The equation for conservation of energy equates the increase in internal energy per unit mass, , to the rate at which work is being done by the stresses and the rate at which heat is being added. In the absence of heat conduction the energy equation can be written as

The equation of state is assumed for the pressure as a function of the current density, , and the internal energy per unit mass, :

A Mie-Grüneisen equation of state is linear in energy. The most common form is

The Hugoniot energy, , is related to the Hugoniot pressure by

The equation of state and the energy equation represent coupled equations for pressure and internal energy. ABAQUS/Explicit solves these equations simultaneously at each material point.

Linear equations of state can always be written in the form

Linear U_s – U_p Hugoniot form

A common fit to the Hugoniot data is given by

where and define the linear relationship between the linear shock velocity, , and the particle velocity, , as follows:

With the above assumptions the linear Hugoniot form is written as

where is equivalent to the elastic bulk modulus at small nominal strains.

There is a limiting compression given by the denominator of this form of the equation of state

or

At this limit there is a tensile minimum; thereafter, negative sound speeds are calculated for the material.

Input File Usage:	Use both of the following options:
	*DENSITY (to specify the reference density ) *EOS, TYPE=USUP (to specify the variables , , and )

ABAQUS/CAE Usage:

Property module: material editor: GeneralDensity (to specify the reference density ) OtherEos: Type: Us - Up (to specify the variables , , and )

Initial state

The initial state of the material is determined by the initial values of specific energy, , and pressure stress, . ABAQUS/Explicit will automatically compute the initial density, , that satisfies the equation of state, . You can define the initial specific energy and initial stress state (see “Initial conditions,” Section 19.2.1). The initial pressure used by the equation of state is inferred from the specified stress states. If no initial conditions are specified, ABAQUS/Explicit will assume that the material is at its reference state:

Input File Usage:	Use either or both of the following options, as required:
	*INITIAL CONDITIONS, TYPE=SPECIFIC ENERGY *INITIAL CONDITIONS, TYPE=STRESS

ABAQUS/CAE Usage:

Initial specific energy and initial stress are not supported in ABAQUS/CAE.

The equation of state is designed for modeling the compaction of ductile porous materials. The implementation in ABAQUS/Explicit is based on the model proposed by Hermann (1968) and Carroll and Holt (1972). The constitutive model provides a detailed description of the irreversible compaction behavior at low stresses and predicts the correct thermodynamic behavior at high pressures for the fully compacted solid material. In ABAQUS/Explicit the solid phase is assumed to be governed by a Mie-Grüneisen equation of state. The relevant properties of the porous material in the virgin state, to be discussed later, and the material properties of the solid phase are specified separately.

The porosity of the material, , is defined as the ratio of pore volume, , to total volume, , where is the solid volume. The porosity remains in the range , with indicating full compaction. It is convenient to introduce a scalar variable , sometimes referred to as “distension,” defined as the ratio of the density of the solid material, , to the density of the porous material, , both evaluated at the same temperature and pressure:

An equation of state is assumed for the pressure of the porous material as a function of ; current density, ; and internal energy per unit mass, , in the form

The equation of state must be supplemented by an equation that describes the behavior of as a function of the thermodynamic state. This equation takes the form

The function captures the general behavior to be expected in a ductile porous material. The unloaded virgin state corresponds to the value , where is the reference porosity of the material. Initial compression of the porous material is assumed to be elastic. Recall that decreasing porosity corresponds to a reduction in . As the pressure increases beyond the elastic limit, , the pores in the material start to crush, leading to irreversible compaction and permanent (plastic) volume change. Unloading from a partially compacted state follows a new elastic curve that depends on the maximum compaction (or, alternatively, the minimum value of ) ever attained during the deformation history of the material. The absolute value of the slope of the elastic curve decreases as decreases, as will be quantified later. The material becomes fully compacted when the pressure reaches the compaction pressure ; at that point , a value that is retained forever. The function therefore has multiple branches: a plastic branch, , and multiple elastic branches, , corresponding to elastic unloading from partially compacted states. The appropriate branch of is selected according to the following rule:

Input File Usage:	Use the following options to specify the properties of the solid phase (the reference density, ; the reference sound speed, ; the slope of the curve, ; and the Grüneisen ratio, ):
	*DENSITY *EOS, TYPE=USUP Use the following option to specify the properties of the porous material (the reference sound speed, ; the reference porosity, ; the elastic limit, ; and the compaction pressure, ): *EOS COMPACTION

ABAQUS/CAE Usage:

The equation of state is not supported in ABAQUS/CAE.

*INITIAL CONDITIONS, TYPE=SPECIFIC ENERGY
*INITIAL CONDITIONS, TYPE=STRESS
*INITIAL CONDITIONS, TYPE=POROSITY

The Jones-Wilkens-Lee (or JWL) equation of state models the pressure generated by the release of chemical energy in an explosive. This model is implemented in a form referred to as a programmed burn, which means that the reaction and initiation of the explosive is not determined by shock in the material. Instead, the initiation time is determined by a geometric construction using the detonation wave speed and the distance of the material point from the detonation points.

The JWL equation of state can be written in terms of the initial energy per unit mass, , as

*DENSITY (to specify the density of the explosive )
*EOS, TYPE=JWL (to specify the material constants  and )

Arrival time of detonation wave

ABAQUS/Explicit calculates the arrival time of the detonation wave at a material point as the distance from the material point to the nearest detonation point divided by the detonation wave speed:

where is the position of the material point, is the position of the th detonation point, is the detonation delay time of the th detonation point, and is the detonation wave speed of the explosive material. The minimum in the above formula is over the detonation points that apply to the material point.

Burn fraction

To spread the burn wave over several elements, a burn fraction, , is computed as

where is a constant that controls the width of the burn wave (set to a value of 2.5) and is the characteristic length of the element. If the time is less than , the pressure is zero in the explosive; otherwise, the pressure is given by the product of and the pressure determined from the JWL equation above.

*EOS, TYPE=JWL
*DETONATION POINT

*INITIAL CONDITIONS, TYPE=SPECIFIC ENERGY

An ideal gas equation of state can be written in the form of

One of the important features of an ideal gas is that its specific energy depends only upon its temperature; therefore, the specific energy can be integrated numerically as

Modeling with an ideal gas equation of state is typically performed adiabatically; the temperature increase is calculated directly at the material integration points according to the adiabatic thermal energy increase caused by the work , where is the specific volume (the volume per unit mass, ). Therefore, unless a fully coupled temperature-displacement analysis is performed, an adiabatic condition is always assumed in ABAQUS/Explicit.

When performing a fully coupled temperature-displacement analysis, the pressure stress and specific energy are updated based on the evolving temperature field. The energy increase due to the change in state will be accounted for in the heat equation and will be subject to heat conduction.

For the ideal gas model in ABAQUS/Explicit you define the gas constant, , and the ambient pressure, . For an ideal gas can be determined from the universal gas constant, , and the molecular weight, , as follows:

*EOS, TYPE=IDEAL GAS
*SPECIFIC HEAT, DEPENDENCIES=n

Initial state

The initial state of the gas is determined from the user-specified initial density, , and either the initial pressure stress, , or the initial temperature, . You can choose between specifying initial pressure or temperature. If both are specified, the value for stress will be used to initialize the state of the gas. For those material points that have zero or no pressure stress specified, the initial state is determined from the initial density and the initial temperature.

You can define the initial specific energy, . The initial specific energy for an ideal gas equation of state affects only the output of the total specific energy and should be mathematically equivalent to

Input File Usage:	Use some or all of the following options, as required:
	*DENSITY, DEPENDENCIES=n *INITIAL CONDITIONS, TYPE=SPECIFIC ENERGY *INITIAL CONDITIONS, TYPE=STRESS *INITIAL CONDITIONS, TYPE=TEMPERATURE

ABAQUS/CAE Usage:	Property module: material editor: GeneralDensity
	Load module: Create Field: Step: Initial: choose Other for the Category and Temperature for the Types for Selected Step Initial specific energy and initial stress are not supported in ABAQUS/CAE.

*PHYSICAL CONSTANTS, ABSOLUTE ZERO=

A special case

In the case of an adiabatic analysis with constant specific heat (both and are constant), the specific energy is linear in temperature

The pressure stress can, therefore, be recast in the common form of

where is the ratio of specific heats and can be defined as

where

for a monatomic;

for a diatomic; and

for a polyatomic gas.

The equation of state defines only the material's hydrostatic behavior. It can be used by itself, in which case the material has only volumetric strength (the material is assumed to have no shear strength). Alternatively, ABAQUS/Explicit allows you to define deviatoric behavior, assuming that the deviatoric and volumetric responses are uncoupled. Two models, a linear isotropic deviatoric model or a Newtonian viscous deviatoric model, are available. The material's volumetric response is governed then by the equation of state model, while its deviatoric response is governed by either the linear isotropic elastic model or the Newtonian viscous fluid model.

You must provide the elastic shear modulus, , or the viscosity, , when you define the deviatoric behavior. For the elastic shear behavior the increment in the deviatoric stress is defined from the deviatoric elastic strain increment as

*EOS
*EOS SHEAR, TYPE=ELASTIC

*EOS
*EOS SHEAR, TYPE=VISCOUS

An equation of state model can be used with the Mises (“Classical metal plasticity,” Section 11.2.1) or the Johnson-Cook (“Johnson-Cook plasticity,” Section 11.2.7) plasticity models to model elastic-plastic behavior. In this case you must define the elastic part of the shear behavior. The material's volumetric response is governed by the equation of state model, while the deviatoric response is governed by the linear elastic shear and the plasticity model.

*EOS
*EOS SHEAR, TYPE=ELASTIC
*PLASTIC

*INITIAL CONDITIONS, TYPE=HARDENING

An equation of state model (except the ideal gas equation of state) can also be used with the tensile failure model (“Dynamic failure models,” Section 11.2.8) to model dynamic spall or a pressure cutoff. The tensile failure model uses the hydrostatic pressure stress as a failure measure and offers a number of failure choices. You must provide the hydrostatic cutoff stress.

You can specify that the deviatoric stresses should fail when the tensile failure criterion is met. In the case where the material's deviatoric behavior is not defined, this specification is meaningless and is, therefore, ignored.

The tensile failure model in ABAQUS/Explicit is designed for high-strain-rate dynamic problems in which inertia effects are important. Therefore, it should be used only for such situations. Improper use of the tensile failure model may result in an incorrect simulation.

*EOS
*EOS SHEAR
*TENSILE FAILURE

An adiabatic condition is always assumed for materials modeled with an equation of state unless a dynamic coupled temperature-displacement procedure is used. In other words, specifying an adiabatic dynamic stress analysis step or specifying temperature as a predefined field has no effect on the behavior of this model.

A linear equation of state model can be used to model incompressible viscous and inviscid laminar flow governed by the Navier-Stokes equation of motion. The volumetric response is governed by the equations of state, where the bulk modulus acts as a penalty parameter for the incompressible constraint.

To model a viscous laminar flow that follows the Navier-Poisson law of a Newtonian fluid, use the Newtonian viscous deviatoric model and define the viscosity as the real linear viscosity of the fluid. Appropriate initial conditions for velocity and stress are essential to get an accurate solution for this class of problem.

To model an incompressible inviscid fluid such as water in ABAQUS/Explicit, it is useful to define a small amount of shear resistance to suppress shear modes that can otherwise tangle the mesh. Here the shear stiffness or shear viscosity acts as a penalty parameter. The shear modulus or viscosity should be small because flow is inviscid; a high shear modulus or viscosity will result in an overly stiff response. To avoid an overly stiff response, the internal forces arising due to the deviatoric response of the material should be kept several orders of magnitude below the forces arising due to the volumetric response. This can be done by choosing an elastic shear modulus that is several orders of magnitude lower than the bulk modulus. If the viscous model is used, the shear viscosity specified should be on the order of the shear modulus, calculated as above, scaled by the stable time increment. The expected stable time increment can be obtained from a data check analysis of the model. This method is a convenient way to approximate a shear resistance that will not introduce excessive viscosity in the material.

If a shear model is defined, the hourglass control forces are calculated based on the shear resistance of the material. Thus, in materials with extremely low or zero shear strengths such as inviscid fluids, the hourglass forces calculated based on the default parameters are insufficient to prevent spurious hourglass modes. Therefore, a sufficiently high hourglass scaling factor is recommended to increase the resistance to such modes.