Biomedical Engineering Reference
In-Depth Information
Table 4.3 Long-term
material parameters of
VE-foam material
VE-Foam
j
l
j
[MPa]
a
j
[-]
m
j
[-]
1
5.280146E - 03
2.208547E ? 01
1.587915E - 04
2
1.042675E - 03
2.669817E ? 01
2.855843E - 03
and VE-foam material, Fig.
4.13
, is shown based on optimized long-term material
parameters provided in tables Table
4.2
and
4.3
.
model parameter N = 2 is performed via the optimization routine described in
are the measured force and displacement data of the indenter and the coordinates
of parameter vector p with the material parameters a
k
, l
k
and b
k
. According to
(
3.364
), using the norm parameter m = 2, the following material parameters are
derived, meeting the requirements deduced in
Sects. 3.4
and
3.4.8
such as
restrictions based on classical linear theory, the B
AKER
-E
RICKSEN
inequalities and
In the parameter sets listed above, stable (nominal) strain ranges according to
the D
RUCKER
stability criterion for the deformation modes of uniaxial compression
and uniaxial tension as well as simple shear are shown:
HR-Foam %
VE-Foam %
Uniaxial compression
Stable for all strains
Stable for all strains
Uniaxial tension
\340
\180
Simple shear
\340
\170
4.2.1.4 Experiments II: Viscoelasticity (Creep)
Experimental Set Up: To mechanically characterize the time domain viscoelas-
ticity of the foam materials HR and VE (see ''Employed Elastomeric Materials'' in
Sect. 4.2.1.2
, Table
4.1
), the following deformation modes at constant climatic
conditions (20C; 50% humidity) were performed under constant indenter weights
and gravity loading:
1. plate compression creep tests with a plate mass of 17.0 kg
2. hemispherical punch creep tests (punch: Ø48 mm, indenter mass: HR-foam:
27.0 kg, VE-foam: 3.3 kg
Test (1) encorporated foam specimen loading with a rigid plane plate with
variable weight. Plate displacement over time was recorded. Test (2) was primarily
used to verify the derived parameters under a multiaxial strain state, cf. Fig.
4.14
.
In
case
of
deviation
from
the
experimental
results
of
the
hemispherical