Kinematics deals with the mathematical description of deformations, displacements
and rotations.
These rigid body motions or deformations are typically due to the forces which are applied to the considered continuum. In this chapter, the kinematics in a material point will be described, assuming that the related external loads that caused it are yet unknown.
The chapter is organized as follows. We start with the general aspects of deformation:
continuity, the displacement vector and the deformation gradient tensorF, together
with the two special cases of rigid body motion and homogeneous deformation. Because F
itself still contains rigid rotation, we then isolate the true deformation through the right
and left Cauchy-Green tensorsC and B, and split F into stretch and rotation
by means of the right and left polar decompositions.
Next, we convert stretch into strain, introducing the linear, logarithmic and Green-Lagrange
strain measures and their tensorial counterparts. Finally, we turn to time derivatives: the
material and spatial time derivatives, the velocity gradient tensor L, and its split into
the rate-of-deformation tensorD and the spin tensorΩ.
Upon deformation of a material, a fundamental distinction is made between the material (or
Lagrangian) framework and the spatial (Eulerian) framework. The governing kinematic relations in continuum mechanics are based on the one-to-one correspondence between these two frameworks.
The continuity of the displacements is one of the basic assumptions in classical continuum mechanics. This assumption implies that the material is described in an average fashion, without considering the physical discrete microstructure or a material (e.g. molecular or crystalline structure). The neighborhood of a material point is considered to be dense and continuous. The kinematic and mechanical quantities that ensue from such a theory are therefore considered as average values over the real microstructure. If a material deforms, changes in distance between “dense” material points will occur. The transformation from the undeformed state to the deformed state is a one-to-one mapping, where each material point in the deformed state is associated with one and only material point from the undeformed state. The continuity of the deformation implies that neighborhoods of a material point P0 in the initial region R0 remain neighborhoods of the transformed material point P in the transformed region R, see Figure 1.1.
Upon deformation a material point changes position from x0 to x. This change
in position is characterized by the displacement vector, which is given by
Let’s consider two material points that are infinitely close, i.e. one material point is currently in the position x, while its neighbour is in position x+dx. The principle of continuity tells us that these two points were also neighbours in the initial undeformed state. Their positions in that initial state are respectively given by x0 and x0+dx0. The vector dx0 that initially
interconnected these two points is thus transformed or deformed into a new vector dx, see Figure 1.2.
Figure 1.2:The linearized deformation map - the deformation tensor F
The linear transformation of the vector dx0 into the vector dx is described
by a second-order tensor, called the deformation gradient tensor F. From the nonlinear deformation map ϕ it appears that
The second-order tensor F is thus the spatial derivative of the nonlinear
deformation map in the considered material point, which leads to a locally linear
deformation map. The tensor is the transposed Lagrangian gradient of the
current position vector. The tensor thus expresses the deformation with respect to the
initial undeformed state. The gradient symbol ∇0 clearly indicates this with its
subscript 0. Since F is a second-order tensor, it is fully identified by means of
the image (i.c. the deformation) of three (i.c. infinitesimal) vectors, which span an
infinitesimally volume as shown in Figure 1.3.
The Lagrangian gradient of the displacement also leads to a second order tensor, called
the displacement gradient tensor u. Its formal definition sounds
Like in equation (1.3) (i.e. the definition of the Lagrangian gradient of a vector), this tensor maps the initial interconnection
vector dx0 on the relative displacement vector between the two considered adjacent material points.
The relative displacement vector du measures the displacement that occurred between
these two adjacent points with respect to their original relative positions
Since F and u are both second-order tensors, they describe linear transformations. This means that the deformation along three independent vectors in (3D) material point suffices to fully characterize these tensors. An initially cubic volume element will always be deformed by F into a parallelepiped.
Consider a volume element that is spanned by three non-coplanar infinitesimal material vectors dX1=dx01, dX2=dx02 and dX3=dx03. After deformation these vectors are transformed into new vectors dx1, dx2 and dx3. The deformation tensor F gives the relation between the two sets of vectors
If both sets of vectors are known, F can be fully determined. The volume dV0 of the parallelepiped spanned by the three vectors in
the initial situation equals:
we can conclude that F is a regular tensor. Thus the
inverse tensor F−1, describing the transformation from the
deformed to the undeformed state, exists:
The response of a continuum on an external load may be a pure rigid
body motion, consisting of translation and rotation. In this case the
mutual displacements of the material points of the body are zero, see Figure 1.4.
We may consider the transformation of the initial to the actual situation as a pure rotation Q of the continuum, followed by a pure translation t. If the centre of rotation is located at a material point P with initial position x0, the actual position y of an arbitrary point in the continuum with initial position y0 is given by:
Now let us consider the change of the angle between two material
vectors, see Figure 1.6.
Figure 1.6:Shear deformation between two infinitesimal vectors dx01 and dx02.
For simplicity we consider two vectors dx01 and dx02
that are mutually perpendicular in the initial situation. For the angle θ between the transformed vectors it holds that:
A change of angle between two vectors is called shear deformation[3]. The expressions for stretch (1.27) and shear (1.29) show that the true deformation is not described by the deformation tensor F itself, but by the so-called right Cauchy-Green deformation tensor[4]C, defined as:
As a consequence of these properties, the eigenvectors m and
eigenvalues μ of C are real, the eigenvalues are positive and the eigenvectors are mutually perpendicular (or may be chosen so, see section Section A.3.6.5). With respect to the basis of eigenvectors {m1,m2,m3}, C can be written as:
Thus we can interpret the directions of the eigenvectors mi of C as three mutually orthogonal directions in the initial state, that remain mutually orthogonal in the deformed state. These directions are called principal directions[5], and denoted by n0i, where n0i=mi. The stretch ratio λ in a principal direction n0i is given by:
The strain ratios λ1,λ2,λ3 are called principal strain ratios[6]. Now we can write the spectral form of C in terms of principal strain ratios λi and principal
directions n0i:
Consider the homogeneous deformation x1=X1+γX2, x2=X2, x3=X3, with
γ the amount of shear. From the definition of F, the matrix representation with
respect to the Cartesian basis {ex,ey,ez} is
Applying λ(e0)=e0⋅C⋅e0 to the two in-plane basis
directions gives λ(e1)=1 and λ(e2)=1+γ2: material lines
along e1 keep their length, while those along e2 are stretched. The angle
θ between the deformed images of e1 and e2 follows from (1.29):
which is nonzero for any γ=0 - the two directions no longer meet at a right angle.
Note that C=I even though the volume is unchanged, confirming that C, and
not det(F), is what measures the true deformation.
1.1.6Right polar decomposition of the deformation tensor¶
Thus, this special block of material, spanned by material vectors
along the eigenvectors of U, is transformed into a block with
identical orientation, but with changed dimensions.
Figure 1.8:Simultaneous stretch and shear of a arbitrary block, after deformation by U.
Now we define a tensor R that relates the deformation gradient
tensor F to the right stretch tensor U according to:
Figure 1.9:Right polar decomposition of the deformation F, into stretch and shear, described by U and a rotation, described by R.
In fact, as Figure 1.9 illustrates, we now decomposed the total deformation, described by F
into two processes: first the material is deformed according to the right
stretch tensor U, next it is rotated according to the rotation tensor R. This decomposition is called right polar decomposition[7]:
The true deformation of a continuum can also be expressed with respect to the current deformed configuration. The stretch of a material vector dx0 that is transformed into dx is then given by:
Now let us reconsider the change of the angle between two material vectors, where we attempt to express this change with respect to the current configuration, see Figure 1.10:
Figure 1.10:Shear deformation towards two infinitesimal vectors dx1 and dx2.
For simplicity we now consider two deformed vectors dx1 and dx2 that are mutually perpendicular in the deformed configuration. The angle ϕ between these two vectors in the initial (undeformed) configuration (i.e. dx01 and dx02) is given by:
Clearly, with respect to the current configuration, the shear between two vectors is characterized by the inverse of the left Cauchy-Green deformation tensor B.
The left Cauchy-Green deformation tensor is symmetric:
As a consequence of these properties, the eigenvectors n and eigenvalues μ of B are real, the eigenvalues are positive and the eigenvectors are mutually perpendicular (or may be chosen so, see section Section A.3.6.5). With respect to the basis of eigenvectors {n1,n2,n3}, B can be written in its spectral form by:
If, in equation (1.29), we choose the directions of the material vectors e1 and e2 along two different eigenvectors of B−1 (or B), it is obvious that:
Thus we can interpret the directions of the eigenvectors ni of B as three mutually orthogonal directions in the current deformed state,
that were already mutually orthogonal in the initial undeformed state. These directions are called the principal directions in the current state[8].
The stretch ratio λ in a principal direction ni is given by:
Now consider a block of material in the deformed configuration, spanned by material vectors dx1=∥dx1∥n1, dx2=∥dx2∥n2 and dx3=∥dx3∥n3, see Figure 1.11.
Figure 1.11:Pure stretch of a block, spanned by eigenvectors of V, before deformation by V.
This material block is the result of the transformation by the tensor V from a block, spanned by the vectors dx1∗, dx2∗ and dx3∗, with:
Thus, this special block of material, spanned by material vectors along the eigenvectors of V, was transformed from a block with identical orientation, but with changed dimensions.
Figure 1.12:Simultaneous stretch and shear of a arbitrary block, after deformation by V.
The tensor that relates the deformation gradient tensor F to the left stretch tensor V is nothing else than the already defined rotation tensor R
Figure 1.13:Left polar decomposition of the deformation F, into a rotation R and a stretch and shear part, described by V.
Again, as shown in Figure 1.13, the total deformation described by F is decomposed into two processes: first the material is rotated according to the rotation tensor R and next deformed according to the left stretch tensor V. This decomposition is called left polar decomposition[9]:
We have introduced the stretch ratio λ as a measure for the
change of length of a material vector. If there is no deformation, the
stretch ratio equals one. Often it is more convenient to describe change
of length with a quantity that equals zero when there is no deformation.
Such a quantity is called a strain[10], often denoted by ϵ. In general, it is a function of the stretch ratio λ: ϵ=f(λ). The function f(λ) should meet the following requirements:
f(λ=1)=0,
f(λ) is monotonously increasing with increasing λ,
the derivative of f(λ) with respect to λ exists,
f(λ)∥λ≈1=λ−1.
Three often used strain measures, that comply with these requirements are the
Figure 1.14 compares these measures. They all coincide with λ−1 near
λ=1, but diverge strongly at large stretches, which is exactly why the choice of
strain measure matters once deformations are no longer small.
Figure 1.14:Comparison of strain definitions as a function of the stretch λ.
The stretch ratio of an arbitrary material vector with orientation e0 in the initial state can be calculated using the right Cauchy-Green deformation tensor:
Thus, for this special case the condition ϵl(e0)=e0⋅E⋅e0 gives indeed the linear strain.
However, application to an arbitrary direction e0, yields that:
Thus, in this case the strain calculated with the strain tensor is in
agreement with the strain definition. Therefore, the Green-Lagrange
strain is frequently used.
An alternative form of E is obtained if we start from the following form of the deformation tensor F:
In this section we will consider the dependence of quantities on time.
Let us consider a scalar quantity a in a continuum, for example temperature, that depends on space and time. The variation of a throughout the continuum can be considered a function of the {\em material coordinates} ∼ξ of the material points:
The material time derivative[14] is the time derivative observed for a specific material point in the continuum. Since we can label a
point by its material coordinates or by its initial position, we get:
The spatial time derivative is often used in fluid mechanics, where we are interested in phenomena at points, fixed in the space.
Consider a material point in the undeformed reference configuration with a position vector that is given by x0. The actual position of that material point in the current configuration at time t is given by x, while at time t+Δt the point has moved to a new current position given by x+dx. The relation between the material and the spatial time derivative can be derived by:
The first term on the right hand side is called the convective time derivative[16]. Often the difference between the value of a quantity a and the functions α, A, and A by which this value can be calculated is neglected. Then, summarising, we can
write for the spatial time derivative:
Consider a material vector dx. The rate of change of this vector
dx˙, i.e. the change of the length and the orientation of the vector per unit of time, equals:
Thus we can split the tensor F˙⋅F−1 into a symmetric (spatial) rate-of-deformation tensor[18]D and a
skew-symmetric spin tensor[19] (or vorticity tensor) Ω,
according to:
We conclude that the part of the rate of change of a material vector dx, described by Ω, is oriented perpendicular to the material vector itself. The vector ω can be interpreted as the angular velocity vector[20], see Figure 1.15.
Since the rate-of-deformation tensor D is symmetric, its
eigenvalues νi are real and positive, and its eigenvectors ηi are mutually orthogonal, or can be chosen so. If we write D in its spectral form, we get:
showing that in this case application of D yields a rate of change of both the length and the orientation of the vector, see Figure 1.17.
Figure 1.17:Change of length and orientation of an arbitrary material vector, after application of D.
Using the rate-of-deformation tensor, we can calculate the rate of
change of the length of a material vector and the volume of a material
element. Let us consider a material vector dx0=∥dx0∥e0, that is transformed into a vector dx=∥dx∥e
in the deformed situation. We have found before that the stretchλ of the vector is given by:
Now let us consider three material vectors, that in the refererence
state were oriented along the orthogonal eigenvectors n0i of C. In the actual state, these material vectors are oriented along the directions ni, which are still orthogonal. Now we can choose these vectors as a basis, with respect to which we calculate the first invariant, or the trace, of the rate-of-deformation tensor D: