Orthotropic material

An orthotropic material has two or three mutually orthogonal twofold axes of rotational symmetry so that its mechanical properties are, in general, different along each axis. Orthotropic materials are thus anisotropic; their properties depend on the direction in which they are measured. An isotropic material, in contrast, has the same properties in every direction.
One common example of an orthotropic material with two axis of symmetry would be a polymer reinforced by parallel glass or graphite fibers. The strength and stiffness of such a composite material will usually be greater in a direction parallel to the fibers than in the transverse direction. Another example would be a biological membrane, in which the properties in the plane of the membrane will be different from those in the perpendicular direction. Such materials are sometimes called transverse isotropic.
A familiar example of an orthotropic material with three mutually perpendicular axis is wood, in which the properties (such as strength and stiffness) along its grain and in each of the two perpendicular directions are different. Hankinson's equation provides a means to quantify the difference in strength in different directions. Another example is a metal which has been rolled to form a sheet; the properties in the rolling direction and each of the two transverse directions will be different due to the anisotropic structure that develops during rolling.
It is important to keep in mind that a material which is anisotropic on one length scale may be isotropic on another (usually larger) length scale. For instance, most metals are polycrystalline with very small grains. Each of the individual grains may be anisotropic, but if the material as a whole comprises many randomly oriented grains, then its measured mechanical properties will be an average of the properties over all possible orientations of the individual grains.
Contents
Orthotropy in physics
Anisotropic material relations
Material behavior is represented in physical theories by constitutive relations. A large class of physical behaviors can be represented by linear material models that take the form of a secondorder tensor. The material tensor provides a relation between two vectors and can be written as
where are two vectors representing physical quantities and is the secondorder material tensor. If we express the above equation in terms of components with respect to an orthonormal coordinate system, we can write
Summation over repeated indices has been assumed in the above relation. In matrix form we have
Examples of physical problems that fit the above template are listed in the table below^{[1]}.
Problem Electrical conduction Electrical current
Electric field
Electrical conductivity
Dielectrics Electrical displacement
Electric field
Electric permittivity
Magnetism Magnetic induction
Magnetic field
Magnetic permeability
Thermal conduction Heat flux
Temperature gradient
Thermal conductivity
Diffusion Particle flux
Concentration gradient
Diffusivity
Flow in porous media Weighted fluid velocity
Pressure gradient
Fluid permeability
Condition for material symmetry
The material matrix has a symmetry with respect to a given orthogonal transformation () if it does not change when subjected to that transformation. For invariance of the material properties under such a transformation we require
Hence the condition for material symmetry is (using the definition of an orthogonal transformation)
Orthogonal transformations can be represented in Cartesian coordinates by a matrix given by
Therefore the symmetry condition can be written in matrix form as
Orthotropic material properties
An orthotropic material has three orthogonal symmetry planes. If we choose an orthonormal coordinate system such that the axes coincide with the normals to the three symmetry planes, the transformation matrices are
It can be shown that if the matrix for a material is invariant under reflection about two orthogonal planes then it is also invariant under reflection about the third orthogonal plane.
Consider the reflection about the plane. Then we have
The above relation implies that K_{13} = K_{23} = K_{31} = K_{32} = 0. Next consider a reflection about the plane. We then have
That implies that K_{12} = K_{21} = 0. Therefore the material properties of an orthotropic material are described by the matrix
Orthotropy in linear elasticity
Anisotropic elasticity
In linear elasticity, the relation between stress and strain depend on the type of material under consideration. This relation is known as Hooke's law. For anisotropic materials Hooke's law can be written as^{[2]}
where is the stress tensor, is the strain tensor, and is the elastic stiffness tensor. If the tensors in the above expression are described in terms of components with respect to an orthonormal coordinate system we can write
where summation has been assumed over repeated indices. Since the stress and strain tensors are symmetric, and since the stressstrain relation in linear elasticity can be derived from a strain energy density function, the following symmetries hold for linear elastic materials
Because of the above symmetries, the stressstrain relation for linear elastic materials can be expressed in matrix form as
An alternative representation in Voigt notation is
or
The stiffness matrix in the above relation satisfies point symmetry ^{[3]}.
Condition for material symmetry
The stiffness matrix satisfies a given symmetry condition if it does not change when subjected to the corresponding orthogonal transformation. The orthogonal transformation may represent symmetry with respect to a point, an axis, or a plane. Orthogonal transformations in linear elasticity include rotations and reflections, but not shape changing transformations and can be represented, in orthonormal coordinates, by a matrix given by
In Voigt notation, the transformation matrix for the stress tensor can be expressed as a matrix given by^{[3]}
The transformation for the strain tensor has a slightly different form because of the choice of notation. This transformation matrix is
It can be shown that .
The elastic properties of a continuum are invariant under an orthogonal transformation if and only if^{[3]}
Stiffness and compliance matrices in orthotropic elasticity
An orthotropic elastic material has three orthogonal symmetry planes. If we choose an orthonormal coordinate system such that the axes coincide with the normals to the three symmetry planes, the transformation matrices are
We can show that if the matrix for a linear elastic material is invariant under reflection about two orthogonal planes then it is also invariant under reflection about the third orthogonal plane.
If we consider the reflection about the plane, then we have
Then the requirement implies that^{[3]}
The above requirement can be satisfied only if
Let us next consider the reflection about the plane. In that case
Using the invariance condition again, we get the additional requirement that
No further information can be obtained because the reflection about third symmetry plane is not independent of reflections about the planes that we have already considered. Therefore, the stiffness matrix of an orthotropic linear elastic material can be written as
The inverse of this matrix is commonly written as^{[4]}
where is the Young's modulus along axis i, is the shear modulus in direction j on the plane whose normal is in direction i, and is the Poisson's ratio that corresponds to a contraction in direction j when an extension is applied in direction i.
Bounds on the moduli of orthotropic elastic materials
The strainstress relation for orthotropic linear elastic materials can be written in Voigt notation as
where the compliance matrix is given by
The compliance matrix is symmetric and must be positive definite for the strain energy density to be positive. This implies from Sylvester's criterion that all the principal minors of the matrix are positive^{[5]}, i.e.,
where is the principal submatrix of .
Then,
We can show that this set of conditions implies that^{[6]}
or
 E_{1} > 0,E_{2} > 0,E_{3} > 0,G_{12} > 0,G_{23} > 0,G_{13} > 0
However, no similar lower bounds can be placed on the values of the Poisson's ratios ν_{ij}^{[5]}.
See also
References
 ^ Milton, G. W., 2002, The Theory of Composites, Cambridge University Press.
 ^ Lekhnitskii, S. G., 1963, Theory of Elasticity of an Anisotropic Elastic Body, HoldenDay Inc.
 ^ ^{a} ^{b} ^{c} ^{d} Slawinski, M. A., 2010, Waves and Rays in Elastic Continua: 2nd Ed., World Scientific. http://samizdat.mines.edu/wavesandrays/WavesAndRays.pdf
 ^ Boresi, A. P, Schmidt, R. J. and Sidebottom, O. M., 1993, Advanced Mechanics of Materials, Wiley.
 ^ ^{a} ^{b} Ting, T. C. T. and Chen, T., 2005, Poisson's ratio for anisotropic elastic materials can have no bounds,, Q. J. Mech. Appl. Math., 58(1), pp. 7382.
 ^ Ting, T. C. T., 1996, Positive definiteness of anisotropic elastic constants,, Mathematics and Mechanics of Solids, 1, pp. 301314.
Further reading
 Orthotropy modeling equations from OOFEM Matlib manual section.
 Hooke's law for orthotropic materials
Categories: Continuum mechanics
 Materials
Wikimedia Foundation. 2010.
Look at other dictionaries:
Orthotropic — may refer to: Orthotropic material is one that has the different materials properties or strengths in different orthogonal directions (e.g., glass reinforced plastic, or wood) Orthotropic deck is one in which the deck is solid steel plate in… … Wikipedia
Orthotropic deck — For other uses, see Deck. Fabricating an orthotropic deck section An orthotropic bridge or orthotropic deck is one whose deck typically comprises a structural steel deck plate stiffened either longitudinally or transversely, or in both directions … Wikipedia
Material ortótropo — La madera es un ejemplo de un material ortótropo: sus propiedades en tres direcciones perpendiculares (axial, radial y circunferencial) son diferentes. Un material ortótropo tiene dos o tres ejes ortogonales entre sí, de doble simetría rotacional … Wikipedia Español
Failure theory (material) — v · d · e Materials failure modes Buckling · Corro … Wikipedia
Hooke's law — models the properties of springs for small changes in length Prof. Walter Lewin explains Hooke s law, in … Wikipedia
Poisson's ratio — ( ν ), named after Simeon Poisson, is the ratio of the relative contraction strain, or transverse strain (normal to the applied load), divided by the relative extension strain, or axial strain (in the direction of the applied load).When a sample… … Wikipedia
Hankinson's equation — is a mathematical relationship for predicting stress wave velocity as a function of grain angle in wood. Because wood is an orthotropic material, its mechanical properties are different along different axes.: V(alpha) = frac{V 0 V {90{V 0… … Wikipedia
Mindlin–Reissner plate theory — Deformation of a plate highlighting the displacement, the mid surface (red) and the normal to the mid surface (blue) The Mindlin Reissner theory of plates is an extension of Kirchhoff–Love plate theory that takes into account shear deformations… … Wikipedia
Nordhordland Bridge — Nordhordland Bridge … Wikipedia
Макромеханическое моделирование каменных стен — Макромеханическое моделирование каменных стен метод моделирования каменной кладки стен, при котором неоднородная (гетерогенная система) кладки, состоящая из кладочных элементов (кирпича, природных или искусственных камней, бетонных блоков и … Википедия