Applying distributed loads
Required parameter for cyclic symmetry models in steady-state dynamics analyses
- CYCLIC MODE
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Set this parameter equal to the cyclic symmetry mode number of loads that are applied in the current steady-state dynamics procedure.
Optional parameters
- AMPLITUDE
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Set this parameter equal to the name of the amplitude curve that defines the variation of the load magnitude during the step.
If this parameter is omitted for uniform load types in an Abaqus/Standard analysis, the reference magnitude is applied immediately at the beginning of the step or linearly over the step, depending on the value assigned to the AMPLITUDE parameter on the STEP option (see Defining an Analysis). If this parameter is omitted in an Abaqus/Explicit analysis, the reference magnitude is applied immediately at the beginning of the step.
Amplitude references are ignored for nonuniform loads given by user subroutine DLOAD in an Abaqus/Standard analysis. Amplitude references are passed into user subroutine VDLOAD in an Abaqus/Explicit analysis.
Only the load magnitude is changed with time. Quantities such as the fluid surface level in hydrostatic pressure loading are not changed.
- CONSTANT RESULTANT
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Set CONSTANT RESULTANT=NO (default) if surface traction vectors, edge traction vectors, or edge moments are to be integrated over the surface in the current configuration.
Set CONSTANT RESULTANT=YES if surface traction vectors, edge traction vectors, or edge moments are to be integrated over the surface in the reference configuration.
The CONSTANT RESULTANT parameter is valid only for uniform and nonuniform surface tractions and edge loads (including edge moments); it is ignored for all other load types.
- FOLLOWER
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Set FOLLOWER=YES (default) if a prescribed traction or shell-edge load is to rotate with the surface or shell edge in a large-displacement analysis (live load).
Set FOLLOWER=NO if a prescribed traction or edge load is to remain fixed in a large-displacement analysis (dead load).
The FOLLOWER parameter is valid only for traction and edge load labels TRVEC, TRVECNU, EDLD, and EDLDNU. It is ignored for all other load labels.
- OP
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Set OP=MOD (default) for existing DSLOADs to remain, with this option modifying existing distributed loads or defining additional distributed loads.
Set OP=NEW if all existing DSLOADs applied to the model should be removed. New distributed loads can be defined.
The OP parameter is ignored for the nodal pressure distributed load type label (NP). All existing DSLOADs are removed before applying the nodal pressure loads.
- ORIENTATION
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Set this parameter equal to the name given for the ORIENTATION option (Orientations) used to specify the local coordinates in which components of traction or shell-edge loads are specified.
The ORIENTATION parameter is valid only for traction and edge load labels TRSHR, TRSHRNU, TRVEC, TRVECNU, EDLD, and EDLDNU. It is ignored for all other load labels.
- REF NODE
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This parameter applies only to Abaqus/Explicit analyses and is relevant only for viscous and stagnation pressure loads when the velocity at the reference node is used.
Set this parameter equal to either the node number of the reference node or the name of a node set containing the reference node. If the name of a node set is chosen, the node set must contain exactly one node. If this parameter is omitted, the reference velocity is assumed to be zero.
Optional, mutually exclusive parameters for matrix generation and steady-state dynamics analysis (direct, modal, or subspace)
- IMAGINARY
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Include this parameter to define the imaginary (out-of-phase) part of the loading.
- REAL
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Include this parameter (default) to define the real (in-phase) part of the loading.
Data lines to define distributed surface pressures
- First line
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Surface name.
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Distributed load type label P, PNU, SP, or VP.
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Reference load magnitude, which can be modified by using the AMPLITUDE option. For nonuniform loads, the magnitude must be defined in user subroutine DLOAD for an Abaqus/Standard analysis or VDLOAD for an Abaqus/Explicit analysis. If given, this value is passed into the user subroutine in an Abaqus/Standard analysis.
Repeat this data line as often as necessary to define distributed loads on different surfaces.
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Data lines to define hydrostatic pressure (Abaqus/Standard only)
- First line
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Surface name.
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Distributed load type label HP.
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Actual magnitude of the load, which can be modified by using the AMPLITUDE option.
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Z-coordinate of zero pressure level.
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Z-coordinate of the point at which the pressure is defined.
Repeat this data line as often as necessary to define hydrostatic pressure loading on different surfaces.
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Data lines to define mechanical pore pressure loads (Abaqus/Standard only)
- First line
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Surface name.
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Distributed load type label PORMECH.
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Scaling factor.
Repeat this data line as often as necessary to define mechanical pore pressure loading on different surfaces.
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Data lines to define nodal pressure loads (Abaqus/Standard only)
- First line
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Surface name.
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Distributed load type label NP.
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Scaling factor. The default is 1.0.
Repeat this data line as often as necessary to define nodal pressure loading on different surfaces.
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Data lines to define a general surface traction vector, a surface shear traction vector, or a general shell-edge traction vector
- First line
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Surface name.
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Distributed load type label TRVEC, TRSHR, EDLD, TRVECNU, TRSHRNU, or EDLDNU.
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Reference load magnitude, which can be modified by using the AMPLITUDE option.
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1-component of the traction vector direction.
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2-component of the traction vector direction.
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3-component of the traction vector direction.
For a two-dimensional or axisymmetric analysis, only the first two components of the traction vector direction need to be specified. For the shear traction load labels TRSHR and TRSHRNU, the loading direction is computed by projecting the specified traction vector direction down upon the surface in the reference configuration. For nonuniform loads in Abaqus/Standard the magnitude and traction vector direction must be defined in user subroutine UTRACLOAD. If given, the magnitude and vector will be passed into the user subroutine in an Abaqus/Standard analysis.
Repeat this data line as often as necessary to define traction vectors on different surfaces.
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Data lines to define a surface normal traction vector, a shell-edge traction vector (in the normal, transverse, or tangent direction), or a shell-edge moment
- First line
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Surface name.
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Distributed load type label EDMOM, EDNOR, EDSHR, EDTRA, EDMOMNU, EDNORNU, EDSHRNU, or EDTRANU.
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Reference load magnitude, which can be modified by using the AMPLITUDE option. For nonuniform loads in Abaqus/Standard the magnitude must be defined in user subroutine UTRACLOAD. If given, the magnitude will be passed into the user subroutine in an Abaqus/Standard analysis.
Repeat this data line as often as necessary to define traction vectors on different surfaces.
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Data lines to define stagnation pressure loads (Abaqus/Explicit only)
- First line
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Surface name.
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Distributed load type label SP.
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Reference load magnitude, which can be modified by using the AMPLITUDE option.
Repeat this data line as often as necessary to define stagnation pressure loads on different surfaces.
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Data lines to define fluid pressure penetration surface pressures
- First line
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Surface name.
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Distributed load type label PPEN.
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Reference magnitude of the fluid pressure, which can be modified by using the AMPLITUDE parameter.
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Critical contact pressure threshold at which fluid penetration starts to occur. The default value is 0.0, in which case fluid penetration occurs only if contact is lost. You can use an amplitude curve defined in entry 8 of the data line to modify a nonzero value.
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Specify WETTING ADVANCE or LOCAL to indicate the algorithm for controlling the evolution of the region exposed to the fluid pressure. The WETTING ADVANCE algorithm is currently available only in Abaqus/Explicit.
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Node or node set on the surface initially exposed to fluid pressure. This node or node set is used only if WETTING ADVANCE is specified.
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Time period over which the fluid pressure on the newly penetrated contact surface segments is ramped up to the current magnitude. The default penetration time period is chosen as 0.001 of the current step time.
This scalar value applies only to Abaqus/Standard analyses and is neglected in a linear perturbation analysis, in which case the fluid pressure is applied immediately once the pressure penetration criterion is satisfied.
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Name of the amplitude curve that defines the variation of the critical contact pressure threshold during the step.
Repeat this data line as often as necessary to define distributed fluid pressure penetration loads on either different surfaces or on the same surface but with different nodes initially exposed to a fluid if WETTING ADVANCE is specified.
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