Generalization of the Bremmer coupling series Maarten V. de Hoopa) Schlumberger Cambridge Research, High Cross, Madingley Road, Cambridge CB3 OEL, England ~Received 20 September 1995; accepted for publication 25 March 1996! An operator formalism is developed to expand the acoustic wave field in a multidimensionally smoothly varying medium, generated by a source localized in space and time, into a sum of constituents each of which can be interpreted as a wave that has traveled up and down with respect to a direction of preference a definite number of times. This expansion is a generalization of the Bremmer coupling series. The condition of smoothness of the medium relates to the width of the signature of the source in the configuration. Both the existence and the convergence ~in the weak sense! of the expansion are discussed. The operator calculus involved leads to a natural generalization of the concept of slowness surface to multi-dimensionally smoothly varying media. The operator associated with the corresponding generalized vertical slowness induces the full one-way wave operator in the type of media under consideration. In addition, a wavefield decomposition operator as well as an interaction operator that couples the decomposed constituents, are derived. © 1996 American Institute of Physics. @S0022-2488~96!01407-7# I. INTRODUCTION In recent years, there has been an increasing interest in the use of one-way ‘‘parabolic’’ approximations to the wave operator in the application of seismic modeling and migrationinversion techniques,1–3 and in the application of long-range waveguiding problems in ocean acoustics4–6 and integrated optics.7,8 The parabolic approximation arises in the decomposition ~or ‘‘splitting’’! of the acoustic wave field into constituents that travel ‘‘up’’ and ‘‘down’’ with respect to a given direction of preference, such that the two constituents satisfy coupled partial differential equations of a specific type. In this paper, we shall discuss the mathematical theory underlying this decomposition technique. The theory builds on the work of Seeley,9,10 Hörmander,11 and Duistermaat and Guilleman,12 and is based on the calculus of pseudodifferential operators. The use of such operators, in particular in the field of underwater acoustics where it yields the factorization of the Helmholtz operator, has been noticed by Fishman and McCoy,13–17 Fishman,18,19 Fishman and Wales,20 McCoy and Frazer,21 and Weston.22 The interaction of up- and downgoing constituents has been discussed by McCoy, Fishman, and Frazer.23 Within the parabolic approximations, Corones24 has put the interaction in the context of the Bremmer series. The direction of preference, which is assigned to the ‘‘vertical’’ direction, arises from the medium’s variations. In its exact form, the decomposition procedure transforms the scattering problem in n dimensions into a continuous family of ~n21!-dimensional problems, such that the remaining scattering phenomenon can be solved with the aid of a Neumann series in the relative vertical changes in the medium parameters. This series is a generalization to multi-dimensionally varying media of the Bremmer coupling series that has been used in one-dimensional scattering problems ~for an example, see Ref. 25!. a! Present address: Center for Wave Phenomena, Colorado School of Mines, Golden, Colorado 80401–1887. 3246 J. Math. Phys. 37 (7), July 1996 0022-2488/96/37(7)/3246/37/$10.00 © 1996 American Institute of Physics Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3247 The decomposition introduced applies to media which vary smoothly on the scale of the irradiating pulse, and generalizes the standard decomposition to media that are no longer translationally invariant in the ‘‘horizontal’’ directions. Owing to this generalization, more refined mathematical tools are required, such as the calculus of pseudo-differential operators. The up/down decomposition does not allow any further decomposition into horizontal, right/left, directions. Media, in which discontinuities in their physical properties occur, should be smoothed on the scale of the irradiating pulse with the aid of equivalent medium averaging prior to the decomposition. With regard to media with discontinuities, we mention the alternative, quasi-decomposition into up- and downgoing waves in the neighborhood of a ‘‘rough’’ interface separating two homogeneous half-spaces with the aid of the modified Rayleigh hypothesis.26,27 The key applications of the Bremmer series are ~i! an efficient way of numerically solving a direct scattering problem, ~ii! identification of multiple scattered wave constituents, and ~iii! formulations of various inverse scattering procedures. Fast numerical schemes require sparse matrix representations of the kernel associated with the relevant integral or pseudo-differential part of the one-way wave operator in space domain. The properties of the kernel, however, are such that generic bases in which its representation becomes sparse do not exist. Parabolic-type approximations of the kernel’s symbol, on the other hand, lead to possible sparsifications. The validity of such approximations has been discussed in previous papers.2,3 They typically capture the precritical angle phenomena in the wave propagation. Beyond this regime, matrix representations for the exact cokernel, acting in horizontal slowness space, have to be considered. A list of references to the development and applications of parabolic theories can be found in Ref. 2. Approximations of a different nature and with a different range of validity result from the method of phase screens.28 Other numerical procedures are based on constructing a spectral representation of the pseudodifferential part of the one-way wave operator and relate to normal-mode summation. The solution of the direct scattering problem in the form of a Bremmer series allows one to identify or predict multiple scattered constituents in the configuration. Applying this process to physical measurements, however, requires some knowledge about the medium in which the experiment has been carried out. In fact, the Bremmer series yields an expansion of the acoustic wavefield in terms of the spatial derivatives of the medium properties, as opposed to an expansion in the medium’s contrast with respect to a given embedding through a contrast-source integral representation. The leading term in the former expansion is a high-frequency ~Rytov-like! approximation to the wavefield; in the latter expansion, the leading term is the ~distorted! Born approximation in the embedding. It is noted that, once the former procedure has led to a construction of the Green’s function in the embedding, the latter procedure can be applied to the contrast ~possibly with discontinuities!. The Bremmer coupling series essentially recomposes the solutions of the system of coupled one-way wave equations into a two-way solution. As such, it connects the one-way wave formulation of scattering to the Dirichlet-to-Neumann map formulation ~see also Refs. 29 and 30!, and also yields a solution of the associated invariant imbedding equations. We note that the decomposition of the direct scattering problem is an integral part of the layer stripping approach to the inverse scattering problem ~see, for example, Ref. 31 for the one-dimensional formulation and Ref. 32, for a multi-dimensional formulation!. In fact, the Bremmer series representation allows one to link the asymptotic single-scattering approach ~see, for example, Ref. 33 and 34! with the mentioned multiple-scattering approach. The Bremmer coupling series becomes a powerful tool in those configurations in which the complexity of the medium is such that ray-theoretic approaches become intractable or the approximation by homogeneous horizontal layers breaks down. The remainder of this paper is organized as follows. In Sec. II, the principle of directional decomposition is explained. In Sec. III, the decomposition problem is related to the solution of an elliptic problem in one dimension less than the original scattering problem. In Sec. IV, the original system of two-way wave equations is transformed into a system of coupled one-way wave equa- J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3248 Maarten V. de Hoop: Generalized Bremmer coupling series tions. The one-way wave equations define a generalization of the concept of slowness surface, which is discussed in Sec. V. In Sec. VI, the fundamental properties of the Green’s functions of the one-way equations are derived. These functions are used in Sec. VII to transform the system of one-way integro-differential equations into a system of integral equations, which is then solved in terms of a Neumann series expansion. Finally, presented in Sec. VIII is a series expansion for the generalized slowness surface that yields an explicit solution of the elliptic problem posed in Sec. III. Section IX concludes the paper. We note that our analysis differs slightly from the standard mathematical treatment of factorizing differential operators, since in our case the ~n21!-dimensional ~‘‘horizontal’’! space is not assumed to be compact. However, with regard to the numerical implementation of the theory, periodic boundary conditions may be imposed in the horizontal directions. The causal acoustic waves are well defined on T n21 3R, where T n21 denotes the ~n21!-dimensional torus, for a finite time window. II. DIRECTIONAL DECOMPOSITION OF THE ACOUSTIC SCATTERING PROCESS In each subdomain of the configuration where the acoustic properties vary continuously with position, the acoustic wavefield satisfies the hyperbolic system of partial differential equations ] k p1 r] i v k 5 f k , ~II.1! k ] t p1 ] r v r 5q, ~II.2! where p5acoustic pressure ~Pa!, v r 5particle velocity ~m/s!, r5volume density of mass ~kg/m3!, k5compressibility ~Pa21!, q5volume source density of injection rate ~s21!, f k 5volume source density of force ~N/m3!, and $ x 1 ,x 2 ,x 3 % are the right-handed, orthogonal, Cartesian coordinates, t is the time, and the subscript notation and the summation convention for Cartesian tensors are employed. We assume that the coefficients r and k are smooth, i.e., infinitely differentiable functions of position, and time independent. Furthermore, we assume that these functions are constant outside a sphere of finite radius. This provision enables us to formulate the acoustic wave propagation, when necessary, as a scattering problem in a homogeneous embedding. The smoothness entails that the singularities of the wavefield ~in particular the ones on the wavefront! arise from the ones in the signatures of the source distributions. Further, causality of the wave motion is enforced. This implies that if the sources that generate the wavefield are switched on at the instant t50, the wavefield quantities satisfy the initial conditions p ~ x m ,t ! 50 for t,0 and all xm , ~II.3! v r ~ x m ,t ! 50 for t,0 and all xm . ~II.4! Due to the time invariance of the medium, the causality of the wave motion can also be taken into account by carrying out a one-sided Laplace transformation with respect to time and requiring that the transform-domain wave quantities are bounded functions of position in all space when the time Laplace-transform parameter s, which is in general complex, lies in the right half Re$ s % .0 of the complex s plane. The limiting case of sinusoidal oscillations of angular frequency vPR is covered by considering the limiting case s→iv , in which i is the imaginary unit, the limit being taken via Re$ s % .0. In view of Lerch’s theorem,35 however, it is sufficient to consider values with Im$ s % 50 and s>s 0.0; s 0 will be specified at several stages in the analysis. To show the notation, we give the expression for the acoustic pressure, p̂ ~ x m ,s ! 5 E ` t50 exp~ 2st ! p ~ x m ,t ! dt. ~II.5! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3249 Under this transformation, assuming zero initial conditions, we have ]t →s. The transformed system of first-order equations follows from Eqs. ~II.1! and ~II.2! as ] k p̂1s r v̂ k 5 f̂ k , ~II.6! s k p̂1 ] r v̂ r 5q̂. ~II.7! The change of the wavefield in space along a direction of preference can now be expressed in terms of the changes of the wavefield in the plane perpendicular to it. The direction of preference is taken along the x 3 axis ~or ‘‘vertical’’ axis! and the remaining ~‘‘horizontal’’! coordinates are denoted by x m , m51,2. The procedure requires a separate handling of the horizontal components of the particle velocity. From Eqs. ~II.6! and ~II.7! we obtain v̂ k 52 r 21 s 21 ~ ] k p̂2 f̂ k ! , ~II.8! leaving, upon substitution, the matrix differential equation ~ ] 3 d I,J 1s I,J ! F̂ J 5N̂ I , I,JP $ 1,2% , ~II.9! in which the elements of the acoustic field matrix are given by @in Eq. ~II.7! r5n,3# F̂ 1 5 p̂, ~II.10! F̂ 2 5 v̂ 3 , ~II.11! the elements of the acoustic system’s operator matrix are given by  1,15 2,250, ~II.12!  1,25 r , ~II.13!  2,152s 21 ] n ~ r 21 s 21 ] n ! 1 k , ~II.14! and the elements of the notional source matrix by N̂ 1 5 f̂ 3 , ~II.15! N̂ 2 52s 21 ] n ~ r 21 f̂ n ! 1q̂. ~II.16! It is observed that the right-hand side of Eq. ~II.8! and  I,J contain spatial derivatives with respect to the horizontal coordinates only. Further, it is noted that  1,2 is a multiplicative operator, whereas  2,1 is a partial differential operator. Equation ~II.9! is sometimes called the two-way wave equation ~Ref. 36!. To be able to solve the scattering process along the vertical direction separately from the scattering process in the ~family of! planes perpendicular to it, we decouple the two operators on the left-hand side of Eq. ~II.9!. This procedure will possibly lead to an additional source term on the right-hand side that accounts for the coupling. To achieve this, we shall construct an appropriate linear operator L̂ I,J with F̂ I 5L̂ I,J Ŵ J ~II.17! that, with the aid of the commutation relation J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3250 Maarten V. de Hoop: Generalized Bremmer coupling series FIG. 1. Directional decomposition. ~ ] 3 L̂ I,J ! 5 @ ] 3 ,L̂ I,J # ~II.18! ~@.,.# denotes the commutator!, transforms Eq. ~II.9! into L̂ I,J ~ ] 3 d J,M 1sL̂J,M ! Ŵ M 52 ~ ] 3 L̂ I,J ! Ŵ J 1N̂ I , ~II.19! so as to make L̂J,M , satisfying  I,J L̂ J,M 5L̂ I,J L̂J,M , ~II.20! a diagonal matrix of operators. We denote L̂ I,J as the composition operator and Ŵ M as the wave matrix. The elements of the wave matrix represent the local weights of the down- and upgoing constituents ~see also Fig. 1!. The expression in parentheses on the left-hand side of Eq. ~II.19! represents the two so-called one-way wave operators ~Ref. 36!. The first term on the right-hand side of Eq. ~II.19! is representative for the scattering due to variations of the medium properties in the vertical direction. The scattering due to variations of the medium properties in the horizontal directions is contained in L̂J,M and, implicitly, in L̂ I,J . To investigate whether solutions (L̂ I,J ,L̂J,M! of Eq. ~II.20! exist, we introduce the column matrix, or generalized eigenvector, operators L̂ (6) according to I L̂ ~I 1 ! 5L̂ I,1 , ~II.21! L̂ ~I 2 ! 5L̂ I,2 . ~II.22! Upon writing the diagonal elements of L̂J,M as L̂1,15Ĝ~ 1 ! , ~II.23! L̂2,25Ĝ~ 2 ! , ~II.24! Eq. ~II.20! decomposes into the two systems of equations  I,J L̂ ~J1 ! 5L̂ ~I 1 ! Ĝ~ 1 ! , ~II.25!  I,J L̂ ~J2 ! 5L̂ ~I 2 ! Ĝ~ 2 ! . ~II.26! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3251 By analogy with the case where the medium is translationally invariant in the horizontal directions, we shall denote Ĝ~6! as the vertical slowness operators. Notice that the operators L̂ ~6! 1 compose the acoustic pressure and that the operators L̂ ~6! 2 compose the vertical particle velocity, whereas the elements of Ŵ M may be physically ‘‘nonobservable.’’ ~6! Through mutual elimination, the equations for L̂ ~6! 1 and L̂ 2 can be decoupled as follows:  1,2 2,1L̂ ~16 ! 5L̂ ~16 ! Ĝ~ 6 ! Ĝ~ 6 ! , ~II.27!  2,1 1,2L̂ ~26 ! 5L̂ ~26 ! Ĝ~ 6 ! Ĝ~ 6 ! . ~II.28! The partial differential operators on the left-hand sides, which are given by  2,1 1,252s 21 ] n ~ r 21 s 21 ] n ~ r ! …1 k r , ~II.29!  1,2 2,152 r s 21 ] n ~ r 21 s 21 ] n ! 1 r k , ~II.30! are strongly elliptic in the horizontal plane R2 for each value of the vertical coordinate x 3PR and all frequencies s under consideration; they differ from one another in case the volume density of mass does vary in the horizontal directions. To ensure that nontrivial solutions of Eqs. ~II.27! and ~II.28! exist, one equation must imply the other. To construct a formal solution, an Ansatz is that restricts the introduced in the form of a commutation relation for one of the components L̂ (6) J freedom in the choice for the other component. Three choices will be considered. A. Acoustic-pressure normalization analog Our first Ansatz assumes that L̂ ~6! 2 can be chosen such that @ L̂ ~26 ! , 2,1 1,2# 50. ~II.31! In view of Eq. ~II.28!, the Ĝ~6! must then satisfy  2,1 1,22Ĝ~ 6 ! Ĝ~ 6 ! 50. ~II.32! (6) The commutation relation for L̂ ~6! follows as [ 21 1 1,2 L̂ 1 , 2,1 1,2#50 and a possible solution of Eqs. ~II.25! and ~II.26! is L̂ ~26 ! 5Ĝ~ 6 ! , L̂ ~16 ! 5 1,2 . ~II.33! as given by Eq. ~II.33! satisfies Eq. ~II.31!, the Ansatz is justified. In view of the Since L̂ ~6! 2 up/down symmetry, the solutions of Eq. ~II.32! are written as Ĝ~ 1 ! 52Ĝ~ 2 ! 5Ĝ5Â1/2, ~II.34! where Â[ 2,1 1,2. Thus, the composition operator becomes L̂5 S  1,2  1,2 Ĝ 2Ĝ D ~II.35! . In terms of the inverse vertical slowness operator, Ĝ215Â21/2, the decomposition operator then follows as L̂ 21 5 1 2 S  21 1,2 Ĝ21  21 1,2 2Ĝ21 D . ~II.36! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3252 Maarten V. de Hoop: Generalized Bremmer coupling series In this normalization, the elements of the wave matrix correspond with pressures up to the action of  1,2; pressures are typically measured with hydrophones. B. Vertical-particle-velocity normalization analog A second Ansatz assumes that L̂ ~6! 1 can be chosen such that @ L̂ ~16 ! , 1,2 2,1# 50. ~II.37! Then, Ĝ~6! must satisfy @cf. Eq. ~II.27!#  1,2 2,12Ĝ~ 6 ! Ĝ~ 6 ! 50, ~II.38! and a possible solution of Eqs. ~II.25! and ~II.26! is L̂ ~16 ! 5Ĝ~ 6 ! , L̂ ~26 ! 5 2,1 , ~II.39! which satisfies the second Ansatz. The solutions of Eq. ~II.38! are written as Ĝ~ 1 ! 52Ĝ~ 2 ! 5Ĝ5Â1/2, ~II.40! where Â[ 1,2 2,1. Thus, the composition operator is given by L̂5 S Ĝ 2Ĝ  2,1  2,1 D ~II.41! . Now, the decomposition operator becomes L̂ 21 5 1 2 S Ĝ21 Â21  1,2 2Ĝ21 Â21  1,2 D . ~II.42! In this normalization,  2,1 acting on the elements of the wave matrix results in vertical particle velocities; particle velocities are typically measured with geophones. C. Vertical-acoustic-power-flux normalization analog It will appear to be advantageous to consider a third Ansatz, viz., the one arising from the acoustic-power-flux normalization. For this, the commutation relation 1/2 1/2 ~6! @  21/2 1,2 L̂ 1 ,  1,2 2,1 1,2 # 50 ~II.43! is imposed on L̂ ~6! 1 . Then the vertical slowness operators must satisfy the equation 1/2 ~6! ~6! Ĝ 50.  1/2 1,2 2,1 1,22Ĝ ~II.44! 1/2 1/2 21 ] n „r 21 s 21 ] n ~ r 1/2 ! …1 k r , Â[ 1/2 1,2 2,1 1,252 r s ~II.45! Note that the operator Â, is self-adjoint with respect to the standard real L 2 inner product in ~almost all of! L 2. A possible solution of Eqs. ~II.25! and ~II.26! is now given by L̂ ~16 ! 5 ~  1,2/2! 1/2~ Ĝ~ 1 ! ! 21/2, L̂ ~26 ! 56 ~ 2 1,2! 21/2~ Ĝ~ 1 ! ! 1/2. ~II.46! The solutions of Eq. ~II.44! are written as J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series Ĝ~ 1 ! 52Ĝ~ 2 ! 5Ĝ5Â1/2. 3253 ~II.47! Thus, the composition operator is given by L̂5 1 & S 21/2  1/2 1,2Ĝ 21/2  1/2 1,2Ĝ 1/2 1/2  21/2 2 21/2 1,2 Ĝ 1,2 Ĝ D ~II.48! . This composition operator L̂: (L 2 ) 2 →(L 2 ) 2 is normalized in the sense that @cf. Eq. ~II.46!# L̂ T JL̂5 S I 0 0 2I D ~II.49! , with J5 S D 0 I I 0 ~II.50! . This normalization establishes the connection with asymptotic ray theory in the vicinity of the wavefronts. Using Eq. ~II.48!, we can map the pressure to the vertical particle velocity, viz., F̂ 2 5Ŷ~ 1 ! F̂ 1 if Ŵ 2 50, ~II.51! F̂ 2 5Ŷ~ 2 ! F̂ 1 if Ŵ 1 50, ~II.52! 21/2 6Ŷ~ 6 ! 5Ŷ5 21/2 1,2 Ĝ 1,2 ~II.53! where has the interpretation of admittance operator. The latter operator discriminates the decomposed constituents. Note that F̂ T1 F̂ 2 represents the vertical component of the Poynting vector. The decomposition operator becomes L̂ 21 5 1 & S Ĝ1/2 21/2 1,2 Ĝ21/2 1/2 1,2 Ĝ1/2 21/2 2Ĝ21/2 1/2 1,2 1,2 D . ~II.54! It is observed that all the operators involved can be directly constructed from Â21/4, viz., Ĝ21/25Â21/4, Ĝ1/25Â~Â21/4!3, and Ĝ5Â~Â21/4!2. All these powers of  are self-adjoint in ~almost all of! L 2 as well as positive definite, since it has been assumed that Im$ s % 50 and Re$s%.0. Apparently a whole class of composition operators L̂ I,J , all leading to different representations of the scattering process in the horizontal space, exists. The final results for the acoustic pressure and the vertical particle velocity, however, will not depend on a particular choice: in terms of observables the decomposition yields F̂ ~I 1 ! 5L̂ ~I 1 ! ~ L̂ 21 ! 1,J F̂ J , ~II.55! F̂ ~I 2 ! 5L̂ ~I 2 ! ~ L̂ 21 ! 2,J F̂ J . ~II.56! For practical applications, one adjusts the normalization to the sensors being used; it is quite common that only one of the two relevant field components is being measured. At this point, it is emphasized that Ĝ~6! are still unknown. It is noted that the key property we have used so far is that the diagonal of the system’s operator matrix  vanishes. For the evaluation J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3254 Maarten V. de Hoop: Generalized Bremmer coupling series of Ĝ~6!, and L̂ (6) J , we need to introduce ~fractional! powers of an elliptic partial differential operator in R2 for each value of x 3PR @cf. Eq. ~II.32!, ~II.38!, or ~II.44!#. How this can be done will be discussed in Sec. III. In this respect it is noted that only a proper definition of a negative ~fractional! power is needed, since positive fractional powers are constructed from the negative ones through the application of the operator itself an appropriate number of times. For the time being, the vertical coordinate will play the role of parameter, which will be indicated by writing R35R23R. In this framework, the wavefield is viewed as a map of x 3 with values in a function space on R2. III. THE DIMENSIONALLY REDUCED SCATTERING PROBLEM In this section we will consider the acoustic-pressure normalization analog. All the other normalizations lead to similar results. Thus, consider the partial differential operator Â5Â2,1Â1,2 on R2 @cf. Eq. ~II.29!# which is elliptic with a parameter yet to be specified. The dependence on x 3 will be suppressed in this section. In the following analysis it is assumed that the field matrix F̂ I and the wave matrix Ŵ M are contained in proper spaces, which, in view of the smoothness of the medium, is controlled by the source distributions @cf. Eqs. ~II.6! and ~II.7!#. The elliptic operator is clearly well-defined on the space C `0 of smooth functions with compact support in R2. It can be extended as a bounded operator Â: H r →H r22 for any real r ~Ref. 37, Theorem 8.9!. Here, H r is a reserved symbol for the Sobolev spaces. @Whenever we write H r , we mean H r ~R2!; otherwise, the underlying space will be specified.# The norm on H r will be denoted as i.ir , and the norm of an operator H r →H r 8 as i . i r,r 8 . The norms are implicitly scaled with the time Laplace-transform parameter s; we postpone the discussion of this aspect to Sec. V. In particular, when r50, we have an operator Â: L2→H22, which is bounded. On the other hand, note that Â: L 2 →L 2 is unbounded in general. First, we shall discuss the existence and integral representations of powers of Â. To this end, we need to analyze the properties of its resolvent. The construction of the resolvent is, essentially, the solution to the reduced scattering problem and will be dealt with in Sec. VIII. A. Properties of the resolvent Let l be a complex variable. The resolvent R̂ l of  is defined as R̂ l 5 ~ Â2lI ! 21 : H r →H r1l , 0<l<2. ~III.1! It exists for l¹s~Â!, which defines the spectrum s~Â! of Â. We refer to this spectrum as the horizontal spectrum. Whenever confusion would arise, the resolvent will be denoted as R̂ ~A! l rather than R̂ l to explicitly show its relation to the operator Â. First, to analyze the spectrum of Â, we consider the case r5l50. We have Â: L 2 →L 2 . In accordance with the structure of our horizontal partial differential operators, we introduce a family of inner products on L 2 with respect to û5û(x m ,s) and v̂ 5 v̂ (x m ,s) as ^ û, v̂ & 0 p 5 E x m PR û * v̂ r p dx 1 dx 2 , ~III.2! where * denotes complex conjugate ~note that for s real all the quantities are, however, real! and corresponding L 2-norms as i û i 20 5 ^ û,û & 0 p p ~III.3! with 21<p<1. For the acoustic-pressure normalization analog we take p51. ~For the verticalparticle-velocity normalization analog we take p521 and for the vertical-acoustic-power-flux normalization analog we take p50. When p50 the subscript will be omitted.! Using J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series E x m PR @ 2s 21 ] n „r 21 s 21 ] n ~ r û ! …# * v̂ r dx 1 dx 2 52 5 3255 E E x m PR x m PR r 21 [2s 21 ] n ~ r û ! ] * ~ s * ! 21 ] n ~ r v̂ ! dx 1 dx 2 û * @ 2 ~ s * ! 21 ] n „r 21 ~ s * ! 21 ] n ~ r v̂ ! …# r dx 1 dx 2 , ~III.4! it is found that  is self-adjoint in L 2, i.e., ^ Âû, v̂ & 0 1 5 ^ û,Âv̂ & 0 1 . ~III.5! In the derivation of Eq. ~III.4! it was used that the sum of contributions from the boundaries in the horizontal plane at infinity vanishes. In fact, the proof is obvious on C `0 ; subsequently, use that C `0 is dense in L 2. Note that the self-adjointness @cf. Eq. ~III.5!# in combination with the unboundedness is not in contradiction with the Hellinger–Toeplitz theorem,38 since it only holds for functions that satisfy boundary conditions associated with causal solutions to the spectral-domain acoustic equations. From Eq. ~III.4! it also follows that ~here, we need the condition Im$ s % 50! ^ Âû,û & 0 1 5 E x m PR r 21 u s 21 ] n ~ r û ! u 2 dx 1 dx 2 1 E x m PR k r u û u 2 r dx 1 dx 2 , ~III.6! so that ^ Âû,û & 0 1 > ^ c 22 &^ û,û & 0 1 , ~III.7! ^ c 22 & 5 inf $ k r % .0. ~III.8! in which x m PR This shows that  is positive and semi-bounded from below in i . i 0 1 . Again, these properties trivially hold, e.g., on C `0 . Since by Cauchy–Schwarz’ inequality i~ Â2lI ! û i 0 1 i û i 0 1 > u ^ ~ Â2lI ! û,û & 0 1 u , ~III.9! while @cf. Eq. ~III.7!# u ^ Âû,û & 0 1 2l * ^ û,û & 0 1 u > @~ ^ c 22 & 2Re$ l % ! 2 1 ~ Im$ l % ! 2 # 1/2^ û,û & 0 1 5 u ^ c 22 & 2l u ^ û,û & 0 1 ~III.10! if Re$l%<^c 22&, we obtain i~ Â2lI ! û i 0 1 i û i 0 1 > u ^ c 22 & 2l u i û i 20 . 1 ~III.11! Hence, when l¹s~Â! and Re$l%<^c 22&, we arrive at the estimate i R̂ l i 0 1 ,01 < u ^ c 22 & 2l u 21 ~III.12! for the operator norm of the resolvent as an operator L 2 →L 2 . When l is large enough, this implies that there exists a constant C 0,0 such that J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3256 Maarten V. de Hoop: Generalized Bremmer coupling series i R̂ l i 0 1 ,01 <C 0,0 / u l u . ~III.13! Now, let the inner product on H r using Parseval’s formula be defined through with Ĝ0 5 @ 2s 22 ] s ] s 1 ^ c 22 & # 1/2. ^ .,. & r p 5 ^ ~ Ĝ0 ! r ., ~ Ĝ0 ! r . & 0 p Thus, the inner product and the corresponding norm contain the parameter s. The estimate for the norm of R̂ l can be generalized following Ref. 9, Theorem 1, Corollary 1, and is given in Sec. VIII: i R̂ l i r,r1l <C r,l / u l u 12l/2, 0<l<2, ~III.14! when l is large enough and lies in the sector L5L0øLsp of the complex plane, where L0 is defined as p/2,uarg~l!u<p and Lsp is defined as 0,uarg~l!u<p/2. From Eq. ~III.7! ~r50! it also follows that the spectrum must be real and positive and bounded from below, i.e., when lPs~Â!, l> ^ c 22 & ; ~III.15! the ‘‘smoothness’’ of the possible eigenfunctions is estimated in their appropriate Sobolev space H r . The property that the spectrum is semibounded from below extends to  as an unbounded operator H r →H r also for rÞ0 ~see also Ref. 37, Theorem 13.31!. We have to ensure that the spectrum is strictly positive in H r for rÞ0. Since the multiplication operator, arising from the multiplicative part, say f̂, of the elliptic operator  satisfies (Ĝ0!rf̂~Ĝ0!2r 5 f̂ 2[ f̂ , (Ĝ0!r#~Ĝ0!2r while [ f̂ ,Ĝ0#5O~s21! as s→ `, it is found that ^ f̂ û,û & r p > 0 if the medium is sufficiently smooth or s is large enough and f̂>0. Anyway, the spectrum can be controlled by imposing constraints on the compressibility or on the topology of the underlying horizontal space. In general, the spectrum will consist of absolute continuous ~branch cut!, pure point and possibly singular continuous contributions. By requiring that k→ ` as uxmu→ `, or by applying periodic boundary conditions in the horizontal directions, the operator  becomes compact, and its spectrum becomes discrete. It is observed that the estimate in Eq. ~III.14! and the properties of  hold at each depth level x 3 , provided that ^c 22& is a positive and bounded function of x 3 . How to obtain, via a parametrix, the resolvent, which is a two-dimensional problem, will be discussed at the end of this paper. Given the resolvent R̂ l for l¹ s~Â!, we then construct general powers of the differential operator Â, following a standard procedure from functional analysis. This will be discussed in the next subsections. B. Negative fractional powers of the elliptic operator Let the power lz of a complex variable l with zPR be defined as l z 5 u l u z exp@ iz arg~ l !# , ~III.16! with arg~l!P~2p,p!. With this definition, the branch cut of lz is along the negative real axis. Let B be a contour of integration in the l plane around the branch cut, counter-clockwise oriented, staying away a small but finite distance from the origin ~the branch point!, not intersecting the spectrum s~Â!, and going to infinity in the sector L0 . Then, for zPR,0, the Dunford integral Âz 5 1 2pi E lPB l z R̂ l dl ~III.17! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3257 FIG. 2. Contours for the Dunford integral ~Seeley’s rays of minimal growth!. converges in the operator norm i•i r,r22z on H r ~the proof relies on the symbol calculus of Secs. V and VIII for the parametrix of Â2lI for lPL0 large, in combination with the knowledge about the spectrum s~Â! near the origin!. The integral satisfies the composition equation Âz Âw 5Âz1w ~III.18! for z, wPR,0. To show this, consider another contour B 8 around the branch cut such that B is in between B 8 and the branch cut. The integral in Eq. ~III.17! remains the same when the contour B is deformed into B 8 ~see Fig. 2!, since the contributions from the arcs connecting B and B 8 at infinity vanish. Using B 8 to evaluate Âz and B to evaluate Âw , we get Âz Âw 52 1 4p2 E E lPB 8 m PB R̂ l R̂ m l z m w dld m 52 1 4p2 E E lPB 8 m PB l zm w ~ R̂ l 2R̂ m ! dld m , l2 m ~III.19! in view of the Hilbert identity. Since for the first term we have owing to the theorem of residues E lPB 8 FE m PB G mw d m l z R̂ l dl52 p i l2 m E lPB 8 l w1z R̂ l dl ~III.20! and, upon changing the order of integration, for the second term E FE m PB G lz dl m w R̂ m d m 50, lPB 8 l2 m ~III.21! in view of Cauchy’s theorem, Eq. ~III.19! reduces to J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3258 Maarten V. de Hoop: Generalized Bremmer coupling series Âz Âw 5 E 1 2pi l z1w R̂ l dl, ~III.22! l 21 R̂ l dl, ~III.23! lPB 8 from which Eq. ~III.18! is found. C. The inverse operator In the case z521, Eq. ~III.17! implies Â21 5 1 2pi E lPS where S encircles the origin counter-clockwise ~note that the contributions from the branch cut cancel!. The spectrum of  lies outside S in the l plane. The change of variables m5l21 leads to Â21 5 E 1 2pi m PS 8 m R̂ m 21 m 22 d m , ~III.24! where S 8 denotes the contour in the m plane corresponding to S in the l plane, but also encircling the origin counter-clockwise. Notice that the spectrum of  lies inside S 8 in the m plane, hence R̂ m21 is well defined on S 8. Since R̂ m 21 5 m Â21 ~ m I2Â21 ! 21 , ~III.25! certainly when mPS 8, substitution in Eq. ~III.24! yields Â21 5 1 Â21 2pi E m PS 8 m 21 ~ I2 m 21  21 ! 21 d m . ~III.26! Since the operator Â21 must be bounded, ~I2 m 21 Â21!21 can be expanded in the Neumann series (I2 m 21 Â21!215( `n50 m 2n Â2n. In view of Cauchy’s theorem, only the term n50 in Eq. ~III.26! contributes, from which it follows that Â215Â21 ~III.27! ~see, e.g., Ref. 39, III Theorem 6.15!. Equations ~III.18! and ~III.27! show that the operators Âz behave like ordinary powers for negative values of z. D. Non-negative fractional powers of the elliptic operator With the aid of Eq. ~III.17! a non-negative fractional power of  can be readily introduced through Âz 5Âk Âz2k , ~III.28! where k is an integer such that k.z. The resulting operators behave, again, like ordinary powers, i.e., Âz Âw 5Âz1w ~III.29! ~note that  and its resolvent commute!. In view of Eqs. ~III.17!, and ~III.28! and ~III.14!, which are based on the results of Sec. VIII, it follows that Âz : H r →H r22z is bounded for general r and for all zPR. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3259 E. The Schrödinger problem If  is compact and self-adjoint, its eigenfunctions c and spectrum can be used to evaluate its negative fractional powers, viz., upon choosing the contour B in the Dunford integral equation ~III.17! in Lsp around s~Â!. Then, applying the theorem of residues leads to Âz c @ N # 5 1 2pi E lPB l z R̂ l c @ N # dl5 1 c 2pi @N# E lPB l z ~ l @ N # 2l ! 21 dl5l @zN # c @ N # . ~III.30! Expanding the components of the wave matrix into the eigenfunctions of  leads to a diagonal representation of Âz , viz., Âz û5 l @zN # û @ N # c @ N # ( @N# with û5 û @ N # c @ N # . ( @N# ~III.31! Finding the horizontal spectrum and eigenfunctions, Âc 5lc, is a Schrödinger problem in two dimensions; note that this spectrum may vary with x 3 . The Dunford integral around the spectrum links the current methodology to the theory of waveguides in two dimensions, since s 2  corresponds with a dimensionally reduced wave equation. F. Vertical derivatives of powers of the elliptic operator Consider, again, Eq. ~II.19!. We are now in a position to show that ~] 3 L̂ I,J ! exists. As before, it is sufficient to prove that the expression for ~] 3 Âz! converges in operator norm when z,0. To this end, we consider the integral 1 2pi E lPB l z ] 3 R̂ l dl, in which ] 3 R̂ l 52R̂ l ~ ] 3 Â! R̂ l , ~III.32! where ]3 in ~]3Â! acts on the coefficients of  only. In fact, ~]3Â!: H r →H r is a multiplication operator. Note that this operator is bounded, since the derivatives of the medium parameters are assumed to be continuous. Further, ]3R̂ l vanishes in those regions where the medium properties are independent of x 3 . The norm of ]3R̂ l satisfies the estimate @cf. Eq. ~III.14!# i ] 3 R̂ l i r,r1l1m < i R̂ l i r1l,r1l1m i~ ] 3 Â!i r1l,r1l i R̂ l i r,r1l <C r,l,m / u l u 22 ~ l1m ! /2 ~III.33! for 0<l, m<2, and lPL0 large. It then also follows that ~]3Âz!: H r →H r22(z21) exists and is bounded for Re$z%,0 ~the proof relies on the symbol expansions to be discussed in Sec. VIII!. Now, use the relation k ~ ] 3 Âz ! 5 ~ ] 3 Âk  z2k ! 5 ( q50 Âq ~ ] 3 Â!Âk2q Âz2k 1Âk ~ ] 3 Âz2k ! to extend the result from z,0 to z>0. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3260 Maarten V. de Hoop: Generalized Bremmer coupling series IV. THE SYSTEM OF ONE-WAY WAVE EQUATIONS IN THE TIME-LAPLACE-TRANSFORM DOMAIN Next, we complete the directional decomposition procedure. Using any of the decomposition schemes, Eq. ~II.19! transforms into ~ ] 3 d I,M 1sL̂I,M ! Ŵ M 52 ~ L̂ 21 ! I,M ~ ] 3 L̂ M ,K ! Ŵ K 1 ~ L̂ 21 ! I,M N̂ M , ~IV.1! which can be interpreted as a coupled system of one-way wave equations. The coupling between the components of Ŵ M is apparent in the first sourcelike term on the right-hand side. In particular, we shall further investigate the decomposition operator associated with the vertical-power-flux normalization and given by Eq. ~II.48!. For this normalization, the coupling operator becomes 2L̂ 21 ~ ] 3 L̂ ! 5 S D T̂ R̂ R̂ T̂ , ~IV.2! in which 21/2 1 2 2 @ Ĝ1/2, ~ ] 3 Ĝ21/2!# , T̂52 41 Ĝ21/2@ Ĝ,  21 1,2 ~ ] 3  1,2 !# Ĝ ~IV.3! where we have used the property that Ĝ1/2~]3Ĝ21/2!52~]3Ĝ1/2!Ĝ21/2, is the transmission operator that consists of commutators only, and 21 21/2 R̂52 41 Ĝ21/2„@ Ĝ,  21 1,2 ~ ] 3  1,2 !# 12 1,2 ~ ] 3  1,2 ! Ĝ22 ~ ] 3 Ĝ ! …Ĝ 21/2 1 52 41 Ĝ21/2$ Ĝ, 21 2 2 $ Ĝ1/2, ~ ] 3 Ĝ21/2! % , 1,2 ~ ] 3  1,2 ! % Ĝ ~IV.4! where $.,.% denotes the anticommutator, is the reflection operator. In the limit of a horizontally homogeneous medium ~or as s→ `!, the physical interpretation of Eq. ~IV.1! simplifies since then L̂ 21 ( ] 3 L̂) becomes purely off-diagonal. In this case, therefore only counter-propagating constituents interact. This property reveals the consistency of the decomposition method with asymptotic ray theory. The reflection and transmission operators are bounded and vanish, due to our initial assumption of a homogeneous, isotropic embedding, outside a closed interval along the x 3-direction. To show the boundedness, note that the multiplication operator, s s  21 1,2 ~ ] 3  1,2 ! : H →H ` with  21 1,2 ~ ] 3  1,2 ! PC 0 , ~IV.5! is bounded for all H s . Further, Ĝ1/2~]3Ĝ21/2!52~]3Ĝ1/2!Ĝ21/2: H r →H r1l with 0<l<2 are bounded. Thus, the norms of the reflection and transmission operators in R2 can be estimated as 1/2 i T̂ i r,r <C Tr,1 @ i Ĝ21/2i r21/2,r i  21 1,2 ~ ] 3  1,2 !i r21/2,r21/2i Ĝ i r,r21/2 21/2 i r,r11/2# 1C Tr,2 i@Ĝ1/2, ~ ] 3 Ĝ21/2!#i r,r 1 i Ĝ1/2i r11/2,r i  21 1,2 ~ ] 3  1,2 !i r11/2,r11/2i Ĝ ~IV.6! and 1/2 i R̂ i r,r <C Rr,1 @ i Ĝ21/2i r21/2,r i  21 1,2 ~ ] 3  1,2 !i r21/2,r21/2i Ĝ i r,r21/2 21/2 i r,r11/2# 1C Rr,2 i $ Ĝ1/2, ~ ] 3 Ĝ21/2! % i r,r 1 i Ĝ1/2i r11/2,r i  21 1,2 ~ ] 3  1,2 !i r11/2,r11/2i Ĝ ~IV.7! uniformly in s>s 0 .0. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3261 So far we have replaced Eq. ~II.9! by Eqs. ~IV.1! and ~II.17!. Equation ~IV.1! shows that at this stage the vertical derivative operator needs further analysis. To illustrate how the source distributions control the space to which the wave matrix belongs, suppose that f̂ k PH r and q̂PH r21 . Then N̂ 1 PH r and N̂ 2 PH r21 @cf. Eqs. ~II.15! and ~II.16!#. In accordance with the matrix operator in Eq. ~II.9!, F̂ 1 PH r11 and F̂ 2 PH r . Further, we have  1,2: H r(11) →H r(11) , whereas  2,1: H r11 →H r21 @cf. Eqs. ~II.12!–~II.14!#. In view of Eq. ~II.48! we then arrive at Ŵ M PH r11/2. In practice, we set r52 21. A. Factorization of the ‘‘Helmholtz’’ operator If we constrain our configuration to a vertically homogeneous ~thin! slab, the directional decomposition implies a factorization of the Laplace-domain analog of the second-order wave equation. Using Eq. ~II.40!, we find that ~ ] 3 1sĜ~ 1 ! !~ ] 3 1sĜ~ 2 ! ! 5 ] 23 2s 2 Â. ~IV.8! Indeed, the pressure satisfies the equation @cf. Eq. ~II.9!# ~ ] 23 2s 2  1,2 2,1! F̂ 1 5 ] 3 N̂ 1 2 1,2 sN̂ 2 . ~IV.9! However, it is emphasized that the factorization does not hold in this form for vertically heterogeneous media. V. THE GENERALIZED VERTICAL SLOWNESS For the proofs of the basic results in Sec. III, for the evaluation of the resolvent R̂ ~A! l and hence of Ĝ and L̂ I,J , as well as in preparation of the evaluation ~and the associated numerical implementation with respect to a Fourier basis! of the Green’s functions belonging to the left-hand side of Eq. ~IV.1!, the calculus of pseudo-differential operators is employed. An overview of the pseudo-differential-operator calculus can be found in several textbooks.11,40–42 It is obvious that Â: H r →H r22 can be interpreted as a pseudo-differential operator of order 2. The existence of the resolvent, via a parametrix, as a pseudo-differential operator has been shown by Seeley,9 Section 6. As a consequence of this, the vertical slowness operator Ĝ5Â1/2: H r →H r21 can be represented by a pseudo-differential operator of order 1. A. General considerations First, we present some rules for a general pseudo-differential operator Ĝ: H r →H r2d of order d; later on, we will focus our attention on the particular case of the vertical slowness operator for which d51. The Fourier transformation in the horizontal plane is defined as ũ ~ a m ,x 3 ,s ! 5 E x m PR û ~ x m ,s ! exp~ is a m x m ! dx 1 dx 2 . ~V.1! Here, i a m are identified as the horizontal slownesses. Now, the Sobolev norm ~with parameter s! on H r is written as ~in view of Plancherel’s theorem! i û i 2r 5 S DE s 2p 2 a m PR †u ũ ~ a m ,x 3 ,s ! u @~ ^ c 22 & 1 a s a s ! 1/2# r ‡2 d a 1 d a 2 . ~V.2! In the space domain, ia l corresponds to the horizontal slowness operator D l 52 1 ] . s l ~V.3! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3262 Maarten V. de Hoop: Generalized Bremmer coupling series Note that D l and the multiplication by x k do not commute, since @ xk , Dl#5 1 d . s k ,l ~V.4! However, in the limit s→` the commutator vanishes. By letting the operator Ĝ act on a Fourier component exp~2is a m x m ! we introduce its left symbol ĝ (x k , a l ), Ĝ~ x k ,D l ! exp~ 2is a m x m ! 5 ĝ ~ x k , a l ! exp~ 2is a m x m ! . ~V.5! For a general test function û this implies E Ĉ ~ x m ,x n8 ! û ~ x n8 ! dx 18 dx 28 , ~V.6! ĝ ~ x m , a n ! exp@ is a n ~ x n8 2x n !# d a 1 d a 2 . ~V.7! „Ĝ~ x k ,D l ! û…~ x m ! 5 x n8 PR in which, with the use of Eq. ~V.1!, Ĉ ~ x m ,x n8 ! 5 S DE 2 s 2p a n PR Here, Ĉ is called the Schwartz kernel of the pseudo-differential operator Ĝ. The left symbol and the Schwartz kernel are related through the Fourier transformation @cf. Eq. ~V.7!# ĝ ~ x m , a l ! 5 E x n8 PR Ĉ ~ x m ,x n8 ! exp@ is ~ x l 2x l8 ! a l # dx 18 dx 28 . ~V.8! In the horizontal space Fourier-transform domain Eq. ~V.6! becomes ~ Ĝũ !~ a m ! 5 S DE 2 s 2p g̃ ~ a m 2 a m8 , a n8 ! ũ ~ a n8 ! d a 18 d a 28 , ~V.9! exp~ is a m x m ! Ĝ~ x k ,D l ! û ~ x n ! dx 1 dx 2 ~V.10! exp~ is a m x m ! ĝ ~ x m , a n8 ! dx 1 dx 2 . ~V.11! a n8 PR where G̃ is defined as ~ Ĝũ !~ a m ! 5 E x n PR and g̃ as g̃ ~ a m , a n8 ! 5 E x n PR Equation ~V.9! explicitly shows the interaction between the different Fourier components ~see also Refs. 43–45!. The quantity g̃ is denoted as the cokernel42 of Ĝ. Its representation is useful for numerical computations. The notation in Eq. ~V.6! is justified by the fact that if ĝ would be a polynomial in al , as is the case when Ĝ is a partial differential operator, then Ĝ would be obtained from ĝ by replacing ia l by D l put to the right of the coefficients. Still, we omit the dependencies of ĝ and û on x 3 and s for the time being. The integral in Eq. ~V.6! converges with Eq. ~V.7! even when ĝ becomes large, as long as ĝ oscillates more slowly than the exponential. The Schwartz kernel @cf. Eq. ~V.7!# is a so-called oscillatory integral. To guarantee that the right-hand side of Eq. ~V.7! exists as a distribution, the symbol ĝ must lie in a space S d ~R23R2!, d being a real number, which means that for all m 1 ,m 2 ,n 1 ,n 2 there exists a constant C m 1 ,m 2 ,n 1 ,n 2 such that ~Ref. 11, Definition 18.1.1! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series u ~ ] a 1 ] a 2 ] x 1 ] x 2 ĝ !~ x k , a l ! u <C m 1 ,m 2 ,n 1 ,n 2 @~ ^ c 22 & 1 a s a s ! 1/2# d2m 1 2m 2 m 1 m n 2 n 1 2 3263 ~V.12! for all x kPR, alPR. The constant C m 1 ,m 2 ,n 1 ,n 2 may depend on s but is O~1! as s→ `. The number d is called the order of the space S d . We write S 2` 5 ù dPRS d . Under the condition Eq. ~V.12! it follows that Ĉ is a distribution of order <k with k.d12 ~Ref. 46, Theorem 7.8.2 and Appendix A!, while Ĝ: H r →H r2d is continuous ~Ref. 11, Theorem 18.1.13! and d is the so-called order of the operator; the corresponding operator norm associated with the Sobolev norm with parameter is O~1! as s→ ` if the symbol is O~1!. Then the kernel is smooth outside the diagonal in R23R2. The space of pseudo-differential operators of which the left symbols are in S d is denoted by Op S d . It is observed that Op S 2` is the space of operators the Schwartz kernels of which are in C `~R23R2!. The expansions of symbols to be considered later on will all be mod S 2`. B. The equation for the slowness surface The left symbol â5â(x m , a n ) of the normalized elliptic differential operator given in Eq. ~II.45!, Â52 r 1/2s 21 ] n „r 21 s 21 ] n ~ r 1/2 ! …1 k r 52s 22 ] n ] n 1 k r 1 43 r 22 s 22 ~ ] n r ! 2 2 21 r 21 s 22 ~ ] n ] n r ! , ~V.13! using Eq. ~V.5!, is obtained as â5 a n a n 1 k r 1 43 r 22 s 22 ~ ] n r ! 2 2 21 r 21 s 22 ~ ] n ] n r ! . ~V.14! The latter expression is real valued, while terms O(s 21 ) do not occur. The symbol lies in S 2 ~note that the third- and higher-order derivatives with respect to an vanish and that the volume density of mass and the compressibility together with their derivatives are bounded functions of position in space!. The corresponding Schwartz kernel is given by Â~ x m ,x m8 ! 52s 22 ] n ] n d ~ x m 2x m8 ! 1 @ k r 1 21 r 21 s 22 $ 23 r 21 ~ ] n r ! 2 2 ~ ] n ] n r ! % #~ x m ! d ~ x m 2x m8 ! , ~V.15! with as its support x m 5 x m8 , i.e., the diagonal in R23R2. To transform the operator equation ~II.44! into an equation for the corresponding left symbols, we consider the composition of two pseudo-differential operators. Representing the operators as in Eqs. ~V.6! and ~V.7!, the composition rule for the respective left symbols is found ~see the Appendix!. Application of this rule yields the definition of the generalized slowness surface as the solutions ĝ~6!PS 1 of @cf. Eq. ~V.14!# 2 S DE E s 2p 2 x 8n PR a 8n PR ĝ ~ x m , a l8 ! exp@ is ~ x s 2x s8 !~ a s 2 a s8 !# ĝ ~ x l8 , a n ! d a 81 d a 82 dx 81 dx 82 1 a n a n 1 k r 1 43 r 22 s 22 ~ ] n r ! 2 2 21 r 21 s 22 ~ ] n ] n r ! 50. ~V.16! The branches are ĝ (6) (x k , a l ) such that Re$ ĝ ~ 1 ! ~ x m , a n ! % >0 and Re$ ĝ ~ 2 ! ~ x m , a n ! % <0. Due to the isotropy ~up/down symmetry! of the medium we have ĝ (1) 52 ĝ (2) . Further, note that as s→ ` the composition of symbols tends to an ordinary multiplication. The solution of the J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3264 Maarten V. de Hoop: Generalized Bremmer coupling series associated equation for the slowness surface yields the principal vertical slowness, which coincides pointwise with the vertical gradient of travel time along a characteristic. So far, we had to assume that the medium properties ~i.e., the coefficients in the elliptic operator! were smooth. This condition can be somewhat relaxed. Media, in which discontinuities in their physical properties occur, should be smoothed on the scale of the irradiating pulse width with the aid of equivalent medium averaging. To allow singularities in the medium and the volume source densities to coexist, however, requires a novel analysis of pseudo-differential operators.47 Further, our analysis in the horizontal plane builds on the one on the torus; thus, we have chosen to use left symbols rather than Weyl symbols ~Ref. 11, Sections 18.4 and 18.5! in this paper. VI. THE GREEN’S FUNCTIONS OF THE ONE-WAY WAVE OPERATORS We now subject the left-hand side of Eq. ~IV.1! to a further investigation. In it, we recognize the operators ] 3 1sĜ~ 6 ! : L„R6 ,H r ~ R2 ! …→L„R6 ,H r21 ~ R2 ! …, ~VI.1! where L„R6 ,H r ~R2!…, denotes a Banach space of maps R6→H r ~R2!. The operators in Eq. ~VI.1! are the full one-way wave operators. A technical complication arises because the operators in Eq. ~VI.1! cannot be identified as pseudo-differential operators H r ~R23R!→ H r21 ~R23R! ~see also Ref. 41!. To arrive at the coupled system of integral equations that is equivalent to Eq. ~IV.1! and that can be solved in terms of a Neumann expansion, we have to invert the operator occurring on the left-hand side. The one-sided elementary kernels Ĝ (6) (x m ,x 3 ;x 8n ,x 83 ) associated with the operators Ĝ~ 6 ! 5 ~ ] 3 1sĜ~ 6 ! ! 21 : L„R6 ,H r ~ R2 ! …→L„R6 ,H r ~ R2 ! … in three-dimensional space are the so-called Green’s functions. They satisfy the equations ] 3 Ĝ ~6! 1sĜ~ 6 ! Ĝ ~6! together with the condition of causality. We will consider the case Ĝ5Ĝ~1!, Ĝ =Ĝ test function û as ~ Ĝû !~ x m ,x 3 ! 5 E E z PR x 8n PR 5 d ~ x n 2x 8n ! d ~ x 3 2x 83 ! , ~VI.2! ~1! , and Ĝ5Ĝ~1! in detail. The operator Ĝ acts on a Ĝ ~ x m ,x 3 ;x 8n , z ! û ~ x 8n , z ! dx 81 dx 82 d z . ~VI.3! Let us define the initial-value problem of determining the function Û(x m ,x 3 ; z ) satisfying ~ ] 3 1sĜ! Û50 for x 3 > z , Û ~ x m , z ; z ! 5û ~ x m , z ! . ~VI.4! Û ~ x m ,x 3 ; z ! d z . ~VI.5! Then it is observed that ~ Ĝû !~ x m ,x 3 ! 5 E x3 z 52` A. Properties of the inverse one-way wave operator Now, to estimate in a proper norm the operator Ĝ, let Ĝ5L̂1Ê, ~VI.6! where J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 1/2 L̂5 @ 2s 22 ] s ] s 1c 22 L # 3265 ~VI.7! is an elliptic operator independent of x 3 ~which can be identified as the vertical slowness operator of order 1 in a homogeneous medium with slowness c 21 L ! and where ~VI.8! Ê5Ĝ2L̂ is a pseudo-differential operator of order <0. Note that @cf. Eq. ~V.1! and below# i L̂û i r >c 21 L i û i r ~VI.9! uniformly in s ~and x 3!. In this framework, our initial-value problem is written as ~ ] 3 1sL̂! Û52sÊÛ for x 3 >x 83 , Û ~ x m ,x 83 ;x 83 ! 5û ~ x m ,x 83 ! . ~VI.10! Thus, the causal or one-sided propagator Û satisfies @cf. Eq. ~VI.10!# Û ~ x 3 ;x 83 ! 5exp@ 2s ~ x 3 2x 83 ! L̂# Û ~ x 83 ;x 83 ! 2s E x3 z 5x 83 exp@ 2s ~ x 3 2 z ! L̂# Ê~ z ! Û ~ z ;x 83 ! d z . ~VI.11! Taking Sobolev norms on both sides yields on account of Eq. ~VI.9! i Û ~ x 3 ;x 83 !i r <exp@ 2s ~ x 3 2x 83 ! c 21 L #i Û ~ x 8 3 ;x 8 3 !i r 1s E x3 z 5x 83 exp@ 2s ~ x 3 2 z ! c 21 3 !i r d z . L #i Ê~ z !i r,r i Û ~ z ;x 8 ~VI.12! Now, let w ~ x 3 ! 5exp~ sx 3 c 21 L !i Û ~ x 3 ;x 8 3 !i r , ~VI.13! then Eq. ~VI.12! leads to w ~ x 3 ! <w ~ x 83 ! 1s h E x3 z 5x 83 w~ z !dz, ~VI.14! where ~note that Ê must be bounded! h ~ c 21 L ! 5 sup i Ê~ x 3 !i r,r . x 3 PR ~VI.15! ~In view of the structure of Ĝ note that h depends on s but that an estimate can be given uniformly in s for values away from zero!. Application of Gronwall’s theorem ~Ref. 48, p. 37! to Eq. ~VI.14! yields w ~ x 3 ! <w ~ x 83 ! exp@ s h ~ x 3 2x 83 !# , ~VI.16! for x 3 > x 83 , so that upon using Eq. ~VI.13! we have i Û ~ x 3 ;x 83 !i r < i Û ~ x 83 ;x 83 !i r exp@ 2s ~ x 3 2x 83 !~ c 21 L 2 h !# ~VI.17! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3266 Maarten V. de Hoop: Generalized Bremmer coupling series for x 3 > x 83 . To find a useful estimate for the norm of Ĝ, c 21 must be chosen such that L 21 c 21 . h (c ) uniformly in s for s>s . Let ê denote the left symbol of Ê. An expansion for this L L 0 symbol follows from Eq. ~V.16! and the results of Sec. VIII: 1/2 ~0! , ê5 ~ a n a n 1c 22 ! 1/22 ~ a s a s 1c 22 L ! 1C ~VI.18! where c 225kr, and C ~0! is in S d , d<0 independent of c L . Let m5 sup u c 21 2c 21 L u. ~VI.19! x m PR3 In a realistic medium, we can arrange the parameters such that there exists an estimate m<m0 with m0 independent of c L . We have 1/2 u ~ a n a n 1c 22 ! 1/22 ~ a s a s 1c 22 L ! u <m. Since C ~0! is continuous, we find the estimate u ê ~ x m , a l ! u <m1c ~ 0 ! . ~VI.20! Further, we obtain ] a m ê5 a m 1/2 22 1/2 ! ~ a s a s 1c 22 L ! 2 ~ a n a n 1c 1/2 ~ a n a n 1c 22 ! 1/2~ a s a s 1c 22 L ! 1C ~ 21 ! , C ~ 21 ! 5 ] a m C ~ 0 ! . ~VI.21! Since C (21) PS d , d<21, we find the estimate u ] a m ê ~ x m , a l ! u < ~ m1c ~ 21 ! !~ ^ c 22 & 1 a s a s ! 21/2 ~VI.22! with c ~21! independent of c L . This way, we can continue to analyze estimates like Eq. ~V.12! for ê up to any order of differentiation. Let c 0 denote the supremum of all c (d) s; the calculus of symbols ~and the proof of continuity of pseudo-differential operators11! then implies the estimate sup i Ê~ x 3 !i r,r < b m1C 0 , x 3 PR C 05 b c 0 , b .1, ~VI.23! where C 0 is independent of c L . Now, choose c L so that 21 c 21 L . b m1C 0 > h ~ c L ! 5 sup i Ê~ x 3 !i r,r . x 3 PR ~VI.24! To be able to find a c 21 L , C 0 must satisfy the inequalities @cf. Eq. ~VI.24!# 0,2C 0 ,2 ~ b 21 ! sup c 21 1 ~ b 11 ! inf c 21 , x m PR3 x m PR3 from which it follows that b.1 must be chosen in accordance with the conditions 1< supx m PR3 c 21 b 11 . , infx m PR3 c 21 b 21 J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3267 Let b1 satisfy the conditions, and let b5b11b2 ; then b m<b1m1b2m0 , and b m0 can be absorbed in C 0 to recover an estimate of the type Eq. ~VI.24!. @In a horizontally homogeneous 21 21 2 c 21 medium we find m(c 21 L ) 5 supx 3 PRu c L u , hence c L must be chosen in accordance with 21 supx 3 PRc 21 .# c 21 L . b (11 b ) Now, take Sobolev norms on both sides of Eq. ~VI.5!: i~ Ĝû !~ x 3 !i r < < 5 E E E x3 z 52` x3 z 52` x3 z 52` i Û ~ x 3 ; z !i r d z exp@ 2s ~ x 3 2 z !~ c 21 L 2 h !# i Û ~ z ; z !i r d z exp@ 2s ~ x 3 2 z !~ c 21 L 2 h !# i û ~ z !i r d z . ~VI.25! Apparently, a useful norm on L„R6 , H r ~R2!… for the wavefield in three-dimensional space is given by i • i r;3 5 sup i • i r . ~VI.26! x 3 PR Then, from Eq. ~VI.25! it follows that i Ĝi r;3,r;3 < 1 s ~ c 21 L 2h! , ~VI.27! s>s 0 . This estimate has been made explicit for r50 @cf. below Eq. ~VI.17!#. Similar steps can be carried out upon replacing ~1! by ~2!. B. Path integral representations With the vertical slowness symbols following from the resolvent, which represents the scattering process in the horizontal directions, we can construct the Green’s functions Ĝ ~6! using a Hamiltonian path integral representation.49–51 First, it is observed that the vertical slowness operators at different levels of x 3 do not necessarily commute with one another due to the heterogeneity of the medium. Thus we arrive at a ‘‘time’’-ordered product integral representation ~see, e.g., Ref. 50! of the one-sided propagators @cf. Eq. ~VI.4!# associated with the one-way wave equations, where ‘‘time’’ refers to the vertical coordinate x 3 , H) J x3 Û ~ 6 ! ~ .,x 3 ;x 83 ! 56H ~ 7 @ x 83 2x 3 # ! exp@ 2sĜ~ 6 ! ~ ., z ! d z # û ~ .,x 83 ! . z 5x 83 ~VI.28! In this expression, the operator ordering is initiated by exp@ 2sĜ(.,x 38 )d z # acting on û(.,x 38 ) followed by applying exp@2sĜ~.,z!dz# to the result, successively for increasing z. If the medium in the interval @ x 38 , x 3 # were weakly varying in the vertical direction, the Trotter product formula can be applied to the product integral in Eq. ~VI.28!. This results in the Hamiltonian path integral representations for the Green’s functions, Ĝ ~6! ~ x n ,x 3 ;x m8 ,x 83 ! 56H ~ 7 @ x 83 2x 3 # ! E P D ~ x 9n , a 9n ! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3268 Maarten V. de Hoop: Generalized Bremmer coupling series F 3exp 2s E x3 z 5x 38 G d z $ i a s9 ~ d z x s9 ! 1 ĝ ~ 6 ! ~ x m9 , z , a n9 ,s ! % , ~VI.29! P being a set of paths „x m9 ( z ), a n9 ( z )… in ~horizontal! phase space satisfying x n9 ~ z 5x 38 ! 5x n8 , x n9 ~ z 5x 3 ! 5x n . ~VI.30! Omitting the Heaviside function in the expression for the Ĝ ~6! yields the kernel ĝ ~6! of the so-called phase shift operator ~Ref. 52!. A perturbative approximation of the latter operator based on the split-step Fourier transform is discussed in Ref. 53. In Eq. ~VI.29! we have restricted ourselves to causal solutions, since the conditions Re$ĝ ~1!%>0 and Re$ĝ ~2!%<0 imply that Ĝ ~6! remain bounded as ux 3u→ `. The path integral in Eq. ~VI.29! is to be interpreted as the lattice multiple integral Ĝ ~6! ~ x n ,x 3 ;x m8 ,x 38 ! E) S N 56H ~ 7 @ x 83 2x 3 # ! lim N→` F i51 s 2p D N21 2 d 2 a ~ni ! ) j51 d 2 x ~nj ! N 3exp 2s ( k51 $ i a ~sk ! ~ x ~sk ! 2x ~sk21 ! ! 1 ĝ ~ 6 ! ~ x ~mk ! , z k 2 21 N 21 Dx 3 , a ~nk ! ,s ! N 21 Dx 3 % G ~VI.31! with x ~n0 ! 5x n8 , x ~nN ! 5x n , ~VI.32! and Dx 3 5x 3 2x 38 . ~VI.33! Note that the function N t ~ x n ,x 8n ! 5 ( $ i a ~sk ! ~ x ~sk ! 2x ~sk21 ! ! 1 ĝ ~ 6 ! ~ x ~mk ! , z k 2 21 N 21 Dx 3 , a ~nk ! ,s ! N 21 Dx 3 % k51 can be associated with travel time along a path. All the integrations are taken over the interval ~2`,`!, N 21 Dx 3 is the step size in z, and (x m( j) , a (nj) ) are the coordinates of a path at the discrete values z j of z as j51,...,N. If Dx 3 is sufficiently small, the path integral reduces to Ĝ ~6! ~ x m ,x 3 ;x n8 ,x 38 ! .6H ~ 7 @ x 38 2x 3 # ! E S pD s 2 2 d a 19 d a 29 3exp@ 2s $ i a s9 ~ x s 2x s8 ! 1 ĝ ~ 6 ! ~ x m ,x 3 2 21 Dx 3 , a 9n ,s ! Dx 3 % # . ~VI.34! In the analysis ĝ ~6! may be interpreted as ~nonstandard square-root! Hamiltonians. If the medium varies strongly in the vertical direction, the interval @ x 83 , x 3 # is divided up into thinner slabs, and the product integral is used to arrive at a composition of one-sided propagators through these slabs, for which the lattice multiple integrals are then substituted. The resulting J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3269 multiple integral is similar to the one in Eq. ~VI.31!. It is conjectured that the stationary-phase approximation of the path integral in Eq. ~VI.29! leads to the leading term of the asymptotic ray expansion54,55 including the KMAH index,55 in the presence of caustics. The expression in Eq. ~VI.34! serves as the basis for numerical computations based on Fourier transformations. Rather than using this thin-slab propagator, quasi-Monte Carlo methods can be applied to numerically calculate the propagator over larger vertical distances. Also techniques from the theory of symplectic integrators ~Ref. 56! may prove to be useful in the propagation over long distances. C. The Schwartz kernel The one-sided Green’s function is directly related to the Schwartz kernel associated with the vertical slowness operator. Since @cf. Eqs. ~VI.3! and ~VI.29!# ] 3 ~ Ĝû !~ x m ,x 3 ! 2û ~ x m ,x 3 ! 5 E E x3 x n8 PR z 52` ] 3 Ĝ ~ x m ,x 3 ;x n8 , z ! û ~ x n8 , z ! dx 18 dx 28 d z , ~VI.35! while @cf. Eq. ~VI.5!# ] 3 ~ Ĝû !~ x m ,x 3 ! 2û ~ x m ,x 3 ! 5 E x3 z 52` ] 3 Û ~ x m ,x 3 ; z ! d z for all x 3 , we have @cf. Eq. ~VI.4!# 2sĜ~ .,.;x 3 ! Û ~ .,x 3 ; z ! 5 E x 8n PR ] 3 Ĝ ~ .,x 3 ;x 8n , z ! û ~ x 8n , z ! dx 81 dx 82 . ~VI.36! Upon taking the limit z↑x 3 , we thus obtain 2s„Ĝ~ .,.;x 3 ! û…~ x m ,x 3 ! 5 E lim ] 3 Ĝ ~ x m ,x 3 ;x 8n , z ! û ~ x 8n , z ! dx 81 dx 82 x 8n PR z ↑x 3 ~VI.37! so that Ĉ ~ x m ,x 8n ;x 3 ! 5 lim 2 z ↑x 3 1 ] Ĝ ~ x m ,x 3 ;x 8n , z ! . s 3 ~VI.38! This expression implies that, in the special case of a homogeneous medium, the Schwartz kernel reduces to the vertical particle velocity ~F̂ 2! response due to a vertical point-force source @ f̂ 3 5 d (x m 2 x m8 ) d (x 3 2 x 83 ) # at zero vertical offset. VII. THE BREMMER COUPLING SERIES The resolvents R̂ ~A! fully describe the scattering in the level surfaces of x 3 . From these l resolvents the left vertical slowness symbols have been derived, which in their turn are used in constructing the Green’s functions introduced in Sec. VI. Employing the Green’s functions of the one-way operators, we are now able to formulate the scattering process along the vertical direction in terms of a coupled system of integral equations. To simplify the notation, we set X̂ 1 5 ~ L̂ 21 ! 1,M N̂ M , X̂ 2 5 ~ L̂ 21 ! 2,M N̂ M . ~VII.1! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3270 Maarten V. de Hoop: Generalized Bremmer coupling series Using Eq. ~VII.1!, we rewrite Eq. ~IV.1! as @cf. Eqs. ~IV.3! and ~IV.4!# ] 3 Ŵ 1 1sĜ~ 1 ! Ŵ 1 5X̂ 1 1T̂Ŵ 1 1R̂Ŵ 2 , ~VII.2! ] 3 Ŵ 2 1sĜ~ 2 ! Ŵ 2 5X̂ 2 1R̂Ŵ 1 1T̂Ŵ 2 . ~VII.3! To derive an integral representation for Ŵ 1,2, we introduce the adjoint Green’s functions Ĝ satisfying ] 3 Ĝ ~6! ~6! T # Ĝ ~a6 ! 5 d ~ x n 2x 8n ! d ~ x 3 2x 83 ! , a 2s @ Ĝ with @ Ĝ~ 6 ! # T 5Ĝ~ 6 ! ~6! a ~VII.4! since Ĝ~6! is self-adjoint in L 2. Note that ~6! a ~x8 n Ĝ ~6! , z ;x m ,x 3 ! 52Ĝ ~ x m ,x 3 ;x 8n , z ! . ~VII.5! In fact, in view of the up/down symmetry of the medium, we also have Ĝ ~6! a ~x8 n , z ;x m ,x 3 ! 5Ĝ ~7! ~ x 8n , z ;x m ,x 3 ! . ~VII.6! @Equations ~VII.5! and ~VII.6! constitute reciprocity relations.# Combining Eq. ~VII.4! for the adjoint Green’s functions with ~VII.2! and ~VII.3!, it is found that ] 3 ^ Ĝ ~1! a ,Ŵ 1 0 5 ^ Ĝ ~1! 8 a ,X̂ 1 1T̂Ŵ 1 1R̂Ŵ 2 0 1Ŵ 1 ~ x n ,x 38 ! d ~ x 3 2x 38 ! , ~VII.7! ] 3 ^ Ĝ ~2! a ,Ŵ 2 0 5 ^ Ĝ ~2! 8 a ,X̂ 2 1R̂Ŵ 1 1T̂Ŵ 2 0 1Ŵ 2 ~ x n ,x 38 ! d ~ x 3 2x 38 ! . ~VII.8! & & & & Now, we have ^ Ĝ ~1! 8 a ~ .,x 3 ;x m ,x 83 ! ,Ŵ 1 ~ .,x 3 ! & 0 50 ~VII.9! as x 3→ ` since Ĝ (1) a 50 when x 3 . x 8 3 while in view of the assumption that in some upper half-space the fluid is homogeneous, Ŵ 150 as x 3→ 2` on the basis of causality. A similar reasoning leads to ^ Ĝ ~2! 8 a ~ .,x 3 ;x m ,x 83 ! ,Ŵ 2 ~ .,x 3 ! & 0 50 ~VII.10! as x 3→6`. Integration of Eqs. ~VII.7! and ~VII.8! over all x 3 then yields a coupled system of integral equations which can be written in operator form as @cf. Eq. ~VII.5!# ~ d I,J 2K̂I,J ! Ŵ J 5Ŵ 0I , ~VII.11! in which S DS Ĝ~ 1 ! Ŵ 01 0 5 Ŵ 2 0 0 ~2! Ĝ DS D X̂ 1 , X̂ 2 ~VII.12! i.e., Ŵ 01 ~ x m ,x 3 ! 5 E E Ĝ E E Ĝ Ŵ 02 ~ x m ,x 3 ! 5 x3 z 52` x n8 PR ` z 5x 3 x 8n PR ~1! ~2! ~ x m ,x 3 ;x n8 , z ! X̂ 1 ~ x n8 , z ! dx 18 dx 28 d z , ~VII.13! ~ x m ,x 3 ;x 8n , z ! X̂ 2 ~ x 8n , z ! dx 81 dx 82 d z ~VII.14! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3271 denote the directly transmitted waves, and K̂5 S Ĝ~ 1 ! 0 0 Ĝ~ 2 ! DS D T̂ R̂ R̂ T̂ ~VII.15! ~note that the second matrix operator acts in the horizontal directions only, whereas the first matrix operator acts in the full space!, i.e., ~ K̂1,1Ŵ 1 !~ x m ,x 3 ! 5 E E Ĝ ~ K̂1,2Ŵ 2 !~ x m ,x 3 ! 5 E E Ĝ E E Ĝ x3 x 8n PR z 52` x3 x 8n PR z 52` ~ K̂2,1Ŵ 1 !~ x m ,x 3 ! 5 ~ K̂2,2Ŵ 2 !~ x m ,x 3 ! 5 ` x 8n PR z 5x 3 E E ` x n8 PR z 5x 3 Ĝ ~1! ~ x m ,x 3 ;x 8n , z !~ T̂Ŵ 1 !~ x 8n , z ! dx 81 dx 82 d z , ~VII.16! ~1! ~ x m ,x 3 ;x 8n , z !~ R̂Ŵ 2 !~ x 8n , z ! dx 81 dx 82 d z , ~VII.17! ~2! ~ x m ,x 3 ;x 8n , z !~ R̂Ŵ 1 !~ x 8n , z ! dx 81 dx 82 d z , ~2! ~ x m ,x 3 ;x n8 , z !~ T̂Ŵ 2 !~ x n8 , z ! dx 18 dx 28 d z ~VII.18! ~VII.19! are representative for the multiple scattering formalism. Now, consider the operators K̂I,J : L„R6 , H 0~R2!…→L„R6 , H 0~R2!…. In the space of wave matrices we introduce the norm @cf. Eq. ~VI.26!# S( 2 i Ŵ i 5 J51 i Ŵ J i 20;3 D 1/2 . ~VII.20! 2 i K̂I,J i 20;3,0;3 . Using the norm estimates of the preceding sections, it is found Hence, i K̂i 2 < ( I,J51 21 that iK̂i5O(s ) as s→ `, which implies that the norm of K̂ is less than 1 when s>s 0 , for s 0 sufficiently large. In that case a convergent Neumann expansion of Eq. ~VII.11! yields its solution. Thus, the solution of Eq. ~VII.11!, Ŵ5R̂ ~ K! Ŵ 0 , ~VII.21! is found in the form of a sum of generalized-ray-like constituents, the Bremmer series,57 upon employing the Neumann expansion for the resolvent of K̂: ` R̂ ~ K! 5 ~ I2K̂! 21 5 ( K̂n . n50 ~VII.22! To emphasize that we have found the solution of the direct scattering problem as a summation over multiple scattered constituents, we write ` Ŵ5 ( n50 Ŵ ~ n ! with Ŵ ~ n ! 5K̂Ŵ ~ n21 ! . ~VII.23! Figure 3 illustrates the decomposition procedure and the interrelation between the different resolvents. The analog of the series in a horizontally shift invariant medium can be found, e.g., in Refs. 58 and 59. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3272 Maarten V. de Hoop: Generalized Bremmer coupling series FIG. 3. The decomposition of the scattering process ~the solid rays refer to one term in the series!. Upon substituting in K̂ the path integral representations for the Green’s functions of Sec. VI, the recursion formula ~VII.23! leads to path integral representations for all the constituents in the coupling series. Upon substituting for the transmission/reflection operators their Schwartz kernel representations, Eq. ~VII.23! essentially composes path integrals at any level where interaction takes place. In particular, one finds a path integral representation for the leading order backscattered field, Ŵ ~1!. Finally, Eq. ~II.17! must be employed to compose the acoustic field matrix per constituent @cf. Eq. ~VII.21!#, i.e., to obtain the observables. The uniqueness of the time-domain counterpart of this result for s>s 0 is guaranteed by Lerch’s theorem ~see Ref. 35!. Note that the convergence of the series is guaranteed essentially in the time domain; the convergence criterium in the frequency or complex Laplace domain as described by Wing,60 and earlier by Atkinson,61 is different from ours. From the final representation of the acoustic field matrix, the associated representation for the Dirichlet-to-Neumann map can be obtained.29 VIII. ANALYSIS OF THE SYMBOLS The scattering process in horizontal space is governed by a composition equation for the ~unknown! resolvent of a ~known! elliptic operator. Here, we shall discuss an asymptotic expansion for the left symbol of the resolvent belonging to  introduced in Sec. III as the slowness vector becomes large to find the solution of the composition equation ~V.16! as well as the other powers needed to transform Eq. ~II.9! into Eq. ~IV.1!. Using the first few terms of the asymptotic expansion, a Neumann series is derived for the resolvent. The latter expansion is the counterpart in horizontal space of the Neumann expansion introduced in Sec. VII. A natural decomposition of the left symbol of the partial differential operator  is @cf. Eq. ~V.14!# â5â ~ ` ! 1â ~ 22 ! , ~VIII.1! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3273 the first term being O~1! and the second term being O(s 22 ) as s→ `. We have â ~ ` ! 5 a n a n 1č 22 c 22 ` , â ~ 22 ! 5 43 r 22 s 22 ~ ] n r ! 2 2 21 r 21 s 22 ~ ] n ] n r ! , ~VIII.2! where č 21 5 ~ c/c ` ! 21 ~VIII.3! c 22 5 k r , ~VIII.4! and in which c 21 ` is an appropriate parameter, introduced to enforce the correct asymptotic behavior. The differential equation for the symbol r̂ l of the resolvent follows from the equation ~Â2lI!R̂ l 5I as @cf. Eq. ~VIII.2!# ~ is 21 ] x s 1 a s ! 2 r̂ l 1 ~ c 22 1â ~ 22 ! 2l ! r̂ l 2150. ~VIII.5! This equation must be solved for r̂ l PS 22. The left symbols of the negative real powers then follow from @cf. Eq. ~III.17!# â z 5 1 2pi E B l z r̂ l dl. ~VIII.6! The symbols of the positive real powers are obtained using the composition equation for left symbols repeatedly ~see the Appendix!. A. The parametrix: asymptotic analysis To carry out the asymptotic analysis, the symbol of the operator Â2lI with parameter is written as â l 5â l,21â l,0 , ~VIII.7! where â l,25â ~ ` ! 2l, â l,05â ~ 22 ! . ~VIII.8! The correct behavior of the symbol of the resolvent as l and c 21 ` become large is achieved by thinking of l and c 22 as the squares of the Fourier domain counterparts of two new independent ` variables. Actually, it is natural to treat the slowness of the medium as if it were a component of the slowness vector. This way, the term 2l and the one linear in c 22 ` are absorbed in the principal part of the symbol. It is noticed that â l,2 is homogeneous of degree 2 in ~am ,l1/2,c 21 ` !, i.e., 21 2 â t 2 l,2~ x m ,t a n ,tc 21 ` ! 5t â l,2~ x m , a n ,c ` ! ~VIII.9! for t.0 such that t 2lPL, while â l,0 is homogeneous of degree 0 in the same sense. Further, it follows that â l,2Þ0 for lPL and ~asas!1/21ulu1/21uc 21 ` uÞ0, where L is, again, the sector in the complex l plane defined by 0,uarg~l!u<p. Hence, the operator associated with â l is ‘‘elliptic 2 2 2 with parameters l and c 21 ` ,’’ whereas the symbol itself is in S L~R 3R ,R!. The extension of this concept to anisotropic elastic media has been given by de Hoop and de Hoop.62 In the following it is crucial to restrict l to the sector L in the complex plane. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3274 Maarten V. de Hoop: Generalized Bremmer coupling series Consider the parametrix B̂ l , which is an approximation to the resolvent R̂ l in the following sense. Let the symbol of the resolvent, too, be expanded in a sum of symbols b̂ l,222 j which are homogeneous of degree 222j in ~am ,l1/2,c 21 ` !; then this sum defines the parametrix, which resembles the resolvent up to an integral operator in Op S 2` with an infinitely differentiable kernel ~Ref. 63, p. 20!. The successive terms in the series have increasingly smooth kernels. This way, a parametrix is constructed with the correct behavior as ulu→ ` or c 21 ` → ` ~the latter corresponds to s→ `!. Thus, the symbol of the parametrix is written as ` b̂ l 5 ( j50 ~VIII.10! b̂ l,222 j . The terms b̂ l,222 j , j50,1,..., are determined as follows. Substitute the expansion Eq. ~VIII.10! into Eq. ~VIII.5! and collect terms of equal degrees. Then we arrive at â l,2b̂ l,22 51, â l,2b̂ l,23 12is 21 a m ] x m b̂ l,22 50, â l,2b̂ l,222 j 12is 21 a m ] x m b̂ l,212 j 1 @ â l,02s 22 ] x m ] x m # b̂ l,2 j 50, ~VIII.11! j52,3,... . It can be shown that the solutions must satisfy ~following Ref. 9! 1/2 22 u ~ ] a 1 ] a 2 ] x 1 ] x 2 b̂ l,222 j !~ x k , a m ! u <s 2 j C m 1 ,m 2 ,n 1 ,n 2 @~ ^ c 22 & 1 a n a n 1c 22 ` 1ulu ! # m 1 m 2 n n 1 2 3 @~ ^ c 22 & 1 a s a s ! 1/2# 2 j2m 1 2m 2 . ~VIII.12! For the asymptotic sum as following from Eq. ~VIII.11!, we have the estimate K21 b̂ l 2 ( j50 b̂ l,222 j 5O ~ u a u 222K ! as u a u → ` ~VIII.13! for K51,2,3,... . Let B̂ l,222 j be the operator that corresponds to the symbol b̂ l,222 j , and let K21 B̂ ~lK ! 5 ( j50 B̂ l,222 j . ~VIII.14! From Eq. ~VIII.12!, using that for l50,1,2 we have 1/2 22 1/2 2l < u l u 211l/2 @~ ^ c 22 & 1 a n a n 1c 22 @~ ^ c 22 & 1 a n a n 1c 22 ` 1ulu ! # ` ! # , ~VIII.15! we obtain the estimate for B̂ (K) l : 9 / u l u 12l/2 i B̂ ~lK ! i r,r1l <C r,l,K ~VIII.16! there is associated the truncated expansion of Â, viz., Â(K) with l50,1,2 and lPL. With B̂ (K) l K21 (`) 5 ( j 8 50 Â22 j 8 ~set â 2 5â , â 0 5â (22) , â j 8 50 otherwise!. In general, if K>2 we have Â2Â(K) POp S 0, so that the latter difference is bounded and continuous as an operator H r →H r ; the same holds for Â2Â(K) : H r →H r1K22 . Using this and Eq. ~VIII.16!, it follows that for K>2 8 / u l u 12l/2. i~ Â2lI ! B̂ ~lK ! 2 ~ Â~ K ! 2lI ! B̂ ~lK ! i r,r1l1K22 <C r,l,K ~VIII.17! J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3275 Using Eqs. ~A15!, ~VIII.11!, and ~VIII.12!, after some manipulations as in Refs. 9 and 10, we arrive at i I2 ~ Â2lI ! B̂ ~lK ! i r,r1l1K22 <C r,l,K / u l u 12l/2 ~VIII.18! with l50,1,2 and lPL, whereas C r,l,K 5O(s 2K ) as s→ `. Hence, for K52, setting Ĉ l 5I2 ~ Â2lI ! B̂ ~l2 ! , ~VIII.19! we get for sufficiently large l @cf. Eq. ~VIII.18!# i Ĉ l i r,r < 21 . ~VIII.20! Thus, the resolvent follows as the convergent Neumann series S( D ` R̂ l 5B̂ ~l2 ! n50 Ĉ nl for lPL large. ~VIII.21! Now, using that ` ( n50 i Ĉ nl i r1l,r1l <2, ~VIII.22! in combination with Eq. ~VIII.16!, finally leads to the estimate in Eq. ~III.14!. Following Ref. 9 ~Theorem 2!, through the explicit evaluation of the symbols @cf. Eq. ~VIII.6!# it can be shown that the integral in Eq. ~III.17! defines a pseudo-differential operator of order 2z. Solving the system of equations ~VIII.11! yields b̂ l,22 5â 21 l,2 , ~VIII.23! b̂ l,23 52 a m ~ is 21 ] x m â l,2! â 23 l,2 , ~VIII.24! while 22 22 b̂ l,24 52â l,0 â 22 ~ ] x m ] x m â l,2! â 23 ~ ] x m â l,2!~ ] x m â l,2! l,2 2s l,2 1 @ 2s 21 14 a m s 21 a n s 21 ~ ] x m ] x n â l,2!# â 24 ] x m â l,2! l,2 212~ a m s 3 ~ a n s 21 ] x n â l,2! â 25 l,2 ~VIII.25! and so on. It is observed that the Neumann series for the vertical scattering gives rise to a decomposition into constituents that have traveled up and down a definite number of times, while the Neumann series in Eq. ~VIII.21! clearly does not separate the wavefield into constituents that travel from right to left or vice versa. B. The vertical slowness From a physical point of view, it is interesting to compare the contributions to the generalized slowness surface from the successive terms of the parametrix. For this, the integration over l has to be carried out and the original elliptic operator has to be applied to the result. Using Eqs. ~VIII.6!, ~VIII.23!, and ~VIII.24!, we have J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3276 Maarten V. de Hoop: Generalized Bremmer coupling series â 21/2~ x m , a n ! 5 ~ c 22 1 a s a s ! 21/2 @ 11 43 ~ c 22 1 a n a n ! 22 i a m s 21 ~ ] x m c 22 ! 1••• # . With this the left symbol for the vertical slowness becomes ĝ ~ x m , a n ! 5 ~ is 21 ] x s 1 a s ! 2 â 21/21 ~ c 22 1â ~ 22 ! ! â 21/2 5 ~ c 22 1 a s a s ! 1/2 @ 11 ~ c 22 1 a n a n ! 21 â ~ 22 ! 1 21 ~ c 22 1 a n a n ! 22 3 $ 2 21 i a m s 21 ~ ] x m c 22 ! 1s 22 ~ ] x m ] x m c 22 ! % 1••• # . ~VIII.26! Note that this expansion is valid for real-valued am; it is, however, nonuniform. In the complex radial horizontal slowness plane, a set of branch points, where the argument of the square root vanishes, has been introduced. Near the branch points the polyhomogeneous expansion does not behave properly, and a uniform expansion must be found. It is an open issue whether a parallel analytic continuation of the symbols into the complex radial horizontal slowness and complex Laplace planes exists and would be stable. However, in the angular frequency ~v! domain with s5i v and an52i a ~nv! , vPR and a~nv!PR, a uniform expansion has been found by Fishman and Gautesen.30 Spectral theory ~Sec. III! can also be employed to construct a convergent expansion for â z , â z ~ x m , a n ! 5 ( @N# l @zN # N@N# c @ N #~ x m ! E x 8n PR c @ N # ~ x 8n ! exp@ is ~ x s 2x s8 ! a s # dx 81 dx 82 ~VIII.27! if E x m PR c @ N # ~ x m ! c @ M # ~ x m ! dx 1 dx 2 5N @ N # d @ N # , @ M # . ~VIII.28! Upon taking z52 21 and composing the result with â, the vertical slowness symbol is found, as before. The latter construction implies an explicit regularization of the vertical slowness operator. Numerical algorithms associated with a construction of this kind can be found in the literature on the Mode Expansion Method64 ~see also Ref. 65!. IX. DISCUSSION OF THE RESULTS In this paper, we have generalized the Bremmer coupling series to configurations with multidimensionally varying media with properties that are up/down symmetric. The setup of the series required the introduction of the directional wavefield decomposition into, the one-way wave equations for, and the interaction of up/down constituents. The decomposition into ‘‘up’’ and ‘‘down’’ no longer permits a separation into ‘‘left’’ and ‘‘right.’’ The convergence of the series in space–time has been proved. The solution of the direct scattering problem in smoothly varying media has been given in terms of two nested series expansions. Both expansions represent resolvents, one associated with the coupling of counter-propagating constituents, and the other associated with the evaluation of the generalized slowness surface and the ~de!composition operators. For practical purposes, one hopes that just a few terms of both series suffice to describe the scattering phenomenon under investigation; particular numerical advantage is achieved when only a few frequencies are of physical importance. Smoothness of the medium is understood relative to the pulse width associated with the irradiating source. The derivation of the generalized Bremmer coupling series implies two basically alternative numerical approaches: a spectral approach based upon the eigenfunctions of the elliptic operator, J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3277 and a phase space approach making direct use of the left symbols. The spectral approach is rigorous, but not as efficient as the phase space approach. The most straightforward way to develop a propagation algorithm of the first kind is based on a matrix representation of the elliptic operator on the torus in terms of a basis of pyramid-type functions ~rather than a basis of eigenfunctions!; this leads to a finite difference approximation of the partial differential operator. The matrix is then diagonalized with the aid of the Lanczos method66 in which only the relevant eigenpairs are calculated and propagated. The remaining calculations make use of the diagonal form thus obtained. The phase space approach lends itself for various different approximations to enhance its computational efficiency. Among those are the ~rational! parabolic approximations and the phasescreen reduction of the vertical slowness symbol. The phase-screen approximation is only valid in relatively weakly heterogeneous media. In the rational approximation method, special care has to be taken to keep the associated, approximate vertical slowness operator self-adjoint; inherently, the distinction between the principal part of and the higher-order contributions to the vertical slowness symbol becomes obscure ~see Ref. 67!. The uniform expansion of Fishman and Gautesen30 lends itself to a competing algorithm, and includes critical scattering-angle phenomena, unlike the rational approximation approach. We note that the generalized Bremmer coupling series as presented in this paper lends itself to understanding the limits of approximate one-way wave theories. Several approaches exist for the transformation back to the time domain. A numerical inverse Laplace transform can be used under the assumption that we restrict our scattered field to a finite time window. It is emphasized that causility in this approach throughout the calculations is preserved. For a review of various algorithms we refer the reader to Ref. 68; pioneering work was carried out by Papoulis.69 As a candidate, we mention the Stehfest algorithm. ACKNOWLEDGMENTS The author would like to thank Professor J. J. Duistermaat and Professor A. T. de Hoop for their interest in this work and their many valuable comments. This research was supported in part by the Institute for Mathematics and its Applications, Minneapolis, MN, with funds provided by the National Science Foundation. Part of the research was carried out at the Koninklijke/Shell Exploratie en Produktie Laboratorium, Rijswijk, the Netherlands. APPENDIX: THE CALCULUS OF PSEUDO-DIFFERENTIAL OPERATORS 1. The composition equation In this subsection we consider the composition of two pseudo-differential operators, B̂35B̂1B̂2 , say. Representing the operators as in Eqs. ~V.6! and ~V.7!, E B̂ ~ x m ,x 8n ! û ~ x 8n ! dx 81 dx 82 , ~A1! b̂ ~ x m , a n ! exp@ is a n ~ x n8 2x n !# d a 1 d a 2 , ~A2! „B̂~ x k ,D l ! û…~ x m ! 5 x 8n PR in which B̂ ~ x m ,x n8 ! 5 S DE s 2p 2 a n PR a composition rule for the corresponding left symbols, b̂ 1 , b̂ 2 , and b̂ 3 , is found. To begin with, the Schwartz kernels must satisfy the composition rule J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3278 Maarten V. de Hoop: Generalized Bremmer coupling series E B̂ 3 ~ x m ,x n8 ! 5 x n9 PR B̂ 1 ~ x m ,x n9 ! B̂ 2 ~ x n9 ,x n8 ! dx 19 dx 29 . ~A3! Hence, S DE s 2p 2 a n PR b̂ 3 ~ x m , a n ! exp@ is a s ~ x s8 2x s !# d a 1 d a 2 5 E x 9n PR B̂ 1 ~ x m ,x 9n ! B̂ 2 ~ x 9n ,x 8n ! dx 91 dx 92 . ~A4! Substituting in Eq. ~A4! u n 5x n and u n 5 2(x 8n 2 x n ), we arrive at S DE s 2p 2 a n PR b̂ 3 ~ u m , a n ! exp~ 2is a s v s ! d a 1 d a 2 5 E x n9 PR B̂ 1 ~ u m ,x n9 ! B 2 ~ x n9 ,u n 2 v n ! dx 19 dx 29 . ~A5! By inverse Fourier transformation it now follows that b̂ 3 ~ u m , a n ! 5 E E x 9n PR v n PR B̂ 1 ~ u m ,x 9n ! B̂ 2 ~ x 9n ,u n 2 v n ! exp~ is a s v s ! dx 91 dx 92 d v 1 d v 2 . ~A6! Substituting Eq. ~A2! twice yields b̂ 3 ~ u m , a n ! 5 S DE E E E 4 s 2p x 9n PR a 8n PR a 9n PR v n PR b̂ 1 ~ u m , a 8n ! b̂ 2 ~ x 9n , a 9n ! 3exp@ is $ ~ a s 2 a s9 !v s 1 ~ u s 2x s9 !~ a s9 2 a s8 ! % # 3d v 1 d v 2 d a 19 d a 92 d a 81 d a 82 dx 91 dx 92 . ~A7! Upon performing four of the integrations, we arrive at (u m 5x m ) b̂ 3 ~ x k , a l ! 5 S DE E s 2p 2 x n9 PR a n8 PR b̂ 1 ~ x m , a n8 ! b̂ 2 ~ x n9 , a n ! 3exp@ is ~ x s 2x s9 !~ a s 2 a s8 !# d a 18 d a 28 dx 19 dx 29 . ~A8! This equation can also be written as a differential equation. To this end, we introduce the fourdimensional Fourier transformation in phase space b5 ~ j m , h n ! 5 S DE E s 2p 2 x m PR a n PR b̂ ~ x m , a n ! exp@ is ~ j k x k 1 h l a l !# d a 1 d a 2 dx 1 dx 2 ~A9! and its inverse b̂ ~ x m , a n ! 5 S DE E s 2p 2 j m PR h n PR b5 ~ j m , h n ! exp@ 2is ~ j k x k 1 h l a l !# d h 1 d h 2 d j 1 d j 2 . ~A10! Using Eq. ~A10!, we have S DE E s 2p 2 x k PR a l PR b̂ ~ x k , a l ! exp~ isx s a s ! d a 1 d a 2 dx 1 dx 2 J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 5 S DE E E E s 2p 4 a l PR x k PR j k PR h l PR 3279 b5 ~ j k , h l ! exp@ 2is ~ j s x s 1 h s a s 2x s a s )]d h 1 d h 2 d j 1 d j 2 dx 1 dx 2 d a 1 d a 2 5 S DE E F G s 2p 5exp 2 j k PR h l PR b5 ~ j k , h l ! exp~ 2is j s h s ! d h 1 d h 2 d j 1 d j 2 i ] ] b̂ ~ x k , a l ! u ~ x k , a l ! 5 ~ 0,0! . s as xs ~A11! Using this equality in Eq. ~A8!, it is found that F b̂ 3 ~ x k , a l ! 5exp G i ] ] b̂ ~ x , a 8 ! b̂ ~ x 8 , a ! s a s8 x s8 1 k n 2 m l U . ~ x k8 , a l8 ! 5 ~ x k , a l ! ~A12! The interpretation of the exponential operator follows upon analyzing F B̂ 3 ~ x k , a l ,x m8 , a 8n ! 5exp G i ] ] b̂ ~ x , a 8 ! b̂ ~ x 8 , a ! s a s8 x s8 1 k n 2 m l ~A13! introducing M 21 r̂ M ~ x k , a l ,x m8 , a 8n ! 5B̂ 3 ~ x k , a l ,x m8 , a 8n ! 2 ( m50 SD 1 i m! s m ~ ] a 8 ] x 8 ! m b̂ 1 ~ x k , a 8n ! b̂ 2 ~ x m8 , a l ! . s s ~A14! Note that b̂ 3 (x k , a l )5B̂ 3 (x k , a l ,x k , a l ). Suppose that b̂ 1 lies in a space S s 1 and that b̂ 2 lies in a space S s 2 . Then the following estimate holds ~see the proof of Theorem 18.1.8 in Ref. 11! m m n n m 81 m 82 n 81 n 82 ] a ] x ] x r̂ M !~ x k , a l ,x m8 , a 8n ! u a 2 18 28 18 28 u~ ] a 1] a 2] x 1] x 2] 1 2 1 <C M ,m 1 ,m 2 ,n 1 ,n 2 ,m 8 ,m 8 ,n 8 ,n 8 @~ 11 a 8r a 8r ! 1/2# s 1 2M 2m 81 2m 82 1 2 1 2 3 @~ 11 a s a s ! 1/2# s 2 2m 1 2m 2 , ~A15! which implies that r̂ M (x m , a n ,x m , a n ) P S s 1 1s 2 2M . 2. Continuity We will review the proof of continuity of a pseudo-differential operator B̂: H r →H r2d , given that its symbol b̂ is contained in S d . Let Ĝ be the pseudo-differential operator of order 1, Ĝ0 5 @ 2D s D s 1 ^ c 22 & # 1/2, ~A16! which, by Fourier analysis, is trivially continuous as an operator H r →H r21 . Then also Ĝd0 : H r →H r2d continuous for dPR. ~A17! r Now, let ûPH r . Then û 0 5Ĝro û P L 2 ; using the parametrix Ĝ2r o of Ĝo , we can write J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3280 Maarten V. de Hoop: Generalized Bremmer coupling series û5Ĝ2r 0 û 0 1 v̂ 0 with û 0 PL 2 and v̂ 0 PC ` . The contribution from v̂ 0 is trivially dealt with. We obtain r2d 2r Ĝr2d 0 B̂û5Ĝ0 B̂Ĝ0 û 0 . ~A18! 2r 2 2 B̂0 [Ĝr2d continuous. 0 B̂Ĝ0 : L →L ~A19! Hence, continuity of B̂ is proved, if From the calculus of symbols, discussed in the preceding subsection, we find that the symbol b̂ 0 of the latter operator is contained in S 0. Step 1: b̂ PS 2n21 . Let m51,...,n, and b̂ PS 2n21 . Then u B̂ ~ x m ,x 8n ! u < S DE s 2p 2 a n PR u b̂ ~ x m , a n ! u 2 d a 1 •••d a n <C. Note that ~ x m 2x m8 ! l m B̂ ~ x m ,x n8 ! corresponding with i l m ] am b̂ ~ x m , a n ! l m must be bounded as well, hence ~ 11 @~ x m 2x m8 ! 2 # 1/2! n11 u B̂ ~ x m ,x 8n ! u <C. Schur’s lemma states that if B̂(x m ,x n8 ) is continuous and sup x 8n E x m PR u B̂ ~ x m ,x 8n ! u dx 1 •••dx n <C and sup xm E x 8n PR u B̂ ~ x m ,x 8n ! u dx 81 •••dx 8n <C, ~A20! that then B̂:L 2 →L 2 is bounded with norm <C. ~This is a consequence of Cauchy–Schwarz inequality.! Conditions ~A20! are satisfied for b̂ PS 2n21 . Step 2: b̂ PS m , m<21. Let b̂ PS m , m<21. Let b̂ * PS m be the symbol of the adjoint operator B̂T. Set Ĉ[B̂T B̂. Then i B̂û i 2 < i Ĉû i i û i . Hence, if Ĉ is continuous, then B̂ must be continuous. Let the symbol of Ĉ be contained in S 2m . By induction, we find continuity for m<2 n11 , 2 m<2 1 n11 , 2 2 ..., m<21. Step 3: b̂ PS 0. Let b̂ PS 0. Then there is an estimate M .2 sup u b̂ ~ x m , a n ! u 2 . Set d̂ ~ x m , a n ! [ @ M 2 u b̂ ~ x m , a n ! u 2 # 1/2PS 0 . Since J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp Maarten V. de Hoop: Generalized Bremmer coupling series 3281 M 2 u b̂ ~ x m , a n ! u 2 >M /2, the symbol d̂ is well defined. Using the calculus of the previous subsection, form the operator D̂T D̂; then D̂T D̂5M 2B̂T B̂1Ê, êPS 21 . From this operator equality, we obtain i B̂û i 2 < i û i 2 M 1 ^ Êû,û & . In the previous step we have shown that Ê must be continuous ~êPS 21!; hence B̂ must be continuous. 1 J. F. Claerbout, ‘‘Coarse grid calculations of waves in inhomogeneous media with application to delineation of complicated seismic structure,’’ Geophysics 35, 407–418 ~1970!. 2 M. V. de Hoop and A. T. de Hoop, ‘‘Scalar space–time waves in their spectral domain first- and second-order Thiele approximations,’’ Wave Motion 15, 229–265 ~1992!. 3 M. V. de Hoop and A. T. de Hoop, ‘‘Interface reflection of spherical acoustic waves in the first- and second-order rational parabolic approximations and their artifacts,’’ J. Acoust. Soc. Am. 93, 22–35 ~1993!. 4 F. D. Tappert, ‘‘The parabolic approximation method,’’ in Wave Propagation in Underwater Acoustics, edited by J. B. Keller and J. S. Papadakis, Lecture Notes in Physics No. 70 ~Springer-Verlag, New York, 1977!, pp. 224–287. 5 R. R. Greene, ‘‘The rational approximation to the acoustic wave equation with bottom interaction,’’ J. Acoust. Soc. Am. 76, 1764–1773 ~1984!. 6 D. J. Thomson and N. R. Chapman, ‘‘A wide-angle split-step algorithm for the parabolic equation,’’ J. Acoust. Soc. Am. 74, 1848–1854 ~1983!. 7 J. van Roey, J. van der Donk, and P. E. Lagasse, ‘‘Beam-propagation method: analysis and assessment,’’ J. Opt. Soc. Am. 71, 803–810 ~1981!. 8 D. Yevick, ‘‘A guide to electric field propagation techniques for guided wave optics,’’ Optic. Quant. Electron. 26, S185–S197 ~1994!. 9 R. T. Seeley, ‘‘Complex powers of an elliptic operator,’’ A. M. S. Proc. Symp. Pure Math. 10, 288–307 ~1967!. 10 R. T. Seeley, ‘‘The resolvent of an elliptic boundary problem,’’ Am. J. Math. 91, 917–919 ~1969!. 11 L. Hörmander, The Analysis of Linear Partial Differential Operators III ~Springer-Verlag, Berlin, 1983!. 12 J. J. Duistermaat and V. W. Guilleman, ‘‘The spectrum of positive elliptic operators and periodic bicharacteristics,’’ Inv. Math. 29, 39–79 ~1975!. 13 L. Fishman and J. J. McCoy, ‘‘Derivation and application of extended parabolic wave theories. I. The factorized Helmholtz equation,’’ J. Math. Phys. 25, 285–296 ~1984!. 14 L. Fishman and J. J. McCoy, ‘‘Derivation and application of extended parabolic wave theories. II. Path integral representations,’’ J. Math. Phys. 25, 297–308 ~1984!. 15 L. Fishman and J. J. McCoy, ‘‘Factorization, path integral representations, and the construction of direct and inverse wave propagation theories,’’ IEEE Trans. Geosci. Remote Sens. GE-22, 682–692 ~1984!. 16 L. Fishman and J. J. McCoy, ‘‘A new class of propagation models based on a factorization of the Helmholtz equation,’’ Geophys. J. R. Astron. Soc. 80, 439–461 ~1985!. 17 L. Fishman and J. J. McCoy, ‘‘Factorization and path integration of the Helmholtz equation: numerical algorithms,’’ J. Acoust. Soc. Am. 81, 1355–1376 ~1987!. 18 L. Fishman, ‘‘Exact and operator rational approximate solutions of the Helmholtz, Weyl composition equation in underwater acoustics—The quadratic profile,’’ J. Math. Phys. 33, 1887–1914 ~1992!. 19 L. Fishman, ‘‘One-way wave propagation methods in direct and inverse scalar wave propagation,’’ Radio Sci. 28, 865–867 ~1993!. 20 L. Fishman and S. C. Wales, ‘‘Phase space methods and path integration: The analysis and computation of scalar wave equations,’’ J. Comp. Appl. Math. 20, 219–238 ~1987!. 21 J. J. McCoy and L. N. Frazer, ‘‘Pseudodifferential operators, operator orderings, marching algorithms and path integrals for one-way equations,’’ Wave Motion 9, 413–427 ~1987!. 22 V. H. Weston, ‘‘Factorization of the wave equation in higher dimensions,’’ J. Math. Phys. 28, 1061–1068 ~1987!. 23 J. J. McCoy, L. Fishman, and L. N. Frazer, ‘‘Reflection and transmission at an interface separating transversely inhomogeneous acoustic half-spaces,’’ Geophys. J. R. Astron. Soc. 85, 543–562 ~1986!. 24 J. Corones, ‘‘Bremmer series that correct parabolic approximations,’’ J. Math. Anal. Appl. 50, 361–372 ~1975!. 25 M. D. Verweij and A. T. de Hoop, ‘‘Determination of seismic wave fields in arbitrarily continuously layered media using the modified Cagniard method,’’ Geoph. J. Int. 103, 731–754 ~1990!. 26 R. F. Millar, ‘‘The Rayleigh hypothesis and a related least-square solution to scattering problems for periodic surfaces and other scatterers,’’ Radio Sci. 8, 785–796 ~1973!. 27 P. M. van den Berg, ‘‘Reflection by a grating: Rayleigh methods,’’ J. Opt. Soc. Am. 71, 1224–1229 ~1981!. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp 3282 Maarten V. de Hoop: Generalized Bremmer coupling series 28 R.-S. Wu, ‘‘Wide-angle elastic wave one-way propagation in heterogeneous media and an elastic wave complex-screen method,’’ J. Geophys. Res. 99, 751–766 ~1994!. 29 A. J. Haines and M. V. de Hoop, ‘‘An invariant imbedding analysis of general wave scattering problems,’’ accepted for publication J. Math. Phys. ~1995!. 30 L. Fishman and A. K. Gautesen ‘‘An exact, well-posed, one-way reformulation of the Helmholtz equation with application to direct and inverse wave propagation modeling,’’ in New Perspectives on Problems in Classical and Quantum Physics, edited by A. W. Saenz and P. P. Delsanto ~Gordon and Breach, Newark, 1996!. 31 J. P. Corones, M. E. Davison, and R. J. Krueger, ‘‘Direct and inverse scattering in the time domain via invariant imbedding equations,’’ J. Acoust. Soc. Am. 74, 1535–1541 ~1983!. 32 V. H. Weston, ‘‘Invariant imbedding and wave splitting in R3: II. The Green function approach to inverse scattering,’’ Inv. Prob. 8, 919–947 ~1992!. 33 A. J. Berkhout, ‘‘Multi-dimensional linearized inversion and seismic migration,’’ Geophysics 49, 1881–1895 ~1984!. 34 D. E. Lumley, ‘‘Angle-dependent reflectivity estimation,’’ SEG Ann. Mtg. Expanded Abstr. 746–749 ~1993!. 35 D. V. Widder, The Laplace Transform ~Princeton U.P., Princeton, NJ, 1946!. 36 C. P. A. Wapenaar and A. J. Berkhout, Elastic Wave Field Extrapolation ~Elsevier, Amsterdam, 1989!. 37 W. Rudin, Functional Analysis ~Tata McGraw–Hill, New Delhi, 1981!. 38 E. Kreyszig, Introductory Functional Analysis with Applications ~Wiley, New York, 1978!. 39 T. Kato, Perturbation Theory for Linear Operators ~Springer-Verlag, Berlin, 1984!. 40 M. E. Taylor, Pseudodifferential Operators ~Princeton U. P., Princeton, 1981!. 41 J. J. Duistermaat, Fourier Integral Operators ~Lecture Notes Courant Institute of Mathematical Sciences, New York, 1973!. 42 H. Kumano-go, Pseudo-differential Operators ~MIT Press, Cambridge, 1981!. 43 B. L. N. Kennett, ‘‘Wavenumber and wave type coupling in laterally heterogeneous media,’’ Geophys. J. R. Astron. Soc. 87, 313–331 ~1986!. 44 D. M. Pai, ‘‘A new solution method for wave equations in inhomogeneous media,’’ Geophysics 50, 1541–1547 ~1985!. 45 D. M. Pai, ‘‘Generalized f – k ~frequency-wavenumber! migration in arbitrarily varying media,’’ Geophysics 53, 1547– 1555 ~1988!. 46 L. Hörmander, The Analysis of Linear Partial Differential Operators I ~Springer-Verlag, Berlin, 1983!. 47 P. Braam ~University of Oxford, personal communication!. 48 E. A. Coddington and N. Levinson, Theory of Ordinary Differential Equations ~McGraw–Hill, New York, 1955!. 49 C. De Witt-Morette, A. Maheshwari, and B. Nelson, ‘‘Path integration in non-relativistic quantum mechanics,’’ Phys. Rep. 50, 255–372 ~1979!. 50 L. S. Schulman, Techniques and Applications of Path Integration ~Wiley, New York, 1981!. 51 L. Fishman, ‘‘Phase space factorization and functional integral methods in direct and inverse scattering-symbol analysis,’’ in Wave Phenomena, edited by L. Lam and H. C. Morris ~Springer-Verlag, New York, 1988!, pp. 76–85. 52 J. Gazdag and P. Sguazzero, ‘‘Migration of seismic data by phase shift plus interpolation,’’ Geophysics 49, 124–131 ~1984!. 53 P. L. Stoffa, J. T. Fokkema, R. M. de Luna Freire, and W. P. Kessinger, ‘‘Split-step Fourier migration,’’ Geophysics 55, 410–421 ~1990!. 54 J. B. Keller and D. W. McLaughlin, ‘‘The Feynman integral,’’ Ann. Math. Mon. 82, 451–465 ~1975!. 55 V. P. Maslov and M. V. Fedoriuk, Semi-classical Approximation in Quantum Mechanics, translation from the Russian by J. Niederle and J. Tolar ~Reidel, Dordrecht, 1981!. 56 M. Suzuki, ‘‘General theory of higher-order decomposition of exponential operators and symplectic propagators,’’ preprint, Dept. of Physics, University of Tokyo ~1992!. 57 H. Bremmer, ‘‘Geometrisch-optische benadering van de golfvergelijking,’’ Handel. Ned. Nat. en Geneeskd. Congr., 88–91 ~1939! ~in Dutch!. 58 L. M. Brekhovskikh, Waves in Layered Media ~Academic, New York, 1960!. 59 A. T. de Hoop, ‘‘Acoustic radiation from an impulsive point source in a continuously layered fluid—An analysis based on the Cagniard method,’’ J. Acoust. Soc. Am. 88, 2376–2388 ~1990!. 60 G. M. Wing, ‘‘Invariant imbedding and generalizations of the WKB method and the Bremmer series,’’ J. Math. Anal. Appl. 48, 400–422 ~1974!. 61 F. V. Atkinson, ‘‘Wave propagation and Bremmer series,’’ J. Math. Anal. Appl. 1, 255–276 ~1960!. 62 M. V. de Hoop and A. T. de Hoop, ‘‘Elastic wave up/down decomposition in inhomogeneous and anisotropic media: an operator approach and its approximations,’’ Wave Motion 20, 57–82 ~1994!. 63 M. A. Shubin, Pseudodifferential Operators and Spectral Theory ~Springer-Verlag, Berlin, 1987!. 64 R. Baets, J. Willems, and R. Haes, ‘‘Diversity in beam propagation methods,’’ ECIO, 13.1–13.3 ~1993!. 65 L. Fishman, ‘‘Numerical solutions of the Helmholtz, Weyl composition equation in ocean seismo-acoustics,’’ in 13th International Congress on Acoustics, edited by P. Pravica ~Sava Centar, Belgrade, 1989!, Vol. 5, pp. 149. 66 R. P. Ratowsky, J. A. Fleck, Jr., and M. D. Feit, ‘‘Helmholtz beam propagation in rib waveguides and couplers by iterative Lanczos reduction,’’ J. Opt. Soc. Am. A 9, 265–273 ~1992!. 67 M. J. N. van Stralen, M. V. de Hoop, and H. Blok, ‘‘Numerical implementation of the Bremmer coupling series,’’ IPR Expanded Abstracts ~1996!. 68 B. Davies and B. Martin, ‘‘Numerical inversion of the Laplace transform; a survey and comparison of methods,’’ J. Comp. Phys. 33, 1–32 ~1979!. 69 A. Papoulis, ‘‘A new method of inversion of the Laplace Transform,’’ Q. Appl. Math. 14, 405–414 ~1957!. J. Math. Phys., Vol. 37, No. 7, July 1996 Downloaded¬09¬Apr¬2009¬to¬128.210.4.214.¬Redistribution¬subject¬to¬AIP¬license¬or¬copyright;¬see¬http://jmp.aip.org/jmp/copyright.jsp
© Copyright 2026 Paperzz