the cowin–mehrabadi theorem for an axis of symmetry

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The Cowin–Mehrabadi theorem for an axis of symmetry Faiz Ahmad * Centre for Advanced Mathematics and Physics, National University of Sciences and Technology, EME College Campus, Peshawar Road, Rawalpindi, Pakistan article info Article history: Received 19 June 2009 Received in revised form 7 December 2009 Available online 13 August 2010 Keywords: Plane of symmetry Axis of symmetry Normal to a plane of symmetry Common eigenvectors abstract The well-known Cowin–Mehrabadi Theorem deals with necessary and sufficient conditions for a normal n to a symmetry plane. Necessary conditions require that n be a common eigenvector of C ijkk , C ikjk and C ijkl n j n l . It is shown that a vector parallel to an axis of symmetry must also satisfy these conditions. An axis of rotational symmetry is also a normal to a plane of symmetry except in the case of a trigonal mate- rial. Being a common eigenvector of C ijkk and C ikjk belonging to a nondegenerate eigenvalue guarantees it to be an axis of symmetry. Ó 2010 Elsevier Ltd. All rights reserved. 1. Introduction Let n be a unit normal to a plane of symmetry of an anisotropic material and let m be any vector lying in the symmetry plane. Cowin and Mehrabadi (1987) proved the following: Theorem 1. A set of necessary and sufficient conditions for a unit vector n to be a normal to a plane of symmetry is that it should be a common eigenvector of the following tensors U ij ¼ C ijkk ; V ij ¼ C ikjk ; W ik ðnÞ¼ C ijks n j n s ; W ik ðmÞ¼ C ijks m j m s ; where summation on the repeated indices is understood and free indi- ces take the values 1, 2, 3. Cowin (1989) modified the above conditions to show that it is necessary and sufficient that n be a common eigenvector of the last two of the above four tensors. Ting (2003) has given several simpli- fied versions of the above Theorem. For example: Theorem 2. A necessary and sufficient condition for n to be a normal to a symmetry plane is that n be an eigenvector of U, V, W(n) and W(m) for any one m. Theorem 3. A necessary and sufficient condition for n to be a normal to a symmetry plane is that n be an eigenvector of U, V or W(n), and an eigenvector of W(m) for any three distinct m. A vector p is said to be an n-fold rotation axis or an axis of sym- metry, A n , if a crystal remains unchanged after a rotation of an an- gle 2p/n about the vector p. It is somewhat curious that, although several results involving a normal to a plane of symmetry, n, such as the Theorems quoted above, are available in the literature, sim- ilar results don’t exist for an axis of symmetry p. This is surprising in view of the fact that in many cases n and p coincide. In this pa- per, we shall attempt to resolve this apparent paradox. We shall also examine the role of second rank tensors U and V in the theory of anisotropic materials. They provide a starting point if one wants to find the system of Cartesian coordinates with reference to which an elasticity tensor will appear in its simplest form. We shall con- sider the question whether or not U, V or a linear combination of them are the only tensors, independent of n, which must possess n as an eigenvector. We find that, on the contrary, any tensor of rank two, which contains the symmetry group of the elasticity ten- sor C, will have this property. We shall show that an axis of sym- metry satisfies first three conditions of Theorem 1, with W ik (n) replaced by W ik (p). These results also follow from the observation that whether the elastic symmetries are characterized by normals to symmetry planes or by axes of rotational symmetry, the trans- formation, in either case, associated with a reflection through a plane or a rotation about an axis belongs to the symmetry group of the material (Chadwick et al., 2001). Even the fourth condition is satisfied, with m replaced by p, if the material is monoclinic, orthorhombic or hexagonal. Thus the trigonal symmetry stands out as an exception. Fraldi and Cowin (2003) have termed the elas- tic constant c 14 as a ‘‘symmetry breaking cross-elastic constant.” The non-vanishing of this constant in a trigonal material leads to chirality in Fraldi and Cowin (2003) and, in the present work, it leads to the result that it is impossible for a threefold axis of sym- metry to simultaneously be a normal to a plane of symmetry. 0020-7683/$ - see front matter Ó 2010 Elsevier Ltd. All rights reserved. doi:10.1016/j.ijsolstr.2010.07.005 * Tel.: +92 3455334211. E-mail address: [email protected] International Journal of Solids and Structures 47 (2010) 3050–3052 Contents lists available at ScienceDirect International Journal of Solids and Structures journal homepage: www.elsevier.com/locate/ijsolstr

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Page 1: The Cowin–Mehrabadi theorem for an axis of symmetry

International Journal of Solids and Structures 47 (2010) 3050–3052

Contents lists available at ScienceDirect

International Journal of Solids and Structures

journal homepage: www.elsevier .com/locate / i jsolst r

The Cowin–Mehrabadi theorem for an axis of symmetry

Faiz Ahmad *

Centre for Advanced Mathematics and Physics, National University of Sciences and Technology, EME College Campus, Peshawar Road, Rawalpindi, Pakistan

a r t i c l e i n f o

Article history:Received 19 June 2009Received in revised form 7 December 2009Available online 13 August 2010

Keywords:Plane of symmetryAxis of symmetryNormal to a plane of symmetryCommon eigenvectors

0020-7683/$ - see front matter � 2010 Elsevier Ltd. Adoi:10.1016/j.ijsolstr.2010.07.005

* Tel.: +92 3455334211.E-mail address: [email protected]

a b s t r a c t

The well-known Cowin–Mehrabadi Theorem deals with necessary and sufficient conditions for a normaln to a symmetry plane. Necessary conditions require that n be a common eigenvector of Cijkk, Cikjk andCijklnjnl. It is shown that a vector parallel to an axis of symmetry must also satisfy these conditions. Anaxis of rotational symmetry is also a normal to a plane of symmetry except in the case of a trigonal mate-rial. Being a common eigenvector of Cijkk and Cikjk belonging to a nondegenerate eigenvalue guarantees it tobe an axis of symmetry.

� 2010 Elsevier Ltd. All rights reserved.

1. Introduction

Let n be a unit normal to a plane of symmetry of an anisotropicmaterial and let m be any vector lying in the symmetry plane.Cowin and Mehrabadi (1987) proved the following:

Theorem 1. A set of necessary and sufficient conditions for a unitvector n to be a normal to a plane of symmetry is that it should be acommon eigenvector of the following tensors

Uij ¼ Cijkk;

Vij ¼ Cikjk;

WikðnÞ ¼ Cijksnjns;

WikðmÞ ¼ Cijksmjms;

where summation on the repeated indices is understood and free indi-ces take the values 1, 2, 3.

Cowin (1989) modified the above conditions to show that it isnecessary and sufficient that n be a common eigenvector of the lasttwo of the above four tensors. Ting (2003) has given several simpli-fied versions of the above Theorem. For example:

Theorem 2. A necessary and sufficient condition for n to be a normalto a symmetry plane is that n be an eigenvector of U, V, W(n) andW(m) for any one m.

Theorem 3. A necessary and sufficient condition for n to be a normalto a symmetry plane is that n be an eigenvector of U, V or W(n), andan eigenvector of W(m) for any three distinct m.

ll rights reserved.

A vector p is said to be an n-fold rotation axis or an axis of sym-metry, An, if a crystal remains unchanged after a rotation of an an-gle 2p/n about the vector p. It is somewhat curious that, althoughseveral results involving a normal to a plane of symmetry, n, suchas the Theorems quoted above, are available in the literature, sim-ilar results don’t exist for an axis of symmetry p. This is surprisingin view of the fact that in many cases n and p coincide. In this pa-per, we shall attempt to resolve this apparent paradox. We shallalso examine the role of second rank tensors U and V in the theoryof anisotropic materials. They provide a starting point if one wantsto find the system of Cartesian coordinates with reference to whichan elasticity tensor will appear in its simplest form. We shall con-sider the question whether or not U, V or a linear combination ofthem are the only tensors, independent of n, which must possessn as an eigenvector. We find that, on the contrary, any tensor ofrank two, which contains the symmetry group of the elasticity ten-sor C, will have this property. We shall show that an axis of sym-metry satisfies first three conditions of Theorem 1, with Wik(n)replaced by Wik(p). These results also follow from the observationthat whether the elastic symmetries are characterized by normalsto symmetry planes or by axes of rotational symmetry, the trans-formation, in either case, associated with a reflection through aplane or a rotation about an axis belongs to the symmetry groupof the material (Chadwick et al., 2001). Even the fourth conditionis satisfied, with m replaced by p, if the material is monoclinic,orthorhombic or hexagonal. Thus the trigonal symmetry standsout as an exception. Fraldi and Cowin (2003) have termed the elas-tic constant c14 as a ‘‘symmetry breaking cross-elastic constant.”The non-vanishing of this constant in a trigonal material leads tochirality in Fraldi and Cowin (2003) and, in the present work, itleads to the result that it is impossible for a threefold axis of sym-metry to simultaneously be a normal to a plane of symmetry.

Page 2: The Cowin–Mehrabadi theorem for an axis of symmetry

F. Ahmad / International Journal of Solids and Structures 47 (2010) 3050–3052 3051

2. An axis of symmetry

We shall define a tensor Q which describes rotation of a rigidbody about an axis p by an arbitrary angle h. Most of the ideasare discussed in standard text books (Goldstein et al., 2006; Gurtin,1976). Also a brief description is presented in Mehrabadi et al.(1995) which we follow here. Let p = (p1,p2,p3)T be a unit vector.Define the tensor P with components

Pij ¼ �eijkpk: ð2:1Þ

The matrix representation for P is

P ¼0 �p3 p2

p3 0 �p1

�p2 p1 0

264

375: ð2:2Þ

P satisfies the following identities

P ¼ �PT ; Pp ¼ 0; P3 ¼ �P; ð2:3Þ

and the matrix representing the tensor Q is defined as

Q ¼ Iþ sin hPþ ð1� cos hÞP2; ð2:4Þ

where I denotes the identity matrix.By using the first and third identities of (2.3), it is easy to verify

that Q is an orthogonal tensor i.e. QQT = I. It has eigenvalues 1, eih,e�ih (Goldstein et al., 2006, Chapter 4). The eigenvector correspond-ing to 1 is the vector p, which is apparent from the second identityof (2.3). Now consider a tensor T of rank two associated with anelastic material such as, for example, U ¼ Cijkk; V ¼ Cikjk; G ¼12 eijkelmnCiljm or H = CijklCijkm. The following argument shows thateach of the above tensors contains the symmetry group of the elas-ticity tensor C. Consider, for example

Uij ¼ Cijkk ¼ Cijkldkl; ð2:5Þ

where dkl is the unit tensor of rank 2. Now (2.5) is a tensor equationwhich is valid in every Cartesian coordinate system. Thus

U0ij ¼ C0ijkld0kl; ð2:6Þ

where an asterisk denotes a component in a transformed coordinatesystem. If the transformation corresponds to a symmetry element ofthe elasticity tensor, Eq. (2.6) becomes

U0ij ¼ Cijkldkl ¼ Cijkk ¼ Uij;

where we have used the fact that the unit tensor is isotropic i.e. ithas same components with respect to every Cartesian coordinatesystem. Thus every element of the symmetry group of C is con-tained in the symmetry group of U.

Among the above tensors, G has a particularly simple matrixrepresentation

G ¼c23 � c44 c45 � c36 c46 � c25

c45 � c36 c13 � c55 c56 � c14

c46 � c25 c56 � c14 c12 � c66

0B@

1CA; ð2:7Þ

where c23 = C2233 etc. This tensor was used by Ahmad (2002) to finda quadratic invariant of the elasticity tensor. Its off-diagonal compo-nents are the same as those of V � U. If p is an axis of symmetry forthe material, a second rank tensor T, invariant with respect to thesimilarity transformation associated with Q, will satisfy

T ¼ QTQ�1: ð2:8Þ

Therefore TQ = QT. Also Q has p as a nondegenerate eigenvector cor-responding to the eigenvalue 1, therefore p must also be an eigen-vector of T (Friedman, 1966).

Using indices, Eq. (2.4) can be written as

Qij ¼ dij þ sin hPij þ ð1� cos hÞPikPkj; ð2:9Þ

where dij denotes the unit tensor and summation over repeatedindices is understood. Using (2.1) in (2.9), Qij can be expressed interms of components of the vector p

Qij ¼ dij cos hþ ð1� cos hÞpipj � sin heijkpk: ð2:10Þ

For an elementary derivation of (2.10) see Beatty (1963).In the next Theorem, we show that p shares with n three out of

four conditions enunciated in Theorem 1.

Theorem 4. A necessary condition for a vector p to be an axis ofsymmetry is that it is a common eigenvector of U, V and W(p) asdefined in Theorem 1.

Proof. An arbitrary vector is indeed a 1-fold axis of symmetry. Itmay or may not be an eigenvector of any of the tensors mentionedin the above statement. We shall exclude this case from the subse-quent discussion. If a rotation through an angle h leaves a materialinvariant, we must have

Cijkl ¼ QirQ jsQ ktQ luCrstu: ð2:11Þ

Multiply both sides with pjpkpl and sum over repeated indices. Not-ing the fact Qvwpv = pw, the above equation becomes

Cijklpjpkpl ¼ Q irpsptpuCrstu:

Substituting from (2.10) and rearranging terms, we get

ð1� cos hÞðCijklpjpkpl � CrstuprpsptpupiÞ þ sin heirkpkpsptpuCrstu ¼ 0:

ð2:12Þ

There are two possible ways of satisfying the above equation. Firstby requiring sin h ¼ 0 and 1� cos h ¼ 0. This leads to the case ofh = 2p i.e. a 1-fold rotation axis, which we have excluded. Otherwisewe must require that the vector Cijklpjpkpl be equal to Crstuprpsptpupi.This implies that p is an eigenvector of W(p), where Wik(p) = Cijklpjpl.Now Crstupsptpu = kpr, where k = Crstuprpsptpu and the second term onthe right in (2.12) vanishes since eirkpkpr = 0. To prove that p is alsoan eigenvector of U and V, the above argument may be repeatedwith the tensors Cijrr and Cirjr. This proves the theorem. h

Theorem 5. A necessary and sufficient condition for an axis of sym-metry An to be a normal to a plane of symmetry is that n be an eveninteger i.e. n = 2, 4 or 6. Thus an A3 axis is the only axis of symmetrywhich is not a normal to a plane of symmetry.

Proof. First suppose n is even. Since a 4-fold or a 6-fold symmetryaxis is also a 2-fold axis, a rotation through 180� leaves the mate-rial invariant. If we let h = p in (2.10), we get

QijðpÞ ¼ �dij þ 2pipj: ð2:13aÞ

The tensor associated with a normal n to a plane of symmetry is

XijðnÞ ¼ dij � 2ninj; ð2:13bÞ

Ting (1996, Chapter 2). The two tensors are of the same form exceptfor the sign which does not matter if the transformation such as(2.13) involves an even number of factors Qij. Now p will satisfyall conditions of Theorems 1–3 and will be a normal to a plane ofsymmetry.

Now assume that a material possesses an axis of symmetry A3.Choose x3-axis parallel to this direction. It is well-known (Dieule-saint and Royer, 1980, Chapter 4) that a matrix representation of C

for the material is

Page 3: The Cowin–Mehrabadi theorem for an axis of symmetry

3052 F. Ahmad / International Journal of Solids and Structures 47 (2010) 3050–3052

ðCÞtrigonal ¼

c11 c12 c13 c14 c15 0c12 c11 c13 �c14 �c15 0c13 c13 c33 0 0 0c14 �c14 0 c44 0 �c15

c15 �c15 0 0 c44 c14

0 0 0 �c15 c14 ðc11 � c12Þ=2

2666666664

3777777775;

ð2:14Þ

where we have used the familiar two index notation to denote com-ponents of C. Now if the threefold axis of symmetry is assumed tobe a normal to a plane of symmetry as well, this will force any com-ponent with an odd number of the index 3 to become zero. Thusc14 = C1123 = 0 and c15 = C1113 = 0. But then the matrix (2.14) will be-come identical to the one representing C for a hexagonal material.Since the trigonal and hexagonal materials are distinct classes, wemust conclude that an A3 axis is not a normal to any plane ofsymmetry. h

In order to verify whether or not a vector is a normal to a planeof symmetry, we need four conditions (see Theorems 1–3). How-ever a sufficient condition for an axis of symmetry is relatively sim-ple. The following theorem bears out this observation.

Theorem 6. A sufficient condition for a vector p to be an axis ofsymmetry is that it is a common eigenvector of U and V correspondingto a nondegenerate eigenvalue.

Proof. It is clear that if p satisfies condition of the Theorem, thetensor C cannot belong to an isotropic, cubic or a triclinic materialbecause for the first two, U and V both have a three fold degenerateeigenvalue and for the third they will not possess a common eigen-vector. That leaves us with the remaining five classes, we dividethem into two parts.

(a) Let C belong to a trigonal, tetragonal or a hexagonal material.For each class the matrix Q, of (2.4), will have distinct eigen-values 1 and e±ih. Eigenvectors corresponding to the two com-plex eigenvalues will be complex. Denote them by Q1 ± iQ2. Ifp is an axis of symmetry, Q will commute with both U and V,consequently they will have the same eigenvectors as Q. But areal matrix can have a complex eigenvector only if both itsreal and imaginary parts are eigenvectors corresponding toa two fold degenerate eigenvalue. Hence U and V each havep as an eigenvector belonging to a nondegenerate eigenvalueand Q1 and Q2 belonging to a degenerate eigenvalue. Aneigenvector of U (or V) belonging to the nondegenerate eigen-value cannot be anything other than the axis of symmetry of C

(b) Now let C belong to a monoclinic or an orthorhombic mate-rial. First we consider the case when U and V have allnondegenerate eigenvalues but only a single common eigen-vector p. Suppose p is not an axis of symmetry but there isanother vector p1 which has this status. But then U and Vmust also have p1 as a common eigenvector which contra-dicts the fact that p is the only common eigenvector. Thusp must be an axis of symmetry. Next let U and V have allthree eigenvectors common to each other. Since we havealready dealt with cases where a single An is present withn = 2, 3, 4, 6, the only remaining case is that of theorthorhombic material possessing three A2 axes. The vectorsparallel to these axes must be eigenvectors of U and V,leaving no room for any other vector to take up this role.Hence any eigenvector of U (or V) must be an axis ofsymmetry. h

Acknowledgements

The author is grateful to the referees for their helpful commentson an earlier version of the paper.

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