Long-Time Relaxation Induced by Dynamic Forcing in Geomaterials
Abstract
Abstract We present a theoretical model and experimental evidence of the long‐time relaxation process (slow dynamics) in rocks and other geomaterials following a dynamic wave excitation, at scales ranging from the laboratory to the Earth. The model is based on the slow recovery of an ensemble of grain contacts and asperities broken by a mechanical impact. It includes an Arrhenius‐type equation for recovery of the metastable, broken contacts. The model provides a characteristic size of the broken contacts (order 10 −9 m) and predicts that their number increases with impact amplitude. Theoretical results are in good agreement with the laboratory and field data in that they predict both the logarithmic law of recovery rate and deviations from this law.
- Authors:
-
[1];
[3];
[3];
[4];
[5];
[5]
- Univ. of Colorado, Boulder, CO (United States); Univ. of North Carolina, Chapel Hill, NC (United States); Russian Academy of Sciences (RAS), Nizhnyi Novgorod (Russian Federation)
- Russian Academy of Sciences (RAS), Nizhnyi Novgorod (Russian Federation)
- Pennsylvania State Univ., University Park, PA (United States)
- Univ. of Memphis, TN (United States)
- Los Alamos National Lab. (LANL), Los Alamos, NM (United States)
- Publication Date:
- Research Org.:
- Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC). Basic Energy Sciences (BES) (SC-22); USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1544732
- Alternate Identifier(s):
- OSTI ID: 1523559
- Report Number(s):
- LA-UR-18-31318
Journal ID: ISSN 2169-9313
- Grant/Contract Number:
- 89233218CNA000001
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Solid Earth
- Additional Journal Information:
- Journal Volume: 124; Journal Issue: 5; Journal ID: ISSN 2169-9313
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 58 GEOSCIENCES; Slow Dynamics; Elasticity and anelasticity; Nonlinear elastic properties of rock; Earthquake dynamics; Nonlinear wave propagation
Citation Formats
Ostrovsky, Lev, Lebedev, A., Riviere, J., Shokouhi, Parisa, Wu, C., Stuber Geesey, Marcie Alberta, and Johnson, Paul Allan. Long-Time Relaxation Induced by Dynamic Forcing in Geomaterials. United States: N. p., 2019.
Web. doi:10.1029/2018JB017076.
Ostrovsky, Lev, Lebedev, A., Riviere, J., Shokouhi, Parisa, Wu, C., Stuber Geesey, Marcie Alberta, & Johnson, Paul Allan. Long-Time Relaxation Induced by Dynamic Forcing in Geomaterials. United States. https://doi.org/10.1029/2018JB017076
Ostrovsky, Lev, Lebedev, A., Riviere, J., Shokouhi, Parisa, Wu, C., Stuber Geesey, Marcie Alberta, and Johnson, Paul Allan. Tue .
"Long-Time Relaxation Induced by Dynamic Forcing in Geomaterials". United States. https://doi.org/10.1029/2018JB017076. https://www.osti.gov/servlets/purl/1544732.
@article{osti_1544732,
title = {Long-Time Relaxation Induced by Dynamic Forcing in Geomaterials},
author = {Ostrovsky, Lev and Lebedev, A. and Riviere, J. and Shokouhi, Parisa and Wu, C. and Stuber Geesey, Marcie Alberta and Johnson, Paul Allan},
abstractNote = {Abstract We present a theoretical model and experimental evidence of the long‐time relaxation process (slow dynamics) in rocks and other geomaterials following a dynamic wave excitation, at scales ranging from the laboratory to the Earth. The model is based on the slow recovery of an ensemble of grain contacts and asperities broken by a mechanical impact. It includes an Arrhenius‐type equation for recovery of the metastable, broken contacts. The model provides a characteristic size of the broken contacts (order 10 −9 m) and predicts that their number increases with impact amplitude. Theoretical results are in good agreement with the laboratory and field data in that they predict both the logarithmic law of recovery rate and deviations from this law.},
doi = {10.1029/2018JB017076},
journal = {Journal of Geophysical Research. Solid Earth},
number = 5,
volume = 124,
place = {United States},
year = {Tue Apr 30 00:00:00 EDT 2019},
month = {Tue Apr 30 00:00:00 EDT 2019}
}
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