<?xml version="1.0" encoding="ISO-8859-1"?><article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
<front>
<journal-meta>
<journal-id>0016-7169</journal-id>
<journal-title><![CDATA[Geofísica internacional]]></journal-title>
<abbrev-journal-title><![CDATA[Geofís. Intl]]></abbrev-journal-title>
<issn>0016-7169</issn>
<publisher>
<publisher-name><![CDATA[Universidad Nacional Autónoma de México, Instituto de Geofísica]]></publisher-name>
</publisher>
</journal-meta>
<article-meta>
<article-id>S0016-71692008000200003</article-id>
<title-group>
<article-title xml:lang="en"><![CDATA[Transient response and multiple scattering of elastic waves by a linear array of regularly distributed cylindrical obstacles: Anti-plane S-wave analytical solution]]></article-title>
</title-group>
<contrib-group>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Ávila-Carrera]]></surname>
<given-names><![CDATA[R.]]></given-names>
</name>
<xref ref-type="aff" rid="A01"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Sánchez-Sesma]]></surname>
<given-names><![CDATA[F. J.]]></given-names>
</name>
<xref ref-type="aff" rid="A02"/>
</contrib>
<contrib contrib-type="author">
<name>
<surname><![CDATA[Avilés]]></surname>
<given-names><![CDATA[J.]]></given-names>
</name>
<xref ref-type="aff" rid="A03"/>
</contrib>
</contrib-group>
<aff id="A01">
<institution><![CDATA[,Instituto Mexicano del Petróleo  ]]></institution>
<addr-line><![CDATA[Mexico, City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="A02">
<institution><![CDATA[,Universidad Nacional Autónoma de México Instituto de Ingeniería ]]></institution>
<addr-line><![CDATA[Mexico City ]]></addr-line>
<country>Mexico</country>
</aff>
<aff id="A03">
<institution><![CDATA[,Instituto Mexicano de Tecnología del Agua  ]]></institution>
<addr-line><![CDATA[Jiutepec Morelos]]></addr-line>
<country>México</country>
</aff>
<pub-date pub-type="pub">
<day>00</day>
<month>06</month>
<year>2008</year>
</pub-date>
<pub-date pub-type="epub">
<day>00</day>
<month>06</month>
<year>2008</year>
</pub-date>
<volume>47</volume>
<numero>2</numero>
<fpage>115</fpage>
<lpage>126</lpage>
<copyright-statement/>
<copyright-year/>
<self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_arttext&amp;pid=S0016-71692008000200003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_abstract&amp;pid=S0016-71692008000200003&amp;lng=en&amp;nrm=iso"></self-uri><self-uri xlink:href="http://www.scielo.org.mx/scielo.php?script=sci_pdf&amp;pid=S0016-71692008000200003&amp;lng=en&amp;nrm=iso"></self-uri><abstract abstract-type="short" xml:lang="es"><p><![CDATA[Estudiamos la difracción múltiple de ondas elásticas por un arreglo lineal finito de obstáculos cilindricos distribuidos regularmente. En particular, se resuelve con detalle la respuesta transitoria del sistema para la incidencia de ondas de corte antiplanas. Presentamos una extensión de la solución original para cilindros rígidos desarrollada por algunos de nosotros en los ochentas. La solución se obtiene formalmente para una excitación armónica en el dominio de la frecuencia y el análisis de Fourier nos permite obtener la respuesta transitoria. En este análisis mejorado se consideran variaciones en las propiedades de los materiales de las inclusiones cilíndricas. La formulación es bidimensional y se construye a partir de la superposición del campo incidente y las ondas difractadas por cada obstáculo. Las soluciones para cada obstáculo se construyen como expansiones de funciones de onda cilíndricas. La solución exacta se obtiene formalmente después de imponer condiciones de continuidad para los desplazamientos y las tracciones en las interfaces matriz-difractor con la ayuda del teorema de adición de Graf. Así, el campo total se puede referir a cualquier sistema de coordenadas cilindrico. El sistema de ecuaciones infinito se aproxima por uno finito y esto permite obtener resultados numéricos para diferentes valores de los parámetros. Se estudian varios casos de cavidades e inclusiones. Se muestra que un doble efecto es producido por la presencia de un material particular de relleno: amplificaciones en el lado de la incidencia y reducciones en el lado opuesto, o vice versa. Se calculan también sismogramas sintéticos e instantáneas de tiempo con el objeto de ilustrar las características complejas de la propagación de ondas en este modelo inhomogéneo.]]></p></abstract>
<abstract abstract-type="short" xml:lang="en"><p><![CDATA[We study the multiple scattering of elastic waves by a finite linear array of regularly distributed cylindrical obstacles. The transient response of the system for incident anti-plane shear waves is given in detail. We present an extension of an original solution for rigid cylinders, developed by some of us in 1983. The solution is formally obtained for harmonic excitation and Fourier analysis provides the transient response. Material properties of the cylindrical inclusions are considered. A 2-D formulation is constructed by superposition of the incident field upon the waves diffracted by each obstacle. The solutions for each obstacle are constructed as expansions of cylindrical wave functions, after imposing continuity conditions for the displacements and tractions at the scatterers matrix interfaces with the aid of Graf's addition theorem. Thus, the total field can be referred to any cylindrical coordinates. The infinite system is approximated by a finite one and numerical results are obtained for different values of the parameters. Various cases of cavities and inclusions are studied. A double effect is produced by different filling materials, f. e. amplification at the incidence side and reductions at the far side, or vice versa. Synthetic seismograms and snapshots are computed to illustrate the complex features of wave propagation for this inhomogeneous model.]]></p></abstract>
<kwd-group>
<kwd lng="es"><![CDATA[Difracción múltiple]]></kwd>
<kwd lng="es"><![CDATA[respuesta transitoria]]></kwd>
<kwd lng="es"><![CDATA[solución analítica]]></kwd>
<kwd lng="es"><![CDATA[ondas elásticas]]></kwd>
<kwd lng="es"><![CDATA[obstáculos cilíndricos]]></kwd>
<kwd lng="es"><![CDATA[instantáneas de tiempo]]></kwd>
<kwd lng="en"><![CDATA[Multiple scattering]]></kwd>
<kwd lng="en"><![CDATA[transient response]]></kwd>
<kwd lng="en"><![CDATA[analytical solution]]></kwd>
<kwd lng="en"><![CDATA[elastic waves]]></kwd>
<kwd lng="en"><![CDATA[cylindrical obstacles]]></kwd>
<kwd lng="en"><![CDATA[snapshots]]></kwd>
</kwd-group>
</article-meta>
</front><body><![CDATA[ <p align="justify"><font face="verdana" size="4">Article</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="center"><font face="verdana" size="4"><b>Transient response and multiple scattering of elastic waves by a </b><b>linear array of regularly distributed cylindrical obstacles: </b><b>Anti&#150;plane S&#150;wave analytical solution</b></font></p>     <p align="center"><font face="verdana" size="2">&nbsp;</font></p>     <p align="center"><font face="verdana" size="2"><b>R. &Aacute;vila&#150;Carrera<sup>1</sup>*, F. J. S&aacute;nchez&#150;Sesma<sup>2</sup> and J. Avil&eacute;s<sup>3</sup></b></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><i><sup>1</sup> Instituto Mexicano del Petr&oacute;leo, Mexico, City, Mexico.</i> <i>Eje  Central L&aacute;zaro   C&aacute;rdenas  152;  Mexico,   City, Mexico.</i><i>*Corresponding author: <a href="mailto:rcarrer@imp.mx">rcarrer@imp.mx</a></i></font></p>     <p align="justify"><font face="verdana" size="2"><i><sup>2</sup> Instituto de Ingenier&iacute;a, Universidad Nacional Aut&oacute;noma de M&eacute;xico. Mexico City, Mexico.</i></font></p>     <p align="justify"><font face="verdana" size="2"><i><sup>3 </sup>Instituto Mexicano de Tecnolog&iacute;a del Agua Jiutepec, Morelos. M&eacute;xico.</i></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2">Received: December 14, 2007     <br> Accepted: January 22, 2008</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Resumen</b></font></p>     <p align="justify"><font face="verdana" size="2">Estudiamos la difracci&oacute;n m&uacute;ltiple de ondas el&aacute;sticas por un arreglo lineal finito de obst&aacute;culos cilindricos distribuidos regularmente. En particular, se resuelve con detalle la respuesta transitoria del sistema para la incidencia de ondas de corte antiplanas. Presentamos una extensi&oacute;n de la soluci&oacute;n original para cilindros r&iacute;gidos desarrollada por algunos de nosotros en los ochentas. La soluci&oacute;n se obtiene formalmente para una excitaci&oacute;n arm&oacute;nica en el dominio de la frecuencia y el an&aacute;lisis de Fourier nos permite obtener la respuesta transitoria. En este an&aacute;lisis mejorado se consideran variaciones en las propiedades de los materiales de las inclusiones cil&iacute;ndricas. La formulaci&oacute;n es bidimensional y se construye a partir de la superposici&oacute;n del campo incidente y las ondas difractadas por cada obst&aacute;culo. Las soluciones para cada obst&aacute;culo se construyen como expansiones de funciones de onda cil&iacute;ndricas. La soluci&oacute;n exacta se obtiene formalmente despu&eacute;s de imponer condiciones de continuidad para los desplazamientos y las tracciones en las interfaces matriz&#150;difractor con la ayuda del teorema de adici&oacute;n de Graf. As&iacute;, el campo total se puede referir a cualquier sistema de coordenadas cilindrico. El sistema de ecuaciones infinito se aproxima por uno finito y esto permite obtener resultados num&eacute;ricos para diferentes valores de los par&aacute;metros. Se estudian varios casos de cavidades e inclusiones. Se muestra que un doble efecto es producido por la presencia de un material particular de relleno: amplificaciones en el lado de la incidencia y reducciones en el lado opuesto, o vice versa. Se calculan tambi&eacute;n sismogramas sint&eacute;ticos e instant&aacute;neas de tiempo con el objeto de ilustrar las caracter&iacute;sticas complejas de la propagaci&oacute;n de ondas en este modelo inhomog&eacute;neo.</font></p>     <p align="justify"><font face="verdana" size="2"><b>Palabras clave: </b>Difracci&oacute;n m&uacute;ltiple, respuesta transitoria, soluci&oacute;n anal&iacute;tica, ondas el&aacute;sticas, obst&aacute;culos cil&iacute;ndricos, instant&aacute;neas de tiempo.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Abstract</b></font></p>     <p align="justify"><font face="verdana" size="2">We study the multiple scattering of elastic waves by a finite linear array of regularly distributed cylindrical obstacles. The transient response of the system for incident anti&#150;plane shear waves is given in detail. We present an extension of an original solution for rigid cylinders, developed by some of us in 1983. The solution is formally obtained for harmonic excitation and Fourier analysis provides the transient response. Material properties of the cylindrical inclusions are considered. A 2&#150;D formulation is constructed by superposition of the incident field upon the waves diffracted by each obstacle. The solutions for each obstacle are constructed as expansions of cylindrical wave functions, after imposing continuity conditions for the displacements and tractions at the scatterers matrix interfaces with the aid of Graf's addition theorem. Thus, the total field can be referred to any cylindrical coordinates. The infinite system is approximated by a finite one and numerical results are obtained for different values of the parameters. Various cases of cavities and inclusions are studied. A double effect is produced by different filling materials, f. e. amplification at the incidence side and reductions at the far side, or <i>vice versa. </i>Synthetic seismograms and snapshots are computed to illustrate the complex features of wave propagation for this inhomogeneous model.</font></p>     <p align="justify"><font face="verdana" size="2"><b>Key words: </b>Multiple scattering, transient response, analytical solution, elastic waves, cylindrical obstacles, snapshots.</font></p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Introduction</b></font></p>     <p align="justify"><font face="verdana" size="2">Mathematical and numerical modeling is fundamental in science and engineering. In particular, geophysical modeling  is   crucial  to  understand basic features  of hydrocarbon reservoirs in the field. Analytical formulations has   allowed   establishing   benchmark   solutions   for some problems. Most of these formulations have been employed, among other uses; (1) to build basic solutions for more complicated problems, (2) for validation and calibration of new results and (3) for trustworthy field data interpretation. In scattering problems exact solutions have been helpful even thoung only some types of obstacles (i.e. cylinders, spheres or ellipsoids) yield exact analytical solutions. The insight gained by such applications is significant and useful.</font></p>     <p align="justify"><font face="verdana" size="2">Multiple scattering of elastic waves by a set of flexible inclusions was treated by Foldy (1945) and Lax (1951) for scalar waves, and subsequently by other authors (e. g. Waterman and Truell, 1961; Frisch, 1968; Varadan <i>et. al., </i>1978; Varadan and Varadan, 1980; Kikuchi, 1981; Avil&eacute;s and S&aacute;nchez&#150;Sesma, 1983). Most recent publications deal with the subject in 3D, e. g., asymptotic solutions of the dispersion equations in the long and short&#150;wavelength regimes (Kanaun <i>et. al., </i>2004), acoustic wave propagation by cylindrical shells (Veksler <i>et. al., </i>2000), and elastic wave scattering by spheres (Gritto <i>et. al., </i>1995; 1999; &Aacute;vila&#150;Carrera and S&aacute;nchez&#150;Sesma, 2006). Some 2&#150;D analytical solutions of the time response of a single cavity are presented by Davis <i>et. al., </i>(2001) and by Yin&#150;Bin <i>et. al., </i>(2000) for the viscoelastic case. The books by Tsang <i>et. al., </i>(2000), Ishimaru (1997) and Sheng (1995) cover the subject in the frequency domain reasonably well, but they leave aside the analysis of the time response. On the other hand, numerical techniques such as finite&#150;difference and finite&#150;element methods face limitations regarding computer time and core required when dealing with realistic scattering problems, even with state&#150;of&#150;the&#150;art&#150;computers (Vlastos <i>et. al., </i>2003).</font></p>     <p align="justify"><font face="verdana" size="2">In a previous work (Avil&eacute;s and S&aacute;nchez&#150;Sesma, 1983) we faced limitations imposed by computational conditions at the time. Only frequency domain results were presented and the cylinders were assumed to be rigid. In this paper, we review the theoretical analysis developed in the early 80's for rigid cylinders and we extend it to solve the transient response of multiple scattering of anti&#150;plane incoming S&#150;waves by a linear array of cylindrical elastic inclusions and cavities. Our aim is to study multiple diffraction of elastic waves presumably generated by a distant seismic source. We assume that the displacement field of the anti&#150;plane shear motion is in the same direction as the axes of the cylinders. In future work we will address more realistic cases, including perpendicular motion of the wave field with respect to the axes. We consider closed&#150;form analytical solutions for diffracted and reflected fields produced by various types of cylinders (cavities, rigid or elastic inclusions). The solution is constructed in the frequency domain as a superposition of incident and diffracted fields by each obstacle. Continuity and equilibrium conditions are enforced at all scatterer&#150;matrix interfaces with the aid of Graf's addition theorem. Thus, the total field may be referred to any cylindrical coordinate system, by uncoupling the odd and even parts of the solution. From results in the frequency domain, Fourier synthesis yields the transient response. Previous work (e.g., Benites <i>et. al, </i>1992), dealt with infinite periodic arrays, and this work was taken into consideration. In our case the array is finite, and the formulation using Graf's addition theorem leads to exact expressions so that edge effects are naturally included, but infinite wave expansions must be truncated to a practical size. In our examples, the order of wave expansions is commonly limited to ten or twelve which movides enough resolution for the studied configurations. Several examples of array configurations are shown. Normalized amplitudes of the displacement field <i>versus </i>distance for a given frequency are depicted. In order to illustrate the complex behavior of wave motion in this inhomogeneous model, synthetic seismograms and snapshots are computed. The results provide insight of multiple scattering behavior, and provide a quantitative description of various types of material fillers that can be used as references for calibration of other modeling techniques.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Formulation of the Problem</b></font></p>     <p align="justify"><font face="verdana" size="2">Consider a linear, elastic, isotropic and homogeneous space and let anti&#150;plane displacement <i>w </i>be defined in the <i>z </i>direction. Consider a regular array of elastic cylinders with properties different from those of the surrounding material, as in <a href="#f1">Fig. 1</a>. The propagation of harmonic plane S&#150;waves satisfies the reduced wave equation, or Helmholtz equation</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s1.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><a name="f1"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f18.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where <i>x, y = </i>Cartesian coordinates, <i>k =&omega;/&beta;  = </i>shear wave&#150;number,<i>&omega;</i>   = angular frequency and <i><img src="/img/revistas/geoint/v47n2/a3s2.jpg"> = </i>shear wave propagation velocity; <i>&micro; = </i>shear modulus and <i>&rho;= </i>mass density of the elastic space.</font></p>     <p align="justify"><font face="verdana" size="2">The excitation consists of a plane wave of amplitude <i>w<sub>0</sub> </i>with angle of incidence <i>&psi;, </i>propagating in the forward direction toward the array of cylindrical inclusions, as shown in <a href="#f1">Fig. 1</a>. This incident wave is expressed in the reference system <i>(x<sub>1</sub> y<sub>1</sub>) </i>with respect to the first obstacle by</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s3.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">The factor exp(i<i>&omega;</i><i>t</i>) ( <img src="/img/revistas/geoint/v47n2/a3s5.jpg"> for the time dependency of harmonic motion will be omitted from here on. The array of aligned cylinders produces diffraction and scattering of the incoming wave field. Thus, the solution can be represented by</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s6.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2">where <i>w<sup>s</sup><sub>j</sub></i> (<i>r<sub>j</sub> , &theta;<sub>j</sub></i><i>) </i>denotes the diffracted waves by the <i>j&#150;th </i>cylinder as referred to its own coordinate system (<i><i>r<sub>j</sub> , &theta;<sub>j</sub></i>), </i>and <i>NS = </i>number of scatterers.</font></p>     <p align="justify"><font face="verdana" size="2">By separation of variables, the diffracted field for each scatterer can be written (Abramowitz and Stegun, 1964)</font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s7.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where <i>A <sup>j</sup><sub>n</sub> B<sup> j</sup><sub>n</sub>= </i>unknown complex coefficients that will be determined from the boundary conditions, and <i>H<sub>n</sub><sup>(2)</sup></i>(.) = Hankel function of the second kind and order <i>n. </i>The wave functions <i>H<sub>n</sub><sup>(2)</sup>cos </i><i>(kr<sub>j</sub>) cos <i>n&theta;<sub>j</sub></i> </i>and <i>H<sub>n</sub><sup>(2)</sup>(kr<sub>j</sub>)</i>  sin <i><i>n&theta;<sub>j</sub></i></i> represent a complete set of solutions of the reduced wave equation in unbounded regions which satisfy the Sommerfeld radiation condition (Mow and Pao, 1971). When we have elastic obstructions, part of the incident wave field is refracted and a stationary wave is generated inside each cylinder. By solving (1), the refracted field in the j&#150;th cylinder can be expressed in the local coordinate system (<i>r<sub>j</sub> , &theta;<sub>j</sub></i><i>) </i>as</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s8.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where <i>C <sup>j</sup><sub>n</sub>, J<sub>n</sub>= </i>unknown complex coefficients that will be determined from the boundary conditions, and <i>J<sub>n</sub> </i>(.)<i> = </i>Bessel function of the first kind and order <i>n; </i>the subscript <i>c </i>of the wave number <i>k<sub>c</sub></i> refers to cylinder. The functions <i> J<sub>n</sub>(k<sub>c </sub>j<sub>r</sub>) </i>cos<i> <i>&theta;<sub>j</sub></i> </i> and <i>J<sub>n</sub>(k<sub>c </sub>j<sub>r</sub>)</i> sin <i><i>n&theta;<sub>j</sub></i></i> represent a complete set of solutions of the reduced wave equation in bounded regions. All coefficients <i>A<sup> j</sup><sub>n</sub>, B<sup> j</sup><sub>n</sub>, C<sup> j</sup><sub>n</sub> </i>and <i>D<sup> j</sup><sub>n</sub><i> </i></i>that define the solution of the problem are obtained when the boundary conditions are fulfilled.</font></p>     <p align="justify"><font face="verdana" size="2">Let us assume perfect contact between the cylinders and the surrounding elastic material, so that the boundary conditions at the matrix&#150;obstruction interfaces are continuity of displacements and stresses:</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s9.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s10.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where <i>a = </i>radius of the cylinders. Salving the problem requires imposing the boundary conditions at each cylinder. For convenience, the total field in (3) will be given with respect to the arbitrary coordinate system (<i>r<sub>l</sub> ,  &theta;<sub>l</sub></i><i>). </i>Eqs. (2) and (4) must be referred to this coordinate system using Graf's addition theorem (see <a href="#a1">Appendix</a>). This the total field becomes</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s11.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where</font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s12.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s13.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2">in which <i>&epsilon;<sub>m</sub> = </i>Neumann factor <i>(&epsilon;<sub>0</sub> = </i>1 and <i>&epsilon;<sub>m</sub> = </i>2, <i>m </i><u>&gt;</u>1), <i>d<sub>jl</sub> = </i>distance between the centers of the j&#150;th and the <i>l&#150;th </i>cylinders and <i>&delta;<sub>lj</sub> = </i>Kronecker delta (= 1 if <i>l</i> = <i>j; = </i>0 if <i>l</i> <img src="/img/revistas/geoint/v47n2/a3s14.jpg"><i>j</i> ).</font></p>     <p align="justify"><font face="verdana" size="2">Inserting (5) and (8) into (6) and (7), and making use of the orthogonal properties of trigonometric functions, we obtain four infinite systems of algebraic equations for the coefficients <i>A<sup> j</sup><sub>n</sub>, B <sup>j</sup><sub>n</sub>, C <sup>j</sup><sub>n</sub></i>and <i>D <sup>j</sup><sub>n</sub>. </i>However, we are interested in the solution for elastic media only, so the coefficients <i>C</i> <i><sup>j</sup><sub>n</sub></i>and <i>D  <sup>j</sup><sub>n</sub></i>can be eliminated and the four equation systems are reduced to two in follows</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s15.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s16.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s17.jpg"></font></p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2">in which the prime denotes differentiation with respect to the argument.</font></p>     <p align="justify"><font face="verdana" size="2">Notice that the azimuthal decomposition of the solution (8), reduces the triple summation to a double one, using the linear independence of the azimuthal functions cos <i>n</i><i><i>&theta;<sub>j</sub></i></i> and sin <i>n</i><i><i>&theta;<sub>j</sub></i></i>This boundary conditions (6) and (7) are imposed at every cylinder l for each azimuthal number <i>m. </i>Similar equations arise for the fields whitin each cylinder. As they are simpler, the constants can be eliminated substituted and the influence of the cylinders can be lumped together in the diagonal. Solving the systems of equations (11) and (12) completes the solution. However, such systems can not be solved exactly. An approximation is obtained by reducing the dimensions of equations to a finite number, by truncating the orders of expansions <i>(m </i>and <i>n) </i>such that the solution converges. By inspection of the systems of equations, it is found that the type of scatterer (elastic, rigid or cavity) modifies only the diagonal coefficients.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Numerical Results</b></font></p>     <p align="justify"><font face="verdana" size="2">In this section we show some relevant results obtained by the analytical technique described above. The aim is to present instructive examples in a simple way. Configurations for each model analyzed are depicted and the ensuing results are discussed. Eight to ten terms were used for the wave expansions, obtaining up to four&#150;digit accuracy in the range of frequencies studied. Normal and oblique incidence of plane waves were considered for all cases presented. The wave field depends on the nondimensional frequency given by</font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3s18.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">where <i>&lambda;<sub>k</sub> = </i>wavelength of the incident S&#150;wave. Thus, the normalized frequency represents the diameter of the cylinder over the wavelength.</font></p>     <p align="justify"><font face="verdana" size="2">In <a href="/img/revistas/geoint/v47n2/a3f2.jpg" target="_blank">Fig. 2</a> the normalized displacement amplitude with respect to the free&#150;field displacement for an array of eight scatterers has been calculated. Displacement is plotted against distance <i>x/a </i>along the array axis. Four cases are analyzed in terms of separation between cylinders and distance <i>y/a </i>at the far side of incidence. Three kinds of material fillers have been considered: short dashed lines correspond to elastic cylinders with <i>&rho;<sub>c </sub>/&rho; = </i>0.5 and <i>&micro;<sub>c</sub> / &micro; = </i>0.3, long dashed lines to cavities with <i>&rho;<sub>c </sub>/&rho; = </i>0 and <i>&micro;<sub>c</sub> / &micro; = </i>0, and solid lines to rigid cylinders with <i>&rho;<sub>c </sub>/&rho; = </i>1.538 and <i>&micro;<sub>c</sub></i><img src="/img/revistas/geoint/v47n2/a3s20.jpg"><i>. </i>Dimensionless frequency <i>&eta;<sub>k</sub> = </i>0.5 and normal incidence of wave excitation have been used for the computations. It is remarkable that, for a given frequency, the amplitude of the displacement field suffer a strong attenuation when an array of rigid cylinders is used. The results for cavities and elastic cylinders are quite similar; they appear to be sensitive to changes in separation between obstacles.</font></p>     <p align="justify"><font face="verdana" size="2">For a more detailed view of the sharp decrease in amplitude due to the presence of rigid scatterers as previously discussed by Avil&eacute;s and S&aacute;nchez&#150;Sesma (1983), it is convenient to compute the displacements at the far side of incidence in a relative distant field <i>(y/a = </i>150). In <a href="/img/revistas/geoint/v47n2/a3f3.jpg" target="_blank">Fig. 3</a>, normalized amplitudes of the displacement field <i>w/w<sub>0</sub> </i>against distance <i>x/a </i>are shown. Separations between cylinders of <i>s<sub>p</sub> / &alpha; = </i>2.5, 3.0, 3.5 and 4.0, and a normalized frequency <i>&eta;<sub>k</sub>= </i>0.5 under incidence of S&#150;waves were taken for the computations. Maximum reductions occur near the center of the array. This effect is clearly appreciated in <a href="/img/revistas/geoint/v47n2/a3f3.jpg" target="_blank">Fig. 3</a> for a normalized separation <i>s<sub>p</sub> / &alpha; = </i>3. In this case, the reductive effect of the system is of the order of 55%, and 60% for a separation of <i>s<sub>p</sub> / &alpha; = </i>2.5. Thus the system behaves like a single unit at long distances and not as a set of independent scatterers. From <a href="/img/revistas/geoint/v47n2/a3f2.jpg" target="_blank">Figs. (2)</a> and <a href="/img/revistas/geoint/v47n2/a3f3.jpg" target="_blank">(3)</a> it is clear that at points near the array of rigid obstacles, the reduced field shows large variability, in contrast with the smooth variations observed at long distances. As expected, when the obstacles are spaced closely, whit a separation of at least one radius, the maximum amplitude reductions take place. As the separation increases reductions become less significant.</font></p>     <p align="justify"><font face="verdana" size="2">To show the scattering effects at the incidence side, normalized displacement amplitudes for an eight obstacle array have been calculated. Three kinds of material fillers (cavities, elastic inclusions and rigid cylinders) were considered. The distance between centers of scatterers is <i>s<sub>p</sub> / &alpha; = </i>4.0 and the nondimensional frequency is <i>&eta;<sub>k</sub>= </i>0.4. Results for several distances at the incidence side <i>(y/a = </i>&#150;5, &#150;10, &#150;15 and &#150;20) are displayed in <a href="#f4">Fig. 4a</a> for cavities with <i>&rho;<sub>c </sub>/&rho;=0 </i>and <i>&micro;<sub>c</sub> / &micro; = </i>0, in <a href="/img/revistas/geoint/v47n2/a3f3.jpg" target="_blank">Fig. 3b</a> for elastic inclusions with <i>&rho;<sub>c </sub>/&rho;</i>= 0.5 and <i>&micro;<sub>c</sub> / &micro; = </i>0.3, and in <a href="#f4">Fig. 4c</a> for rigid cylinders with <i>&rho;<sub>c </sub>/&rho; = </i>1.538 and<i> &micro;<sub>c</sub></i><img src="/img/revistas/geoint/v47n2/a3s20.jpg">. For the arrays with cavities and elastic inclusions, a smooth amplification occurs that tends to disappear when we get close to the edges. With rigid cylinders the amplification effect occurs everywhere and maximum amplitudes at <i>x/a = </i>22.25 for <i>y/a = </i>&#150;20.</font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><a name="f4"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f4.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">So far, with the available set of results we observe a common double effect produced by several configurations of cylinders. Amplifications are generated at the incidence side and reductions take place at the far side. <a href="#f5">Fig. 5</a> shows the normalized amplitudes of the displacement field along <i>x/a = </i>0, that is at the end of the array, for eight cylinders with separation <i>s<sub>p</sub> / &alpha; = </i>3.0 and dimensionless frequency <i>&eta;<sub>k</sub>= </i>0.4. The short dashed line corresponds to an array of elastic cylinders with <i>&rho;<sub>c </sub>/&rho; = </i>0.5 and <i>&micro;<sub>c</sub> / &micro; = </i>0.3, long dashed line for cavities with <i>&rho;<sub>c </sub>/&rho; = </i>0.0 and <i>&micro;<sub>c</sub> / &micro; = </i>0.0, and solid line for rigid scatterers with <i>&rho;<sub>c </sub>/&rho; = </i>1.538 and <i>&micro;<sub>c</sub><img src="/img/revistas/geoint/v47n2/a3s20.jpg"></i>. Notice the strong attenuation by the array for all three cases computed. The effect is strongest for rigid cylinders. The type of material filler seems ir relevant to amplitude reductions after the array. This fact must be checked by some time domain computations to follow.</font></p>     <p align="center"><font face="verdana" size="2"><a name="f5"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f5.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">In order to show the characteristic time response of the studied models, several computations of time history in a fixed linear or spatial distribution of receivers were performed. <a href="/img/revistas/geoint/v47n2/a3f19.jpg" target="_blank">Figs. 6 to 9</a> show the Fourier synthetic seismograms computed for models of two and four cylindrical scatterers. Normal and oblique incidences of S&#150;waves were considered. Cavities, elastic inclusions and rigid cylinders were used in the computations. The seismometers are located at the far side of the array with respect to the incoming wave field. These configurations were adopted in order to observe forward scattering and the behavior of the propagating wave front due to the presence of the array.</font></p>     <p align="justify"><font face="verdana" size="2"><a href="#f6">Fig. 6</a> shows a simple model of two obstacles with radius <i><i>r = &alpha;</i> = </i>1 and separation between centers of <i>s<sub>p</sub> / &alpha; = </i>4.0. There are 51 receivers at <i>x = &plusmn;4<i>&alpha;</i> </i>and <i>z = </i>1.5a; this configuration will be the same for all synthetic examples. The source is given by an S&#150;wave field with an incidence angle of <i>&psi; = </i>90&deg;, the time variation is constructed a Ricker pulse with <i>t<sub>p</sub> </i>= 1.5s and <i>t<sub>p</sub> = </i>4s. The elastic parameters are given by <i>&rho;<sub>c </sub>/&rho;</i>=0.0 and <i>&micro;<sub>c</sub> / &micro; = </i>0.0 for cavities (<a href="#f6">Fig. 6(a)</a>), <i>&rho;<sub>c </sub>/&rho; = </i>0.5 and <i>&micro;<sub>c</sub> / &micro; = </i>0.3 for elastic cylinders (<a href="#f6">Fig. 6(b)</a>), and <i>&rho;<sub>c </sub>/&rho;= </i>1.538 and <i>&micro;<sub>c</sub><img src="/img/revistas/geoint/v47n2/a3s20.jpg"></i> for rigid cylinders (<a href="#f6">Fig. 6(c)</a>). <a href="#f7">Fig. 7</a> corresponds to the same model as in <a href="#f6">Fig. 6</a>, except that the incidence angle is <i>&psi;= </i>75&deg;. Notice the arrival phases <i>r<sub>1</sub> , c<sub>1 </sub>, r<sub>2 </sub>, </i>and <i>c<sub>2</sub> </i>produced by the interaction between the incident wave <i>d </i>and the obstacles <i>1 </i>and 2 respectively. The letter <i>r </i>means <i>"reflecting", </i>and the letter <i>c </i>means <i>"creeping", </i>following the notation proposed by Benites <i>et. al., </i>(1992). To observe the wave motion produced by the various configurations sketched here, note the 3<sup>rd </sup>generation arrival phases, i. e. <i>r<sub>121</sub> </i>and <i>r<sub>212</sub> </i>. These phases correspond to the reflected and creeping waves between the boundaries of the two scatterers, taking into account the order in which the reflection or creeping occurs. The indices are related to the order in which each interaction take place. For example, <i>r<sub>21</sub> </i>indicates that the wave was reflected by scatterer 2 and next by scatterer <i>1, </i>before reaching receiver, in similar way for <i>r<sub>121</sub> </i>These phases are called <i>"interactive phases" </i>(Benites <i>et. al., </i>1992). Note that for the cases of cavities and elastic inclusions such phases are separated by time intervals of approximately <i>2&alpha; / &beta;</i>. Normal S&#150;wave incidence clearly shows how the incident field is delayed by the presence of the cavities. In the elastic examples, we observe a strong delayed amplification of the incident field due to the soft properties of obstacles. Creeping waves <i>c<sub>1</sub> </i>and <i>c<sub>2</sub> , </i>are easily identified due to their higher amplitude relative to reflected phases <i>r<sub>1</sub> r<sub>2</sub>, </i>and <i>r<sub>21</sub> </i>. The traces for rigid obstacles reveal that creeping and reflecting phases follow the same wave paths.</font></p>     <p align="center"><font face="verdana" size="2"><a name="f6"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f6.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f7"></a></font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f7.jpg"></font></p>     <p align="justify"><font face="verdana" size="2"><a href="#f8">Fig. 8</a> shows the same examples as in <a href="#f6">Fig. 6</a>, except that for a four&#150;scatterer array. Again, the response of three kinds of obstacles before an incoming plane S&#150;wave field is depicted. <a href="#f9">Fig. 9</a> corresponds to the same parameter configuration as in <a href="#f8">Fig. 8</a>, except for the case of <i>&psi;= </i>75&deg;. In both figures, it is possible to identify the phases generated by the four scatterers, reflections <i>r<sub>3 </sub>, r<sub>4 </sub>, r<sub>32 </sub>, r<sub>31</sub> , r<sub>4</sub> , r<sub>43 </sub>, r<sub>42 </sub></i>and <i>r<sub>41</sub> , </i>Creeping phases <i>c<sub>3</sub> </i>and <i>c<sub>4</sub> </i>are also observed. While the wave paths appear to be regular, a graphic detail and longer duration is required to improve identification of 4<sup>th</sup> and 5th order phases. For cavities and elastic inclusions, the wave slopes follow similar propagation paths, but for rigid obstacles propagation suffers an interference effect between cylinders. With the four obstacle types we are able to generalize the wave motion and scattering patterns caused by any number of scatterers for linear arrays.</font></p>     <p align="center"><font face="verdana" size="2"><a name="f8"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f8.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f9"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f9.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">Finally, consider wave motion and scattering patterns for the previously presented models. We have studied the spatial of amplitudes distribution during a lapse of propagation time, by means of snapshot series for meshes with 101 x 101 evenly spaced receivers located within squares of lengths 8<i><i>&alpha;</i></i> and 16<i><i>&alpha;</i></i>. In all cases twelve frames of displacement field are depicted. <a href="#f10">Figs. 10</a> and <a href="#f11">11</a> show snapshots for a two cavity model <i>(&rho;<sub>c </sub>/&rho; = </i>0.0, <i>&micro;<sub>c</sub> / &micro; = </i>0.0) for <i>&psi;= </i>90&deg; and <i>&psi;= </i>75&deg; respectively. The centers of the cavities are located at <i>x = &plusmn;</i>2 and <i>y = </i>0. The observation area is given by a square grid of receptors with length 8<i><i>&alpha;</i></i>. Excitation is given by anti&#150;plane S&#150;waves with a Ricker wavelet of <i>t<sub>p</sub> = </i>0.8s. <a href="#f12">Figs. 12</a> and <a href="#f13">13</a> show a similar case for elastic cylinders <i>(&rho;<sub>c </sub>/&rho; = </i>0.5, <i>&micro;<sub>c</sub> / &micro; = </i>0.3). These set of results illustrate how the wavefront reaches the array and then reflections and diffractions are produced. Forward and backward scattering patterns are generated in the whole space. Delay and degeneration of wavefront by geometrical multiple diffraction from cavities is notorious. However, diffraction at the far side of incidence creates a shadow or gap due to the cavities, unlike elastic inclusions where an amplification effect is clearly seen. Results from elastic inclusions reveal that the wavefront is attenuated at reflecting phases and amplified at creeping phases, due to the softer material filler. As time increases the wavefront recovers and the scattering of the wave field by the array wave diminishes. Again, it is possible to identify the interactive phases over the entire propagation space, but this exercise is left to the reader.</font></p>     <p align="center"><font face="verdana" size="2"><a name="f10"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f10.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f11"></a></font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f11.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f12"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f12.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f13"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f13.jpg"></font></p>     <p align="justify"><font face="verdana" size="2"><a href="#f14">Figs. 14</a> and <a href="#f15">15</a> show snapshots for a four cavity model with <i>&psi;= </i>90&deg; and <i>&psi;= </i>75&deg; respectively. The centers of the cavities are located at <i>x = &plusmn;</i>2 and <i>x = </i>&plusmn;6 with <i>y = </i>0. The observation area is given by a square region of length 16<i><i>&alpha;</i></i>. Excitation is given by anti&#150;plane S&#150;waves with a Ricker wavelet of <i>t<sub>p</sub> = </i>1.0s. <a href="#f16">Figs. 16</a> and <a href="#f17">17</a> show a similar previous case, just that for a four elastic inclusions model <i>(&rho;<sub>c </sub>/&rho; = </i>0.5, <i>&micro;<sub>c</sub> l &micro; = </i>0.3). The same responses described for the two cylinder models are recognized. The scattering patterns from the reflecting and creeping phases are dearly due to the higher number of regular obstacles in the array. Time analysis permits the observation of propagation properties that are not seen in the frequency domain, e. g. conspicuous amplification peaks produced by the diffraction of the wavefront due to softer elastic inclusions. Wave motion and scattering patterns produced by any number of cylinders in linear arrays may be characterized by the interaction between afew of them.</font></p>     <p align="center"><font face="verdana" size="2"><a name="f14"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f14.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f15"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f15.jpg"></font></p>     ]]></body>
<body><![CDATA[<p align="center"><font face="verdana" size="2"><a name="f16"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f16.jpg"></font></p>     <p align="center"><font face="verdana" size="2"><a name="f17"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3f17.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Conclusions</b></font></p>     <p align="justify"><font face="verdana" size="2">We have studied an analytic solution to compute the transient response and multiple scattering by a linear array of empty, elastic, and rigid cylinders. The formulation is two&#150;dimensional and is constructed by the superposition of the incident field and the waves diffracted by each obstacle. Here, the incident wave field is given by an anti&#150;plane S&#150;wave. The new interpretation of results and relevant examples were discussed. The normalized displacement amplitude relative to the incident field versus distance was plotted for specific frequencies. It was possible to identify the wave propagation behavior by means of computed synthetic seismograms and snapshots. It is shown that a conspicuous attenuation effect is observed by the array. A double response is produced by the presence of the elastic obstacles: reductions at the incidence side and amplifications at the opposite side, rather than the rigid cylinders, where the inverse response was identified.</font></p>     <p align="justify"><font face="verdana" size="2">The results reported here allow us to aim new paths of research and practical ways to describe and analyze the seismic response and multiple scattering in heterogeneous media. The analytical formulation reviewed in this paper offers a relatively simple way, with low computation cost, to understand the diffraction and multiple scattering of elastic waves by linear array of regularly distributed obstacles. The advantages and limitations of these techniques give us a complementary view of a not widely explored field of research. We are interested in the close future to develop these analytical formulations for several scatterers in arbitrary or randomly distributed configurations. The treatment of vector problem is been reviewed and constitutes the second part of this work. It is obvious that the 3D problem is extremely expensive in CPU and more, if the numerical computations do not take advantage of the mathematical properties of models. The most popular methods (finite differences, finite elements and spectral methods) are commonly used due to their easy implementation and programming. The 2D analytic formulation presented here appears to be a very low demand computational technique that only requires a good mathematical treatment and a PC. The applications of the numerical and analytical solutions for 3D multiple scattering problems are still open and offer a wide research area in several fields of science and engineering. The solution for 2 and 3D problems are now available using super computers or clusters and it is possible to carry on with complicated models. However, the characterization and the fundamental comprehension of the simplest parameters in a realistic model require more versatile mathematical formulations.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Acknowledgements</b></font></p>     ]]></body>
<body><![CDATA[<p align="justify"><font face="verdana" size="2">We wish to thank Jim Spurlin for his valuable suggestions to this work and Sergio Ch&aacute;vez&#150;P&eacute;rez for his critical reading. To Dimitri Komatitsch for previous comparisons and computations of some results. This work was partly supported by Instituto Mexicano del Petr&oacute;leo through The Naturally Fractured Reservoir Program, under Grant D01341, and the Exploration Technologies Research Program, by CONACYT ,under grant NC&#150;204, and Instituto de Ingenier&iacute;a, UNAM.</font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b><a href="#a1">Appendix</a>. Graf's Addition Theorem</b></font></p>     <p align="justify"><font face="verdana" size="2">In this paper, Graf's addition theorem is used to represent the scattered waves by the j&#150;th cylinder in terms of the coordinate system l as follows:</font></p>     <p align="center"><font face="verdana" size="2"><a name="a1"></a></font></p>     <p align="center"><font face="verdana" size="2"><img src="/img/revistas/geoint/v47n2/a3a1.jpg"></font></p>     <p align="justify"><font face="verdana" size="2">&nbsp;</font></p>     <p align="justify"><font face="verdana" size="2"><b>Bibliography</b></font></p>     <!-- ref --><p align="justify"><font face="verdana" size="2">Abramowitz, M., and I. A. Stegun. 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<source><![CDATA[Handbook of Mathematical Functions with Formulas, Graphs and Mathematical Tables]]></source>
<year>1964</year>
<volume>55</volume>
<publisher-loc><![CDATA[Washington ]]></publisher-loc>
<publisher-name><![CDATA[National Bureau of Standards]]></publisher-name>
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<surname><![CDATA[Sánchez-Sesma]]></surname>
<given-names><![CDATA[F. J.]]></given-names>
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<article-title xml:lang="en"><![CDATA[Scattering and Diffraction of Elastic P- and S-waves by a Spherical Obstacle: A Review of the Classical Solution]]></article-title>
<source><![CDATA[Geof. Inter.]]></source>
<year>2006</year>
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