Hysteretic nonlinear elasticity of Berea sandstone at low-vibrational strain revealed by dynamic acousto-elastic testing

G. Renaud, J. Rivière, P. Y. Le Bas, P. A. Johnson

Research output: Contribution to journalArticle

37 Scopus citations

Abstract

Through changes in wave speed of ultrasonic pulses traversing the sample, we measure variations in the elasticity of dry Berea sandstone as a function of the applied low-frequency (LF) axial strain (varied from 10-7 to 10-5). The approach, termed dynamic acousto-elasticity, is the dynamic analog of static acousto-elasticity where the wave speed is measured as a function of the applied static load. Dynamic acousto-elasticity uses low-frequency vibrational loading of smaller strain amplitude, typically below 10-4, and it includes inertial effects. At strain amplitudes around 10-6, compression and tension produce a material softening of the material. In contrast, a quasi-static compression inducing a strain between 10-4 and 10-3 leads to a material stiffening. At 10 -5 strain amplitude, elaborate hysteretic signatures of modulus strain are observed. The measurements provide the first direct experimental evidence of hysteretic nonlinear (wave amplitude dependent) elasticity in a sandstone at low dynamic strains. Key Points Each wave amplitude brings the material to a different metastable state First direct evidence of dynamic hysteretic nonlinear elasticity at low strain Nonlinear elastic parameters and hysteresis are wave amplitude dependent

Original languageEnglish (US)
Pages (from-to)715-719
Number of pages5
JournalGeophysical Research Letters
Volume40
Issue number4
DOIs
StatePublished - Feb 28 2013

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Earth and Planetary Sciences(all)

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