Flamant solution
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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 ...
) : \begin \sigma_ & = \frac + \frac \\ \sigma_ & = 0 \\ \sigma_ & = 0 \end where C_1, C_3 are constants that are determined from the boundary conditions and the geometry of the wedge (i.e., the angles \alpha,\beta) and satisfy : \begin F_1 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)\,\cos\theta\, d\theta = 0 \\ F_2 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)\,\sin\theta\, d\theta = 0 \end where F_1,F_2 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 \sigma = f(r)g(\theta). The stresses vary as (1/r).


Forces acting on a half-plane

For the special case where \alpha = -\pi, \beta = 0, the wedge is converted into a half-plane with a normal force and a tangential force. In that case : C_1 = - \frac,\quad C_3 = -\frac Therefore, the stresses are : \begin \sigma_ & = -\frac (F_1\cos\theta + F_2\sin\theta) \\ \sigma_ & = 0 \\ \sigma_ & = 0 \end and the displacements are (using Michell's solution) : \begin u_r & = -\cfrac\left _1\ + \right. \\ & \qquad \qquad \left. F_2\\right\ u_\theta & = -\cfrac\left _1\ - \right. \\ & \qquad \qquad \left. F_2\\right \end The \ln r 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 x_1, x_2 directions at the surface of the half-plane are given by :\begin u_1 & = \frac + \frac \\ u_2 & = \frac + \frac \end where : \kappa = \begin 3 - 4\nu & \qquad \text \\ \cfrac & \qquad \text \end \nu 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 ...
, \mu 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 : \text(x) = \begin +1 & x > 0 \\ -1 & x < 0 \end


Derivation of Flamant solution

If we assume the stresses to vary as (1/r), we can pick terms containing 1/r 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 : \varphi = C_1 r \theta\sin\theta + C_2 r\ln r \cos\theta + C_3 r \theta\cos\theta + C_4 r\ln r \sin\theta Therefore, from the tables in Michell's solution, we have :\begin \sigma_ & = C_1\left(\frac\right) + C_2\left(\frac\right) + C_3\left(\frac\right) + C_4\left(\frac\right) \\ \sigma_ & = C_2\left(\frac\right) + C_4\left(\frac\right) \\ \sigma_ & = C_2\left(\frac\right) + C_4\left(\frac\right) \end The constants C_1, C_2, C_3, C_4 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 a\,. Along the arc of the circle, the unit outward normal is \mathbf = \mathbf_r where the basis vectors are (\mathbf_r, \mathbf_\theta). The tractions on the arc are : \mathbf = \boldsymbol\cdot\mathbf \quad \implies t_r = \sigma_, ~ t_\theta = \sigma_ ~. Next, we examine the force and moment equilibrium in the bounded wedge and get : \begin \sum f_1 & = F_1 + \int_^ \left sigma_(a,\theta)~\cos\theta - \sigma_(a,\theta)~\sin\theta\righta~d\theta = 0 \\ \sum f_2 & = F_2 + \int_^ \left sigma_(a,\theta)~\sin\theta + \sigma_(a,\theta)~\cos\theta\righta~d\theta = 0 \\ \sum m_3 & = \int_^ \left ~\sigma_(a,\theta)\righta~d\theta = 0 \end We require that these equations be satisfied for all values of a\, and thereby satisfy the boundary conditions. The traction-free boundary conditions on the edges \theta=\alpha and \theta=\beta also imply that : \sigma_ = \sigma_ = 0 \qquad \text~~\theta=\alpha, \theta=\beta except at the point r = 0. If we assume that \sigma_=0 everywhere, then the traction-free conditions and the moment equilibrium equation are satisfied and we are left with : \begin F_1 & + \int_^ \sigma_(a,\theta)~a~\cos\theta ~d\theta = 0 \\ F_2 & + \int_^ \sigma_(a,\theta)~a~\sin\theta ~d\theta = 0 \end and \sigma_ = 0 along \theta=\alpha, \theta=\beta except at the point r = 0. But the field \sigma_ = 0 everywhere also satisfies the force equilibrium equations. Hence this must be the solution. Also, the assumption \sigma_=0 implies that C_2 = C_4 = 0. Therefore, : \sigma_ = \frac + \frac ~;~~ \sigma_ = 0 ~;~~ \sigma_ = 0 To find a particular solution for \sigma_ we have to plug in the expression for \sigma_ into the force equilibrium equations to get a system of two equations which have to be solved for C_1, C_3: : \begin F_1 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)~\cos\theta~ d\theta = 0 \\ F_2 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)~\sin\theta~ d\theta = 0 \end


Forces acting on a half-plane

If we take \alpha = -\pi and \beta = 0, the problem is converted into one where a normal force F_2 and a tangential force F_1 act on a half-plane. In that case, the force equilibrium equations take the form : \begin F_1 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)~\cos\theta~ d\theta = 0 \qquad \implies F_1 + C_1\pi = 0\\ F_2 & + 2\int_^ (C_1\cos\theta + C_3\sin\theta)~\sin\theta~ d\theta = 0 \qquad \implies F_2 + C_3\pi = 0 \end Therefore : C_1 = - \cfrac ~;~~ C_3 = - \cfrac ~. The stresses for this situation are : \sigma_ = -\frac(F_1\cos\theta + F_2\sin\theta) ~;~~ \sigma_ = 0 ~;~~ \sigma_ = 0 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 : \begin u_r & = -\cfrac\left _1\ + \right. \\ & \qquad \qquad \left. F_2\\right\ u_\theta & = -\cfrac\left _1\ - \right. \\ & \qquad \qquad \left. F_2\\right \end


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 x_1 (\theta=0) and negative x_1 (\theta = \pi) keeping in mind that r = , x_1, along these locations. For \theta=0 we have : \begin u_r = u_1 & = \cfrac\left x_1, \right\\ u_\theta = u_2 & = \cfrac\left x_1, \right \end For \theta = \pi we have : \begin u_r = -u_1 & = -\cfrac\left x_1, \right+ \cfrac(\kappa-1)\\ u_\theta = -u_2 & = \cfrac(\kappa-1) - \cfrac\left x_1, \right \end 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) : u_1 = \cfrac(\kappa-1) ~;~~ u_2 = \cfrac(\kappa-1) and removing the redundant rigid body displacements : u_1 = \cfrac ~;~~ u_2 = \cfrac ~. Then the displacements at the surface can be combined and take the form : \begin u_1 & = \cfrac(\kappa+1)\ln , x_1, + \cfrac(\kappa-1)\text(x_1) \\ u_2 & = \cfrac(\kappa+1)\ln , x_1, +\cfrac(\kappa-1)\text(x_1) \end where : \text(x) = \begin +1 & x > 0 \\ -1 & x < 0 \end{cases}


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)