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5.17 Foundation slabs
Winkler model
In the Winkler model it is assumed that the soil acts like a system of isolated
springs that move independently and exert a force cw on the underside of the
slab. This leads to the differential equations
EIwIV + cw = p beam (5.95)
KΔΔw + cw = p slab . (5.96)
The strain energy products associated with these two equations are
model and gravity
470 5 Slabs
Fig. 5.52. Concentrated forces acting
on the surface of the half-space
a(w, ˆ w) =
_ l
0
M ˆM
EI
dx + c
_ l
0
w ˆ wdx (5.97)
a(w, ˆ w) =
_
Ω
m•ˆκ dΩ + c
_
Ω
w ˆ wdΩ. (5.98)
Hence to the stiffness matrix K of a beam or plate element must only be
added the mass matrix M,
mij =
_
Ω
ϕi ϕj dΩ , (5.99)
so that
(K + cM)u = f . (5.100)
A consequence of this simple spring model is that under gravity load G, the
slab deflection w = G/c is constant and the bending moments are zero; see
Fig. 5.51. Because the individual springs move independently, the soil outside
the loaded region simply retains its original level; see Fig. 5.51.
Inasmuch as this model does not properly replicate even the most basic
aspects of actual soil behavior, it is no surprise that the modulus of subgrade
reaction c is not a genuine physical quantity, but an artificial (albeit
convenient) tool to simplify the design of foundation slabs. Theoretically the
coefficient not only depends on the soil, but also on the extensions of the
foundation slab. And in principle it is also not a constant, because otherwise
it would not be possible to recover the rapidly increasing soil pressure p near
the edge of a rigid punch from the formula p(x) = c(x)w; see Fig. 1.123 on
p. 175.
Various strategies have been proposed to circumvent these defects. Mostly
these techniques modify the modulus of subgrade reaction c iteratively and
locally in such a way that the shape of the deformed slab and the soil are
approximately the same; see Fig. 5.53.
Half-space model
In a linear elastic isotropic half-space, the displacement field u(x) is the
solution of the system
5.17 Foundation slabs 471
Lij uj := −μui,jj − μ
1 − 2 ν
uj ,ji = pi (5.101)
where the pi are volume forces and μ and ν are elastic constants.
The displacement field due to a concentrated normal force P on the edge of
the elastic half-space was found by Boussinesq [49]. The vertical displacement
is (see Fig. 5.52)
uB := u3(x, y) =
1 + ν
2πE
_
(x3 − y3)2
r3 + 2
1 − ν
r
_
P (5.102)
and the stresses are
σij = − P
2π r
r,i r,j r,2
r
r,i = ∂r
∂yi
= yi − xi
r
. (5.103)
Note that the stresses σij are independent of the modulus of elasticity E. How
this solution can be extended to layered soils was explained in Sect. 2.2, p.
256.
Next let us consider the coupled problem of a foundation slab and the soil.
On the free surface the tractions must be zero, t = 0, while at the interface
between the slab and the soil the deflection must be the same, and the vertical
stresses must have opposite signs,
w = wS t3 − pS = 0 (5.104)
where pS is the soil pressure, which also appears on the right-hand side of the
plate equation with a negative sign because it opposes the load p coming from
the building:
KΔΔw = p − pS . (5.105)
If the soil pressure p(y) is expanded in terms of nodal shape functions ψi(y)
(hat functions)
p(y) =
_
i
ψi(y)p i , (5.106)
the soil deflection at a point x is
wS(x) =
_
i
_
Ω
uB(x, y) ψi(y) dΩy pi =
_
i
ηi(x) pi (5.107)
and the stress in the soil is
σzz(x) =
_
i
_
Ω
3
2π
(x3 − y3)3
r3 ψi(y) dΩy pi =
_
i
θi(x) pi . (5.108)
Hence the coupled problem leads to the system
472 5 Slabs
Fig. 5.53. Deformation patterns
_
K(nn) L(nm)
Iw(
mn)
−J(mm)
__
u(n)
p(m)
_
=
_
f(n)
0(m)
_
FE with soil pressure
wslab
− wsoil = 0 (5.109)
where
k ij = a(ϕi, ϕj) l ij =
_
Ω
ψi ϕj dΩ Jij = ηj(xi) . (5.110)
The matrix Iw results if the n × n unit matrix I is reduced to an m × m
matrix by deleting certain rows and columns. Because only the deflections at
the soil interface are equated, the rotational degrees of freedom in the vector
u are meaningless. So that if the underlined rows
1, 2, 3, 4, 5, 6, 7, 8, 9, . . . (5.111)
in the unit matrix are deleted, the result is the matrix Iw.
With the equivalent nodal forces −Lp of the soil pressure the extended
set of equations becomes Ku = f − Lp, or Ku+ Lp = f.
The Boussinesq solution is based on the linear theory of elasticity, so E
is Young’s modulus, while in soil mechanics a one-dimensional modulus Es is
used instead, which corresponds to consolidation or oedometer testing, and is
therefore also called the constrained modulus. The two moduli are related via
elasticity theory:
E =
(1 + ν)(1 − 2 ν)
(1 − ν) Es , (5.112)
5.17 Foundation slabs 473
Fig. 5.54. Foundation slab: a) model; b) cross section; c) bending moments mxx
in the half-space model; d) Winkler model
where ν is the (drained) Poisson’s ratio. For ν = 0 this becomes E = Es
and for ν = 0.2 Young’s modulus E is 90 percent of Es so there is not much
difference between the two.
Comparisons of the Winkler model and half-space model
Ultimately there is little agreement between results based on the Winkler
model and the half-space model, as in the case of the slab in Fig. 5.54 or the
slab in Fig. 5.55, which is stiffened by a ring of shear walls.
474 5 Slabs
Fig. 5.55. Modified Winkler model: a) plan view and load; b) bending moments
mxx in two sections, constant modulus of subgrade reaction: c) half-space model;
d) in a 1 m strip the modulus of subgrade reaction was raised by a factor of 4
In the half-space model the soil pressure increases towards the edge of the
slab, while in the Winkler model the deflection increases near the edge; see
Fig. 5.55 b. In a first analysis, the modulus of subgrade reaction was assumed
to be constant, c = 10 000 kN/m3 (Fig. 5.55 b), and in a second analysis the
modulus was increased by a factor of 4 in a 1 m strip along the edge. In this
second improved model the agreement of the bending moments mxx with the
half-space model (ES = 50 000 kN/m2) (Fig. 5.55 c and d) is much better.
x
y
6.0
6.0
x
y
6.0
6.0
x
y
6.0
6.0
gravity load g = 9.0 kN/m2
30.0 kN/m
30.0 kN/m
30.0 kN/m
30.0 kN/m
P1 100.0 kN
P2 100.0 kN
x
y
6.0
6.0
5.17 Foundation slabs 475
Fig. 5.56. 3-D model of a multi-story building on an elastic foundation: a) global
view of the deformed model (the deformation are of course not to scale); b) partial
view
476 5 Slabs
3-D models
A 3-D analysis of a multi-story building itself is a complex undertaking. Even
for an experienced structural engineer it is not easy to verify the results of
a 3-D FE analysis with independent models. Too many effects combine—the
modeling of the girders, the floor plates, shear walls, columns, etc. usually has
a much larger influence on the accuracy than questions of mathematical rigor:
’If the mechanical model is false high-precision arithmetic will not save the
analysis’.
Given the large deviations between the Winkler model and the half-space
model it should be no surprise then that the choice of the foundation model has
a great impact on practically all results in a 3-D model of a building, see Fig.
5.56. This shows clearly in numerical studies, [94]. Placing a sophisticated 3-D
model of a building on a simple Winkler foundation cannot be recommended.
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