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5.7 Singularities of a Reissner–Mindlin plate
Slab models are usually developed by starting with a 3-D elastic continuum
and then simplifying the kinematics. Depending on the assumptions made in
this process, the result is either a Kirchhoff plate or a Reissner–Mindlin plate.
The loss of accuracy in the transition from a 3-D model to a 2-D model
is often felt the most near the boundary where the models differ most. With
regard to the Reissner–Mindlin plate we speak of a boundary layer effect [9],
[238]. To some extent this effect seems to be due to the fact that we cannot put
an elastic solid on a line support such as a hinged support (see Sect. 1.16, p.
55), and the Reissner–Mindlin plate—not surprisingly—seems to suffer more
from such adverse effects.
In a Reissner–Mindlin plate we have a choice of two support conditions
for a hinged edge: the hard support, w = w,t = 0, which corresponds to the
hinged support of a Kirchhoff plate, and the soft support, w = 0, where the
slope w,t = w,x tx +w,y ty in the tangential direction is released, w,t = 0; see
Fig. 5.20.
As in a Kirchhoff plate, the boundary conditions and the angle of the
boundary points determine when and where singularities will develop; see
Table 5.2 [205].
Table 5.2. Corner singularities of a Reissner–Mindlin plate
Boundary conditions Bending moment Shear force
clamped–clamped 180
◦
180
◦
sliding edge–sliding edge 90
◦
180
◦
hard support–hard support 90
◦
180
◦
soft support–soft support 180
◦
180
◦
free-free 180
◦
180
◦
clamped–sliding edge 90
◦
180
◦
clamped–hard support 90
◦
180
◦
clamped–soft support ≈ 61.70
◦
(ν = 0.29) 180
◦
clamped–free ≈ 61.70
◦
(ν = 0.29) 90
◦
sliding edge–hard support 45
◦
90
◦
sliding edge–soft support 90
◦
180
◦
sliding edge–free 90
◦
90
◦
hard support–soft support ≈ 128.73
◦
180
◦
hard support–free ≈ 128.73
◦
90
◦
soft support–free 180
◦
90
◦
5.7 Singularities of a Reissner–Mindlin plate 437
Shear locking
The main advantages of a Reissner–Mindlin plate are essentially the relaxed
continuity requirements for the shape functions, and its inner “richness” of
kinematic variables. On the other hand shear locking can become a problem.
The transition from a Reissner–Mindlin plate model—relatively thick slabs
(foundation slabs)—to a Kirchhoff plate model, which is the standard model
for thin slabs, can cause problems.
Clearly the Reissner–Mindlin plate theory subsumes the Kirchhoff slab
theory, because the transition from the former to the latter model is simply
achieved by setting the shearing strains to zero:
γx = w,x +θx = 0 γy = w,y +θy = 0. (5.53)
Because in normal slabs shear deformations are negligible, a Reissner–Mindlin
plate should behave like a Kirchhoff plate. But this does not happen. The
more the slab thickness h shrinks, the more a Reissner–Mindlin plate tends
to stiffen, until the slab ultimately seems to freeze.
This is primarily a problem of the finite elements. If the equations could be
solved exactly, then if h tends to zero the Reissner–Mindlin results should tend
(in the sense of the strain energy [238], p. 263) to the results of a Kirchhoff
plate.
Shear locking is best explained by studying the example of a Timoshenko
beam, u = [w, θ]T , see Fig. 5.21. The strain energy product is
a(u,ˆu) =
_ l
0
[EI θ
_ ˆθ
_ + GAs (w
_ + θ) ( ˆ w
_ + ˆθ)] dx , (5.54)
so that with appropriate unit displacements (2 at each node)
ϕ1(x) =
_
w10
_
ϕ2(x) =
_
0
θ2
_
_ _ _
node 1
ϕ3(x) =
_
w30 _
ϕ4(x) =
_
0
θ4
_
_ _ _
node 2
. . .
(5.55)
for example linear functions
wi(x) = l − x
l
θj(x) = x
l
(5.56)
a result like
(KB +KS)u = f (5.57)
is obtained, where the entries in the matrix KB come from the bending terms,
and the entries in KS from the shear terms:
438 5 Slabs
Fig. 5.21. Cantilever beam
kB
ij =
_ l
0
EI θ
_
i θ
_
j dx kS
ij =
_ l
0
GAs (w
_
i + θi) (w
_
j + θj) dx . (5.58)
If the cantilever beam in Fig. 5.21 is modeled with just one element, the
end deflection is [70],
w(l) =
12(h/l)2 + 20
12(h/l)2 + 5
· 1.2 Pl
GAs
(5.59)
where As is the equivalent shear cross-sectional area. For a short beam, l 1,
the first fraction is approximately 1 and the end deflection is identical to the
shear deformation
w(l) = 1.2 Pl
GAs
. (5.60)
If l ! h, i.e., if the length l is much greater than the width h of the beam,
the first fraction is about 20/5 and the end deflection will be much too small:
w(l) = 4 · 1.2 Pl
GAs
= 9.6 Pl
E bh
(G = 0.5 E, ν = 0) (5.61)
compared with the exact value (let l/h = 8)
w(l) = Pl3
3 EI
= 4 Pl
E bh
_
l
h
_2
= 256 Pl
E bh
. (5.62)
This is shearlocking.
The reason for this stiffening effect is the different sensitivity of the bending
stiffness EI and the shear stiffness GAs with respect to the width h of the
beam:
EI = bh3
12 GAs _ Gbh (rectangular cross section) . (5.63)
If the width h—and thus the shear deformations γ = w_ + θ—tend to zero,
the bending stiffness decreases much faster than the shear stiffness. As in an
equation such as
5.8 Reissner–Mindlin elements 439
Fig. 5.22. Plate elements: a) Bathe–Dvorkin element b) DKT element. At the nodes
of a DKT element, the shearing strain is zero, θxi = −∂w/∂xi, θyi = −∂w/∂yi
(1 + 105) u = 10 (solution u = 9.9999 · 10−5 ≈ 0) , (5.64)
where the large second term enforces a nearly zero solution, the matrix KS—
because of the rapidly increasing influence of GAs—tends to dominate (5.57).
If (5.57) could be solved exactly, the increasing influence of GAs would be
canceled by the opposing tendency of w_ + θ = γ _→ 0.
All this holds for slabs as well: the transition from a Reissner–Mindlin
plate model (average to large slab thickness) to a Kirchhoff plate model (small
thickness) does not succeed numerically.
A whole catalog of measures has been proposed to circumvent shearlocking.
Reduced integration is the best-known remedy. Although a better and
simpler approach is to raise the order of the polynomials. This holds in similar
situations as well, where internal constraints force an element to sacrifice
all the degrees of freedom to satisfy the constraints, so that nothing is left to
describe the movements of the element [70].
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