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[[Image:Plaque mince deplacement element matiere.svg|thumb | 250px | Deformation of a thin plate highlighting the displacement, the mid-surface (red) and the normal to the mid-surface (blue)]]
The '''Kirchhoff–Love theory of plates''' is a two-dimensional [[mathematical model]] that is used to determine the [[stress (mechanics)|stress]]es and [[deformation (mechanics)|deformation]]s in thin [[plate]]s subjected to [[force]]s and [[Moment (physics)|moment]]s. This theory is an extension of [[beam theory|Euler-Bernoulli beam theory]] and was developed in 1888 by [[Augustus Edward Hough Love|Love]]<ref>A. E. H. Love, ''On the small free vibrations and deformations of elastic shells'', Philosophical trans. of the Royal Society (London), 1888, Vol. série A, N° 17 p. 491–549.</ref> using assumptions proposed by [[Gustav Kirchhoff|Kirchhoff]]. The theory assumes that a mid-surface plane can be used to represent a three-dimensional plate in two-dimensional form.
 
The following kinematic assumptions that are made in this theory:<ref name=Reddy>Reddy, J. N., 2007, '''Theory and analysis of elastic plates and shells''', CRC Press, Taylor and Francis.</ref>
* straight lines normal to the mid-surface remain straight after deformation
* straight lines normal to the mid-surface remain normal to the mid-surface after deformation
* the thickness of the plate does not change during a deformation.
 
== Assumed displacement field ==
Let the [[position vector]] of a point in the undeformed plate be <math>\mathbf{x}</math>.  Then
:<math>
  \mathbf{x} = x_1\boldsymbol{e}_1+x_2\boldsymbol{e}_2+x_3\boldsymbol{e}_3 \equiv x_i\boldsymbol{e}_i\,.
</math> 
The vectors <math>\boldsymbol{e}_i</math> form a [[Cartesian coordinate system|Cartesian]] [[Basis (linear algebra)|basis]] with origin on the mid-surface of the plate, <math>x_1</math> and <math>x_2</math> are the Cartesian coordinates on the mid-surface of the undeformed plate, and <math>x_3</math> is the coordinate for the thickness direction.
 
Let the [[displacement (vector)|displacement]] of a point in the plate be <math>\mathbf{u}(\mathbf{x})</math>.  Then
:<math>
  \mathbf{u} = u_1\boldsymbol{e}_1+u_2\boldsymbol{e}_2+u_3\boldsymbol{e}_3 \equiv u_i\boldsymbol{e}_i
</math>
This displacement can be decomposed into a vector sum of the mid-surface displacement and an out-of-plane displacement <math>w^0</math> in the <math>x_3</math> direction.  We can write the in-plane displacement of the mid-surface as
:<math>
  \mathbf{u}^0 = u^0_1\boldsymbol{e}_1+u^0_2\boldsymbol{e}_2 \equiv u^0_\alpha\boldsymbol{e}_\alpha
</math>
Note that the index <math>\alpha</math> takes the values 1 and 2 but not 3.
 
Then the Kirchhoff hypothesis implies that
<blockquote style="border: 1px solid black; padding:10px; width:500px">
:<math>
  \begin{align}
    u_\alpha(\mathbf{x}) & = u^0_\alpha(x_1,x_2) - x_3~\frac{\partial w^0}{\partial x_\alpha}
        \equiv u^0_\alpha - x_3~w^0_{,\alpha} ~;~~\alpha=1,2 \\
    u_3(\mathbf{x}) & = w^0(x_1, x_2)
  \end{align}
</math>
</blockquote>
If <math>\varphi_\alpha</math> are the angles of rotation of the [[normal]] to the mid-surface, then in the Kirchhoff-Love theory
:<math>
  \varphi_\alpha = w^0_{,\alpha}
</math>
Note that we can think of the expression for <math>u_\alpha</math> as the first order [[Taylor series]] expansion of the displacement around the mid-surface.
{|
|[[Image:Plaque mince deplacement rotation fibre neutre new.svg|thumb|600px|Displacement of the mid-surface (left) and of a normal (right)]]
|}
 
== Quasistatic Kirchhoff-Love plates ==
The original theory developed by Love was valid for infinitesimal strains and rotations.  The theory was extended by [[Theodore von Kármán|von Kármán]] to situations where moderate rotations could be expected.
 
===Strain-displacement relations===
For the situation where the strains in the plate are infinitesimal and the rotations of the mid-surface normals are less than 10° the [[infinitesimal strain theory|strain-displacement]] relations are {{clarify|reason=\beta not defined|date=September 2012}}
:<math>
  \begin{align}
    \varepsilon_{\alpha\beta} & = \frac{1}{2}\left(\frac{\partial u_\alpha}{\partial x_\beta} +
      \frac{\partial u_\beta}{\partial x_\alpha}\right) \equiv \frac{1}{2}(u_{\alpha,\beta}+u_{\beta,\alpha})\\
    \varepsilon_{\alpha 3} & = \frac{1}{2}\left(\frac{\partial u_\alpha}{\partial x_3} +
      \frac{\partial u_3}{\partial x_\alpha}\right) \equiv \frac{1}{2}(u_{\alpha,3}+u_{3,\alpha})\\
    \varepsilon_{33} & = \frac{\partial u_3}{\partial x_3} \equiv u_{3,3}
  \end{align}
</math>
Using the kinematic assumptions we have
<blockquote style="border: 1px solid black; padding:10px; width:300px">
:<math>
  \begin{align}
    \varepsilon_{\alpha\beta} & = \tfrac{1}{2}(u^0_{\alpha,\beta}+u^0_{\beta,\alpha})
      - x_3~w^0_{,\alpha\beta} \\
    \varepsilon_{\alpha 3} & = - w^0_{,\alpha} + w^0_{,\alpha} = 0 \\
    \varepsilon_{33} & = 0
  \end{align}
</math>
</blockquote>
Therefore the only non-zero strains are in the in-plane directions.
 
===Equilibrium equations===
The equilibrium equations for the plate can be derived from the [[principle of virtual work]]. For a thin plate under a quasistatic transverse load <math>q(x)</math> these equations are
:<math>
  \begin{align} 
      &\cfrac{\partial N_{11}}{\partial x_1} + \cfrac{\partial N_{21}}{\partial x_2} = 0 \\
      &\cfrac{\partial N_{12}}{\partial x_1} + \cfrac{\partial N_{22}}{\partial x_2} = 0\\
      &\cfrac{\partial^2 M_{11}}{\partial x_1^2} + 2\cfrac{\partial^2 M_{12}}{\partial x_1 \partial x_2} +
      \cfrac{\partial^2 M_{22}}{\partial x_2^2} = q
  \end{align}
</math>
where the thickness of the plate is <math>2h</math>.  In index notation,
<blockquote style="border: 1px solid black; padding:10px; width:450px">
:<math>
  \begin{align}
    N_{\alpha\beta,\alpha} & = 0 \quad  \quad N_{\alpha\beta} := \int_{-h}^h \sigma_{\alpha\beta}~dx_3 \\
    M_{\alpha\beta,\alpha\beta} - q & = 0 \quad  \quad M_{\alpha\beta} := \int_{-h}^h x_3~\sigma_{\alpha\beta}~dx_3
  \end{align}
</math>
</blockquote>
where <math>\sigma_{\alpha\beta}</math> are the [[stress (physics)|stress]]es.
 
{| border="0"
|-
| valign="bottom"|
[[Image:Plaque moment flechissant contrainte new.svg|thumb|300px|none|Bending moments and normal stresses]]
| valign="bottom"|
[[Image:Plaque moment torsion contrainte new.svg|thumb|300px|none|Torques and shear stresses]]
|-
|}
:{| class="toccolours collapsible collapsed" width="60%" style="text-align:left"
!Derivation of equilibrium equations for small rotations
|-
|For the situation where the strains and rotations of the plate are small the virtual internal energy is given by
:<math>
  \begin{align}
  \delta U & = \int_{\Omega^0} \int_{-h}^h \boldsymbol{\sigma}:\delta\boldsymbol{\epsilon}~dx_3~d\Omega
          = \int_{\Omega^0} \int_{-h}^h \sigma_{\alpha\beta}~\delta\varepsilon_{\alpha\beta}~dx_3~d\Omega \\
    & = \int_{\Omega^0} \int_{-h}^h \left[\frac{1}{2}~\sigma_{\alpha\beta}~(\delta u^0_{\alpha,\beta}+\delta u^0_{\beta,\alpha}) - x_3~\sigma_{\alpha\beta}~\delta w^0_{,\alpha\beta}\right]~dx_3~d\Omega \\
    & = \int_{\Omega^0} \left[\frac{1}{2}~N_{\alpha\beta}~(\delta u^0_{\alpha,\beta}+\delta u^0_{\beta,\alpha}) - M_{\alpha\beta}~\delta w^0_{,\alpha\beta}\right]~d\Omega
  \end{align}
</math>
where the thickness of the plate is <math>2h</math> and the stress resultants and stress moment resultants are defined as
:<math>
  N_{\alpha\beta} := \int_{-h}^h \sigma_{\alpha\beta}~dx_3 ~;~~
  M_{\alpha\beta} := \int_{-h}^h x_3~\sigma_{\alpha\beta}~dx_3
</math>
Integration by parts leads to
:<math>
  \begin{align}
  \delta U & = \int_{\Omega^0} \left[-\frac{1}{2}~(N_{\alpha\beta,\beta}~\delta u^0_{\alpha}+N_{\alpha\beta,\alpha}~\delta u^0_{\beta})
    + M_{\alpha\beta,\beta}~\delta w^0_{,\alpha}\right]~d\Omega \\
  & + \int_{\Gamma^0} \left[\frac{1}{2}~(n_\beta~N_{\alpha\beta}~\delta u^0_\alpha+n_\alpha~N_{\alpha\beta}~\delta u^0_{\beta})
- n_\beta~M_{\alpha\beta}~\delta w^0_{,\alpha}\right]~d\Gamma
  \end{align}
</math>
The symmetry of the stress tensor implies that <math>N_{\alpha\beta} = N_{\beta\alpha}</math>.  Hence,
:<math>
  \delta U = \int_{\Omega^0} \left[-N_{\alpha\beta,\alpha}~\delta u^0_{\beta}
    + M_{\alpha\beta,\beta}~\delta w^0_{,\alpha}\right]~d\Omega
  + \int_{\Gamma^0} \left[n_\alpha~N_{\alpha\beta}~\delta u^0_{\beta}
- n_\beta~M_{\alpha\beta}~\delta w^0_{,\alpha}\right]~d\Gamma
</math>
Another integration by parts gives
:<math>
  \delta U = \int_{\Omega^0} \left[-N_{\alpha\beta,\alpha}~\delta u^0_{\beta}
    - M_{\alpha\beta,\beta\alpha}~\delta w^0\right]~d\Omega
  + \int_{\Gamma^0} \left[n_\alpha~N_{\alpha\beta}~\delta u^0_{\beta}
    + n_\alpha~M_{\alpha\beta,\beta}~\delta w^0
    - n_\beta~M_{\alpha\beta}~\delta w^0_{,\alpha}\right]~d\Gamma
</math>
For the case where there are no prescribed external forces, the principle of virtual work implies that <math>\delta U =0</math>.  The equilibrium equations for the plate are then given by
:<math>
  \begin{align}
    N_{\alpha\beta,\alpha} & = 0 \\
    M_{\alpha\beta,\alpha\beta} & = 0
  \end{align}
</math>
If the plate is loaded by an external distributed load <math>q(x)</math> that is normal to the mid-surface and directed in the positive <math>x_3</math> direction, the external virtual work due to the load is
:<math>
    \delta V_{\mathrm{ext}} = \int_{\Omega^0} q~\delta w^0~d\Omega
</math>
The principle of virtual work then leads to the equilibrium equations
:<math>
  \begin{align}
    N_{\alpha\beta,\alpha} & = 0 \\
    M_{\alpha\beta,\alpha\beta} - q & = 0
  \end{align}
</math>
|}
 
===Boundary conditions===
The boundary conditions that are needed to solve the equilibrium equations of plate theory can be obtained from the boundary terms in the principle of virtual work.  In the absence of external forces on the boundary, the boundary conditions are
:<math>
  \begin{align}
      n_\alpha~N_{\alpha\beta} & \quad \mathrm{or} \quad u^0_\beta \\
      n_\alpha~M_{\alpha\beta,\beta} & \quad \mathrm{or} \quad w^0 \\
      n_\beta~M_{\alpha\beta} & \quad \mathrm{or} \quad w^0_{,\alpha}
  \end{align}
</math>
Note that the quantity <math> n_\alpha~M_{\alpha\beta,\beta}</math> is an effective shear force.
 
===Constitutive relations===
The stress-strain relations for a linear elastic Kirchhoff plate are given by
:<math>
  \begin{align}
    \sigma_{\alpha\beta} & = C_{\alpha\beta\gamma\theta}~\varepsilon_{\gamma\theta} \\
    \sigma_{\alpha 3} & = C_{\alpha 3\gamma\theta}~\varepsilon_{\gamma\theta} \\
    \sigma_{33} & = C_{33\gamma\theta}~\varepsilon_{\gamma\theta}
  \end{align}
</math>
Since <math>\sigma_{\alpha 3}</math> and <math>\sigma_{33}</math> do not appear in the equilibrium equations it is implicitly assumed that these quantities do not have any effect on the momentum balance and are neglected.  The remaining stress-strain relations, in matrix form, can be written as
:<math>
  \begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix} =
  \begin{bmatrix} C_{11} & C_{12} & C_{13} \\ C_{12} & C_{22} & C_{23} \\
                  C_{13} & C_{23} & C_{33} \end{bmatrix}
  \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix}
</math>
Then,
:<math>
  \begin{bmatrix}N_{11} \\ N_{22} \\ N_{12} \end{bmatrix} =
  \int_{-h}^h \begin{bmatrix} C_{11} & C_{12} & C_{13} \\ C_{12} & C_{22} & C_{23} \\
                  C_{13} & C_{23} & C_{33} \end{bmatrix}
  \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix}
    dx_3 = \left\{
  \int_{-h}^h \begin{bmatrix} C_{11} & C_{12} & C_{13} \\ C_{12} & C_{22} & C_{23} \\
                  C_{13} & C_{23} & C_{33} \end{bmatrix}~dx_3 \right\}
  \begin{bmatrix} u^0_{1,1} \\ u^0_{2,2} \\ \frac{1}{2}~(u^0_{1,2}+u^0_{2,1}) \end{bmatrix}
</math>
and
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  \int_{-h}^h x_3~\begin{bmatrix} C_{11} & C_{12} & C_{13} \\ C_{12} & C_{22} & C_{23} \\
                  C_{13} & C_{23} & C_{33} \end{bmatrix}
  \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix}
    dx_3 = -\left\{
  \int_{-h}^h x_3^2~\begin{bmatrix} C_{11} & C_{12} & C_{13} \\ C_{12} & C_{22} & C_{23} \\
                  C_{13} & C_{23} & C_{33} \end{bmatrix}~dx_3 \right\}
  \begin{bmatrix} w^0_{,11} \\ w^0_{,22} \\ w^0_{,12} \end{bmatrix}
</math>
The ''' extensional stiffnesses''' are the quantities
:<math>
  A_{\alpha\beta} := \int_{-h}^h C_{\alpha\beta}~dx_3
</math>
The ''' bending stiffnesses''' (also called '''flexural rigidity''') are the quantities
:<math>
  D_{\alpha\beta} := \int_{-h}^h x_3^2~C_{\alpha\beta}~dx_3
</math>
The Kirchhoff-Love constitutive assumptions lead to zero shear forces.  As a result, the equilibrium equations for the plate have to be used to determine the shear forces in thin Kirchhoff-Love plates.  For isotropic plates, these equations lead to
:<math>
  Q_\alpha = - D\frac{\partial}{\partial x_\alpha}(\nabla^2 w^0) \,.
</math>
Alternatively, these shear forces can be expressed as
:<math>
  Q_\alpha = \mathcal{M}_{,\alpha}
</math>
where
:<math>
  \mathcal{M} := -D\nabla^2 w^0 \,.
</math>
 
=== Small strains and moderate rotations ===
If the rotations of the normals to the mid-surface are in the range of 10<math>^{\circ}</math> to 15<math>^\circ</math>, the strain-displacement relations can be approximated as
:<math>
  \begin{align}
    \varepsilon_{\alpha\beta} & =  \tfrac{1}{2}(u_{\alpha,\beta}+u_{\beta,\alpha}+u_{3,\alpha}~u_{3,\beta})\\
    \varepsilon_{\alpha 3} & = \tfrac{1}{2}(u_{\alpha,3}+u_{3,\alpha})\\
    \varepsilon_{33} & = u_{3,3}
  \end{align}
</math>
Then the kinematic assumptions of Kirchhoff-Love theory lead to the classical plate theory with [[Theodore von Kármán|von Kármán]] strains
:<math>
  \begin{align}
    \varepsilon_{\alpha\beta} & = \frac{1}{2}(u^0_{\alpha,\beta}+u^0_{\beta,\alpha}+w^0_{,\alpha}~w^0_{,\beta})
      - x_3~w^0_{,\alpha\beta} \\
    \varepsilon_{\alpha 3} & = - w^0_{,\alpha} + w^0_{,\alpha} = 0 \\
    \varepsilon_{33} & = 0
  \end{align}
</math>
This theory is nonlinear because of the quadratic terms in the strain-displacement relations.
 
If the strain-displacement relations take the von Karman form, the equilibrium equations can be expressed as
:<math>
  \begin{align}
    N_{\alpha\beta,\alpha} & = 0 \\
    M_{\alpha\beta,\alpha\beta} + [N_{\alpha\beta}~w^0_{,\beta}]_{,\alpha} - q & = 0
  \end{align}
</math>
 
== Isotropic quasistatic Kirchhoff-Love plates ==
For an isotropic and  homogeneous plate, the stress-strain relations are
:<math>
  \begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
  = \cfrac{E}{1-\nu^2}
  \begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
    \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix} \,.
</math>
The moments corresponding to these stresses are
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  -\cfrac{2h^3E}{3(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} w^0_{,11} \\ w^0_{,22} \\ w^0_{,12} \end{bmatrix}
</math>
In expanded form,
:<math>
  \begin{align}
    M_{11} & = -D\left(\frac{\partial^2 w^0}{\partial x_1^2} + \nu \frac{\partial^2 w^0}{\partial x_2^2}\right) \\
    M_{22} & = -D\left(\frac{\partial^2 w^0}{\partial x_2^2} + \nu \frac{\partial^2 w^0}{\partial x_1^2}\right) \\
    M_{12} & = -D(1-\nu)\frac{\partial^2 w^0}{\partial x_1 \partial x_2}
  \end{align}
</math>
where <math> D = 2h^3E/[3(1-\nu^2)] = H^3E/[12(1-\nu^2)]</math> for plates of thickness <math>H = 2h</math>.  Using the stress-strain relations for the plates, we can show that the stresses and moments are related by
:<math>
  \sigma_{11} = \frac{3x_3}{2h^3}\,M_{11} = \frac{12 x_3}{H^3}\,M_{11} \quad \text{and} \quad
  \sigma_{22} = \frac{3x_3}{2h^3}\,M_{22} = \frac{12 x_3}{H^3}\,M_{22} \,.
</math>
At the top of the plate where <math>x_3 = h = H/2</math>, the stresses are
:<math>
  \sigma_{11} = \frac{3}{2h^2}\,M_{11} = \frac{6}{H^2}\,M_{11} \quad \text{and} \quad
  \sigma_{22} = \frac{3}{2h^2}\,M_{22} = \frac{6}{H^2}\,M_{22} \,.
</math>
 
=== Pure bending ===
For an isotropic and homogeneous plate under [[pure bending]], the governing equations reduce to
:<math>
  \frac{\partial^4 w^0}{\partial x_1^4} + 2\frac{\partial^4 w^0}{\partial x_1^2  \partial x_2^2} + \frac{\partial^4 w^0}{\partial x_2^4} = 0 \,.
</math>
Here we have assumed that the in-plane displacements do not vary with <math>x_1</math> and <math>x_2</math>. In index notation,
:<math>
  w^0_{,1111} + 2~w^0_{,1212} +  w^0_{,2222} = 0
</math>
and in direct notation
<blockquote style="border: 1px solid black; padding:10px; width:150px">
:<math>
  \nabla^2\nabla^2 w = 0
</math>
</blockquote>
The bending moments are given by
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  -\cfrac{2h^3E}{3(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} w^0_{,11} \\ w^0_{,22} \\ w^0_{,12} \end{bmatrix}
</math>
:{| class="toccolours collapsible collapsed" width="60%" style="text-align:left"
!Derivation of equilibrium equations for pure bending
|-
|For an isotropic, homogeneous plate under pure bending the governing equations are
:<math>
  \begin{align}
  N_{\alpha\beta,\alpha} & = 0 \implies N_{11,1} + N_{21,2} = 0 ~,~~ N_{12,1} + N_{22,2} = 0 \\
  M_{\alpha\beta,\alpha\beta} & = 0 \implies M_{11,11} + 2 M_{12,12} + M_{22,22} = 0
  \end{align}
</math>
and the stress-strain relations are
:<math>
  \begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
  = \cfrac{E}{1-\nu^2}
  \begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
    \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix}
</math>
Then,
:<math>
  \begin{bmatrix}N_{11} \\ N_{22} \\ N_{12} \end{bmatrix} =
  \cfrac{2hE}{(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} u^0_{1,1} \\ u^0_{2,2} \\ \frac{1}{2}~(u^0_{1,2}+u^0_{2,1}) \end{bmatrix}
</math>
and
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  -\cfrac{2h^3E}{3(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} w^0_{,11} \\ w^0_{,22} \\ w^0_{,12} \end{bmatrix}
</math>
Differentiation gives
:<math>
  \begin{align}
    N_{11,1} & = \cfrac{2hE}{(1-\nu^2)}\left(u^0_{1,11} + \nu~u^0_{2,21}\right) ~;~~
    N_{22,2}  = \cfrac{2hE}{(1-\nu^2)}\left(\nu~u^0_{1,12} + u^0_{2,22}\right) \\
    N_{12,1} & = \cfrac{hE(1-\nu)}{(1-\nu^2)}\left(u^0_{1,21}+u^0_{2,11}\right) ~;~~
    N_{12,2} = \cfrac{hE(1-\nu)}{(1-\nu^2)}\left(u^0_{1,22}+u^0_{2,12}\right)
  \end{align}
</math>
and
:<math>
  \begin{align}
  M_{11,11} & = -\cfrac{2h^3E}{3(1-\nu^2)}\left( w^0_{,1111} + \nu~w^0_{,2211}\right) \\
  M_{22,22} & = -\cfrac{2h^3E}{3(1-\nu^2)}\left( \nu~w^0_{,1122} + w^0_{,2222}\right) \\
  M_{12,12} & = -\cfrac{2h^3E}{3(1-\nu^2)}(1-\nu)~w^0_{,1212}
  \end{align}
</math>
Plugging into the governing equations leads to
:<math>
  \begin{align}
  & u^0_{1,11} + \nu~u^0_{2,21} + \tfrac{1}{2}(1-\nu)\left(u^0_{1,22}+u^0_{2,12}\right) = 0 \\
  & \nu~u^0_{1,12} + u^0_{2,22} + \tfrac{1}{2}(1-\nu)\left(u^0_{1,21}+u^0_{2,11}\right) = 0 \\
  & w^0_{,1111} + \nu~w^0_{,2211} + 2(1-\nu)~w^0_{,1212} +  \nu~w^0_{,1122} + w^0_{,2222} = 0
  \end{align}
</math>
Since the order of differentiation is irrelevant we have <math>u^0_{1,12}=u^0_{1,21}</math>, <math>u^0_{2,21}=u^0_{2,12}</math>, and <math>w^0_{,2211} = w^0_{,1212} = w^0_{,1122}</math>.  Hence
:<math>
  \begin{align}
  & u^0_{1,11} + \tfrac{1}{2}(1-\nu)~u^0_{1,22} + \tfrac{1}{2}(1+\nu)~u^0_{2,12} = 0 \\
  & u^0_{2,22} + \tfrac{1}{2}(1-\nu)~u^0_{2,11} + \tfrac{1}{2}(1+\nu)~u^0_{1,12} = 0 \\
  & w^0_{,1111} + 2~w^0_{,1212} +  w^0_{,2222} = 0
  \end{align}
</math>
In direct tensor notation, the governing equation of the plate is
:<math>
  \nabla^2\nabla^2 w = 0
</math>
where we have assumed that the displacements <math>u^0_1,u^0_2</math> are constant.
|}
 
=== Bending under transverse load ===
If a distributed transverse load <math>-q(x)</math> is applied to the plate, the governing equation is <math>M_{\alpha\beta,\alpha\beta} = -q</math>.  Following the procedure shown in the previous section we get<ref name=Timo>Timoshenko, S. and Woinowsky-Krieger, S., (1959), '''Theory of plates and shells''', McGraw-Hill New York.</ref>
<blockquote style="border: 1px solid black; padding:10px; width:300px">
:<math>
  \nabla^2\nabla^2 w = \cfrac{q}{D} ~;~~ D := \cfrac{2h^3E}{3(1-\nu^2)}
</math>
</blockquote>
In rectangular Cartesian coordinates, the governing equation is
:<math>
  w^0_{,1111} + 2\,w^0_{,1212} + w^0_{,2222} = -\cfrac{q}{D}
</math>
and in cylindrical coordinates it takes the form
:<math>
  \frac{1}{r}\cfrac{d }{d r}\left[r \cfrac{d }{d r}\left\{\frac{1}{r}\cfrac{d }{d r}\left(r \cfrac{d w}{d r}\right)\right\}\right] = - \frac{q}{D}\,.
</math>
Solutions of this equation for various geometries and boundary conditions can be found in the article on [[bending of plates]].
:{| class="toccolours collapsible collapsed" width="60%" style="text-align:left"
!Derivation of equilibrium equations for transverse loading
|-
|For a transversely loaded plate without axial deformations, the governing equation has the form
:<math>
  M_{\alpha\beta,\alpha\beta} = q \implies M_{11,11} + 2 M_{12,12} + M_{22,22} = q
</math>
where <math>q</math> is a distributed transverse load (per unit area).  Substitution of the expressions for the derivatives of <math>M_{\alpha\beta}</math> into the governing equation gives
:<math>
  -\cfrac{2h^3E}{3(1-\nu^2)}\left[w^0_{,1111} + 2\,w^0_{,1212} + w^0_{,2222}\right] = q \,.
</math>
Noting that the bending stiffness is the quantity
:<math>
  D := \cfrac{2h^3E}{3(1-\nu^2)}
</math>
we can write the governing equation in the form
<blockquote style="border: 1px solid black; padding:10px; width:180px">
:<math>
  \nabla^2\nabla^2 w = -\frac{q}{D} \,.
</math>
</blockquote>
In cylindrical coordinates <math>(r, \theta, z)</math>,
:<math>
  \nabla^2 w \equiv \frac{1}{r}\frac{\partial }{\partial r}\left(r \frac{\partial w}{\partial r}\right) +
      \frac{1}{r^2}\frac{\partial^2 w}{\partial \theta^2} + \frac{\partial^2 w}{\partial z^2} \,.
</math>
For symmetrically loaded circular plates, <math> w = w(r)</math>, and we have
:<math>
  \nabla^2 w \equiv \frac{1}{r}\cfrac{d }{d r}\left(r \cfrac{d w}{d r}\right) \,.
</math>
|}
 
=== Cylindrical bending ===
Under certain loading conditions a flat plate can be bent into the shape of the surface of a cylinder.  This type of bending is called cylindrical bending and represents the special situation where <math>u_1 = u_1(x_1), u_2 = 0, w = w(x_1)</math>.  In that case
:<math>
  \begin{bmatrix}N_{11} \\ N_{22} \\ N_{12} \end{bmatrix} =
  \cfrac{2hE}{(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} u^0_{1,1} \\ 0 \\ 0 \end{bmatrix}
</math>
and
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  -\cfrac{2h^3E}{3(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} w^0_{,11} \\ 0 \\ 0 \end{bmatrix}
</math>
and the governing equations become<ref name=Timo/>
:<math>
  \begin{align}
  N_{11} & = A~\cfrac{\mathrm{d}u}{\mathrm{d} x_1} \quad \implies \quad
    \cfrac{\mathrm{d}^2 u}{\mathrm{d} x_1^2} = 0\\
  M_{11} & = -D~\cfrac{\mathrm{d}^2 w}{\mathrm{d} x_1^2} \quad \implies \quad \cfrac{\mathrm{d}^4 w}{\mathrm{d} x_1^4} = \cfrac{q}{D} \\
  \end{align}
</math>
 
== Dynamics of Kirchhoff-Love plates ==
The dynamic theory of thin plates determines the propagation of waves in the plates, and the study of standing waves and vibration modes.
 
=== Governing equations ===
The governing equations for the dynamics of a Kirchhoff-Love plate are
<blockquote style="border: 1px solid black; padding:10px; width:350px">
:<math>
  \begin{align}
    N_{\alpha\beta,\beta} & = J_1~\ddot{u}^0_\alpha \\
    M_{\alpha\beta,\alpha\beta} + q(x,t) & = J_1~\ddot{w}^0 - J_3~\ddot{w}^0_{,\alpha\alpha}
  \end{align}
</math>
</blockquote>
where, for a plate with density <math>\rho = \rho(x)</math>,
:<math>
  J_1 := \int_{-h}^h \rho~dx_3 = 2~\rho~h ~;~~
  J_3 := \int_{-h}^h x_3^2~\rho~dx_3 = \frac{2}{3}~\rho~h^3
</math>
and
:<math>
  \dot{u}_i = \frac{\partial u_i}{\partial t} ~;~~ \ddot{u}_i = \frac{\partial^2 u_i}{\partial t^2} ~;~~
  u_{i,\alpha} = \frac{\partial u_i}{\partial x_\alpha} ~;~~ u_{i,\alpha\beta} = \frac{\partial^2 u_i}{\partial x_\alpha \partial x_\beta}
</math>
 
:{| class="toccolours collapsible collapsed" width="60%" style="text-align:left"
!Derivation of equations governing the dynamics of Kirchhoff-Love plates
|-
|
The total kinetic energy of the plate is given by
:<math>
  K = \int_0^T \int_{\Omega^0} \int_{-h}^h \cfrac{\rho}{2}\left[
    \left(\frac{\partial u_1}{\partial t}\right)^2 + \left(\frac{\partial u_2}{\partial t}\right)^2 +
    \left(\frac{\partial u_3}{\partial t}\right)^2\right]~\mathrm{d}x_3~\mathrm{d}A~\mathrm{d}t
</math>
Therefore the variation in kinetic energy is
:<math>
  \delta K = \int_0^T \int_{\Omega^0} \int_{-h}^h \cfrac{\rho}{2}\left[
    2\left(\frac{\partial u_1}{\partial t}\right)\left(\frac{\partial \delta u_1}{\partial t}\right) +
    2\left(\frac{\partial u_2}{\partial t}\right)\left(\frac{\partial \delta u_2}{\partial t}\right) +
    2\left(\frac{\partial u_3}{\partial t}\right)\left(\frac{\partial \delta u_3}{\partial t}\right) \right]
    ~\mathrm{d}x_3~\mathrm{d}A~\mathrm{d}t
</math>
We use the following notation in the rest of this section.
:<math>
  \dot{u}_i = \frac{\partial u_i}{\partial t} ~;~~ \ddot{u}_i = \frac{\partial^2 u_i}{\partial t^2} ~;~~
  u_{i,\alpha} = \frac{\partial u_i}{\partial x_\alpha} ~;~~ u_{i,\alpha\beta} = \frac{\partial^2 u_i}{\partial x_\alpha \partial x_\beta}
</math>
Then
:<math>
  \delta K = \int_0^T \int_{\Omega^0} \int_{-h}^h \rho \left(
      \dot{u}_\alpha~\delta\dot{u}_\alpha + \dot{u}_3~\delta\dot{u}_3\right)
    ~\mathrm{d}x_3~\mathrm{d}A~\mathrm{d}t
</math>
For a Kirchhof-Love plate
:<math>
  u_\alpha = u^0_\alpha - x_3~w^0_{,\alpha} ~;~~ u_3 = w^0
</math>
Hence,
:<math>
  \begin{align}
  \delta K & = \int_0^T \int_{\Omega^0} \int_{-h}^h \rho \left[
      \left(\dot{u}^0_\alpha - x_3~\dot{w}^0_{,\alpha}\right)~
      \left(\delta\dot{u}^0_\alpha - x_3~\delta\dot{w}^0_{,\alpha}\right)
    + \dot{w}^0~\delta\dot{w}^0\right] ~\mathrm{d}x_3~\mathrm{d}A~\mathrm{d}t \\
    & = \int_0^T \int_{\Omega^0} \int_{-h}^h \rho
      \left(\dot{u}^0_\alpha~\delta\dot{u}^0_\alpha
      - x_3~\dot{w}^0_{,\alpha}~ \delta\dot{u}^0_\alpha
      - x_3~\dot{u}^0_\alpha~\delta\dot{w}^0_{,\alpha}
      + x_3^2~\dot{w}^0_{,\alpha}~\delta\dot{w}^0_{,\alpha}
    + \dot{w}^0~\delta\dot{w}^0\right) ~\mathrm{d}x_3~\mathrm{d}A~\mathrm{d}t
  \end{align}
</math>
Define, for constant <math>\rho</math> through the thickness of the plate,
:<math>
  J_1 := \int_{-h}^h \rho~dx_3 = 2~\rho~h ~;~~
  J_2 := \int_{-h}^h x_3~\rho~dx_3 = 0 ~;~~ J_3 := \int_{-h}^h x_3^2~\rho~dx_3 = \frac{2}{3}~\rho~h^3
</math>
Then
:<math>
  \delta K =
      \int_0^T \int_{\Omega^0} \left[
      J_1\left(\dot{u}^0_\alpha~\delta\dot{u}^0_\alpha
              + \dot{w}^0~\delta\dot{w}^0\right)
      + J_3~\dot{w}^0_{,\alpha}~\delta\dot{w}^0_{,\alpha}\right]
      ~\mathrm{d}A~\mathrm{d}t
</math>
Integrating by parts,
:<math>
  \delta K =
      \int_{\Omega^0} \left[\int_0^T \left\{
      - J_1\left(\ddot{u}^0_{\alpha}~\delta u^0_\alpha
              + \ddot{w}^0~\delta w^0\right)
      - J_3~\ddot{w}^0_{,\alpha}~\delta w^0_{,\alpha}\right\}~\mathrm{d}t
      + \left|J_1\left(\dot{u}^0_{\alpha}~\delta u^0_\alpha
              + \dot{w}^0~\delta w^0\right)
      + J_3~\dot{w}^0_{,\alpha}~\delta w^0_{,\alpha}\right|_0^T
    \right]~\mathrm{d}A
</math>
The variations <math>\delta u^0_\alpha</math> and <math>\delta w^0</math> are zero at <math>t = 0</math> and <math>t = T</math>.
Hence, after switching the sequence of integration, we have
:<math>
  \delta K =
      -\int_0^T \left\{ \int_{\Omega^0} \left[
      J_1\left(\ddot{u}^0_{\alpha}~\delta u^0_\alpha
              + \ddot{w}^0~\delta w^0\right)
      + J_3~\ddot{w}^0_{,\alpha}~\delta w^0_{,\alpha}\right]
      ~\mathrm{d}A\right\}~\mathrm{d}t
      + \left| \int_{\Omega^0} J_3~\dot{w}^0_{,\alpha}~\delta w^0_{,\alpha}\mathrm{d}A\right|_0^T
</math>
Integration by parts over the mid-surface gives
:<math>
  \begin{align}
  \delta K & =
      -\int_0^T \left\{ \int_{\Omega^0} \left[
      J_1\left(\ddot{u}^0_{\alpha}~\delta u^0_\alpha
              + \ddot{w}^0~\delta w^0\right)
      - J_3~\ddot{w}^0_{,\alpha\alpha}~\delta w^0\right] ~\mathrm{d}A
      + \int_{\Gamma^0} J_3~n_\alpha~\ddot{w}^0_{,\alpha}~\delta w^0~\mathrm{d}s
    \right\}~\mathrm{d}t \\
    & \qquad
    - \left| \int_{\Omega^0} J_3~\dot{w}^0_{,\alpha\alpha}~\delta w^0~\mathrm{d}A
      - \int_{\Gamma^0} J_3~\dot{w}^0_{,\alpha}~\delta w^0~\mathrm{d}s \right|_0^T
  \end{align}
</math>
Again, since the variations are zero at the beginning and the end of the time interval under consideration, we have
:<math>
  \delta K =
      -\int_0^T \left\{ \int_{\Omega^0} \left[
      J_1\left(\ddot{u}^0_{\alpha}~\delta u^0_\alpha
              + \ddot{w}^0~\delta w^0\right)
      - J_3~\ddot{w}^0_{,\alpha\alpha}~\delta w^0\right] ~\mathrm{d}A
      + \int_{\Gamma^0} J_3~n_\alpha~\ddot{w}^0_{,\alpha}~\delta w^0~\mathrm{d}s
    \right\}~\mathrm{d}t
</math>
For the dynamic case, the variation in the internal energy is given by
:<math>
  \delta U = - \int_0^T \left\{\int_{\Omega^0} \left[N_{\alpha\beta,\alpha}~\delta u^0_{\beta}
    + M_{\alpha\beta,\beta\alpha}~\delta w^0\right]~\mathrm{d}A
  - \int_{\Gamma^0} \left[n_\alpha~N_{\alpha\beta}~\delta u^0_{\beta}
    + n_\alpha~M_{\alpha\beta,\beta}~\delta w^0
    - n_\beta~M_{\alpha\beta}~\delta w^0_{,\alpha}\right]~\mathrm{d}s \right\}\mathrm{d}t
</math>
Integration by parts and invoking zero variation at the boundary of the mid-surface gives
:<math>
  \delta U = - \int_0^T \left\{\int_{\Omega^0} \left[N_{\alpha\beta,\alpha}~\delta u^0_{\beta}
    + M_{\alpha\beta,\beta\alpha}~\delta w^0\right]~\mathrm{d}A
  - \int_{\Gamma^0} \left[n_\alpha~N_{\alpha\beta}~\delta u^0_{\beta}
    + n_\alpha~M_{\alpha\beta,\beta}~\delta w^0
    + n_\beta~M_{\alpha\beta,\alpha}~\delta w^0\right]~\mathrm{d}s \right\}\mathrm{d}t
</math>
If there is an external distributed force <math>q(x,t)</math> acting normal to the surface of the plate, the virtual external work done is
:<math>
  \delta V_{\mathrm{ext}} = \int_0^T \left[\int_{\Omega^0} q(x,t)~\delta w^0~\mathrm{d}A\right]\mathrm{d}t
</math>
From the principle of virtual work <math>\delta U + \delta V_{\mathrm{ext}} = \delta K </math>. Hence the governing balance equations for the plate are
:<math>
  \begin{align}
    N_{\alpha\beta,\beta} & = J_1~\ddot{u}^0_\alpha \\
    M_{\alpha\beta,\alpha\beta} - q(x,t) & = J_1~\ddot{w}^0 - J_3~\ddot{w}^0_{,\alpha\alpha}
  \end{align}
</math>
|}
 
Solutions of these equations for some special cases can be found in the article on [[vibration of plates|vibrations of plates]].  The figures below show some vibrational modes of a circular plate.
<gallery widths="250px">
Image:Drum vibration mode01.gif|mode ''k'' = 0, ''p'' = 1
Image:Drum vibration mode02.gif|mode ''k'' = 0, ''p'' = 2
Image:Drum vibration mode12.gif|mode ''k'' = 1, ''p'' = 2
</gallery>
 
=== Isotropic plates ===
The governing equations simplify considerably for isotropic and homogeneous plates for which the in-plane deformations can be neglected.  In that case we are left with one equation of the following form (in rectangular Cartesian coordinates):
:<math>
  D\,\left(\frac{\partial^4 w}{\partial x^4} + 2\frac{\partial^4 w}{\partial x^2\partial y^2} + \frac{\partial^4 w}{\partial y^4}\right) = -q(x, y, t) - 2\rho h\, \frac{\partial^2 w}{\partial t^2} \,.
</math>
where <math>D</math> is the bending stiffness of the plate.  For a uniform plate of thickness <math>2h</math>,
:<math>
  D := \cfrac{2h^3E}{3(1-\nu^2)} \,.
</math>
In direct notation
:<math>
  D\,\nabla^2\nabla^2 w = -q(x, y, t) - 2\rho h \, \ddot{w} \,.
</math>
For free vibrations, the governing equation becomes
:<math>
  D\,\nabla^2\nabla^2 w = -2\rho h \, \ddot{w} \,.
</math>
:{| class="toccolours collapsible collapsed" width="60%" style="text-align:left"
!Derivation of dynamic governing equations for isotropic Kirchhoff-Love plates
|-
|
For an isotropic and  homogeneous plate, the stress-strain relations are
:<math>
  \begin{bmatrix}\sigma_{11} \\ \sigma_{22} \\ \sigma_{12} \end{bmatrix}
  = \cfrac{E}{1-\nu^2}
  \begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
    \begin{bmatrix}\varepsilon_{11} \\ \varepsilon_{22} \\ \varepsilon_{12} \end{bmatrix} \,.
</math>
where <math>\varepsilon_{\alpha\beta}</math> are the in-plane strains.  The strain-displacement relations
for Kirchhoff-Love plates are
:<math>
  \varepsilon_{\alpha\beta} = \frac{1}{2}(u_{\alpha,\beta}+u_{\beta,\alpha})
      - x_3\,w_{,\alpha\beta} \,.
</math>
Therefore, the resultant moments corresponding to these stresses are
:<math>
  \begin{bmatrix}M_{11} \\ M_{22} \\ M_{12} \end{bmatrix} =
  -\cfrac{2h^3E}{3(1-\nu^2)}~\begin{bmatrix} 1 & \nu & 0 \\
                  \nu & 1 & 0 \\
                  0 & 0 & 1-\nu \end{bmatrix}
  \begin{bmatrix} w_{,11} \\ w_{,22} \\ w_{,12} \end{bmatrix}
</math>
The governing equation for an isotropic and homogeneous plate of uniform thickness <math>2h</math> in the
absence of in-plane displacements is
:<math>
  M_{11,11} + 2 M_{12,12} + M_{22,22}
  - q(x,t) = 2\rho h\ddot{w} - \frac{2}{3}\rho h^3\left(\ddot{w}_{,11}+\ddot{w}_{,22} + \ddot{w}_{,33}\right) \,.
</math>
Differentiation of the expressions for the moment resultants gives us
:<math>
  \begin{align}
  M_{11,11} & = -\cfrac{2h^3E}{3(1-\nu^2)}\left( w_{,1111} + \nu~w_{,2211}\right) \\
  M_{22,22} & = -\cfrac{2h^3E}{3(1-\nu^2)}\left( \nu~w_{,1122} + w_{,2222}\right) \\
  M_{12,12} & = -\cfrac{2h^3E}{3(1-\nu^2)}(1-\nu)~w_{,1212}
  \end{align}
</math>
Plugging into the governing equations leads to
:<math>
  \begin{align}
  -\cfrac{2h^3E}{3(1-\nu^2)}& \left(w_{,1111} + \nu~w_{,2211} + 2(1-\nu)~w_{,1212} +  \nu~w_{,1122} + w_{,2222}\right) =  \\
    &  q(x,t) + 2\rho h\ddot{w} - \frac{2}{3}\rho h^3\left(\ddot{w}_{,11}+\ddot{w}_{,22} + \ddot{w}_{,33}\right) \,.
  \end{align}
</math>
Since the order of differentiation is irrelevant we have <math>w_{,2211} = w_{,1212} = w_{,1122}</math>. Hence
:<math>
  \begin{align}
  -\cfrac{2h^3E}{3(1-\nu^2)}& \left(w_{,1111} + 2w_{,1212} + w_{,2222}\right) =  \\
    &  q(x,t) + 2\rho h\ddot{w} - \frac{2}{3}\rho h^3\left(\ddot{w}_{,11}+\ddot{w}_{,22} + \ddot{w}_{,33}\right) \,.
  \end{align}
</math>
If the flexural stiffness of the plate is defined as
:<math>
  D := \cfrac{2h^3E}{3(1-\nu^2)}
</math>
we have
:<math>
  D\left(w_{,1111} + 2w_{,1212} + w_{,2222}\right) = 
    -q(x,t) - 2\rho h\ddot{w} + \frac{2}{3}\rho h^3\left(\ddot{w}_{,11}+\ddot{w}_{,22} + \ddot{w}_{,33}\right) \,.
</math>
For small deformations, we often neglect the spatial derivatives of the transverse acceleration of the
plate and we are left with
:<math>
  D\left(w_{,1111} + 2w_{,1212} + w_{,2222}\right) = -q(x,t) - 2\rho h\ddot{w} \,.
</math>
Then, in direct tensor notation, the governing equation of the plate is
:<math>
  D\nabla^2\nabla^2 w = -q(x,t) - 2\rho h\ddot{w} \,.
</math>
|}
 
== References ==
<references/>
 
== See also ==
*[[Bending]]
*[[Bending of plates]]
*[[Infinitesimal strain theory]]
*[[Linear elasticity]]
*[[Plate theory]]
*[[Stress (mechanics)]]
*[[Stress resultants]]
*[[Vibration of plates]]
 
{{DEFAULTSORT:Kirchhoff-Love plate theory}}
[[Category:Continuum mechanics]]

Revision as of 06:19, 5 February 2013

Deformation of a thin plate highlighting the displacement, the mid-surface (red) and the normal to the mid-surface (blue)

The Kirchhoff–Love theory of plates is a two-dimensional mathematical model that is used to determine the stresses and deformations in thin plates subjected to forces and moments. This theory is an extension of Euler-Bernoulli beam theory and was developed in 1888 by Love[1] using assumptions proposed by Kirchhoff. The theory assumes that a mid-surface plane can be used to represent a three-dimensional plate in two-dimensional form.

The following kinematic assumptions that are made in this theory:[2]

  • straight lines normal to the mid-surface remain straight after deformation
  • straight lines normal to the mid-surface remain normal to the mid-surface after deformation
  • the thickness of the plate does not change during a deformation.

Assumed displacement field

Let the position vector of a point in the undeformed plate be 𝐱. Then

𝐱=x1𝒆1+x2𝒆2+x3𝒆3xi𝒆i.

The vectors 𝒆i form a Cartesian basis with origin on the mid-surface of the plate, x1 and x2 are the Cartesian coordinates on the mid-surface of the undeformed plate, and x3 is the coordinate for the thickness direction.

Let the displacement of a point in the plate be 𝐮(𝐱). Then

𝐮=u1𝒆1+u2𝒆2+u3𝒆3ui𝒆i

This displacement can be decomposed into a vector sum of the mid-surface displacement and an out-of-plane displacement w0 in the x3 direction. We can write the in-plane displacement of the mid-surface as

𝐮0=u10𝒆1+u20𝒆2uα0𝒆α

Note that the index α takes the values 1 and 2 but not 3.

Then the Kirchhoff hypothesis implies that

uα(𝐱)=uα0(x1,x2)x3w0xαuα0x3w,α0;α=1,2u3(𝐱)=w0(x1,x2)

If φα are the angles of rotation of the normal to the mid-surface, then in the Kirchhoff-Love theory

φα=w,α0

Note that we can think of the expression for uα as the first order Taylor series expansion of the displacement around the mid-surface.

Displacement of the mid-surface (left) and of a normal (right)

Quasistatic Kirchhoff-Love plates

The original theory developed by Love was valid for infinitesimal strains and rotations. The theory was extended by von Kármán to situations where moderate rotations could be expected.

Strain-displacement relations

For the situation where the strains in the plate are infinitesimal and the rotations of the mid-surface normals are less than 10° the strain-displacement relations are Template:Clarify

εαβ=12(uαxβ+uβxα)12(uα,β+uβ,α)εα3=12(uαx3+u3xα)12(uα,3+u3,α)ε33=u3x3u3,3

Using the kinematic assumptions we have

εαβ=12(uα,β0+uβ,α0)x3w,αβ0εα3=w,α0+w,α0=0ε33=0

Therefore the only non-zero strains are in the in-plane directions.

Equilibrium equations

The equilibrium equations for the plate can be derived from the principle of virtual work. For a thin plate under a quasistatic transverse load q(x) these equations are

N11x1+N21x2=0N12x1+N22x2=02M11x12+22M12x1x2+2M22x22=q

where the thickness of the plate is 2h. In index notation,

Nαβ,α=0Nαβ:=hhσαβdx3Mαβ,αβq=0Mαβ:=hhx3σαβdx3

where σαβ are the stresses.

Bending moments and normal stresses
Torques and shear stresses

Boundary conditions

The boundary conditions that are needed to solve the equilibrium equations of plate theory can be obtained from the boundary terms in the principle of virtual work. In the absence of external forces on the boundary, the boundary conditions are

nαNαβoruβ0nαMαβ,βorw0nβMαβorw,α0

Note that the quantity nαMαβ,β is an effective shear force.

Constitutive relations

The stress-strain relations for a linear elastic Kirchhoff plate are given by

σαβ=Cαβγθεγθσα3=Cα3γθεγθσ33=C33γθεγθ

Since σα3 and σ33 do not appear in the equilibrium equations it is implicitly assumed that these quantities do not have any effect on the momentum balance and are neglected. The remaining stress-strain relations, in matrix form, can be written as

[σ11σ22σ12]=[C11C12C13C12C22C23C13C23C33][ε11ε22ε12]

Then,

[N11N22N12]=hh[C11C12C13C12C22C23C13C23C33][ε11ε22ε12]dx3={hh[C11C12C13C12C22C23C13C23C33]dx3}[u1,10u2,2012(u1,20+u2,10)]

and

[M11M22M12]=hhx3[C11C12C13C12C22C23C13C23C33][ε11ε22ε12]dx3={hhx32[C11C12C13C12C22C23C13C23C33]dx3}[w,110w,220w,120]

The extensional stiffnesses are the quantities

Aαβ:=hhCαβdx3

The bending stiffnesses (also called flexural rigidity) are the quantities

Dαβ:=hhx32Cαβdx3

The Kirchhoff-Love constitutive assumptions lead to zero shear forces. As a result, the equilibrium equations for the plate have to be used to determine the shear forces in thin Kirchhoff-Love plates. For isotropic plates, these equations lead to

Qα=Dxα(2w0).

Alternatively, these shear forces can be expressed as

Qα=,α

where

:=D2w0.

Small strains and moderate rotations

If the rotations of the normals to the mid-surface are in the range of 10 to 15, the strain-displacement relations can be approximated as

εαβ=12(uα,β+uβ,α+u3,αu3,β)εα3=12(uα,3+u3,α)ε33=u3,3

Then the kinematic assumptions of Kirchhoff-Love theory lead to the classical plate theory with von Kármán strains

εαβ=12(uα,β0+uβ,α0+w,α0w,β0)x3w,αβ0εα3=w,α0+w,α0=0ε33=0

This theory is nonlinear because of the quadratic terms in the strain-displacement relations.

If the strain-displacement relations take the von Karman form, the equilibrium equations can be expressed as

Nαβ,α=0Mαβ,αβ+[Nαβw,β0],αq=0

Isotropic quasistatic Kirchhoff-Love plates

For an isotropic and homogeneous plate, the stress-strain relations are

[σ11σ22σ12]=E1ν2[1ν0ν10001ν][ε11ε22ε12].

The moments corresponding to these stresses are

[M11M22M12]=2h3E3(1ν2)[1ν0ν10001ν][w,110w,220w,120]

In expanded form,

M11=D(2w0x12+ν2w0x22)M22=D(2w0x22+ν2w0x12)M12=D(1ν)2w0x1x2

where D=2h3E/[3(1ν2)]=H3E/[12(1ν2)] for plates of thickness H=2h. Using the stress-strain relations for the plates, we can show that the stresses and moments are related by

σ11=3x32h3M11=12x3H3M11andσ22=3x32h3M22=12x3H3M22.

At the top of the plate where x3=h=H/2, the stresses are

σ11=32h2M11=6H2M11andσ22=32h2M22=6H2M22.

Pure bending

For an isotropic and homogeneous plate under pure bending, the governing equations reduce to

4w0x14+24w0x12x22+4w0x24=0.

Here we have assumed that the in-plane displacements do not vary with x1 and x2. In index notation,

w,11110+2w,12120+w,22220=0

and in direct notation

22w=0

The bending moments are given by

[M11M22M12]=2h3E3(1ν2)[1ν0ν10001ν][w,110w,220w,120]

Bending under transverse load

If a distributed transverse load q(x) is applied to the plate, the governing equation is Mαβ,αβ=q. Following the procedure shown in the previous section we get[3]

22w=qD;D:=2h3E3(1ν2)

In rectangular Cartesian coordinates, the governing equation is

w,11110+2w,12120+w,22220=qD

and in cylindrical coordinates it takes the form

1rddr[rddr{1rddr(rdwdr)}]=qD.

Solutions of this equation for various geometries and boundary conditions can be found in the article on bending of plates.

Cylindrical bending

Under certain loading conditions a flat plate can be bent into the shape of the surface of a cylinder. This type of bending is called cylindrical bending and represents the special situation where u1=u1(x1),u2=0,w=w(x1). In that case

[N11N22N12]=2hE(1ν2)[1ν0ν10001ν][u1,1000]

and

[M11M22M12]=2h3E3(1ν2)[1ν0ν10001ν][w,11000]

and the governing equations become[3]

N11=Adudx1d2udx12=0M11=Dd2wdx12d4wdx14=qD

Dynamics of Kirchhoff-Love plates

The dynamic theory of thin plates determines the propagation of waves in the plates, and the study of standing waves and vibration modes.

Governing equations

The governing equations for the dynamics of a Kirchhoff-Love plate are

Nαβ,β=J1u¨α0Mαβ,αβ+q(x,t)=J1w¨0J3w¨,αα0

where, for a plate with density ρ=ρ(x),

J1:=hhρdx3=2ρh;J3:=hhx32ρdx3=23ρh3

and

u˙i=uit;u¨i=2uit2;ui,α=uixα;ui,αβ=2uixαxβ

Solutions of these equations for some special cases can be found in the article on vibrations of plates. The figures below show some vibrational modes of a circular plate.

Isotropic plates

The governing equations simplify considerably for isotropic and homogeneous plates for which the in-plane deformations can be neglected. In that case we are left with one equation of the following form (in rectangular Cartesian coordinates):

D(4wx4+24wx2y2+4wy4)=q(x,y,t)2ρh2wt2.

where D is the bending stiffness of the plate. For a uniform plate of thickness 2h,

D:=2h3E3(1ν2).

In direct notation

D22w=q(x,y,t)2ρhw¨.

For free vibrations, the governing equation becomes

D22w=2ρhw¨.

References

  1. A. E. H. Love, On the small free vibrations and deformations of elastic shells, Philosophical trans. of the Royal Society (London), 1888, Vol. série A, N° 17 p. 491–549.
  2. Reddy, J. N., 2007, Theory and analysis of elastic plates and shells, CRC Press, Taylor and Francis.
  3. 3.0 3.1 Timoshenko, S. and Woinowsky-Krieger, S., (1959), Theory of plates and shells, McGraw-Hill New York.

See also