scispace - formally typeset
Open AccessBook

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.

read more

Content maybe subject to copyright    Report

Citations
More filters
Journal ArticleDOI

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.
Journal ArticleDOI

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.
Journal ArticleDOI

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.
Journal ArticleDOI

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.
Journal ArticleDOI

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
More filters
Journal ArticleDOI

Relationships among compressional wave attenuation, porosity, clay content, and permeability in sandstones

Theodoros Klimentos, +1 more
- 01 Aug 1990 - 
TL;DR: In this paper, the attenuation coefficients of compressional waves in 42 sandstones at a confining pressure of 40 MPa (equivalent to a depth of burial of about 1.5 km) were measured using a pulse-echo method in which the sample was sandwiched between perspex buffer rods inside the high pressure rig.
Journal ArticleDOI

Synthetic microseismograms; logging in porous formations

J. H. Rosenbaum
- 01 Feb 1974 - 
TL;DR: In this paper, the amplitude of wave propagation in a fluid-filled porous elastic solid was analyzed for a cylindrical borehole and along a plane interface, and it was found that properties such as permeability affect the attenuation of the signal only at high frequencies.
Book

Foundations of Anisotropy for Exploration Seismics

Klaus Helbig
TL;DR: In this paper, one-parameter expressions for the slowness surfaces of transversely isotropic media and the curve in the planes of symmetry of orthorhombic media are given.
Journal ArticleDOI

3-D description of normal moveout in anisotropic inhomogeneous media

TL;DR: In this article, a new equation for normal-moveout (NMO) velocity that describes azimuthally dependent reflection traveltimes of pure modes from both horizontal and dipping reflectors in arbitrary anisotropic inhomogeneous media is presented.
Journal ArticleDOI

Elastic constants of single‐crystal forsterite as a function of temperature and pressure

TL;DR: Adiabatic elastic stiffness constants of single crystal forsterite measured as function of hydrostatic pressure and temperature, using pulse superposition technique as discussed by the authors, were derived from a single-crystal single crystal FER.
Related Papers (5)