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- W2392141810 abstract "Endochronic theory is employed herein to study the attenuation of rock, under cyclic loading. According to endochronic theory, the relationship between attenuation and strain amplitude of rock samples can be briefly at intermediate strain levels by introducing an inelastic parameter α. A derived series of uniaxial stress cycling tests were conducted on sandstone and granite sample′s using MTS testing machine, and a set of hysteresis graphs of stress-strain were obtained. The attenuation values of rock samples were calculate based upon the area under those stress-strain curves. It is found that the theoretical predictions by e.t. agree well with the experimental findings which show that attenuation increases with strain amplitude when the average stress of each loop is fixed. Finally, the inelastic parameter α was briefly discussed. For sandstone, the α values are steady at about 0.5, whereas for granite, the α values are not constant. But they all increase with stress increment. This result may be useful to the study of attenuation of seismic waves in the medium of earth." @default.
- W2392141810 created "2016-06-24" @default.
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- W2392141810 date "2004-01-01" @default.
- W2392141810 modified "2023-09-23" @default.
- W2392141810 title "A Study on the Relationship Between Attenuation and Strain Amplitude in Rock Using Endochronic Theory" @default.
- W2392141810 hasPublicationYear "2004" @default.
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