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Journal ArticleDOI

A simplification of the Zoeppritz equations

R. T. Shuey
- 01 Apr 1985 - 
- Vol. 50, Iss: 4, pp 609-614
TLDR
In this paper, the compressional wave reflection coefficient R(θ) given by the Zoeppritz equations is simplified to the following: R0+[A0R0+Δσ(1-σ)2]sin2θ+1/2ΔVpVp(tan 2θ-sin2
Abstract
The compressional wave reflection coefficient R(θ) given by the Zoeppritz equations is simplified to the following: R(θ)=R0+[A0R0+Δσ(1-σ)2]sin2θ+1/2ΔVpVp(tan2θ-sin2θ). The first term gives the amplitude at normal incidence (θ = 0), the second term characterizes R(θ) at intermediate angles, and the third term describes the approach to critical angle. The coefficient of the second term is that combination of elastic properties which can be determined by analyzing the offset dependence of event amplitude in conventional multichannel reflection data. If the event amplitude is normalized to its value for normal incidence, then the quantity determined is A=A0+1(1-σ)2ΔσR0. A0 specifies the normal, gradual decrease of amplitude with offset; its value is constrained well enough that the main information conveyed is Δσ/R0, where Δσ is the contrast in Poisson’s ratio at the reflecting interface and R0 is the amplitude at normal incidence. This simplified formula for R(θ) accounts for all of the relations between R(θ...

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Citations
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Book

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

TL;DR: 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.
MonographDOI

The Rock Physics Handbook

TL;DR: The third edition of the reference book as discussed by the authors has been thoroughly updated while retaining its comprehensive coverage of the fundamental theory, concepts, and laboratory results, and highlights applications in unconventional reservoirs, including water, hydrocarbons, gases, minerals, rocks, ice, magma and methane hydrates.
Book

Quantitative Seismic Interpretation: Applying Rock Physics Tools to Reduce Interpretation Risk

TL;DR: In this paper, the authors present a statistical rock physics approach combining rock physics, information theory, and statistics to reduce uncertainty in seismic data. But they do not discuss the use of statistical methods for quantitative seismic interpretation.
Journal ArticleDOI

Amplitude‐versus‐offset variations in gas sands

TL;DR: In this paper, the amplitude-versus-offset (AVO) characteristics of a gas sand reflector were investigated and the two factors that most strongly determine the AVO behavior of gas sand reflections were the normal incidence reflection coefficient R0 and the contrast in Poisson's ratio at the reflector.
Journal ArticleDOI

Weighted stacking for rock property estimation and detection of gas

G.C. Smith, +1 more
TL;DR: In this article, the angle of incidence of a P-wave as a function of time and offset was computed for each sample in a normal moveout corrected CMP gather, which can then be fitted to the amplitudes of all traces at each time sample of the gather, and certain rock properties can be estimated.
References
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Journal ArticleDOI

Plane-wave reflection coefficients for gas sands at nonnormal angles of incidence

TL;DR: The P-wave reflection coefficient at an interface separating two media is known to vary with angle of incidence and the manner in which it varies is strongly affected by the relative values of Poisson's ratio in the two media as mentioned in this paper.
Journal ArticleDOI

Fluid saturation effects on dynamic elastic properties of sedimentary rocks

A. R. Gregory
- 01 Oct 1976 - 
TL;DR: The influence of saturation by water, oil, gas, and mixtures of these fluids on the densities, velocities, reflection coefficients, and elastic moduli of consolidated sedimentary rocks was determined in the laboratory by ultrasonic wave propagation methods as discussed by the authors.
Journal ArticleDOI

Vp/Vs and Poisson’s ratios in marine sediments and rocks

TL;DR: In this article, the ratio of compressional wave velocity Vp to shear wave velocity Vs, and Poisson's ratio in marine sediments and rocks are important in modeling the sea floor for underwater acoustics, geophysics, and foundation engineering.
Journal ArticleDOI

On the effect of poisson's ratios of rock strata on the reflection coefficients of plane waves

TL;DR: In this article, the authors presented the reflection coefficients of plane longitudinal waves incident at oblique angles on boundary planes between elastic media and showed that the manner in which these reflection coefficients vary with the angle of incidence is strongly affected by the values of the Poisson's ratios of the two media.
Proceedings ArticleDOI

SAMPLE: Seismic Amplitude Measurement For Primary Lithology Estimation

TL;DR: SAMPLE as mentioned in this paper is a method of seismic interpretation that extracts shear wave velocities or Poisson's ratios from the seldom used amplitude variations within a common-depth point (CDP) gather.