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The Rock Physics Handbook: Tools for Seismic Analysis of Porous Media

TLDR
In this article, the authors present basic tools for elasticity and Hooke's law, effective media, granular media, flow and diffusion, and fluid effects on wave propagation for wave propagation.
Abstract
Preface 1. Basic tools 2. Elasticity and Hooke's law 3. Seismic wave propagation 4. Effective media 5. Granular media 6. Fluid effects on wave propagation 7. Empirical relations 8. Flow and diffusion 9. Electrical properties Appendices.

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Citations
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Empirical relations between elastic wavespeeds and density in the Earth's crust

TL;DR: A compilation of compressional-wave (V p) and shear-wave velocities and densities for a wide variety of common lithologies is used to define new nonlinear, multivalued, and quantitative relations between these properties for the Earth's crust as mentioned in this paper.
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Physical properties of hydrate-bearing sediments

TL;DR: A review of the current understanding of phenomena involved in gas hydrate formation and the physical properties of hydrate-bearing sediments can be found in this paper, where the magnitudes and interdependencies of these properties are critically important for predicting and quantifying macroscale responses of hydrates to changes in mechanical, thermal, or chemical boundary conditions.
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Digital rock physics benchmarks-part II: Computing effective properties

TL;DR: This analysis provides the DRP community with a range of possible outcomes which can be expected depending on the solver and its setup, and falls within the ranges consistent with the relevant laboratory data.
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The brittle-ductile transition in porous rock: A review

TL;DR: In this article, Bifurcation analysis can be used in conjunction with a constitutive model to predict the onset of strain localization, which is in qualitative agreement with the laboratory data.
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Computation of linear elastic properties from microtomographic images: Methodology and agreement between theory and experiment

TL;DR: In this article, the elastic properties of the digitized images under dry, water-saturated, and oil -saturated conditions were derived from a suite of four samples of Fontainebleau sandstone with porosities ranging from 7.5% to 22%.
References
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AVO and elastic impedance

TL;DR: In this article, a linear fit of P-wave reflection amplitude to the sine square of the angle-of-incidence (AoI) was proposed to obtain additional AVO attributes such as pseudo S-wave data and Poisson's ratio contrast.
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Theory of elastic constants of heterogeneous media

TL;DR: The theory of elastic equilibrium of heterogeneous, macrohomogeneous bodies is cast in the form of a linear integral equation with the following properties: (1) the equation contains a constant elastic tensor which can be chosen freely to optimize any approximation method.
Journal ArticleDOI

Estimation of net-to-gross from P and S impedance in deepwater turbidites

Lev Vernik, +2 more
- 01 Apr 2002 - 
TL;DR: In this article, the authors used both acoustic and shear impedance (AI and SI) to estimate the net-to-gross (N/G) of the Horn Mountain deepwater reservoirs, Gulf of Mexico (GOM), where six appraisal wells were available for calibration.
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Seismic-wave traveltimes in random media

TL;DR: In this paper, a ray-theoretical relation between the autocorrelation function of the slowness fluctuations of a random medium and the traveltime fluctuations on a profile perpendicular to the general propagation direction of an originally plane wave is established.
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The influence of fluids on grain contact stiffness and frame moduli in sedimentary rocks

TL;DR: In this article, a modified Hertz contact theory is presented for the self consistent calculation of deformation, equilibrium separation distance (film thickness), and contact area for two spherical asperities in contact and subjected to an external load.
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