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Slow dynamics in the nonlinear elastic response of Berea sandstone

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/96GL02884· OSTI ID:435091
;  [1]
  1. Los Alamos National Laboratory, Los Alamos, New Mexico (United States)

A typical resonance curve{emdash}measured acceleration versus drive frequency{emdash}made on a thin bar of rock shows peak bending with a softening (nonlinear) modulus as drive levels are increased. The shapes of these nonlinear resonance curves were found in earlier work to depend somewhat on sweep rate; these {open_quote}{open_quote}slow dynamics{close_quote}{close_quote} are now examined and quantified. We have measured slow dynamics in a 0.3 m long, 50 mm diameter bar of Berea sandstone under ambient conditions. Peak strain levels during the experiments ranged from 10{sup {minus}11} to 10{sup {minus}5} at driving frequencies near 4 kHz, the fundamental longitudinal resonance frequency of the bar. Slow dynamics begin to manifest themselves at strain amplitudes above 10{sup {minus}6} at ambient conditions and at the onset of nonlinear peak bending. Strains above this value condition the rock, altering its response for minutes to hours after the drive has been turned off. {copyright} American Geophysical Union 1996

Research Organization:
Los Alamos National Laboratory
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
435091
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 21 Vol. 23; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English

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