Axisymmetric Solid Elements with Nonlinear, Asymmetric Deformation
This section provides a reference to the axisymmetric solid elements
available in
Abaqus/Standard.
These elements are intended for analysis of hollow bodies, such as pipes and
pressure vessels. They can also be used to model solid bodies, but spurious
stresses may occur at zero radius, particularly if transverse shear loads are
applied.
Coordinate 1 is
r, coordinate 2 is z. Referring to
the figures shown in
Choosing the Element's Dimensionality,
the r-direction corresponds to the global
X-direction in the
plane and the negative global Z-direction in the
plane, and the z-direction corresponds to the global
Y-direction. Coordinate 1 must be greater than or equal to
zero.
Degree of freedom 1 is ,
degree of freedom 2 is .
The
degree of freedom is an internal variable: you cannot control
it.
Element Types
Stress/Displacement Elements
CAXA4N
Bilinear, Fourier quadrilateral with 4 nodes per
r–z plane
CAXA4HN
Bilinear, Fourier quadrilateral with 4 nodes per
r–z plane, hybrid with constant
Fourier pressure
CAXA4RN
Bilinear, Fourier quadrilateral with 4 nodes per
r–z plane, reduced integration in
r–z planes with hourglass control
CAXA4RHN
Bilinear, Fourier quadrilateral with 4 nodes per
r–z plane, reduced integration in
r–z planes, hybrid with constant
Fourier pressure
CAXA8N
Biquadratic, Fourier quadrilateral with 8 nodes per
r–z plane
CAXA8HN
Biquadratic, Fourier quadrilateral with 8 nodes per
–z
plane, hybrid with linear Fourier pressure
CAXA8RN
Biquadratic, Fourier quadrilateral with 8 nodes per
r–z plane, reduced integration in
r–z planes
CAXA8RHN
Biquadratic, Fourier quadrilateral with 8 nodes per
r–z plane, reduced integration in
r–z planes, hybrid with linear
Fourier pressure
Active Degrees of Freedom
1, 2
Additional Solution Variables
The bilinear elements have 4N and the biquadratic
elements 8N additional variables relating to
.
Element types CAXA4HN and CAXA4RHN have
additional variables relating to the pressure stress.
Element types CAXA8HN and CAXA8RHN have
additional variables relating to the pressure stress.
Pore Pressure Elements
CAXA8PN
Biquadratic, Fourier quadrilateral with 8 nodes per
r–z plane, bilinear Fourier pore
pressure
CAXA8RPN
Biquadratic, Fourier quadrilateral with 8 nodes per
r–z plane, bilinear Fourier pore
pressure, reduced integration in r–z
planes
Active Degrees of Freedom
1, 2, 8 at corner nodes
1, 2 at midside nodes
Additional Solution Variables
8N additional variables relating to
.
Nodal Coordinates Required
r,
z
Element Property Definition
Element-Based Loading
Even though the symmetry in the
r–z plane at
allows the modeling of half of the initially axisymmetric structure, the
loading must be specified as the total load on the full axisymmetric body.
Consider, for example, a cylindrical shell loaded by a unit uniform axial
force. To produce a unit load on a CAXA element with 4 modes, the nodal forces are 1/8, 1/4, 1/4, 1/4,
and 1/8 at ,
,
,
,
and ,
respectively.
Seepage (outward normal flow) proportional to the difference between surface
pore pressure and a reference sink pore pressure on face
n (units of FL−2).
Load ID (*FLOW/
*DFLOW): QnD
F−1L3T−1
Drainage-only seepage (outward normal flow) proportional to the surface pore
pressure on face n only when that pressure is
positive.
Load ID (*FLOW/
*DFLOW): QnNU
F−1L3T−1
Nonuniform seepage (outward normal flow) proportional to the difference
between surface pore pressure and a reference sink pore pressure on face
n (units of FL−2) with
magnitude supplied via user subroutine
FLOW.
Load ID (*FLOW/
*DFLOW): Sn
LT−1
Prescribed pore fluid velocity (outward from the face) on face
n.
Load ID (*FLOW/
*DFLOW): SnNU
LT−1
Nonuniform prescribed pore fluid velocity (outward from the face) on face
n with magnitude supplied via user subroutine
DFLOW.
Element Output
The
numerical integration with respect to
employs the trapezoidal rule. There are
equally spaced integration planes in the element, including the
and
planes, with N being the number of Fourier modes.
Consequently, the radial nodal forces corresponding to pressure loads applied
in the circumferential direction are distributed in this direction in the ratio
of
in the 1 Fourier mode element,
in the 2 Fourier mode element, and
in the 4 Fourier mode element. The sum of these consistent nodal forces is
equal to the integral of the applied pressure over .
Output is as defined below unless a local coordinate system in the
r–z plane is assigned to the element
through the section definition (Orientations)
in which case the components are in the local directions. These local
directions rotate with the motion in large-displacement analysis. See
State storage
for details.
Stress, Strain, and Other Tensor Components
Stress and other tensors (including strain tensors) are available for
elements with displacement degrees of freedom. All tensors have the same
components. For example, the stress components are as follows:
S11
Stress in the radial direction or in the local 1-direction.
S22
Stress in the axial direction or in the local 2-direction.
S33
Hoop direct stress.
S12
Shear stress.
S13
Shear stress.
S23
Shear stress.
Node Ordering and Face Numbering on Elements
The node ordering in the first r–z
plane of each element, at ,
is shown below. Each element must have N more planes
of nodes defined, where N is the number of Fourier
modes. The node ordering is the same in each plane. You can specify the nodes
in each plane. Alternatively, you can specify the node ordering in the first
r–z plane of an element, and
Abaqus/Standard
will generate all other nodes for the element by adding successively a constant
offset to each node for each of the N planes of the
element. By default,
Abaqus/Standard
uses an offset of 100000 (see
Element Definition).
Table 1. Element faces
Face 1
1 – 2 face
Face 2
2 – 3 face
Face 3
3 – 4 face
Face 4
4 – 1 face
Numbering of Integration Points for Output
The integration points in the first
r–z plane of integration, at
,
are shown below. The integration points follow in sequence at the
r–z integration planes in ascending
order of
location.