On orthogonal transformations of Christoffel equations
Len Bos, Michael A. Slawinski, Theodore Stanoev, Maurizio, Vianello

TL;DR
This paper proves the equivalence of different forms of Christoffel equations under orthogonal transformations, broadening the understanding of wave propagation in elastic solids beyond traditional assumptions.
Contribution
It introduces a general proposition that establishes the invariance of Christoffel equations under orthogonal transformations, without restrictions on space dimension or tensor symmetries.
Findings
Proves equivalence of Christoffel equations under rotations and orthogonal transformations.
Extends validity beyond R^3 and symmetric elasticity tensors.
Provides a general mathematical framework for wave propagation analysis.
Abstract
The purpose of this paper is to prove the equivalenceunder rotations of distinct termsof different forms of a determinantal equation that appears in the studies of wave propagation in Hookean solids, in the context of the Christoffel equations. To do so, we prove a general proposition that is not limited to , nor is it limited to the elasticity tensor with its index symmetries. Furthermore, the proposition is valid for orthogonal transformations, not only for rotations. The sought equivalence is a corollary of that proposition.
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On orthogonal transformations of Christoffel equations
Len Bos111Dipartimento di Informatica, Università di Verona, Italy; [email protected] , Michael A. Slawinski222Department of Earth Sciences, Memorial University of Newfoundland, Canada; [email protected] , Theodore Stanoev333Department of Earth Sciences, Memorial University of Newfoundland, Canada; [email protected] , Maurizio Vianello444Dipartimento di Matematica, Politecnico di Milano, Italy; [email protected]
Abstract:
The purpose of this paper is to prove the equivalence—under rotations of distinct terms—of different forms of a determinantal equation that appears in the studies of wave propagation in Hookean solids, in the context of the Christoffel equations. To do so, we prove a general proposition that is not limited to , nor is it limited to the elasticity tensor with its index symmetries. Furthermore, the proposition is valid for orthogonal transformations, not only for rotations. The sought equivalence is a corollary of that proposition.
1 Introduction
The existence and properties of three waves that propagate in a Hookean solid are a consequence of the Christoffel equations (e.g., Slawinski, 2015, Chapter 9), whose solubility condition is
[TABLE]
which is a cubic polynomial, whose roots are the eikonal equations (e.g., Slawinski, 2015, Section 7.3). Let us examine the matrix therein,
[TABLE]
where is a density-normalized elasticity tensor, whose units are , and is the wavefront-slowness vector, whose units are .
Studies of Hookean solids by Ivanov and Stovas (2016, equations (7)–(12)) and Ivanov and Stovas (2017, equations (10)–(11)) invoke a property that we state as Corollary 1, which is a consequence of Proposition 1. Ivanov and Stovas (2016, 2017) verify the equivalence of equations given in Corollary 1, without a general proof, hence, this paper.
The purpose of this paper is to prove Proposition 1 and, hence, Corollary 1. In doing so, we gain an insight into a tensor-algebra property that results in this corollary. The equivalence of the aforementioned equations is not a result of the invariance of a determinant, as suggested by Ivanov (pers. comm., 2018); it is a consequence of two orthogonal transformations of and that result in two matrices that are similar to one another.
2 Proposition and its corollary
Proposition 1**.**
Consider a tensor, , in . Also, consider a vector, , in , and an orthogonal transformation, It follows that matrices
[TABLE]
and
[TABLE]
where
[TABLE]
are similar to one another and, consequently, have the same spectra.
Proof.
The fourth-rank tensor, , in can be viewed as a matrix, whose entries are matrices,
[TABLE]
with and . Thus, matrix (1) can be written as
[TABLE]
where t denotes the transpose.
We claim that matrix (2) can be written as
[TABLE]
To see this, we let matrix (4) be
[TABLE]
where , to write
[TABLE]
Defining , we have
[TABLE]
where
[TABLE]
Hence,
[TABLE]
and, in turn,
[TABLE]
which is matrix (2), as required. ∎
Corollary 1**.**
From Proposition 1—and the aforementioned fact that the similar matrices share the same spectrum, as well as the fact that the similarity of matrices is not affected by subtracting from them the identity matrices—it follows that
[TABLE]
and, hence, equations
[TABLE]
and
[TABLE]
are equivalent to one another.
Corollary 1 is valid even without requiring the index symmetries of Hookean solids. Also, , not only , which is more general than the property invoked by Ivanov and Stovas (2016, 2017).
3 Numerical example
Consider an orthotropic tensor (Ivanov and Stovas, 2016, Table 2), whose components are
[TABLE]
Also, consider vector p=\Big{[}0,0,\sqrt{\tfrac{1}{c_{3333}}}\,\Big{]} . Rotating this vector by
[TABLE]
with an arbitrary angle of , and the tensor by , we obtain
[TABLE]
and
[TABLE]
respectively. The eigenvalues of these matrices are the same, , and , as required for similar matrices. Their corresponding eigenvectors are related by transformation (7).
Herein, . In general, the two determinants are equal to one another. Hence, if , so does , and vice versa.
The equivalence of equations (5) and (6) does not imply their equivalence to
[TABLE]
The eigenvalues of
[TABLE]
are , and , which are distinct from the eigenvalues of and . Herein—in view of and representing, respectively, the slowness vector along the -axis and its corresponding elasticity tensor— , which results in the eikonal equations. We emphasize, however, that Proposition 1 and Corollary 1 are valid for arbitrary vectors and fourth-rank tensors, even though, in this example, they are related by the Christoffel equations.
Acknowledgments
The authors wish to acknowledge Igor Ravve for bringing this issue to their attention, Yuriy Ivanov for presenting and clarifying aspects of this problem, Sandra Forte for fruitful discussions, and David Dalton for insightful proofreading.
This research was performed in the context of The Geomechanics Project supported by Husky Energy. Also, this research was partially supported by the Natural Sciences and Engineering Research Council of Canada, grant 202259.
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1Ivanov and Stovas (2016) Ivanov, Y. and Stovas, A. (2016). Normal moveout velocity ellipse in tilted orthorhombic media. Geophysics , 81(6):319–336.
- 2Ivanov and Stovas (2017) Ivanov, Y. and Stovas, A. (2017). Traveltime parameters in tilted orthorhombic medium. Geophysics , 82(6):187–200.
- 3Slawinski (2015) Slawinski, M. A. (2015). Waves and rays in elastic continua . World Scientific, 3 edition.
