher harmonic frequencies.-Author
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Hsi-Ping Liu. 1980. Driving- stress waveform and the determination of rock internal friction by the stress-strain curve method.. https://doi.org/10.1111/j.1365-246x.1980.tb02638.x
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