Rock Physics in a Nutshell

Slides:



Advertisements
Similar presentations
PH0101 UNIT 1 LECTURE 1 Elasticity and Plasticity Stress and Strain
Advertisements

Lesson 1 – The Nature of Force
Springs and Elasticity ClassAct SRS enabled. In this presentation you will: Explore the concept of elasticity as exhibited by springs.
1 Thin Walled Pressure Vessels. 2 Consider a cylindrical vessel section of: L = Length D = Internal diameter t = Wall thickness p = fluid pressure inside.
Mechanics of Materials – MAE 243 (Section 002) Spring 2008 Dr. Konstantinos A. Sierros.
ELASTIC CONSTANTS IN ISOTROPIC MATERIALS
Jump to first page 1 Normal stress = Chapter 2 Mechanics of Materials Example: Estimate the normal stress on a shin bone ( 脛骨 ) ATensile stress (+) Compressive.
Deformation of Solids Stress is proportional to Strain stress = elastic modulus * strain The SI unit for stress is the Newton per meter squared (N/m 2.
CHAPTER OBJECTIVES Apply the stress transformation methods derived in Chapter 9 to similarly transform strain Discuss various ways of measuring strain.
Seismic Wave Propagation. LL F L F = k *  L/L (Hooke’s Law) k = Young’s modulus Rand quartzite strain Elastic Materials.
Stress-Strain Theory Under action of applied forces, solid bodies undergo deformation, i.e., they change shape and volume. The static mechanics of this.
Seismic Wave Propagation. LL F L F = k *  L/L (Hooke’s Law) k = Young’s modulus Rand quartzite strain Elastic Materials.
Mechanics of Materials – MAE 243 (Section 002) Spring 2008 Dr. Konstantinos A. Sierros.
Material Testing.
CTC / MTC 222 Strength of Materials
Finite Element Method in Geotechnical Engineering
Copyright © 2009 Pearson Education, Inc. Chapter 12 Elasticity.
Material Strength.
EART162: PLANETARY INTERIORS
Physics. Properties of Matter Session Session Objectives.
Solid mechanics 1.1 – key points
Objectives  Understand how elasticity is related to Hooke’s Law for springs.  Know that the change in length of an object is proportional to the force.
Spring Forces and Simple Harmonic Motion
Mechanics of Materials Goal:Load Deformation Factors that affect deformation of a structure P PPP Stress: intensity of internal force.
Conduits –To conduct blood to the organs and periphery Impedance matching –Minimise cardiac work –Minimise pulse pressure –Control flow according to demand.
GG 450 March 19, 2008 Stress and Strain Elastic Constants.
Rheology I. Rheology Part of mechanics that deals with the flow of rocks, or matter in general Deals with the relationship of the following: (in terms.
Elastic Properties of Solids, Part III Topics Discussed in Kittel, Ch. 3, pages Another Lecture Found on the Internet!
Defining sign of stress tensor Kittel’s Fig. 15 may be confusing about sign of T xx (which he calls X x ) Stress tensor component T xx is defined as the.
Shrieking Rod Prof. Chih-Ta Chia Dept. of Physics NTNU.
R. Field 10/31/2013 University of Florida PHY 2053Page 1 Definition of Strain System Response – Linear Deformation: System Response – Volume Deformation:
What’s seismology about?
EGR 280 Mechanics 6 – Introduction to Mechanics of Materials.
Objectives 1.Define stress & strain. 2.Utilize Hooke’s Law to calculate unknown stresses and strains. 3.Determine material parameters from a stress-strain.
Happyphysics.com Physics Lecture Resources Prof. Mineesh Gulati Head-Physics Wing Happy Model Hr. Sec. School, Udhampur, J&K Website: happyphysics.com.
– SOLID MECHANICS S.ARAVINDAN Lecturer Department of Aeronautical Engineering Rajalakshmi Engineering College 1.
ENGR-45_Lec-14_Metal_MechProp-1.ppt 1 Bruce Mayer, PE Engineering-45: Materials of Engineering Bruce Mayer, PE Registered Electrical.
Geology 5660/6660 Applied Geophysics Last time: Brief Intro to Seismology & began deriving the Seismic Wave Equation: Four types of seismic waves:  P.
Internal stress measurement using XRD
1 Waves 7 Lecture 7 Longitudinal waves and Fourier Analysis. D Aims: ëSound waves: > Wave equation derived for a sound wave in a gas. ëAcoustic impedance.
States of matter Solid: Liquid Gas Plasma Fluid: Crystalline Amorphous.
Geology 5660/6660 Applied Geophysics 13 Jan 2014
Presented By : Ketulkumar Amin Enroll No:
UNIT-01. SIMPLE STRESSES and STRAINS Lecture Number - 02 Prof. M. N. CHOUGULE MECHANICAL DEPARTMENT SIT LONAVALA Strength of Materials.
EXPLORATION GEOPHYSICS THE EXPLORATION TASK PLAN EXPLORATION APPROACH FOR A MATURE TREND GATHER DATA FOR A MATURE TREND DEVELOP PLAY PROSPECT FRAMEWORK.
States of Matter Deformation of Solids Density and Pressure
PHY1039 Properties of Matter Macroscopic (Bulk) Properties: Thermal Expansivity, Elasticity and Viscosity 20 & 23 February, 2012 Lectures 5 and 6.
STRESS-STRAIN RELATIONSHIP
What’s seismology about? Seismology is the study of the generation, propagation and recording of elastic waves in the Earth (and other celestial bodies)
Chapter 11 Outline Equilibrium and Elasticity
III. Strain and Stress Strain Stress Rheology A rheological law relates strain to stress and time.
Rheology two basic relationships between stress and strain (geologic rheology) Elastic (Hookes law) Viscous Combinations of elastic and viscous Strain.
MZK Rafiqul Islam Asstant Professor( Civil ) TTTC Subject: Structural Mechanics for 1st Year BSc Tech.
Lecture 18: Elasticity and Oscillations I l Simple Harmonic Motion: Definition l Springs: Forces l Springs: Energy l Simple Harmonic Motion: Equations.
Expectations after this section
Elasticity Yashwantarao Chavan Institute of Science Satara Physics
Copyright ©2011 by Pearson Education, Inc. All rights reserved. Mechanics of Materials, Eighth Edition Russell C. Hibbeler General Plane-Strain Transformation.
Review Questions: Chapter 0 Given, calculate all the possible binary products of a, a T, b and b T What are the eigenvalues of the matrix ? Is it positive.
Clemson Hydro Deformation of Solids. Clemson Hydro Tensile test.
Strain Linear strain-displacement relationships What is the physical meaning of the strain components? What is the maximum normal and shear strains that.
Equilibrium, Elasticity, and Hooke’s Law
STRESS-STRAIN RELATIONSHIP
Material Strength.
Continuum Mechanics (MTH487)
Elasticity Yasser Assran 27/10/2015.
Continuum Mechanics for Hillslopes: Part V
CTC / MTC 222 Strength of Materials
(a) Describe what material the spring is made from;
Mechanics of Materials Engr Lecture 21
Chapter 2 Mechanics of Materials
Presentation transcript:

Rock Physics in a Nutshell F dP dV

Some Rock Physics Definitions Hooke’s Law F = k X Robert Hooke 1635 - 1703 English gentleman scientist, paleontologist, experimential scientist. Contemporary of Issac Newton. Assisted Robert Boyle in the study of the physics of gases. F DF = k DX Just a constant of proportionality. This is a function of both material and geometry. Young’s Modulus E Thomas Young 1773 – 1829 English “polymath”, and physician. Contemporary of W. Herschel. F A (area) Uniaxial stress DL E = Uniaxial strain Lo E = Modulus of elasticity This is just a function of the material; the geometry has been unitized.

m Some Rock Physics Definitions Bulk Modulus K dP dV Ratio of stress to volumetric strain K = dP dV Shear Modulus m Ratio of shear stress to shear strain A (area) DX m F I = F DX A I

Some Rock Physics Definitions Poisson’s Ratio s Simeon Poisson 1781 – 1841 French mathematician and physicist. Succeeded Fourier and Laplace. Contemporary of Faraday. Dx Spring constants from Hook’s law: Dy ex dx ey dy = = x y ex Poisson’s ratio = ey Lateral expanshion = Longitudinal contraction Young’s Modulus E Thomas Young 1773 – 1829 English “polymath”, and physician. Contemporary of W. Herschel. F A (area) Uniaxial stress DL E = Uniaxial strain Lo E = Modulus of elasticity

m m m s m s, m s m m Vp Vs r r r r r r K + K, m E, m 4 3 2 1 - 1 - 2 Compressional velocity Shear velocity Vp Vs Bulk modulus, Shear modulus 4 3 m m K + K, m r r Poisson’s ratio, Shear modulus m s m s, m 2 1 - r s 1 - 2 r Young’s modulus, Shear modulus m 4m - m E, m E r 3m - E r

Poisson’s ratio related to Vp/Vs ratio C. A little rock physics - Poisson’s ratio Poisson’s ratio related to Vp/Vs ratio Reduces to .5 (fluid) 2 Vp .6 - 2 s 1 Vs = 2 2 .5 Vp - 1 Vs s .4 .3 Vp Poisson’s ratio is another measure of the Vp/Vs ratio. Here we see that the value of Poisson’s ratio converges to a value of .5 which represents a fluid, and on the other end, the Vp/Vs ratio converges to a value equal to the square root of 2.0 which is 1.14 A typical Vp/Vs ratio of 2.0 corresponds to a Poisson’s ratio of .333 s 2 - 2 .2 = s Vs 2 - 1 .1 2 4 6 8 Vp Vs Reduces to 2 C - 28

So what’s the “Big Deal” about the Vp / Vs ratio and Poisson’s ratio s ??? Answer: they explain the reflection coefficients and AVO

r r s s Vp r - r r + r Vp q Vp Vp Vp Vp Ds q q q = 0 The R Reflection Coefficient r Vp Vp r - Vp r 1 1 2 2 1 1 R = r Vp r + Vp r Vp 2 2 1 1 2 2 The Shuey Equation 2 Ds 9 2 R = R Cos q + Sin q q 4 10 20 30 40 .20 q .15 .10 s .05 1 R .00 s Wet -.05 2 -.10 -.15 Gas -.20 10 20 30 40