Review of Scientific Instruments · 2018 · 21 citations · 38 references
EngineeringEarth SciencesGeophysicsFinite Element AnalysisMechanical Behavior Of MaterialsRock MechanicsElasticity TheoryGeomechanicsRock DeformationRock PhysicsStrain In RocksStress In RocksElastic ModuliFrequency MeasurementPoisson's RatioResonance FrequenciesStress-strain AnalysisStress-strain CurveStress-strain RelationsStress-strain Relationships
We built a broad-frequency-band measurement system for rock elastic parameters based on the stress-strain method following Batzle et al., Geophysics 71, N1-N9 (2006). The system gives strain amplitude anomalies at some measurement frequencies. These anomalies put limitations on the range of the measurement frequency and jeopardize the credibility of the measurement results over a broad frequency band. To overcome these limitations, we investigated the cause of these anomalous strains by numerical model simulations with a finite element method based on the experimental apparatus. Through the systematic analysis of the modeling results, we conclude that the resonances caused by non-axial perturbations lead to such anomalous measurement results. Based on the analysis, we give a solution to reduce the effect of the resonances and shift the first resonance frequency beyond the frequency band of 1-2000 Hz. The enhanced measurement system can provide robust and reliable measurements on the elastic parameters of rocks between 1 and 2000 Hz, which is crucial for a quantitative study of the frequency-dependent phenomenon related to fluid effects. This in turn will provide a powerful tool for the experimental characterization of elastic properties of oil/gas reservoir rocks, thus laying a solid foundation for low-frequency rock physics analysis and quantitative seismic interpretation.
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Pore fluids and seismic attenuation in rocks
Kenneth W. Winkler, Amos Nur · Geophysical Research Letters · 1979 · 391 citations · Full text