10.5 Motion and Deformation
of thin shells General theory

The figure illustrates the problem to
be solved. The solid of interest is a
shell with uniform thickness h. The shell’s thickness is assumed to be much
smaller than any relevant in-plane dimension.
The exterior surface of the shell is subjected to a prescribed distribution
of traction, while the edge of the shell may either be supported so as to
constrain its motion, or may be subjected to prescribed forces. Our objective is to calculate the internal
forces in the shell, and to compute its deformed shape.
10.5.1 Coordinate systems and variables characterizing deformation of shells
· To specify the position of a point on the mid-plane of the undeformed
shell, we introduce a convenient curvilinear
coordinate system (examples include cylindrical or spherical
polar coordinates). Note that need not necessarily be distances along the
surface: for example, for a cylindrical shell, we would use the axial distance z and the angle as the coordinate system.
· The position vector
of a material particle on the mid-section of the initial shell is denoted by
· To characterize the
orientation of an arbitrary point in the undeformed shell, we introduce three
basis vectors , with
.
Thus, are tangent to the coordinate lines in the undeformed shell, and is a unit vector perpendicular to the mid-section
of the shell. This basis is called the covariant
basis or natural basis for the coordinate system. Note that the basis vectors are not unit vectors, and are not, in general,
orthogonal.
·
Because are not orthogonal, it is convenient to
introduce a second set of basis vectors defined so that
where is the Kronecker delta symbol (the index i has been raised to match the indices
on the basis vectors), i.e. for i=j
and zero otherwise. This second triad of
vectors is called the contravariant basis or reciprocal
basis for the
coordinate system. The contravariant basis vectors can be constructed by
taking cross products of the covariant basis vectors, as follows
where . The reciprocal basis is shown in the figure.
· The position vector of an arbitrary point in the undeformed shell can be
expressed as , where is the perpendicular distance of the material
particle from the mid-section of the shell.
· After deformation, the mid-section of
the shell is deformed to another smooth surface. The point that
lies at on the mid-section of the undeformed shell
moves to a new position after deformation.
· To characterize the orientation of the deformed shell,
we introduce three basis vectors , with
.
Now, are tangent to the coordinate lines in the deformed shell, and is a unit vector perpendicular to the
mid-section of the deformed shell. We
can introduce a reciprocal basis in exactly the same way as for the undeformed
shell.
· A few special vectors and tensors, such as the angular
velocity of the shell, and the internal stress couple in the shell are most
conveniently expressed in terms of vectors or . Special symbols will not be introduced for
these vectors; they will always be written out as a cross product.
10.5.2 Vectors and tensor components in non-orthogonal bases: Covariant
and Contravariant components
In this section we introduce some
additional notation that helps deal with the complicated sets of basis vectors
that characterize the deformation of a shell.
· Vectors can be expressed as linear
combinations of some subset of the twelve possible basis vectors , , or . For example, we can write an arbitrary vector
a as
Here, the
coefficients are called the contravariant components of a
in , and are called the covariant components of a.
Note that the contravariant components are coefficients of the covariant
basis vectors, and vice-versa.. The
reason for this confusing terminology is given below. Note also that the components do not in
general have the same units as the vector, because the basis vectors may have
length dimensions.
· The various components of a can be expressed as
To see the first
result, take dot products of with and recall that . The
`contravariant’ and `covariant’ terms assigned to and refer to the fact that they represent projections
of the vector a onto the
contravariant and covariant basis vectors, respectively. The raised and lowered indices for vector
components follow the same convention: raised indices indicate contravariant
components, while lowered indices represent covariant components.
· Tensors can also be expressed as sums
of nine dyadic products of various combinations of basis vectors. For example, if S is a tensor we could write
or equivalent expressions in terms of
and/or . Here are called contravariant and covariant
components of S, respectively, while
are called mixed tensor components. The dot that appears before the indices in
the mixed tensors is introduced to identify whether the index should be
associated with the first or second basis vector in the dyadic product (the dot
appears before the index associated with the second basis vector). For symmetric tensors, the dot can be
dropped.
· The various components of S can be regarded as projections of the tensor onto the
contravariant or covariant basis vectors, as , with similar
results for the mixed components.
· Once again, it is important to note that the components do not have a convenient physical
interpretation. In general the
components do not even have the same units as the tensor itself, because the
basis vectors themselves have units.
· The various sets of components can be
related by defining the components of the fundamental tensor or metric
tensor g as follows
We can define in terms of and/or in the same way. With these definitions, we see that the covariant and
contravariant basis vectors are related by
· The metric tensor can be expressed as
the sum of three dyadic products , with a similar expression for .
From this expression we see that
g is therefore
its own inverse it is a representation of the identity tensor.
10.5.3 Additional Deformation Measures and Kinematic Relations
· An infinitesimal line element that lies in the mid-section of the undeformed
plate can be expressed in terms of infinitesimal changes in the coordinates as
The length ds of can be computed as
This expression is known as the first
fundamental form for the surface.
A similar expression can be constructed for the deformed surface.
· The variation of the normal vectors and with position in the mid-plane of the shell play
a particularly important role in describing the shape and deformation of the
shell, because they characterize its curvature and bending. To quantify this variation, let and be the vectors normal to the surface at
positions and in the undeformed shell, with a similar
notation for the deformed shell. We introduce symmetric curvature tensors and that satisfy
The curvatures and are called surface tensors, because
they transform like tensors under changes of surface coordinates.
· The curvature components can be
expressed in terms of their covariant, contravariant or mixed components. This can be used to deduce expressions such
as
· The curvature components can be
calculated from the position vector of the mid-plane of the shell, using any of
the following expressions
where . The mixed components follow as , where are the components of the metric tensor
defined in Sect 10.5.2.
· The magnitude of the curvature of a
shell is quantified by principal curvatures - these are simply the principal values of . The mean curvature , and Gaussian curvature are also used.
· We will also need to calculate the
variation of the remaining basis vectors with position in the surface. These are quantified by Christoffel symbols of the second
kind which satisfy
The Christoffel symbols are functions
of position on the surface, and can be related to the position vector of the
mid-plane of the shell and its curvature components as
· Some relationships between the time derivatives of these
various kinematic quantities are also needed in subsequent calculations. The rate of change in shape of the shell can
be characterized by the velocity of its middle surface . The velocity vector can be described as
components in any of the various bases: the representation is particularly useful.
· The time derivatives of the basis vectors are a convenient way to characterize the rate
of change of bending of the shell.
These are related to the velocity of the shell’s mid-plane by
· We will also need to calculate the time derivative of
the vector normal to the mid-plane of the shell . Since is a unit vector, its time derivative can be
quantified by an angular velocity vector , defined so that
The components of can be related to as
Recalling that , we see also that
Finally we may write
this as
The components can also be regarded as the components of the angular
velocity vector in a basis in the sense that
· The time derivative of the curvature tensor , is related to by
Note that
The components of
the time derivative of curvature can therefore be expressed in terms of as
It is important to
note that are not equal to the time derivatives of the
curvature components.
· We will also need to characterize the linear and angular
acceleration of the shell. The linear
acceleration can be quantified by the acceleration of the mid-plane .
· The angular acceleration of the shell can be
characterized by the angular acceleration of the normal to its mid-plane, . The angular acceleration can be related to
the acceleration of the mid-plane of the shell as follows
where we have used and noted that to obtain the final result.
· It is convenient to express in the form , where and the can be related to the velocity and
acceleration of the mid-plane of the shell as follows
· These results show that
where we have used and noted to obtain the second line.
HEALTH
WARNING: The sign convention used to characterize the curvature of a shell
can be confusing. In the convention used
here, a convex surface has positive
curvature. For example, a spherical shell with coordinate system chosen so
that points radially out of the sphere would have
two equal positive principal curvatures. The mathematical analysis of curved
surfaces usually uses the opposite sign convention for curvature, and a few
texts on shell theory use curvature measures with the opposite sign to the one
used here.
10.5.4 Approximating the displacement and velocity field
The position vector of a material
point in the shell before deformation can be expressed as , where is the distance of the material particle from
the mid-section of the shell.
After deformation of the material
point that has coordinates in the undeformed shell moves to a new
position, which can be expressed as
where . This is a completely general
expression. We now introduce a series
of approximations that are based on the assumptions that
1.The shell is thin compared with its
in-plane dimensions;
2.The principal radii of curvature of
the shell (both before and after deformation) are much larger than the
characteristic dimension of its cross section;
With this in mind, we assume that can be approximated by
a function of the form
where can be regarded as the first term in a Taylor
expansion of with respect to .
Note that represents transverse shear deformation of the
shell, while quantifies the through-thickness stretching.
Several versions of plate theory
exist, which use different approximations for the shear deformation. Here, we will present only the simplest approach,
known as Kirchhoff shell theory, which is to assume that .
This implies that material fibers that are perpendicular to the
mid-plane of the shell remain perpendicular to the mid-plane of the deformed
shell, and the shell does not change its thickness, as shown in the figure. This
reduces the displacement field to
The velocity field can be approximated as
while the acceleration is
where and denote the angular acceleration and angular
velocity of the unit vector normal to the mid-plane of the plate.
HEALTH WARNING:
In addition to using this approximation to the displacement and velocity field,
Kirchhoff shell theory assumes that the transverse stress vanishes in the shell. Strictly speaking, this is inconsistent with
the deformation. A more rigorous
approach would be to introduce a uniform transverse strain , which could be calculated as part of the
solution. However, this approach yields
results that are essentially indistinguishable from the plane-stress
approximation.
10.5.5 Approximating the deformation gradient
The deformation gradient can be approximated as
where and are the metric tensors for shell before and
after deformation, and and are the curvature tensors for the mid-surface
of the shell before and after deformation, respectively. The three terms in the second formula for F can be interpreted as (i) the effects
of in-plane stretching of the shell; (ii) the effects of bending; and (iii) the
effects of a change in the shell’s thickness.
Derivation By definition, the deformation
gradient relates infinitesimal line elements in the shell before and after deformation by .
We wish to construct a tensor with these properties.
1. An infinitesimal line element in the
deformed shell can be expressed in terms of a small change in coordinates
where we have used
2. This expression can be rearranged
into the form
3. An infinitesimal line element dx
in the undeformed shell can also be related to as
This can be re-written as
so that
4. Finally, note that
We can substitute this result into
(2) above to see that
and the deformation gradient can be
read off as the coefficient of dx.
5. The approximate expression for F is obtained by assuming that for a
thin shell
To see this, multiply out , recall that and neglect the term of order . Finally, substitute this
approximation into the formula for F, multiply
out the terms and neglect terms to obtain the approximation for F.
10.5.6 Other deformation measures.
It is straightforward to calculate
any other deformation of interest from the deformation gradient. A few examples that will be used in
calculations to follow are listed below.
The inverse of the deformation
gradient can be approximated by
The velocity gradient tensor , which relates the relative velocity
of two material particles at positions and in the deformed shell as can be approximated by
where are the covariant components of the time
derivative of the surface curvature tensor.
The Lagrange strain tensor can be approximated by
where terms of order have been neglected, we have used and .
When we write constitutive equations relating forces to
deformations, it is convenient to introduce two new strain measures defined as
follows:
1. The `mid-plane Lagrange strain
tensor’
,
where and .
The tensor quantifies length changes of infinitesimal material elements
in the mid-plane of the shell, in the sense that the lengths and of a line element before and after deformation
are related by
2. The `Curvature change tensor’ , which quantifies the additional
stretch induced by bending and twisting the shell.
10.5.7 Representation of forces and moments in shells
The figure shows a generic cross-section of the shell, in the deformed
configuration. To define measures of internal and external forces acting on the
shell, we define the following variables
· A basis with vectors chosen following the scheme
described in 10.5.1. Vector and tensor
quantities will be quantified by their contravariant components in this basis
· The body force acting on the plate , or in component
form
· The tractions acting on the exterior
surface of the shell .
It is convenient to define separate variables to characterize the
tractions acting on the various parts of the shell, as indicated in the sketch:
the upper surface of the shell (denoted by ) is subjected to traction ; the lower surface is subjected to , while the surface around the edge
of the shell is subjected to
· The Cauchy stress within the shell .
External forces and moments acting on the shell
are characterized by
1. The external force per unit area
acting on the shell, .
The force components can be calculated from the tractions and body force
acting on the shell as
2. The external moment per unit area acting on the shell. It is most convenient to express the external
moment as where the components can be calculated from the tractions and body
force as
The vector q is work conjugate to the angular velocity of the normal to the mid-plane of the shell,
in the sense that is the rate of work done by the external
couple per unit area of the shell’s mid-plane.
3. The resultant force per unit length
acting on the external edge of the shell.
The force per unit length can be expressed as components as .
The components are related to the tractions acting on the external
surface at the edge of the shell by
4. The resultant moment per unit length
acting on the external edge of the shell.
The moment per unit length can be expressed as components as .
The components are related to the tractions acting on external surface
at the edge of the shell
Internal forces and moments within the shell are
characterized by three surface tensors , and , To visualize their physical significance,
suppose that the shell is cut through so as to expose an internal surface,
which lies perpendicular to the mid-plane of the shell, as shown in the figure.
Let denote a unit vector normal to the internal surface,
and let ds denote an infinitesimal
line element that lies in the both the exposed surface and the mid-plane of the
shell. The exposed surface is subjected
to a distribution of traction, so that an small element of area with dimensions
is subjected to a resultant force and resultant moment . These forces and moments are related to , and as outlined below:
1. The in-plane stress
resultant tensor quantifies internal forces that tend to
stretch and shear the shell in its own plane.
It is related to the internal tractions by , and its components
can be calculated from the stress distribution in the shell as
2. The transverse shearing stress tensor quantifies internal forces that act to impose
the constraint that material fibers that are perpendicular to the mid-plane of
the shell before deformation remain perpendicular to the mid-plane after
deformation. Strictly speaking, in
Kirchoff shell theory it is a Lagrange multiplier, but can be regarded as
quantifying the transverse shear force . Its value cannot be computed from the
deformation of the shell, because the transverse shearing has been neglected:
instead, it must be determined by solving the equilibrium equations given in
the next section.
3. The internal moment tensor characterizes internal bending and twisting
moments in the shell. It is related to
the moment acting on internal through-thickness sections of the shell by . The components can be calculated from the internal stresses
in the shell as
The tensor is work conjugate to the gradient of the
angular velocity of the normal to the mid-plane of the shell , or alternatively, to the rate of
change of curvature in the sense that
is the rate of work done by M per unit area of the mid-plane of the
shell.
10.5.8 Equations of motion and boundary conditions
We consider a shell with thickness h and mass density . The internal forces and moments
must satisfy
The operator represents the surface divergence, T, V
and M are the internal forces
defined in Sect 10.5.7; p and q are the external force and couple per
unit area acting on the shell, a is
the acceleration of the mid-plane and is the angular acceleration of the unit vector
normal to the mid-plane of the shell. The
two equations can be interpreted as linear and angular momentum balance for an
infinitesimal element of the shell. Note
that:
1. If the system is in static
equilibrium, the right hand sides of all the equations of motion are zero.
2. In addition, in many dynamic
problems, the right hand sides of the angular momentum balance equations may be
taken to be approximately zero. For
example, the rotational inertia may be ignored when modeling the vibration of a
shell. The rotational inertia terms can
be important if the shell is rotating rapidly: for example, they would
influence the out-of-plane vibration of a spinning disk.
The equations of motion can also be expressed in terms of
components of the various force and moment tensors by substituting , , , , and and recalling that
The result is
The last equation shows that the
stress resultant and moment tensors are not symmetric. The asymmetry is small, and is ignored in
simplified versions of shell theory.
However, there are a few special shell geometries (a cylindrical shell
subjected to torsional loading is one example) where neglecting the asymmetry
can lead to substantial errors.
Edge boundary conditions for a shell are complicated and
confusing. To understand them, it is
helpful to visualize the possible types of motion that can occur at the edge of
a shell. The edge of the shell is
characterized by a curve C that lies
in the mid-plane of the shell, encircling in a counterclockwise sense. We let denote arc-length measured around C from some convenient origin, and use and denote unit vectors tangent and normal to C, as shown in the figure. Elements of the shell that lie on C have four independent degrees of
freedom, as follows:
1. The material element can have an
arbitrary velocity, with three components
2. The material element can rotate about
the tangent vector . To visualize this motion, imagine
that the shell is supported around C by
a hinge.
The motion of the edge of the shell
can be prescribed by constraining one or more of these degrees of freedom. Alternatively, the edge of the shell can be
subjected to one or more of four generalized forces, which are
work-conjugate to these degrees of freedom.
The generalized forces can be expressed in terms of the forces and couples acting on the edge of the shell as
1. is work-conjugate to the in-plane displacement
of the shell
2. is work-conjugate to the out-of-plane
displacement of the edge of the shell
3. is work-conjugate to the rotation of the shell
about its edge.
The four boundary conditions can be
expressed in terms of these forces as follows:
Derivation:
Measures of internal force, the equilibrium equations, and the boundary
conditions emerge naturally from the principle of virtual work. The principle of virtual work states that,
for any deformable solid that is in static equilibrium, the Cauchy stress
distribution must satisfy
for all virtual velocity fields and compatible velocity gradients .
The virtual velocity field in the shell must have the same general form
as the actual velocity, as outlined in Section 10.2.4. The virtual velocity can therefore be
characterized by the virtual velocity of the mid-plane of the shell .
It is convenient to introduce the time derivative of the normal vector
to the plate’s mid-plane as an additional kinematic variable, which
must of course be compatible with .
We will show the following:
· The virtual work principle can be
expressed in terms of the generalized deformation measures and forces defined
in the preceding sections as
· If the virtual work equation is satisfied
for all and compatible , then the internal forces and
moments must satisfy the following equilibrium equations
as well as the boundary conditions
listed above.
· The last equilibrium
equation does not emerge from the virtual work
principle. Instead, this equation is a consequence of the symmety of the Cauchy
stress tensor , as shown below. It
is automatically satisfied if the components
and are calculated by integrating the stresses
through the thickness of the shell.
However, for some statically
determinate shell problems it is possible to avoid evaluating these integrals
explicitly, in which case the equilibrium equation is useful.
Expressing the virtual work equation in terms of generalized
force measures is a straightforward but lengthy algebraic exercise.
1. When applying the virtual work
principle, we will need to integrate over the volume of the shell. It is convenient to write the volume integral
as separate integrals over the mid-plane of the shell and through its
thickness, as follows
Recall that , so that
Therefore
where the term of order has been neglected. Substituting this result into the volume
integral yields
where the area integral is understood
to be taken over the mid-plane of the shell.
2. Similarly, the integrals over the
outer surface of the shell can be separated into integrals taken over the upper
and lower surfaces of the shell ( and ), together with an integral over the surface
at the edge of the shell , as follows
Following the procedure in step (1),
the integrals over and can be expressed in terms of integrals taken
over the mid-plane of the shell as
The integral over can be reduced to a line integral taken around
the curve(s) bounding the edge of the shell, as
The procedure to derive this result
is very similar to the steps required to simplify the volume integral and is
left as an exercise.
3. Next, consider the integrand
To reduce this to a scalar
combination of the components of the various tensors and vectors, substitute , together with the kinematic
formulas:
with the result
4. Substituting this result into the
first integral of the virtual work principle, reducing the volume integral to
an integral over the mid-plane of the shell, and using the definitions of and gives
5. Similar manipulations can be used to
reduce the remaining terms in the virtual work principle to
Substituting the equations in (4) and
(5) into the virtual work equation gives the first result.
Next, we show that the equilibrium equations and boundary
conditions follow from the virtual work principle.
1. The virtual work equation must first
be augmented by a Lagrange multiplier to enforce compatibility between the
velocity field and the time derivative of the vector normal
to the shell’s mid plane .
To this end, we regard the unit vector as an independent degree of freedom, and
introduce a vector valued Lagrange multiplier which must satisfy
for all admissible variations , and .
The second integral can simply be added to the virtual work equation to
ensure compatibility of and
2. The augmented virtual work equation
now reads
3. The remaining steps are routine, but
fiddly. The partial derivatives of and must be removed by integrating by parts. This is accomplished by applying the surface
divergence theorem, which states that if is a differentiable vector field on an area A of the surface, and C is the curve bounding A, then
where is the outward normal to C. To see how to use this
theorem, consider
The integrand can be re-written as
Applying the surface divergence
theorem to the first term on the right hand side of this equation shows that
Finally, substituting and and remembering to differentiate the basis
vectors gives the component form
4. Applying the procedure outlined in
step (3) to similar terms, the virtual work equation can be re-written as
This equation must be satisfied for
all and , which immediately gives the
equilibrium equations.
5. Some further algebra is required to
derive the boundary conditions. It is tempting to conclude that coefficients of
and in the boundary terms must all vanish, but
this is not the case, because and are related by compatibility equations. The
boundary terms must be expressed in terms of four independent degrees of
freedom. To this end, recall that , so the integral around the boundary
can be re-written as
6. The vector can be expressed in terms of components
parallel and perpendicular to the boundary of the plate C, as
Here, and represent unit vectors tangent and normal to C, and is an independent degree of freedom that
represents the rotation of the shell about .
Finally, we integrate by parts to see that
(The terms associated with the ends
of C vanish because C is a closed curve).
7. Substituting the result of (6) back
into (5) gives
This condition must be satisfied for
all , which gives the boundary conditions.
Finally, we must derive the last equilibrium equation .
Using the definitions of , and noting that , it is straightforward to show that
Adding these two equations gives the last equilibrium
equation.
10.5.9 Constitutive equations relating forces to deformation measures in elastic
shells
The internal forces in a shell are
related to its deformation by the stress-strain law for the material. Here, we give force-deformation equations for
an isotropic elastic shell which experiences small shape changes (but possibly
large rotations).
Shape changes are characterized using the following
deformation measures, defined in Sections 10.5.6
1. The in-plane components of the metric
tensors for the mid-plane of the shell before and after deformation are denoted
2. The `mid-plane Lagrange strain
tensor’ ,
3. The `Curvature change tensor’ , which quantifies the bending and
twisting the shell.
Internal forces are characterized using the stress resultant
tensor components and internal moment components defined in Section 10.5.7.
The shell is assumed to have a
uniform thickness h, and is assumed
to be made from an isotropic, linear elastic solid, with Young’s modulus E and Poisson’s ratio .
We assume for simplicity that the shell is homogeneous, and neglect
thermal expansion (the effects of thermal expansion are included an example
problem solved in Section 10.7.4)
It is convenient to introduce a plane
stress elasticity tensor with components
The force-deformation relations can then be expressed as
For all but a few very rare shell geometries these
expressions may be approximated by
Derivation
1. We have assumed that the material in
the shell experiences small distortions, but arbitrary rotations. Material behavior can therefore be modeled
using the generalized Hooke’s law described in Section 3.3, which relates the
Material stress to the Lagrange strain using the isotropic linear elastic
constitutive equations.
2. We assume that the shell is in a
state of plane stress, so that the material stress tensor has the form
3. The Lagrange strain tensor is given in Section 10.5.6 as
4. The material stress is related to the
Lagrange strain by the plane stress version of the linear elastic constitutive
equations, which can be expressed as
where is the
in-plane component of the metric tensor associated with the undeformed shell
(this replaces the identity tensor in the Cartesian version of the constitutive
equations)
5. The Cauchy stress is related to the
material stress by .
Substituting the formulas for from (4) and approximating F as , we find after some algebra that
where
6. The components of the stress-resultant
tensor are given by
Substituting the
formula for stress components into this expression and integrating through the
thickness of the shell gives
Here, terms of order
have been neglected.
7. The components of
the internal moment tensor are
Substituting the
formula for stress components into this expression and integrating through the
thickness of the shell gives
where terms of order
and higher have been neglected.
10.5.10 Strain energy and kinetic energy of an elastic shell
It is useful to express the strain energy and
kinetic energy of a deformed shell in terms of the motion and deformation of
its mid-plane. To this end:
1. Consider an isotropic, linear elastic shell,
with Young’s modulus E, Poission’s ratio , mass density and thickness h. Denote the contravariant
components of the tensor of elastic constants by
2. Let and denote the covariant components of the
mid-plane Lagrange strain tensor, defined in the preceding section,
3. Let and denote the linear and angular velocity of the
mid-plane of the shell.
The total strain energy of the shell can be
calculated as
For all but a very few special shell
geometries this result may be approximated by
The kinetic energy can be calculated using the formula
The second term in the expression for
the kinetic energy represents the rotational energy. In many practical
problems, such as vibration of a shell, the rotational energy can be neglected.
Derivation: The
strain energy density in the shell is given by , where is the material stress tensor and E is the Lagrange strain tensor,
defined in the preceding section. The
stress can be expressed in terms of the strain using the constitutive equation,
while the strain can be expressed in terms of and using step (3) in Section 10.5.8. Integrating over the volume of material in
the shell, and evaluating the integral through the shell’s thickness explicitly
gives the result stated. The kinetic
energy is calculated using the formula for the velocity field in 10.5.8.