The Flamant solution provides expressions for the
stresses and
displacements in a
linear elastic wedge
A wedge is a triangular shaped tool, and is a portable inclined plane, and one of the six simple machines. It can be used to separate two objects or portions of an object, lift up an object, or hold an object in place. It functions by converti ...
loaded by point forces at its sharp end. This solution was developed by A. Flamant in 1892 by modifying the three-dimensional solution of
Boussinesq.
The stresses predicted by the Flamant solution are (in
polar coordinates
In mathematics, the polar coordinate system is a two-dimensional coordinate system in which each point on a plane is determined by a distance from a reference point and an angle from a reference direction. The reference point (analogous to th ...
)
:
where
are constants that are determined from the boundary conditions and the geometry of the wedge (i.e., the angles
) and satisfy
:
where
are the applied forces.
The wedge problem is ''
self-similar'' and has no inherent length scale. Also, all quantities can be expressed in the separated-variable form
. The stresses vary as
.
Forces acting on a half-plane
For the special case where
,
, the wedge is converted into a half-plane with a normal force and a tangential force. In that case
:
Therefore, the stresses are
:
and the displacements are (using
Michell's solution)
:
The
dependence of the displacements implies that the displacement grows the further one moves from the point of application of the force (and is unbounded at infinity). This feature of the Flamant solution is confusing and appears unphysical. For a discussion of the issue se
http://imechanica.org/node/319
Displacements at the surface of the half-plane
The displacements in the
directions at the surface of the half-plane are given by
:
where
:
is the
Poisson's ratio
In materials science and solid mechanics, Poisson's ratio \nu ( nu) is a measure of the Poisson effect, the deformation (expansion or contraction) of a material in directions perpendicular to the specific direction of loading. The value of Po ...
,
is the
shear modulus
In materials science, shear modulus or modulus of rigidity, denoted by ''G'', or sometimes ''S'' or ''μ'', is a measure of the elastic shear stiffness of a material and is defined as the ratio of shear stress to the shear strain:
:G \ \stackre ...
, and
:
Derivation of Flamant solution
If we assume the stresses to vary as
, we can pick terms containing
in the stresses from
Michell's solution. Then the
Airy stress function In linear elasticity, the equations describing the deformation of an elastic body subject only to surface forces (or body forces that could be expressed as potentials) on the boundary are (using index notation) the equilibrium equation:
:\sigma_=0\ ...
can be expressed as
:
Therefore, from the tables in
Michell's solution, we have
:
The constants
can then, in principle, be determined from the wedge geometry and the applied
boundary conditions.
However, the concentrated loads at the vertex are difficult to express in terms of
traction boundary conditions because
# the unit outward normal at the vertex is undefined
# the forces are applied at a point (which has zero area) and hence the traction at that point is infinite.
To get around this problem, we consider a bounded region of the wedge and consider equilibrium of the bounded wedge.
[J. R. Barber, 2002, ''Elasticity: 2nd Edition'', Kluwer Academic Publishers.] Let the bounded wedge have two traction free surfaces and a third surface in the form of an arc of a circle with radius
. Along the arc of the circle, the unit outward normal is
where the basis vectors are
. The tractions on the arc are
:
Next, we examine the force and moment equilibrium in the bounded wedge and get
:
We require that these equations be satisfied for all values of
and thereby satisfy the
boundary conditions.
The traction-free
boundary conditions on the edges
and
also imply that
:
except at the point
.
If we assume that
everywhere, then the traction-free conditions and the moment equilibrium equation are satisfied and we are left with
:
and
along
except at the point
. But the field
everywhere also satisfies the force equilibrium equations. Hence this must be the solution. Also, the assumption
implies that
.
Therefore,
:
To find a particular solution for
we have to plug in the expression for
into the force equilibrium equations to get a system of two equations which have to be solved for
:
:
Forces acting on a half-plane
If we take
and
, the problem is converted into one where a normal force
and a tangential force
act on a half-plane. In that case, the force equilibrium equations take the form
:
Therefore
:
The stresses for this situation are
:
Using the displacement tables from the
Michell solution The Michell solution is a general solution to the elasticity equations in polar coordinates ( r, \theta \,) developed by J. H. Michell. The solution is such that the stress components are in the form of a Fourier series in \theta \, .
Michell ...
, the displacements for this case are given by
:
Displacements at the surface of the half-plane
To find expressions for the displacements at the surface of the half plane, we first find the displacements for positive
(
) and negative
(
) keeping in mind that
along these locations.
For
we have
:
For
we have
:
We can make the displacements symmetric around the point of application of the force by adding rigid body displacements (which does not affect the stresses)
:
and removing the redundant rigid body displacements
:
Then the displacements at the surface can be combined and take the form
:
where
:
References
See also
*
Michell solution The Michell solution is a general solution to the elasticity equations in polar coordinates ( r, \theta \,) developed by J. H. Michell. The solution is such that the stress components are in the form of a Fourier series in \theta \, .
Michell ...
*
Linear elasticity
Linear elasticity is a mathematical model of how solid objects deform and become internally stressed due to prescribed loading conditions. It is a simplification of the more general nonlinear theory of elasticity and a branch of continuum mec ...
*
Stress (physics)
Elasticity (physics)