Short‐Period Nonlinear Viscoelastic Memory of Rocks Revealed by Copropagating Longitudinal Acoustic Waves. Issue 5 (12th May 2018)

• Record Type: Journal Article
• Authors: Feng, Xuan; Fehler, Michael; Brown, Stephen; Szabo, Thomas L.; Burns, Daniel
• Is Part Of: Journal of geophysical research. Volume 123:Issue 5(2018)
• Page Start: 3993
• Page End: 4006
• Publication Date: 2018-05-12
• Subjects: rock memory -- wave propagation -- nonlinear acoustic -- viscoelastic -- hysteresis -- attenuation; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1029/2017JB015012
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: We describe a new sensitive acoustic method to measure nonlinear viscoelastic properties of rocks directly in the time domain. Unlike static stress‐strain measurements, or dynamic acousto‐elastic methods that use steady state resonance to load a strain field into a rock, our method uses two copropagating longitudinal acoustic waves, one to perturb the strain in the sample and the other to probe the effect of that strain. Experiments on Crab Orchard Sandstone and Lucite samples are presented. We evaluate the time‐dependent nonlinear effects and find strong evidence that rocks have a short‐period nonlinear viscoelastic memory that is a function of the time history of the loaded strain. We develop a phenomenological model to describe both this nonlinear viscoelastic memory and the nonlinear elastic behavior of rock. Our model shows that the viscoelastic memory is controlled by both the traditional nonlinear elastic coefficients and a memory strength parameter. These new observations and methods have significance for quantifying changes in microstructure. This short‐term memory effect, on the order of a small fraction of a cycle, is shown to be related through viscoelasticity to absorption in the sample. Plain Language Summary: By using propagating ultrasound waves to probe rocks, we have developed measurement methods to characterize very small changes in the stiffness of rocks in response applied dynamic strains. When strained, rocks become softer and have a short‐term memory. Our sensitive methods reveal that rock microstructure is responsive to environmental conditions such as overload and fluid content. These new approaches may allow earth scientists to better understand earthquake fault zones or sense environmental problems such as fluid leaks in near‐surface reservoirs. Key Points: A new sensitive method to quantify the nonlinearity of rocks directly in the time domain using copropagating acoustic waves was developed Rocks are found to have a short‐period nonlinear viscoelastic memory that is a function of the time history of the loaded strain A new phenomenological model can estimate the short‐period nonlinear viscoelastic memory and the nonlinear elastic coefficients of rocks