Rheology and wave propagation by J. M. Carcione (OGS)

Slides:



Advertisements
Similar presentations
Auto slide change for this page, WAIT…..
Advertisements

Title Petrophysical Analysis of Fluid Substitution in Gas Bearing Reservoirs to Define Velocity Profiles – Application of Gassmann and Krief Models Digital.
The Asymptotic Ray Theory
Earthquake Seismology: The stress tensor Equation of motion
Constitutive Equations CASA Seminar Wednesday 19 April 2006 Godwin Kakuba.
Rheology and wave propagation by J. M. Carcione (OGS)
Jiaguo Liu, Mingyu Xu School of Mathematics, Shandong University, Jinan, , P.R. China.
Mechanical Properties of Biological Materials Chapter 14 KINE 3301 Biomechanics of Human Movement.
Introduction to Viscoelasticity
The acoustic-electromagnetic analogy José M. Carcione OGS, Trieste, Italy.
Basic Terminology • Constitutive Relation: Stress-strain relation
Session: Computational Wave Propagation: Basic Theory Igel H., Fichtner A., Käser M., Virieux J., Seriani G., Capdeville Y., Moczo P.  The finite-difference.
8-1 Interpretation of The stress-strain relationship at a point in an elastic material each stress component is related to each of the nine strain components.
Constitutive Relations in Solids Elasticity
Fluid substitution effects on seismic anisotropy Long Huang, Robert Stewart, Samik Sil, and Nikolay Dyaur Houston April 2 nd,
NSF-JHU Workshop on Probability & Materials Multi-Scale Micro-Mechanical Poroelastic Modeling of Fluid Flow in Cortical Bone Colby C. Swan, HyungJoo Kim.
Measureable seismic properties
Rheology Different materials deform differently under the same state of stress. The material response to a stress is known as rheology. Ideal materials.
Engineering Properties of Wood
BGA 2007 Different aspects of seismic amplitude decay in viscous magma Patrick Smith Supervisor: Jürgen Neuberg School of Earth and Environment, The University.
Low frequency coda decay: separating the different components of amplitude loss. Patrick Smith Supervisor: Jürgen Neuberg School of Earth and Environment,
By Paul Delgado Advisor – Dr. Vinod Kumar Co-Advisor – Dr. Son Young Yi.
Geology 5660/6660 Applied Geophysics 17 Jan 2014 © A.R. Lowry 2014 Read for Wed 22 Jan: Burger (Ch 2.2–2.6) Last time: The Wave Equation; The Seismometer.
Role of Geodynamic Models in Interpreting Upper Mantle Images Magali Billen University of California, Davis MARGINS Workshop, May 2006.
VostokVostok José M. Carcione (OGS, Italy). Location in Antarctica.
Geology 5640/6640 Introduction to Seismology 20 Apr 2015 © A.R. Lowry 2015 Read for Wed 22 Apr: S&W (§3.7) Last time: Anisotropy(Cont’d) Anisotropy.
U.S. Geological Survey Menlo Park, CA Workshop Active and Passive Seismics in Laterally Inhomogeneous Media Loučeň Castle, Czech Republic.
Rheology Relations between stress and strain. Not easy to define Rheology: describes the ability of stressed materials to deform. strain rate creep regimes.
The kinematic representation of seismic source. The double-couple solution double-couple solution in an infinite, homogeneous isotropic medium. Radiation.
Geology 5660/6660 Applied Geophysics Last time: Brief Intro to Seismology & began deriving the Seismic Wave Equation: Four types of seismic waves:  P.
Equation of State Thermal Expansion Bulk Modulus Shear Modulus Elastic Properties.
WAVES Wave - a periodic disturbance that propagates energy through a medium or space, without a corresponding transfer of matter. e.g.1 sound wave (regular.
1 Vibration: A repeated back-and-forth or up-and-down motion. Energy: The ability to do work.
Geol 4068 Class presentation to accompany reading of Chapter 2- Waves in Fluids Elements of 3D Seismology, 2nd Edition by Christopher Liner September 6,
Waves Disturbances which travel through space and matter Carry energy and information Sometimes need medium to propagate in (mechanical waves, sound),
Geology 5660/6660 Applied Geophysics 13 Jan 2014
Tom Wilson, Department of Geology and Geography Environmental and Exploration Geophysics II tom.h.wilson Department of Geology.
Beyond Elasticity stress, strain, time Don Weidner Stony Brook.
11-5 Damped Harmonic Motion Typically, harmonic motion decreases in amplitude with time….this realistic model describes damped harmonic motion. The damping.
Stress Analysis in Viscoelastic Materials
Computational Continuum Mechanics in M&M SMR A. V. Myasnikov D.Sc., Senior Research Scientist, SMR Stavanger, 28 th April, 2006 From Seismics to Simulations.
6. Seismic Anisotropy A.Stovas, NTNU Definition (1) Seismic anisotropy is the dependence of seismic velocity upon angle This definition yields both.
Material Point Method Solution Procedure Wednesday, 10/9/2002 Map from particles to grid Interpolate from grid to particles Constitutive model Boundary.
WAVES.
On the Physics and Simulation of Waves at Fluid-Solid Interfaces: Application to NDT, Seismic Exploration and Earthquake Seismology by José M. Carcione.
Ground Vibrations and Air Blasts: Causes, Effects and Abatement.
A Biot model describing wave propagation in a porous solid saturated by a three-phase fluid Juan E. Santos 1,2 and Gabriela B. Savioli Instituto.
Linear Viscoelasticity
MODELLING OF THE HYDRO- ACOUSITC SIGNAL AS A TSUNAMI PRECURSOR F. Chierici (IRA-INAF) L. Pignagnoli (ISMAR-CNR) D. Embriaco (INGV) Nearest meeting, Berlin.
Wave-Equation Migration in Anisotropic Media Jianhua Yu University of Utah.
Rheology two basic relationships between stress and strain (geologic rheology) Elastic (Hookes law) Viscous Combinations of elastic and viscous Strain.
Geology 5660/6660 Applied Geophysics 20 Jan 2016
Topic 3: Constitutive Properties of Tissues
1D Kinematics Equations and Problems. Velocity The rate at an object changes position relative to something stationary. X VT ÷ x ÷
Geology 5640/6640 Introduction to Seismology 30 Jan 2015 © A.R. Lowry 2015 Read for Mon 2 Feb: S&W (§2.4); Last time: The Equations of Motion.
Viscoelasticity – 1 Lumped Parameter Models for time-dependent behavior DEQ’s as Constitutive Equations.
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale - OGS ( Italy) Modeling techniques to study CO 2 -injection induced micro-seismicity by.
Viscoelasticity Soft tissues and cells exhibit several anelastic properties: –hysteresis during loading and unloading –stress relaxation at constant strain.
Introduction to Seismology
Viscoelasticity and Wave Propagation
Hamiltonian formalism, seismic waves, and seismic barriers
Twin Wavefield (Pump-Probe*) Exploration
Class presentation to accompany reading of Chapter 2- Waves in Fluids
Eng. Mohamed Ossama Ashour
Acoustic Reflection 2 (distance) = (velocity) (time) *
Class presentation to accompany reading of Chapter 2- Waves in Fluids
Prestack Depth Migration in a Viscoacoustic Medium
V. Fault Mechanisms and Earthquake Generation
Waves.
Class presentation to accompany reading of Chapter 2- Waves in Fluids
Presentation transcript:

Rheology and wave propagation by J. M. Carcione (OGS)

Page: 2 Shot gather Distance (m) Distance (m) Depth (m) Geological model Seismic exploration

Page: 3

Page: 4

Page: 5 Poro-elasticity

Page: 6 Strain energy - Stress-strain relation

Page: 7 Jacketed test

Page: 8 Unjacketed test

Page: 9 Elastic moduli

Page: 10 Gassmann modulus

Page: 11 Gassmann modulus- variation of fluid content

Page: 12 Gassmann modulus - Examples

Page: 13 Gassmann modulus - Examples

Page: 14 Gassmann modulus - Examples

Page: 15 Gassmann modulus - Fluid substitution

Page: 16 Kinematics of the porous medium

Page: 17 Dissipation and equations of motion

Page: 18 The waves

Page: 19 Visco-elasticity

Page: 20 Burgers model

Page: 21 Burgers model - stress-strain relation

Page: 22 Burgers model - Creep function

Page: 23 Mechanical models Maxwell Kelvin-Voigt Zener

Page: 24 Zener model - Creep function

Page: 25 Zener model - Relaxation function

Page: 26 Zener model - velocity and attenuation

Page: 27 Maxwell model - creep and relaxation

Page: 28 Memory variable

Page: 29 Viscoelastic equations

Page: 30 Anisotropy

Page: 31 Stress-strain relation

Page: 32 Triclinic media (21)

Page: 33 Transversely-isotropic media (5)

Page: 34 Orthorhombic media (9)

Page: 35 Monoclinic media (12)

Page: 36 Anisotropy - eigenstrains - attenuation iso

Page: 37 Anisotropy - Kelvin-Christoffel matrix

Page: 38 Anisotropy - Slowness-Wavefronts

Page: 39 Anisotropy and attenuation

Page: 40 Relevant references

Page: 41

Feedback: Privacy Policy Feedback
Do Not Sell My Personal Information
About project: SlidePlayer Terms of Service

© 2025 SlidePlayer.com. Inc. All rights reserved.