Imaging with Multiply Scattered Waves: Removing Artifacts

Size: px
Start display at page:

Download "Imaging with Multiply Scattered Waves: Removing Artifacts"

Transcription

1 Imaging with Multiply Scattered Waves: Removing Artifacts Alison Malcolm Massachusetts Institute of Technology Collaborators: M. de Hoop, Purdue University B. Ursin, Norwegian University of Science and Technology

2 Subsalt imaging 0 lateral position (km) depth (km) 5

3 Subsalt imaging 0 lateral position (km) depth (km) 5

4 Outline Overview of nonlinearity Standard Reverse-time imaging One-way approximate method Interferometric improvements

5 Nonlinearity c 0 (x) 2 2 t u 0(x, t) u 0 (x, t) = 0 L 0 u 0 = 0 c(x) 2 2 t u(x, t) u(x, t) = 0 Lu = 0 V = L L 0 = (c(x) 2 c 0 (x) 2 ) 2 t c 0 (x) C δc(x) oscillatory

6 Nonlinearity Lippmann-Schwinger: L 0 δu = Vu Born Approximation: L 0 δu = Vu 0 c 0 (x) 2 2 t u 0(x, t) u 0 (x, t) = 0 L 0 u 0 = 0 c(x) 2 2 t u(x, t) u(x, t) = 0 Lu = 0 V = L L 0 = (c(x) 2 c 0 (x) 2 ) 2 t

7 Outline Overview of nonlinearity Standard Reverse-time imaging One-way approximate method Interferometric improvements

8 Reverse-Time Migration d(s, r, t) = Ω { G(s, x, t t 0 ) V(x)G(x, r, t 0 )dxdt 0 }

9 Reverse-Time Migration I(x) = S x,t G(x, s, ω) x,t d (x, s, ω)dsdω Separation of Scales δc(x) = c 0 (x) + δc(x) c 0 C δc(x) oscillatory Include part of δc in c 0

10 Jones et al I(x) = Reverse-Time Migration S x,t G(x, s, ω) x,t d (x, s, ω)dsdω

11 I(x) = Reverse-Time Migration S x,t G(x, s, ω) x,t d (x, s, ω)dsdω 0 lateral position (km) depth (km) 5 Top Balder Ekofisk Top Chalk Top Hod Base Chalk m/s

12 Outline Overview of nonlinearity Standard Reverse-time imaging One-way approximate method Interferometric improvements

13 One-Way Migration Lu = f ( ) u z z u = ( )( ) ( ) 0 1 u 0 + A 0 z u f A(z, x, x, t ) = 2 x c(z, x) 2 2 t Taylor (81), Stolk & de Hoop (05)

14 One-way Migration Diagonalize (parabolic approx.) in smooth background ( ) ( )( ) ( ) u+ ib+ 0 u+ f+ z = + u 0 ib u f b ± (ξ, x, ω) = ± ξ 2 c 0 (x) 2 ω 2

15 Artifacts Series setup Solution: z U = BU + F L 0D G := (I z B)G = Iδ ( ) G+ 0 G = 0 G G propagator in c 0

16 Artifacts Series setup Bremmer Series (Bremmer 51, de Hoop 96) Born Series (Lippmann & Schwinger 50) L 0D δu = VU (I GV) δu = G(VU 0 ),

17 Artifacts Series setup Bremmer Series (Bremmer 51, de Hoop 96) Born Series (Lippmann & Schwinger 50) δu 1 = G(VU 0 ) δu m = G(VδU m 1 ) m = 2,..., M δu M δu m m=1

18 Artifacts Series setup δu = G(VU 0 ) + G(VG(VU 0 )) +... Set V = j V j equate orders G(V 1 U 0 ) = δu G(V 2 U 0 ) = G(V 1 G(V 1 U 0 )) G(V 3 U 0 ) = G(V 1 G(V 1 G(V 1 U 0 ))) e.g. Moskow (2008), Weglein (2003), AM & de Hoop (2005)

19 Nullspace series setup G(V 1 U 0 ) = δu G(V 2 U 0 ) = G(V 1 G(V 1 U 0 )) V 1 = V 1 + V 1 + V 1 G(V 2 U 0 ) = G(V 1 G(V 1 U 0)) G(V 1 G(V 1 U 0)) G(V 1 G(V 1 U 0)) G(V 1 G(V 1 U 0)) AM, Ursin, de Hoop (2009)

20 Nullspace series setup G(V 1 U 0 ) = δu G(V 2 U 0 ) = G(V 1 G(V 1 U 0 )) V 1 = V 1 + V 1 + V 1 G(V 1 G(V 1 U 0)) + G(V 1 G(V 1 U 0)) + G(V 1 U 0) = δd Similar to Cheney & Bonneau (2004)

21 One-Way Imaging Algorithm forward propagate source backward propagate data imaging condition s r Claerbout (71,85)

22 Imaging Algorithms source side u s (z, x, ω) = (G + (z, 0))(x, ω, s) receiver side u Σs (z, x, ω) = dr(g (z, 0))(r, ω, x)d(s, r, ω) Σ s

23 Imaging Algorithms source side u s (z, x, ω) = (G + (z, 0))(x, ω, s) receiver side u Σs (z, x, ω) = dr(g (z, 0))(r, ω, x)d(s, r, ω) Σ s V 1 (z, x) ds dωu s (z, x, ω)u Σ s (z, x, ω)ω 2

24 Nullspace series setup G(V 1 U 0 ) = δu G(V 2 U 0 ) = G(V 1 G(V 1 U 0 )) V 1 = V 1 + V 1 + V 1 G(V 1 G(V 1 U 0)) + G(V 1 G(V 1 U 0)) + G(V 1 U 0) = δd Similar to Cheney & Bonneau (2004)

25 Algorithm multiples propagate down store W form image, I V 1 W I propagate up W I form image r s

26 Algorithm multiples propagate down store W form image, I V 1 W I propagate up W I form image r r s

27 One-Way Example 0 lateral position (km) depth (km) 2 4

28 Nullspace Examples 0 lateral position (km) depth (km)

29 Nullspace Examples 0 receiver position (km) time (s) 2 3 4

30 Nullspace Examples 0 receiver position (km) time (s) 2 3 4

31 Nullspace Examples 0 lateral position (km) depth (km) 1 2 3

32 Nullspace Examples 0 lateral position (km) depth (km) 1 2 3

33 Nullspace Examples 0.5 lateral position (km) lateral position (km) depth (km) depth (km) V 1 V 1 V 1 V 1 V 1 V 1

34 Comparing Models depth (km) depth (km) depth (km)

35 Outline Overview of nonlinearity Standard Reverse-time imaging One-way approximate method Interferometric improvements

36 Interferometry r 1 r 2 s H(r 1, r 2, ω) S G(s, r 1, ω)g (s, r 2, ω)ds Vasconcelos (2007)

37 Interferometry r 1 r 2 s H(r 1, r 2, ω) S G(s, r 1, ω)g (s, r 2, ω)ds Vasconcelos (2007)

38 Interferometry H(r 1, r 2, ω) = C Assuming: Far-field ν G iωg Radiation condition S G (s, r 1, ω) ν G(s, r 2, ω) ν G (s, r 1, ω)g(s, r 2, ω) Homogeneous model outside S, S circle H(r 1, r 2, ω) G(s, r 1, ω)g (s, r 2, ω)ds S

39 Interferometry and RTM s x d Born (x, ω, s) = Ω y x H Σ s 0 (x, ω, x )V(x )G 0 (x, ω, s)dx Stolk et al. (2009) x

40 Interferometry and RTM r 1 r 2 s d Born (x, ω, s) = Ω H Σ s 0 (x, ω, x )V(x )G 0 (x, ω, s)dx Stolk et al. (2009)

41 Interferometry and RTM Standard imaging: d Born (x, ω, s) = G 0 (x, ω, x )V(x )G 0 (x, ω, s)dx Ω Ω G 0 (s, ω, y)d Born (y, ω, s)ds V(y) Interferometry from migration: d Born (x, ω, s) = H Σ s 0 (x, ω, x )V(x )G 0 (x, ω, s)dx Ω

42 Interferometry and RTM s x Ω y x G 0 (s, ω, x )d Born (x, ω, s)ds x = H Σ s 0 (x, ω, x )V(x ) Esmersoy (1988), van Manen (2006), Thorbecke (2007) Vasconcelos et al. (2009)

43 Interferometry and RTM s x s x y x x x x similar to extended images of e.g. Symes (2008), Vasconcelos (2009)

44 Summary Standard Reverse-time imaging ignores separation of scales One-way approximate method respects separation of scales requires multiple passes Interferometric improvements respects separation of scales single pass artifacts?

45 Acknowledgements Ivan Vasconcelos & Ian Jones GX Technologies Total

46 [?,?] [?] [?,?] [?] [?,?] [?] [?,?,?,?,?]

Introduction to Seismic Imaging

Introduction to Seismic Imaging Introduction to Seismic Imaging Alison Malcolm Department of Earth, Atmospheric and Planetary Sciences MIT August 20, 2010 Outline Introduction Why we image the Earth How data are collected Imaging vs

More information

Introduction to Seismic Imaging

Introduction to Seismic Imaging Introduction to Seismic Imaging Alison Malcolm Department of Earth, Atmospheric and Planetary Sciences MIT August 20, 2010 Outline Introduction Why we image the Earth How data are collected Imaging vs

More information

When is the single-scattering approximation valid? Allan Greenleaf

When is the single-scattering approximation valid? Allan Greenleaf When is the single-scattering approximation valid? Allan Greenleaf University of Rochester, USA Mathematical and Computational Aspects of Radar Imaging ICERM October 17, 2017 Partially supported by DMS-1362271,

More information

Seismic inverse scattering by reverse time migration

Seismic inverse scattering by reverse time migration Seismic inverse scattering by reverse time migration Chris Stolk 1, Tim Op t Root 2, Maarten de Hoop 3 1 University of Amsterdam 2 University of Twente 3 Purdue University MSRI Inverse Problems Seminar,

More information

Image amplitudes in reverse time migration/inversion

Image amplitudes in reverse time migration/inversion Image amplitudes in reverse time migration/inversion Chris Stolk 1, Tim Op t Root 2, Maarten de Hoop 3 1 University of Amsterdam 2 University of Twente 3 Purdue University TRIP Seminar, October 6, 2010

More information

5. A step beyond linearization: velocity analysis

5. A step beyond linearization: velocity analysis 5. A step beyond linearization: velocity analysis 1 Partially linearized seismic inverse problem ( velocity analysis ): given observed seismic data S obs, find smooth velocity v E(X), X R 3 oscillatory

More information

Extended isochron rays in prestack depth (map) migration

Extended isochron rays in prestack depth (map) migration Extended isochron rays in prestack depth (map) migration A.A. Duchkov and M.V. de Hoop Purdue University, 150 N.University st., West Lafayette, IN, 47907 e-mail: aduchkov@purdue.edu (December 15, 2008)

More information

[2] (a) Develop and describe the piecewise linear Galerkin finite element approximation of,

[2] (a) Develop and describe the piecewise linear Galerkin finite element approximation of, 269 C, Vese Practice problems [1] Write the differential equation u + u = f(x, y), (x, y) Ω u = 1 (x, y) Ω 1 n + u = x (x, y) Ω 2, Ω = {(x, y) x 2 + y 2 < 1}, Ω 1 = {(x, y) x 2 + y 2 = 1, x 0}, Ω 2 = {(x,

More information

Attenuation compensation in least-squares reverse time migration using the visco-acoustic wave equation

Attenuation compensation in least-squares reverse time migration using the visco-acoustic wave equation Attenuation compensation in least-squares reverse time migration using the visco-acoustic wave equation Gaurav Dutta, Kai Lu, Xin Wang and Gerard T. Schuster, King Abdullah University of Science and Technology

More information

Comparison between least-squares reverse time migration and full-waveform inversion

Comparison between least-squares reverse time migration and full-waveform inversion Comparison between least-squares reverse time migration and full-waveform inversion Lei Yang, Daniel O. Trad and Wenyong Pan Summary The inverse problem in exploration geophysics usually consists of two

More information

Seismic Imaging. William W. Symes. C. I. M. E. Martina Franca September

Seismic Imaging. William W. Symes. C. I. M. E. Martina Franca September Seismic Imaging William W. Symes C. I. M. E. Martina Franca September 2002 www.trip.caam.rice.edu 1 0 offset (km) -4-3 -2-1 1 2 time (s) 3 4 5 How do you turn lots of this... (field seismogram from the

More information

Seismic Modeling, Migration and Velocity Inversion

Seismic Modeling, Migration and Velocity Inversion Seismic Modeling, Migration and Velocity Inversion Inverse Scattering Bee Bednar Panorama Technologies, Inc. 14811 St Marys Lane, Suite 150 Houston TX 77079 May 30, 2014 Bee Bednar (Panorama Technologies)

More information

A Numerical Approach To The Steepest Descent Method

A Numerical Approach To The Steepest Descent Method A Numerical Approach To The Steepest Descent Method K.U. Leuven, Division of Numerical and Applied Mathematics Isaac Newton Institute, Cambridge, Feb 15, 27 Outline 1 One-dimensional oscillatory integrals

More information

Reverse Time Shot-Geophone Migration and

Reverse Time Shot-Geophone Migration and Reverse Time Shot-Geophone Migration and velocity analysis, linearizing, inverse problems, extended models, etc. etc. William W. Symes PIMS Geophysical Inversion Workshop Calgary, Alberta July 2003 www.trip.caam.rice.edu

More information

Edinburgh Research Explorer

Edinburgh Research Explorer Edinburgh Research Explorer Nonlinear Scattering-based Imaging in Elastic Media Citation for published version: Ravasi, M & Curtis, A 213, 'Nonlinear Scattering-based Imaging in Elastic Media' Paper presented

More information

Tu G Nonlinear Sensitivity Operator and Its De Wolf Approximation in T-matrix Formalism

Tu G Nonlinear Sensitivity Operator and Its De Wolf Approximation in T-matrix Formalism Tu G13 7 Nonlinear Sensitivity Operator and Its De Wol Approximation in T-matrix Formalism R.S. Wu* (University o Caliornia), C. Hu (Tsinghua University) & M. Jakobsen (University o Bergen) SUMMARY We

More information

Kirchhoff, Fresnel, Fraunhofer, Born approximation and more

Kirchhoff, Fresnel, Fraunhofer, Born approximation and more Kirchhoff, Fresnel, Fraunhofer, Born approximation and more Oberseminar, May 2008 Maxwell equations Or: X-ray wave fields X-rays are electromagnetic waves with wave length from 10 nm to 1 pm, i.e., 10

More information

Marchenko redatuming: advantages and limitations in complex media Summary Incomplete time reversal and one-sided focusing Introduction

Marchenko redatuming: advantages and limitations in complex media Summary Incomplete time reversal and one-sided focusing Introduction Marchenko redatuming: advantages and limitations in complex media Ivan Vasconcelos*, Schlumberger Gould Research, Dirk-Jan van Manen, ETH Zurich, Matteo Ravasi, University of Edinburgh, Kees Wapenaar and

More information

Wave equation techniques for attenuating multiple reflections

Wave equation techniques for attenuating multiple reflections Wave equation techniques for attenuating multiple reflections Fons ten Kroode a.tenkroode@shell.com Shell Research, Rijswijk, The Netherlands Wave equation techniques for attenuating multiple reflections

More information

An Approximate Inverse to the Extended Born Modeling Operator Jie Hou, William W. Symes, The Rice Inversion Project, Rice University

An Approximate Inverse to the Extended Born Modeling Operator Jie Hou, William W. Symes, The Rice Inversion Project, Rice University Jie Hou, William W. Symes, The Rice Inversion Project, Rice University SUMMARY We modify RTM to create an approximate inverse to the extended Born modeling operator in 2D. The derivation uses asymptotic

More information

Wave field extrapolation using a new multiplication/convolution method. work in progress

Wave field extrapolation using a new multiplication/convolution method. work in progress Wave field extrapolation using a new multiplication/convolution method work in progress Christiaan C. Stolk ABSTRACT In this paper we consider numerical methods for the acoustic equation, based on evolution

More information

Note that, when perturbing c(x) instead of m(x), an additional Taylor approximation is necessary: 1 c 2 (x) 1. c 2 0(x) 2εc 1(x).

Note that, when perturbing c(x) instead of m(x), an additional Taylor approximation is necessary: 1 c 2 (x) 1. c 2 0(x) 2εc 1(x). Chapter 3 Scattering series In this chapter we describe the nonlinearity of the map c u in terms of a perturbation (Taylor) series. To first order, the linearization of this map is called the Born approximation.

More information

Extensions and Nonlinear Inverse Scattering

Extensions and Nonlinear Inverse Scattering Extensions and Nonlinear Inverse Scattering William W. Symes CAAM Colloquium, September 2004 Data parameters: time t, source location x s, and receiver location x r, (vector) half offset h = x r x s, scalar

More information

Mathematics of Seismic Imaging Part II - addendum on Wave Equation Migration

Mathematics of Seismic Imaging Part II - addendum on Wave Equation Migration Mathematics of Seismic Imaging Part II - addendum on Wave Equation Migration William W. Symes PIMS, July 2005 Wave Equation Migration Techniques for computing F[v] : (i) Reverse time (ii) Reverse depth

More information

THE WAVE EQUATION. d = 1: D Alembert s formula We begin with the initial value problem in 1 space dimension { u = utt u xx = 0, in (0, ) R, (2)

THE WAVE EQUATION. d = 1: D Alembert s formula We begin with the initial value problem in 1 space dimension { u = utt u xx = 0, in (0, ) R, (2) THE WAVE EQUATION () The free wave equation takes the form u := ( t x )u = 0, u : R t R d x R In the literature, the operator := t x is called the D Alembertian on R +d. Later we shall also consider the

More information

Maximum Principles for Parabolic Equations

Maximum Principles for Parabolic Equations Maximum Principles for Parabolic Equations Kamyar Malakpoor 24 November 2004 Textbooks: Friedman, A. Partial Differential Equations of Parabolic Type; Protter, M. H, Weinberger, H. F, Maximum Principles

More information

Numerical Solutions to Partial Differential Equations

Numerical Solutions to Partial Differential Equations Numerical Solutions to Partial Differential Equations Zhiping Li LMAM and School of Mathematical Sciences Peking University Numerical Methods for Partial Differential Equations Finite Difference Methods

More information

Chapter 4. Adjoint-state methods

Chapter 4. Adjoint-state methods Chapter 4 Adjoint-state methods As explained in section (3.4), the adjoint F of the linearized forward (modeling) operator F plays an important role in the formula of the functional gradient δj of the

More information

Homogeniza*ons in Perforated Domain. Ki Ahm Lee Seoul Na*onal University

Homogeniza*ons in Perforated Domain. Ki Ahm Lee Seoul Na*onal University Homogeniza*ons in Perforated Domain Ki Ahm Lee Seoul Na*onal University Outline 1. Perforated Domain 2. Neumann Problems (joint work with Minha Yoo; interes*ng discussion with Li Ming Yeh) 3. Dirichlet

More information

An interferometric theory of source-receiver scattering and imaging

An interferometric theory of source-receiver scattering and imaging GEOPHYSICS, VOL. 75, NO. 6 NOVEMBER-DECEMBER 21; P. SA95 SA13, 7 FIGS. 1.119/1.3486453 An interferometric theory of source-receiver scattering and imaging David Halliday 1 and Andrew Curtis 2 ABSTRACT

More information

Topic: Introduction to Green s functions

Topic: Introduction to Green s functions Lecture notes on Variational and Approximate Methods in Applied Mathematics - A Peirce UBC 1 Topic: Introduction to Green s functions (Compiled 2 September 212) In this lecture we provide a brief introduction

More information

The second-order 1D wave equation

The second-order 1D wave equation C The second-order D wave equation C. Homogeneous wave equation with constant speed The simplest form of the second-order wave equation is given by: x 2 = Like the first-order wave equation, it responds

More information

Reconstructing inclusions from Electrostatic Data

Reconstructing inclusions from Electrostatic Data Reconstructing inclusions from Electrostatic Data Isaac Harris Texas A&M University, Department of Mathematics College Station, Texas 77843-3368 iharris@math.tamu.edu Joint work with: W. Rundell Purdue

More information

Renormalized scattering series for frequency domain. waveform modelling of strong velocity contrasts

Renormalized scattering series for frequency domain. waveform modelling of strong velocity contrasts Geophysical Journal International Advance Access published April 28, 216 Renormalized scattering series for frequency domain waveform modelling of strong velocity contrasts M. Jakobsen 1,2 and R.S. Wu

More information

1.4 Kirchhoff Inversion

1.4 Kirchhoff Inversion 1.4 Kirchhoff Inversion 1 Recall: in layered case, F [v]r(h, t) A(z(h, t), h) 1 dr (z(h, t)) 2dz F [v] d(z) z dh A(z, h) t (z, h)d(t(z, h), h) z [ F [v] F [v]r(z) = dh dt z dz (z, h)a2 (z, h) z r(z) thus

More information

Finite Difference Methods for Boundary Value Problems

Finite Difference Methods for Boundary Value Problems Finite Difference Methods for Boundary Value Problems October 2, 2013 () Finite Differences October 2, 2013 1 / 52 Goals Learn steps to approximate BVPs using the Finite Difference Method Start with two-point

More information

UNIVERSITY of LIMERICK OLLSCOIL LUIMNIGH

UNIVERSITY of LIMERICK OLLSCOIL LUIMNIGH UNIVERSITY of LIMERICK OLLSCOIL LUIMNIGH Faculty of Science and Engineering Department of Mathematics and Statistics END OF SEMESTER ASSESSMENT PAPER MODULE CODE: MA4006 SEMESTER: Spring 2011 MODULE TITLE:

More information

Iterative Solution methods

Iterative Solution methods p. 1/28 TDB NLA Parallel Algorithms for Scientific Computing Iterative Solution methods p. 2/28 TDB NLA Parallel Algorithms for Scientific Computing Basic Iterative Solution methods The ideas to use iterative

More information

Finite difference method for elliptic problems: I

Finite difference method for elliptic problems: I Finite difference method for elliptic problems: I Praveen. C praveen@math.tifrbng.res.in Tata Institute of Fundamental Research Center for Applicable Mathematics Bangalore 560065 http://math.tifrbng.res.in/~praveen

More information

Reverse time migration and Green s theorem: Part II-A new and consistent theory that progresses and corrects current RTM concepts and methods

Reverse time migration and Green s theorem: Part II-A new and consistent theory that progresses and corrects current RTM concepts and methods Reverse time migration and Green s theorem: Part II-A new and consistent theory that progresses and corrects current RTM concepts and methods A. B. Weglein, R. H. Stolt and J. D. Mayhan M-OSRP, University

More information

SUMMARY REVIEW OF THE FREQUENCY DOMAIN L2 FWI-HESSIAN

SUMMARY REVIEW OF THE FREQUENCY DOMAIN L2 FWI-HESSIAN Efficient stochastic Hessian estimation for full waveform inversion Lucas A. Willemsen, Alison E. Malcolm and Russell J. Hewett, Massachusetts Institute of Technology SUMMARY In this abstract we present

More information

Identification Methods for Structural Systems. Prof. Dr. Eleni Chatzi Lecture March, 2016

Identification Methods for Structural Systems. Prof. Dr. Eleni Chatzi Lecture March, 2016 Prof. Dr. Eleni Chatzi Lecture 4-09. March, 2016 Fundamentals Overview Multiple DOF Systems State-space Formulation Eigenvalue Analysis The Mode Superposition Method The effect of Damping on Structural

More information

Geometric PDE and The Magic of Maximum Principles. Alexandrov s Theorem

Geometric PDE and The Magic of Maximum Principles. Alexandrov s Theorem Geometric PDE and The Magic of Maximum Principles Alexandrov s Theorem John McCuan December 12, 2013 Outline 1. Young s PDE 2. Geometric Interpretation 3. Maximum and Comparison Principles 4. Alexandrov

More information

Chapter 3 Second Order Linear Equations

Chapter 3 Second Order Linear Equations Partial Differential Equations (Math 3303) A Ë@ Õæ Aë áöß @. X. @ 2015-2014 ú GA JË@ É Ë@ Chapter 3 Second Order Linear Equations Second-order partial differential equations for an known function u(x,

More information

INTRODUCTION TO PDEs

INTRODUCTION TO PDEs INTRODUCTION TO PDEs In this course we are interested in the numerical approximation of PDEs using finite difference methods (FDM). We will use some simple prototype boundary value problems (BVP) and initial

More information

LECTURE # 0 BASIC NOTATIONS AND CONCEPTS IN THE THEORY OF PARTIAL DIFFERENTIAL EQUATIONS (PDES)

LECTURE # 0 BASIC NOTATIONS AND CONCEPTS IN THE THEORY OF PARTIAL DIFFERENTIAL EQUATIONS (PDES) LECTURE # 0 BASIC NOTATIONS AND CONCEPTS IN THE THEORY OF PARTIAL DIFFERENTIAL EQUATIONS (PDES) RAYTCHO LAZAROV 1 Notations and Basic Functional Spaces Scalar function in R d, d 1 will be denoted by u,

More information

Can There Be a General Theory of Fourier Integral Operators?

Can There Be a General Theory of Fourier Integral Operators? Can There Be a General Theory of Fourier Integral Operators? Allan Greenleaf University of Rochester Conference on Inverse Problems in Honor of Gunther Uhlmann UC, Irvine June 21, 2012 How I started working

More information

Earthscope Imaging Science & CIG Seismology Workshop

Earthscope Imaging Science & CIG Seismology Workshop Earthscope Imaging Science & CIG Seismology Introduction to Direct Imaging Methods Alan Levander Department of Earth Science Rice University 1 Two classes of scattered wave imaging systems 1. Incoherent

More information

SUMMARY ANGLE DECOMPOSITION INTRODUCTION. A conventional cross-correlation imaging condition for wave-equation migration is (Claerbout, 1985)

SUMMARY ANGLE DECOMPOSITION INTRODUCTION. A conventional cross-correlation imaging condition for wave-equation migration is (Claerbout, 1985) Comparison of angle decomposition methods for wave-equation migration Natalya Patrikeeva and Paul Sava, Center for Wave Phenomena, Colorado School of Mines SUMMARY Angle domain common image gathers offer

More information

Numerical schemes for short wave long wave interaction equations

Numerical schemes for short wave long wave interaction equations Numerical schemes for short wave long wave interaction equations Paulo Amorim Mário Figueira CMAF - Université de Lisbonne LJLL - Séminaire Fluides Compréssibles, 29 novembre 21 Paulo Amorim (CMAF - U.

More information

2D Imaging in Random Media with Active Sensor Array

2D Imaging in Random Media with Active Sensor Array 2D Imaging in Random Media with Active Sensor Array Paper Presentation: Imaging and Time Reversal in Random Media Xianyi Zeng rhodusz@stanford.edu icme, Stanford University Math 221 Presentation May 18

More information

Elastic least-squares migration with two-way wave equation forward and adjoint operators

Elastic least-squares migration with two-way wave equation forward and adjoint operators Elastic least-squares migration with two-way wave equation forward and adjoint operators Ke Chen and Mauricio D. Sacchi, Department of Physics, University of Alberta Summary Time domain elastic least-squares

More information

Investigating advection control in parabolic PDE systems for competitive populations

Investigating advection control in parabolic PDE systems for competitive populations Investigating advection control in parabolic PDE systems for competitive populations Kokum De Silva Department of Mathematics University of Peradeniya, Sri Lanka Tuoc Phan and Suzanne Lenhart Department

More information

Reverse Time Migration for Extended Obstacles: Acoustic Waves

Reverse Time Migration for Extended Obstacles: Acoustic Waves Reverse Time Migration for Extended Obstacles: Acoustic Waves Junqing Chen, Zhiming Chen, Guanghui Huang epartment of Mathematical Sciences, Tsinghua University, Beijing 8, China LSEC, Institute of Computational

More information

First order Partial Differential equations

First order Partial Differential equations First order Partial Differential equations 0.1 Introduction Definition 0.1.1 A Partial Deferential equation is called linear if the dependent variable and all its derivatives have degree one and not multiple

More information

Coercivity of high-frequency scattering problems

Coercivity of high-frequency scattering problems Coercivity of high-frequency scattering problems Valery Smyshlyaev Department of Mathematics, University College London Joint work with: Euan Spence (Bath), Ilia Kamotski (UCL); Comm Pure Appl Math 2015.

More information

On positive solutions of semi-linear elliptic inequalities on Riemannian manifolds

On positive solutions of semi-linear elliptic inequalities on Riemannian manifolds On positive solutions of semi-linear elliptic inequalities on Riemannian manifolds Alexander Grigor yan University of Bielefeld University of Minnesota, February 2018 Setup and problem statement Let (M,

More information

Seismic imaging and multiple removal via model order reduction

Seismic imaging and multiple removal via model order reduction Seismic imaging and multiple removal via model order reduction Alexander V. Mamonov 1, Liliana Borcea 2, Vladimir Druskin 3, and Mikhail Zaslavsky 3 1 University of Houston, 2 University of Michigan Ann

More information

Wave-equation Hessian by phase encoding

Wave-equation Hessian by phase encoding Wave-equation Hessian by phase encoding Yaxun Tang ABSTRACT I present a method for computing wave-equation Hessian operators, also known as resolution functions or point-spread functions, under the Born

More information

Existence of viscosity solutions for a nonlocal equation modelling polymer

Existence of viscosity solutions for a nonlocal equation modelling polymer Existence of viscosity solutions for a nonlocal modelling Institut de Recherche Mathématique de Rennes CNRS UMR 6625 INSA de Rennes, France Joint work with P. Cardaliaguet (Univ. Paris-Dauphine) and A.

More information

Background. Background. C. T. Kelley NC State University tim C. T. Kelley Background NCSU, Spring / 58

Background. Background. C. T. Kelley NC State University tim C. T. Kelley Background NCSU, Spring / 58 Background C. T. Kelley NC State University tim kelley@ncsu.edu C. T. Kelley Background NCSU, Spring 2012 1 / 58 Notation vectors, matrices, norms l 1 : max col sum... spectral radius scaled integral norms

More information

The Finite Element Method for the Wave Equation

The Finite Element Method for the Wave Equation The Finite Element Method for the Wave Equation 1 The Wave Equation We consider the scalar wave equation modelling acoustic wave propagation in a bounded domain 3, with boundary Γ : 1 2 u c(x) 2 u 0, in

More information

1. Nonlinear Equations. This lecture note excerpted parts from Michael Heath and Max Gunzburger. f(x) = 0

1. Nonlinear Equations. This lecture note excerpted parts from Michael Heath and Max Gunzburger. f(x) = 0 Numerical Analysis 1 1. Nonlinear Equations This lecture note excerpted parts from Michael Heath and Max Gunzburger. Given function f, we seek value x for which where f : D R n R n is nonlinear. f(x) =

More information

1 POTENTIAL FLOW THEORY Formulation of the seakeeping problem

1 POTENTIAL FLOW THEORY Formulation of the seakeeping problem 1 POTENTIAL FLOW THEORY Formulation of the seakeeping problem Objective of the Chapter: Formulation of the potential flow around the hull of a ship advancing and oscillationg in waves Results of the Chapter:

More information

LECTURE 5 APPLICATIONS OF BDIE METHOD: ACOUSTIC SCATTERING BY INHOMOGENEOUS ANISOTROPIC OBSTACLES DAVID NATROSHVILI

LECTURE 5 APPLICATIONS OF BDIE METHOD: ACOUSTIC SCATTERING BY INHOMOGENEOUS ANISOTROPIC OBSTACLES DAVID NATROSHVILI LECTURE 5 APPLICATIONS OF BDIE METHOD: ACOUSTIC SCATTERING BY INHOMOGENEOUS ANISOTROPIC OBSTACLES DAVID NATROSHVILI Georgian Technical University Tbilisi, GEORGIA 0-0 1. Formulation of the corresponding

More information

Preconditioned space-time boundary element methods for the heat equation

Preconditioned space-time boundary element methods for the heat equation W I S S E N T E C H N I K L E I D E N S C H A F T Preconditioned space-time boundary element methods for the heat equation S. Dohr and O. Steinbach Institut für Numerische Mathematik Space-Time Methods

More information

Lecture No 1 Introduction to Diffusion equations The heat equat

Lecture No 1 Introduction to Diffusion equations The heat equat Lecture No 1 Introduction to Diffusion equations The heat equation Columbia University IAS summer program June, 2009 Outline of the lectures We will discuss some basic models of diffusion equations and

More information

Chapter 6: Rational Expr., Eq., and Functions Lecture notes Math 1010

Chapter 6: Rational Expr., Eq., and Functions Lecture notes Math 1010 Section 6.1: Rational Expressions and Functions Definition of a rational expression Let u and v be polynomials. The algebraic expression u v is a rational expression. The domain of this rational expression

More information

Numerical Analysis and Methods for PDE I

Numerical Analysis and Methods for PDE I Numerical Analysis and Methods for PDE I A. J. Meir Department of Mathematics and Statistics Auburn University US-Africa Advanced Study Institute on Analysis, Dynamical Systems, and Mathematical Modeling

More information

where F denoting the force acting on V through V, ν is the unit outnormal on V. Newton s law says (assume the mass is 1) that

where F denoting the force acting on V through V, ν is the unit outnormal on V. Newton s law says (assume the mass is 1) that Chapter 5 The Wave Equation In this chapter we investigate the wave equation 5.) u tt u = and the nonhomogeneous wave equation 5.) u tt u = fx, t) subject to appropriate initial and boundary conditions.

More information

2.4 Eigenvalue problems

2.4 Eigenvalue problems 2.4 Eigenvalue problems Associated with the boundary problem (2.1) (Poisson eq.), we call λ an eigenvalue if Lu = λu (2.36) for a nonzero function u C 2 0 ((0, 1)). Recall Lu = u. Then u is called an eigenfunction.

More information

B.Tech. Theory Examination (Semester IV) Engineering Mathematics III

B.Tech. Theory Examination (Semester IV) Engineering Mathematics III Solved Question Paper 5-6 B.Tech. Theory Eamination (Semester IV) 5-6 Engineering Mathematics III Time : hours] [Maimum Marks : Section-A. Attempt all questions of this section. Each question carry equal

More information

Medical Image Analysis

Medical Image Analysis Medical Image Analysis CS 593 / 791 Computer Science and Electrical Engineering Dept. West Virginia University 23rd January 2006 Outline 1 Recap 2 Edge Enhancement 3 Experimental Results 4 The rest of

More information

Imaging with Ambient Noise III

Imaging with Ambient Noise III Imaging with Ambient Noise III George Papanicolaou Stanford University http://math.stanford.edu/ papanico Department of Mathematics Richard E. Phillips Lectures April 23, 2009 With Liliana Borcea (Rice

More information

Gradient estimates and global existence of smooth solutions to a system of reaction-diffusion equations with cross-diffusion

Gradient estimates and global existence of smooth solutions to a system of reaction-diffusion equations with cross-diffusion Gradient estimates and global existence of smooth solutions to a system of reaction-diffusion equations with cross-diffusion Tuoc V. Phan University of Tennessee - Knoxville, TN Workshop in nonlinear PDES

More information

MATH 173: PRACTICE MIDTERM SOLUTIONS

MATH 173: PRACTICE MIDTERM SOLUTIONS MATH 73: PACTICE MIDTEM SOLUTIONS This is a closed book, closed notes, no electronic devices exam. There are 5 problems. Solve all of them. Write your solutions to problems and in blue book #, and your

More information

Test #2 Math 2250 Summer 2003

Test #2 Math 2250 Summer 2003 Test #2 Math 225 Summer 23 Name: Score: There are six problems on the front and back of the pages. Each subpart is worth 5 points. Show all of your work where appropriate for full credit. ) Show the following

More information

Reverse time migration image improvement using integral transforms

Reverse time migration image improvement using integral transforms Reverse time migration image improvement using integral transforms Juan Guillermo Paniagua C. M.Sc. in Engineering Ph.D. student in Mathematical Engineering GRIMMAT - Research group in mathematical modeling

More information

Approximation of fluid-structure interaction problems with Lagrange multiplier

Approximation of fluid-structure interaction problems with Lagrange multiplier Approximation of fluid-structure interaction problems with Lagrange multiplier Daniele Boffi Dipartimento di Matematica F. Casorati, Università di Pavia http://www-dimat.unipv.it/boffi May 30, 2016 Outline

More information

Solving the Fisher s Equation by Means of Variational Iteration Method

Solving the Fisher s Equation by Means of Variational Iteration Method Int. J. Contemp. Math. Sciences, Vol. 4, 29, no. 7, 343-348 Solving the Fisher s Equation by Means of Variational Iteration Method M. Matinfar 1 and M. Ghanbari 1 Department of Mathematics, University

More information

Using SVD for improved interferometric Green s function retrieval

Using SVD for improved interferometric Green s function retrieval Using SVD for improved interferometric Green s function retrieval Gabriela Melo, Alison Malcolm, Dylan Mikesell 2,3, and Kasper van Wijk 3 Earth Resources Laboratory - Earth, Atmospheric, and Planetary

More information

Observability and measurable sets

Observability and measurable sets Observability and measurable sets Luis Escauriaza UPV/EHU Luis Escauriaza (UPV/EHU) Observability and measurable sets 1 / 41 Overview Interior: Given T > 0 and D Ω (0, T ), to find N = N(Ω, D, T ) > 0

More information

Existence Theory: Green s Functions

Existence Theory: Green s Functions Chapter 5 Existence Theory: Green s Functions In this chapter we describe a method for constructing a Green s Function The method outlined is formal (not rigorous) When we find a solution to a PDE by constructing

More information

National Taiwan University

National Taiwan University National Taiwan University Meshless Methods for Scientific Computing (Advisor: C.S. Chen, D.L. oung) Final Project Department: Mechanical Engineering Student: Kai-Nung Cheng SID: D9956 Date: Jan. 8 The

More information

Fast Algorithms for the Computation of Oscillatory Integrals

Fast Algorithms for the Computation of Oscillatory Integrals Fast Algorithms for the Computation of Oscillatory Integrals Emmanuel Candès California Institute of Technology EPSRC Symposium Capstone Conference Warwick Mathematics Institute, July 2009 Collaborators

More information

MATH 220: MIDTERM OCTOBER 29, 2015

MATH 220: MIDTERM OCTOBER 29, 2015 MATH 22: MIDTERM OCTOBER 29, 25 This is a closed book, closed notes, no electronic devices exam. There are 5 problems. Solve Problems -3 and one of Problems 4 and 5. Write your solutions to problems and

More information

Introduction to numerical schemes

Introduction to numerical schemes 236861 Numerical Geometry of Images Tutorial 2 Introduction to numerical schemes Heat equation The simple parabolic PDE with the initial values u t = K 2 u 2 x u(0, x) = u 0 (x) and some boundary conditions

More information

(V.C) Complex eigenvalues and other topics

(V.C) Complex eigenvalues and other topics V.C Complex eigenvalues and other topics matrix Let s take a closer look at the characteristic polynomial for a 2 2 namely A = a c f A λ = detλi A = λ aλ d bc b d = λ 2 a + dλ + ad bc = λ 2 traλ + det

More information

Nonlocal Symmetry and Generating Solutions for the Inhomogeneous Burgers Equation

Nonlocal Symmetry and Generating Solutions for the Inhomogeneous Burgers Equation Proceedings of Institute of Mathematics of NAS of Ukraine 004, Vol. 50, Part, 77 8 Nonlocal Symmetry and Generating Solutions for the Inhomogeneous Burgers Equation Valentyn TYCHYNIN and Olexandr RASIN

More information

Introduction to PDEs and Numerical Methods Tutorial 1: Overview of essential linear algebra and analysis

Introduction to PDEs and Numerical Methods Tutorial 1: Overview of essential linear algebra and analysis Platzhalter für Bild, Bild auf Titelfolie hinter das Logo einsetzen Introduction to PDEs and Numerical Methods Tutorial 1: Overview of essential linear algebra and analysis Dr. Noemi Friedman, 25.10.201.

More information

ψ( ) k (r) which take the asymtotic form far away from the scattering center: k (r) = E kψ (±) φ k (r) = e ikr

ψ( ) k (r) which take the asymtotic form far away from the scattering center: k (r) = E kψ (±) φ k (r) = e ikr Scattering Theory Consider scattering of two particles in the center of mass frame, or equivalently scattering of a single particle from a potential V (r), which becomes zero suciently fast as r. The initial

More information

Model Extensions and Inverse Scattering: Inversion for Seismic Velocities

Model Extensions and Inverse Scattering: Inversion for Seismic Velocities Model Extensions and Inverse Scattering: Inversion for Seismic Velocities William W. Symes Rice University October 2007 William W. Symes ( Rice University) Model Extensions and Inverse Scattering: Inversion

More information

A Nonlinear Differential Semblance Strategy for Waveform Inversion: Experiments in Layered Media Dong Sun and William W Symes, Rice University

A Nonlinear Differential Semblance Strategy for Waveform Inversion: Experiments in Layered Media Dong Sun and William W Symes, Rice University A Nonlinear Differential Semblance Strategy for Waveform Inversion: Experiments in Layered Media Dong Sun and William W Symes, Rice University SUMMARY This paper proposes an alternative approach to the

More information

3. Wave equation migration. (i) Reverse time. (ii) Reverse depth

3. Wave equation migration. (i) Reverse time. (ii) Reverse depth 3. Wave equation migration (i) Reverse time (ii) Reverse depth 1 Reverse time computation of adjoint F [v] : Start with the zero-offset case - easier, but only if you replace it with the exploding reflector

More information

PARTIAL DIFFERENTIAL EQUATIONS MIDTERM

PARTIAL DIFFERENTIAL EQUATIONS MIDTERM PARTIAL DIFFERENTIAL EQUATIONS MIDTERM ERIN PEARSE. For b =,,..., ), find the explicit fundamental solution to the heat equation u + b u u t = 0 in R n 0, ). ) Letting G be what you find, show u 0 x) =

More information

Inverse Transport Problems and Applications. II. Optical Tomography and Clear Layers. Guillaume Bal

Inverse Transport Problems and Applications. II. Optical Tomography and Clear Layers. Guillaume Bal Inverse Transport Problems and Applications II. Optical Tomography and Clear Layers Guillaume Bal Department of Applied Physics & Applied Mathematics Columbia University http://www.columbia.edu/ gb23 gb23@columbia.edu

More information

Finite Difference Method

Finite Difference Method Capter 8 Finite Difference Metod 81 2nd order linear pde in two variables General 2nd order linear pde in two variables is given in te following form: L[u] = Au xx +2Bu xy +Cu yy +Du x +Eu y +Fu = G According

More information

COURSE Iterative methods for solving linear systems

COURSE Iterative methods for solving linear systems COURSE 0 4.3. Iterative methods for solving linear systems Because of round-off errors, direct methods become less efficient than iterative methods for large systems (>00 000 variables). An iterative scheme

More information

Numerical Solutions to Partial Differential Equations

Numerical Solutions to Partial Differential Equations Numerical Solutions to Partial Differential Equations Zhiping Li LMAM and School of Mathematical Sciences Peking University The Implicit Schemes for the Model Problem The Crank-Nicolson scheme and θ-scheme

More information

Renormalized scattering series for frequency domain waveform modelling of strong velocity contrasts

Renormalized scattering series for frequency domain waveform modelling of strong velocity contrasts Renormalized scattering series for frequency domain waveform modelling of strong velocity contrasts Journal: Manuscript ID GJI--.R Manuscript Type: Research Paper Date Submitted by the Author: -Nov- Complete

More information