4. Reflection/transmisson coefficients Introduction R/T coefficient – reflectivity/transmissivity Zoeppritz type equations Critical angles/complex R/T.

Slides:



Advertisements
Similar presentations
Surface Waves and Free Oscillations
Advertisements

Wave Incidence at Oblique angles
The Asymptotic Ray Theory
Earthquake Seismology: The stress tensor Equation of motion
Chapter 1- General Properties of Waves Reflection Seismology Geol 4068
What happens to a light wave when it travels from air into glass?
Reflection and Refraction of Light
Identification of seismic phases
Reflection Coefficients For a downward travelling P wave, for the most general case: Where the first term on the RHS is the P-wave displacement component.
Reflection and refraction
EEE340Lecture 391 For nonmagnetic media,  1 =  2 =  : Total reflection When  1 >  2 (light travels from water to air)  t >  i If  t = 
Wave spreads over a larger surface as it travels through the medium. For a spherical wave, the wave energy falls off as the square of the distance. Its.
Chapter 33 Electromagnetic Waves
Lecture 14 (11/13/2006) Analytical Mineralogy Part 1: Nature of Light Introduction to Optical Mineralogy.
Reflection+ Transmission Coefficients for 2-Layer Problem.
Reflection and Refraction. Plane wave A plane wave can be written as follows: Here A represent the E or B fields, q=i,r,t and j=x,y,z So this is a representation.
Reflection and Refraction of Plane Waves
EE3321 ELECTROMAGNETIC FIELD THEORY
The Electromagnetic Field. Maxwell Equations Constitutive Equations.
Chapter 12. Interaction of Light and Sound
Seismology Part III: Body Waves and Ray Theory in Layered Medium.
Waves. The Nature of Waves What is a mechanical wave?  A wave is a repeating disturbance or movement that transfers energy through matter or space 
The Hong Kong Polytechnic University Optics II----by Dr.H.Huang, Department of Applied Physics1 Light Waves Nature of Light: Light can be viewed as both.
What causes waves (in general)? What do waves transfer?
GHSGT Review Day 2 – Describe the Properties of a Wave.
CHAPTER 12- WAVES. WHAT IS A WAVE? Mechanical waves vs non-mechanical waves?
Kinematic Representation Theorem KINEMATIC TRACTIONS Time domain representation Frequency domain representation Green Function.
ECEN5341/4341Bioelectromagnetics Spring 2015 Frank S. Barnes Contact Info: (303) ECOT 250
Optics of a single Homogeneous and Isotropic Layer
Wave Incidence at Oblique angles Sandra Cruz-Pol ECE Dept. UPRM.
The elastic wave equation Seismology and the Earth’s Deep Interior The Elastic Wave Equation Elastic waves in infinite homogeneous isotropic media Numerical.
Prof. D. R. Wilton Notes 18 Reflection and Transmission of Plane Waves Reflection and Transmission of Plane Waves ECE 3317 [Chapter 4]
The University of Delaware
Seismology Part VI: Surface Waves: Love Augustus Edward Hough Love
1 Outline Full space, half space and quarter space Traveltime curves of direct ground- and air- waves and rays Error analysis of direct waves and rays.
The elastic wave equationSeismology and the Earth’s Deep Interior The Elastic Wave Equation  Elastic waves in infinite homogeneous isotropic media 
Feb 26, John Anderson: GE/CEE 479/679: Lecture 11 Earthquake Engineering GE / CEE - 479/679 Topic 11. Wave Propagation 1 John G. Anderson Professor.
Geophysics/Tectonics GLY 325. Elastic Waves, as waves in general, can be described spatially...
Reflection and Refraction. Regular Reflection Light travels in straight lines through a uniform medium. This is called rectilinear propogation. Light.
Lale T. Ergene Fields and Waves Lesson 5.5 Wave Reflection and Transmission.
1 AVO INVERSION OF LONG-OFFSET SYNTHETIC PP DATA BASED ON EFFECTIVE REFLECTION COEFFICIENTS 10 April 2008 Lyubov Skopintseva Milana Ayzenberg, Martin Landrø.
Physics 213 General Physics Lecture Last Meeting: Electromagnetic Waves, Maxwell Equations Today: Reflection and Refraction of Light.
6. Seismic Anisotropy A.Stovas, NTNU Definition (1) Seismic anisotropy is the dependence of seismic velocity upon angle This definition yields both.
Reflection and Refraction A short overview. Plane wave A plane wave can be written as follows: Here A represent the E or B fields, q=i,r,t and j=x,y,z.
Waves GCSE Physics. Objectives of the Lesson Understand the concept of wave motion in the physical world Recall that there are two types of wave motion-
Seismology Part V: Surface Waves: Rayleigh John William Strutt (Lord Rayleigh)
On the Physics and Simulation of Waves at Fluid-Solid Interfaces: Application to NDT, Seismic Exploration and Earthquake Seismology by José M. Carcione.
Superposition of Waves
Refraction The bending of light due to a change in speed.
Reflection Coefficients For a downward travelling P wave, for the most general case: Where the first term on the RHS is the P-wave displacement component.
Characteristics of Light.  Identify the components of the electromagnetic spectrum.  Calculate the frequency or wavelength of electromagnetic radiation.
Waves Quiz What are the two different types of waves? How are they different? Draw an example of each type. Define: Amplitude Wavelength Frequency.
7. Electromagnetic Waves 7A. Plane Waves Consider Maxwell’s Equations with no sources We are going to search for waves of the form To make things as general.
ECEN5341/4341 Spring 2017 Lecture 2 January 20,2017.
Waves & Energy Transfer
Introduction to Seismology
Reflection and Refraction of Electromagnetic Waves
Announcements 1/25/12 Prayer
Announcements 1/23/12 Prayer SPS social.
ENE 325 Electromagnetic Fields and Waves
Wave a disturbance that propagates through a material medium or space.
Does AVO Inversion Really Reveal Rock Properties?
Wireless Communications Chapter 4
Plane EM Wave: Oblique Incidence
1. , , and the direction of propagation are all
ECEN5341/4341 Spring 2019 Lecture 2 January 16,2019.
Notes 18 ECE 3317 Applied Electromagnetic Waves Prof. David R. Jackson
Antenna Theory Chapter.4.7.4~4.8.1 Antennas
1st Week Seminar Sunryul Kim Antennas & RF Devices Lab.
Reflection.
Presentation transcript:

4. Reflection/transmisson coefficients Introduction R/T coefficient – reflectivity/transmissivity Zoeppritz type equations Critical angles/complex R/T Weak-contrast approximation Parametrization Second order approximation Reflection from single layer Reflection from free surface

Introduction Reflection/transmission coefficient describes the effect of interface between two half spaces: Solid, Liquid, Vacuum There are 5 different cases to be considered: - Solid-solid - Solid-liquid - Solid-vacuum - Liquid-liquid - Liquid-vacuum

Introduction There are two types of boundary conditions at the interface: -Strains -Stress components They have be continuous (boundary conditions) or discontinuous (slip effect)

Introduction There are two types reflection/transmission problems: -Amplitudes -Energy (energy flux), symmetries+geometrical spreading Reflection/transmission coefficients are frequency independent for pre-critical elastic reflections from flat smooth interface

R/T coefficient – reflectivity/transmissivity Figure 4.1. The R/T coefficients

Zoeppritz type equations assumptions Plane wave Isotropic elastic medium Plane interface

Zoeppritz type equations (4.1) (4.2)(4.3)

Zoeppritz type equations Figure 4.2. The real part of Zoeppritz reflection coefficients Critical angle Pre-critical reflection Post-critical reflection

Zoeppritz type equations Figure 4.3. The imaginary part of Zoeppritz reflection coefficients Post-critical reflection

Complex reflection coefficient  is the phase shift at interface (4.4)

Zoeppritz type equations Figure 4.4. The real part of Zoeppritz reflection coefficients (index interchange)

Zoeppritz type equations Figure 4.5. The real part of Zoeppritz reflection coefficients (no post-critical)

Zoeppritz type equations Figure 4.6. The real part of Zoeppritz reflection coefficients (weak contrast)

Energy flux (4.5)

Weak-contrast approximation Zoeppritz equation – 6 medium parameters. Weak-contrast approximation – 3 medium parameters. All angles are real (pre-critical): (4.6) Contrast in medium parameter m (4.7) What is now happened with index interchange?

Weak-contrast approximation Figure 4.7. Weak contrast model

Weak-contrast approximation Figure 4.7. Strong contrast model

Parametrization 1.Velocities 2.Impedances 3.Stiffness coefficients (elastic moduli) (4.9) (4.8)

Parametrization Figure 4.8. Parametrization effect for the strong contrast model

Parametrization (4.10) Exact expression for normal incidence reflection coefficient

Second order approximation Stovas&Ursin, 2002 (4.12) (4.11)

Second order approximation Figure 4.9. Interpretation of second order R/T

Second order approximation Figure Second order R/T for weak-contrast model

Second order approximation Figure Second order R/T for strong-contrast model

Reflection from single layer Figure Sketch of the models (Helle, Stovas & Carcione, 1999)

Reflection from single layer Figure Reflection for model A (frequency 40 Hz)

Reflection from single layer (4.15) (4.14) (4.13) Figure Frequency dependent normal incidence reflection coefficient

Reflection from free surface water air (4.16) Source Receiver