Constitutive Theories for Linear Micromorphic Thermoviscoelastic Solids ()
1. Introduction
In a recent paper, Surana et al. [1] presented a review of published works on microcontinuum theories, including micromorphic theories. The published works discussed in this reference are included here in the list of references [2]-[32] for the convenience of the reader, but the details of these works are not repeated here for the sake of brevity. The majority of the published works on 3M microcontinuum theories are due to Eringen and Eringen et al. [7]-[24]. The other published works generally follow the concepts and the theories published in references [7]-[24]. Surana et al. [1] presented detailed derivations of micro and macro conservation and balance laws from the first principles for linear micromorphic microcontinuum solid medium.
In the following, we summarize the basic concepts and steps used in reference [1] in deriving the conservation and balance laws for linear micromorphic continua for micro and macro deformation physics. 1) the deformation/strain measures derived by Surana et al. [33] serve as the basic measures of deformation for the micromorphic theory. The microconstituents are deformable, hence there is a micro deformation gradient tensor associated with them. 2) All conservation and balance laws are initiated for the micro deformation of the microconstituent, using laws of thermodynamics in classical continuum mechanics, yielding micro conservation and balances. From the micro conservation and balance laws, “integral-average” definitions are introduced that permit derivation of macro conservation and balance laws and constitutive theories using principles of thermodynamics and well-established concepts in applied mathematics. 3) In deriving conservation and the balance laws and constitutive theories for micromorphic continua, we maintain and adhere to the concepts of classical rotations, the Cauchy moment tensor, and the theory of isotropic tensors, introduced and used by Surana et al. [33]-[55] in conjunction with linear and nonlinear micropolar theories for solid and fluid continua. This is necessary because the physics of rigid rotations of microconstituents exists in all 3M theories, arising from the skew-symmetric part of the micro deformation gradient tensor. Thus, we must have exactly the same mathematical treatment of rigid rotation physics in 3M theories, requiring that we maintain the micropolar theory as a subset of micromorphic theory.
Surana et al. presented conservation and balance laws for micro as well as macro deformation physics with clarity of valid “integral-average” definitions that are essential for deriving the conservation and balance laws at the macro level. This was followed by constitutive theories for the macro Cauchy stress tensor, the microconstituent Cauchy stress tensor, the Cauchy moment tensor, and the heat vector for thermoelastic medium. Constitutive theories were initiated using conjugate pairs in the entropy inequality establishing constitutive tensors and their argument tensors. In all three constitutive theories (microconstituent Cauchy stress tensor, macro Cauchy stress tensor and macro Cauchy moment tensor), mechanisms of elasticity for the micro Cauchy stress tensor (
) and the macro stress tensor
(symmetric part) were considered. All constitutive theories were derived using the representation theorem [56]-[67], and are therefore always thermodynamically (not in violation of entropy inequality) and mathematically consistent. Constitutive theories and material coefficients were first derived using integrity (complete basis of the spaces of constitutive tensors), after which their simplified forms were presented, linear in the components of the argument tensors.
The micromorphic theory derived by Surana et al. was shown to be thermodynamically and mathematically consistent, and is therefore a valid and physical linear micromorphic theory. This linear micromorphic theory was also compared with Eringen’s micromorphic theory. The differences in the two theories were identified, discussed and evaluated for their validity based on thermodynamic principles and well accepted mathematical concepts to establish their validity or lack thereof, and hence the validity of the resulting micromorphic theory. In the context of Eringen’s microcontinuum theories, authors showed certain omissions, use of incorrect approaches, inconsistencies, and the thermodynamic and mathematical inconsistency of the resulting micromorphic theories, casting serious doubts on their validity. All of these shortcomings and issues were addressed and corrected in reference [1] in the linear micromorphic microcontinuum theory for solid continua presented by the authors.
In this paper, the conservation and balance laws for linear micromorphic microcontinuum solids derived by Surana et al. and the strain/deformation measures derived in reference [33] are utilized to derive the constitutive theories for the microconstituent Cauchy stress tensor, the macro Cauchy stress tensor, the macro Cauchy moment tensor and the heat vector for thermoviscoelastic physics without rheology. Important aspects of the scope of work in this paper are summarized below:
1) Microconstituents have elasticity and dissipation physics. The dissipation physics is a function of micro strain rates up to order
yielding an ordered rate dissipation theory with a micro dissipation spectrum consisting of
pairs of dissipation coefficients corresponding to
micro strain rates.
2) The solid medium also has elasticity and dissipation (macro dissipation). The dissipation mechanism is a function of macro strain rates up to order
, yielding an ordered rate dissipation theory with a macro dissipation spectrum consisting of
pairs of dissipation coefficients corresponding to
macro strain rates.
3) The resistance offered by the elastic and viscous medium to the rigid rotations of the micro constituents is the third mechanism of elasticity and dissipation. The dependence of the Cauchy moment tensor on the symmetric part of the classical rotation gradient tensor provides additional elasticity, i.e., stiffness, and its dependence on rates of up to order
of the symmetric part of the rotation gradient tensor provides an additional ordered rate dissipation mechanism with a dissipation spectrum consisting of
pairs of dissipation coefficients corresponding to
rotation gradient rates.
4) All constitutive theories are derived using the representation theorem, integrity (the complete basis of the space of the constitutive tensors), and the conjugate pairs in the entropy inequality, hence are always thermodynamically and mathematically consistent.
5) Material coefficients are derived for the constitutive theories based on integrity, using the principle of smooth neighborhood and a Taylor series expansion of the coefficients used in the linear combination of the invariants and temperature about a known configuration.
6) Simplified (yet general) forms of the constitutive theories are presented, in which the physical meaning of the material coefficients can be established.
7) The constitutive theories derived here are compared with those of Eringen to highlight differences and identify serious shortcomings of the constitutive theories of Eringen et al.
2. Micro and Macro Deformations, Some Basic Considerations
In microcontinuum theories microdeformation of microconstituents influences the macro response of a volume of matter. Consideration of each microconstituent deformation at different locations within a volume of matter is a formidable task. Instead, we consider the entire volume of matter divided into material points, each material point containing microconstituents, with each microconstituent having its own volume
(). Still, the problem is intractable, as each microconstituent location and deformation within the material point would require individual microconstituent considerations. To address this complex problem we assume that the center of mass
of the material point only sees the statistically average response of all microconstituents in its volume
. We further assume that there is a surrogate configuration of microconstituents in which the response of each microconstituent at the material point
is the same, and this response is also the same as the statistically average response of the original configuration of microconstituents. With this assumption, we only need to consider the microdeformation of one microconstituent in a material point. If the matter is isotropic and homogeneous then this treatment for a material point holds for all material points within the volume, and therefore for the entire volume of matter.
Details of this approach are discussed in refs [1] [33] and have been used in ref [33] for deriving nonlinear deformation measures for 3M physics. In ,
is the center of mass of the material point,
and
are the locations of microconstituent
from the center of mass P of the material point and with respect to the fixed
-frame;
is the location of the center of mass
of the material point in the reference or undeformed configuration. Similarly,
and
are the corresponding quantities in the current configuration.
and
are the undeformed and deformed volumes of the material point. Likewise
and
are the undeformed and deformed volumes associated with microconstituent
(see ).
Figure 1. Undeformed and deformed configurations of a material point volume.
and
are called directors in the reference and current configurations. The deformation of
due to
characterizes the micro-mechanics of the microconstituent
. Deformation measures using this concept have been presented by Surana et al. in reference [33].
We note that rigid rotation physics of the microconstituents is present in all 3M theories and appears in exactly the same form. Thus, this physics requires a consistent treatment in the development of 3M theories, independent of type of microcontinuum theory. Eringen uses rigid rotation
of the microconstituents as an unknown degrees of freedom to account for rigid rotation physics. Our view and approach to incorporating this physics in 3M theories [1] [33]-[55] [68]-[70] differs from than that of Eringen.
In every deforming isotropic, homogeneous solid matter classical rotations
due to
constitute a free field in classical continuum mechanics. This field is always present in every deforming solid but does not influence classical continuum physics as it is a free field [1] [33]. Due to the presence of microconstituents, this free field is no longer a free field, since the microconstituent offer resistance to this free field. Surana et al. [1] [33]-[55] [68]-[70] have shown that in all microcontinuum theories the classical rotations
(known) describe rigid rotations of the microconstituent, thus eliminating the need for
as unknown degrees of freedom for the microconstituents. Many other measures, definitions and notations used in this paper are described in references [1] [40] and are not repeated here for the sake of brevity.
3. Degrees of Freedom in Micro Deformation Physics
These have also been discussed by Surana et al., but are essential to describe here as they play a crucial role in the derivation of the constitutive theories. Our views and approach here also differ completely from those of Eringen and are based more on the physics of deformation and available means in the theory to describe it. Conceptually, if we knew the microconstituent displacements, hence the microconstituent strain measures and what follows would be straight forward, but this is not the case, hence an alternate approach is necessary.
, the symmetric part of the microconstituent displacement gradient tensor
, is completely defined if
are known, but in the absence of
we have no choice but to consider six independent components of
as unknown deformational degrees of freedom for the microconstituents. Thus, in our micromorphic theory, a microconstituent has nine degrees of freedom: three rigid rotations
(known) and six independent components of
that are unknown. This choice of degrees of freedom is valid for deriving physically and mathematically consistent constitutive theories.
In Eringen’s work all nine components of
are considered as unknown deformational degrees of freedom in addition to three unknown rigid rotations
. We remark that
contains rigid rotation field of the microconstituents, and therefore should not be used in deriving constitutive theories for the microconstituent stress tensor, as was is in Eringen’s work [16].
4. Conservation and Balance Laws for Linear Micromorphic Continua
The derivation of the conservation and the balance laws for a linear micromorphic microcontinuum solid medium begins by applying the conservation and balance laws of classical continuum mechanics to the microconstituents. From these microconstituent conservation and balance laws, “integral-average” definitions are introduced to derive the corresponding macro conservation and balance laws. There are major differences between the approach used by Surana et al. [1] compared to Eringen [7]-[24]. Major weaknesses in the micromorphic theory presented by Eringen [7]-[24] are summarized in section 9. The conservation and balance laws for a linear micromorphic solid in the Lagrangian descriptions are given in the following.
Conservation of mass, balance of linear momenta, balance of angular momenta, first and second law of thermodynamics and balance of moment of moments are given in the following.
(1)
(2)
(3)
(4)
(5)
(6)
This mathematical model consists of seven partial differential equations: balance of linear momenta (3), balance of angular momenta (3) and the energy Equation (1) in thirty four dependent variables:
. Thus, additional twenty seven equations are needed for closure. Constitutive theories provide twenty one equations:
. Thus, additional six equations are needed for closure. These are discussed in the following section.
5. Additional Six Equations in the Mathematical Model
From the conservation and the balance laws, we note that the microconstituent stress
only appears in the energy equation and the entropy inequality. This, of course, implies that if we were to solve a boundary value problem for isothermal physics, in which case the energy equation is not part of the mathematical model, then the microconstituent stress
is completely absent from the mathematical model. This certainly is not physical, as the microconstituent deformation contributes to macro physics for stationary processes as well as evolutionary processes. Thus, we must have another relationship that considers symmetric stress tensor
and the symmetric part of
.
There are many differences between our work and Eringen’s work on nonclassical theories.
1) Moment tensor (nonclassical mechanics) is defined using
, due to classical mechanics, thus this definition is in error.
2) Due to not using balance of moment of moments balance law, the moment tensor is nonsymmetric.
3) Moment tensor in balance of angular momenta contains permutation tensor. This is obviously in error as the permutation tensor only appears in force terms due to their cross product with distance. This is obviously not needed in case of moment tensor as it is already a moment.
4) In Eringen’s work in the derivation of balance of angular momenta, the skew symmetric components of
are balanced by the gradients of the skew symmetric part of the moment tensor (as the moment tensor has permutation tensor in Eringen’s derivations resulting in three equations). Eringen [7]-[24] and those following his work also suggest that in the derivation of the balance of angular momenta, the permutation tensor must be dropped to obtained another balance law, moments of
and
(only symmetric part) that must balance with gradients of the symmetric part of the moment tensor to obtain additional equations.
5) In references [7]-[24] it is stated that the nine equations in 4) are suitable for determining nine components of
.
6) It has been pointed, discussed and demonstrated that in 3M theories, balance of moment of moments balance law is essential [55] [71]. Due to this balance law, the Cauchy moment tensor is symmetric. Thus, in the balance of angular momenta
are balanced by the gradients of symmetric moment tensor. This is the correct balance of angular momenta.
7) We must recognize that the permutation tensor in balance of angular moment only appears with force terms due to their cross product with distance vector, we just cannot discard it (as suggested by Eringen) as it is due to the physics of moment of forces. It is obvious that what is suggested in (4) has no basis, hence will not lead to any meaningful relations.
8) Thus, in Eringen’s work on balance of angular momenta as well as the six additional equations, both are in error. Our view, approach and outcome to obtain the six additional equations is completely different than Eringen.
Derivation of Additional Six Equations
From the derivation of balance of angular momenta leading to (3) (in Lagrangian description), we note that
has nine independent components, three in
and six in
and
has six independent components. However, presence of permutation tensor on the left side of Equation (3) forces us to discard six symmetric components of
as well as
. This is an important observation that suggests that some how
from the left side of (3) must be eliminated. This of course can be done by premultiplying Equation (3) with
, the inverse of
. Symbolically we can write
(7)
or
(8)
But inverse of
(for values of 1, 2, 3 for
) is
, thus we can write (8) as
(9)
or
(10)
Since
(11)
is balance of angular momenta, (10) reduces to the following.
(12)
At this point choice of negative sign is physical as it would suggest that symmetric part of
and
balance each other, this obviously has to be true at an interface between the microconstituent and the medium, recalling that
are balanced by the gradients of
. Thus, we rewrite (12) with only negative sign.
(13)
Equation (13) are additional six equations that provide closure of the mathematical model.
Remarks
1) First, we note that (3) (balance of angular momenta) only contains nonclassical physics, both
and
are due to nonclassical physics, whereas (13) contains stresses due to classical mechanics. This is necessary for maintaining consistency of physics in the derivations.
2) When the microconstituents and the medium are of the same material, then naturally (13) must hold. When the microconstituents and the medium are of different material, (13) must also hold at the interface, continuity of stress due to classical physics, while
is taken care by the gradients of moment tensor, both
and moment tensor are due to nonclassical physics.
6. Microconstituent Stress Tensor
Due to Micro Cauchy Stress Tensor
(or
)
The integral average definition
(14)
considers total stresses
and
without any additive decomposition into equilibrium and deviatoric components. Secondly, if we consider a decomposition of the stress tensor
and
to define volumetric and distortional deformation of the microconstituent, then the microconstituent density
would be needed to describe volumetric deformation, but
is removed by the integral-average definition. Both of these aspects suggest that we must consider
or
purely as arising from mechanical loading, and therefore as a function of the work conjugate strain tensor and the elastic properties of the microconstituents. Thus, in the following, we consider
or
as a constitutive tensor with the work conjugate strain tensor and temperature
as its arguments.
7. Constitutive Theories for Linear Micromorphic Solid Continua
In deriving the constitutive theories we consider comprehensive thermoelastic behavior with dissipation (without rheology). We assume that the medium is elastic and has dissipation mechanism. The micro constituents naturally have elasticity but we assume that each microconstituent has its own dissipation mechanism. Additionally, rigid rotations of the microconstituents in a viscous elastic medium result in elasticity as well as a dissipation mechanism. Thus, in the derivation of the constitutive theory for
and
, elasticity and dissipation physics are considered for the microconstituents, the solid medium, and the interaction of rigid rotations of the microconstituents with the viscoelastic solid medium. Furthermore, all three dissipation mechanisms use higher order rates of strains, and therefore result in ordered rate constitutive theories with dissipation spectra for each of the three constitutive theories, corresponding to the strain rates considered.
7.1. Initial Determination of Constitutive Tensors and Their Argument Tensors
In deriving constitutive theories, we always begin with rate of work or the corresponding conjugate pairs in entropy inequality for determination of constitutive tensors based on causality axiom of constitutive theory and their possible argument tensors. The choice of constitutive tensors can be altered if the physics requires so and the argument tensors of the constitutive tensors can be augmented with additional tensors such physics was not considered when deriving the entropy inequality. We follow the details and guidelines presented in references [72] [73]. Once the constitutive tensors and their argument tensors are established, we follow the theory of isotropic tensors or the representation theorem in deriving the constitutive theories, and the standard procedure of a Taylor series expansion of the coefficients used in the linear combination of the basis of the constitutive tensor space [72] [73].
Consider entropy inequality (5)
(15)
The macro stress tensor
is nonsymmetric, and therefore cannot serve as a constitutive tensor due to the representation theorem. Thus, we need an additive decomposition of
into the symmetric tensor
and the skew-symmetric tensor
. There cannot be a constitutive theory for
, as it is already defined by gradients of Cauchy moment tensor due to the balance of angular momenta. Thus,
is the constitutive tensor and not
or
.
(16)
Secondly
(17)
in which
is the displacement gradient tensor and
and
are the symmetric and skew symmetric tensors obtained by the additive decomposition of
.
(18)
Likewise, additive decomposition of
and
into symmetric and skew symmetric tensors gives:
(19)
Also
(20)
and
(21)
in which
is micro displacement gradient tensor and
and
are symmetric and skew symmetric tensors due to additive decomposition of
. Furthermore,
(22)
also
(23)
Substituting (16)-(23) in the entropy inequality (5) and noting that
(24)
We can write (15) as follows:
(25)
From balance of angular momenta
(26)
Substituting (26) in (25)
(27)
A simple calculation shows that
(28)
Using (28) in (27), (28) reduces to
(29)
Further additive decomposition of
into equilibrium and deviatoric stress
is needed to derive constitutive theory for volumetric and distortional deformation physics that are mutually exclusive.
(30)
substituting (30) in (29)
(31)
rate of work conjugate pairs and the last term in (31) in conjunction with the axiom of causality [72] [73] imply that
and
are valid choices of constitutive tensors provided volumetric change for microconstituents i.e.,
(equilibrium micro constituent stress) is not considered in which case
. The initial choice of constitutive tensors and their argument tensors is (with
included as an argument tensor in all constitutive tensors because of non-isothermal physics):
(32)
(33)
(34)
(35)
(36)
Even though we do not need a constitutive theory for Φ, its argument tensors are essential to establish, since it is used to simplify the entropy inequality (31) as well as to derive the constitutive theory for
. The presence of
in (31) must be addressed as well. The Helmholtz free energy density Φ must show dependence on
and
. In the Lagrangian description
is not permissible as an argument tensor as it is not a dependent variable, but we use it in (32) in a symbolic sense. Other argument tensors of Φ and
are chosen based on the principle of equipresence as we do not have any other basis for their choice. However, the principle of equipresence is not used in (32) - (36) as the conjugate pairs in the entropy inequality (31) clearly dictate the choices of argument tensors:
(37)
(38)
7.2. Constitutive Theory for Equilibrium Cauchy Stress Tensor
In Lagrangian description, density
is deterministic from the conservation of mass
once the deformation gradient tensor
is known,
hence
cannot be an argument tensor of the constitutive tensors [73]. However, compressibility and incompressibility physics is related to density and temperature. Thus, the constitutive theory for
cannot be derived using entropy inequality (31) in Lagrangian description, instead we must consider entropy inequality similar to (31) in Eulerian description.
(39)
In this case
is unknown, hence is a dependent variable in the mathematical model. Following same procedure as for Lagrangian description, the constitutive tensors and their argument tensors (including
and
) are given by:
(40)
(41)
(42)
(43)
(44)
(45)
(46)
Using (45) we can write
(47)
From conservation of mass in Eulerian description
(48)
substituting from (48) for
in (47) and then substituting (47) in (39), we obtain the following after regrouping the terms
(49)
The entropy inequality (49) holds for arbitrary but admissible choices of
and
if the following conditions hold:
(50)
(51)
(52)
(53)
(54)
Equations (50)-(54) implies that
is not a function of and
. Equation (54) implies that
is deterministic from
, hence
is not a constitutive or dependent variable. Using (50)-(54), the constitutive tensor and their argument tensors in (40)-(44) remain the same, but the argument tensors of
and
can be modified:
(55)
(56)
and the entropy inequality (49) reduces to
(57)
Constitutive theory for
for compressible matter can be obtained by setting coefficient of
in the first term of (57) to zero.
(58)
(59)
in which
is thermodynamic pressure or equation of state for the compressible matter. When the deforming matter is incompressible, there is no change in volume. Thus, for a fixed mass, the density is constant i.e.,
. For this case, from conservation of mass, we have:
(60)
and
(61)
Hence, for incompressible solid, the constitutive theory for
cannot be derived using (58) and (59). First, using (61), the entropy inequality (57) reduces to
(62)
In order to derive constitutive theory for
for incompressible solid matter, we must introduce incompressibility condition in (62). From continuity equation, the velocity field for incompressible matter is divergence free i.e.,
(63)
If (63) holds, then the following holds too:
(64)
in which,
is a Lagrange multiplier. Adding (64) to (62) and regrouping terms
(65)
Entropy inequality (65) holds for arbitrary but admissible
, if the coefficient of
in the first term in (65) is set to zero, giving:
(66)
In (66),
is mechanical pressure. The reduced form of entropy inequality is given by:
(67)
In Lagrangian description, the constitutive theory for
can be obtained directly from (58), (59) and (66).
(68)
(69)
The reduced form of entropy inequality in Lagrangian description follows directly from (67).
(70)
In the following, we present derivation of constitutive theories for
and
using representation theorem [56]-[67].
are symmetric tensors of rank two and their conjugate
and are also symmetric tensors of rank two.
and
are tensors of rank one. Thus, there is no difficulty in deriving constitutive theories for all four constitutive tensors using representation theorem. Furthermore, in the constitutive theories for
and
we consider elasticity and dissipation mechanisms. Dissipation mechanisms are ordered rate mechanism, hence yield dissipation spectrum in each constitutive theory.
7.3. Constitutive Theory for
Cauchy Stress Tensor
We consider the medium to be linear elastic. We begin with conjugate pair
in the reduced form of the entropy inequality (70). This conjugate pair in conjunction with axiom of causality suggest that
is the constitutive tensor and
as its argument tensor. Thus, we can write (
is included as the argument tensors due to non isothermal physics)
(71)
We know from physics of viscous fluids that dissipation requires strain rate, same as rate of strain in Lagrangian description, thus
or
should be argument tensor of
. We generalize the dissipation mechanism by considering strain rates up to orders
i.e., by considering
as argument tensors of
. Thus, we have
(72)
are symmetric tensors of rank two and
is a tensor of rank zero. Thus, we can use representation theorem to derive constitutive theory for
.
Let
be the combined generators of the argument tensors of
in (72) that are symmetric tensors of rank two and let
be the combined invariants of the same argument tensors of
in (72). Then,
constitute the basis of the space of tensor
, also referred to as integrity. Now,
can be expressed as a linear combination of the basis in the current configuration.
(73)
in which
are coefficients in the linear combination (73). The material coefficients in (73) are determined by expanding
in the invariants
and the temperature
about a known configuration
and only retaining up to linear terms in
and temperature
(to simplify the resulting constitutive theory).
(74)
Substituting
and
from (74) into (73)
(75)
Collecting coefficients of
and
, we can write (75) as follows:
(76)
The material coefficients
and
are defined in the following:
(77)
The constitutive theory (76) with material coefficients (77) is based on integrity, complete basis of the space of constitutive tensor
. Desired simplified forms can be obtained from (76) by retaining specific generators and invariants. This constitutive theory is ordered rate constitutive theory of orders
of strain tensors. Material coefficients can be functions of
and
in a known configuration.
Simplified form of (76) can be obtained by retaining desired generators and the invariants. Perhaps a simplified yet most general constitutive theory for
is one in which
is a linear function of the components of its argument tensors. Redefining material coefficients and rearranging terms in (76) we can write the following:
(78)
in which
is initial stress field,
and
are Lames constants,
and
is the spectrum of damping coefficients corresponding to strain rates
,
is thermal modulus.
A further simplified model that is commonly used is obtained for
i.e., strain rate of order one only. In this case (78) reduces to
(79)
7.4. Constitutive Theory for Micro Stress Tensor
We consider microconstituent to have elasticity and dissipation mechanisms. Thus, following Section 7.3, we can choose the following for the constitutive tensor and its argument tensors related to microconstituent stress.
(80)
where
is the highest order of rate of strain
. Let
be the combined generators of the argument tensors of
in (80) and let
be the combined invariants of the same argument tensors of
in (80), then
constitutes the basis of the space of constitutive tensor
and we can write the following for
.
(81)
in which
(82)
Following the procedure described in Section 7.3 (Taylor series expansion) we can derive the following constitutive theory for
(83)
in which material coefficients are given by (77) after replacing
with
and replacing
and
by
and
and
by
. The material coefficients can be functions of
and
in a known configuration
. This constitutive theory is based on integrity. A constitutive theory for
that is linear in the components of the argument tensors and is of order
is given by (after redefining material coefficients)
(84)
This constitutive theory is of orders
in rates of microconstituent strain
. When
, we obtain the most simplified constitutive theory for
.
(85)
7.5. Constitutive Theory for Moment Tensor
Rigid rotations and rotation rates of the microconstituents in the elastic and viscous medium result in: 1) elasticity due to rotation gradient tensor, 2) dissipation due to viscous drag experienced by the microconstituents due to rates of the rotation gradients. If
are the rate of symmetric part of rotation gradient tensor, then we can write:
(86)
Let
be the combined generators and let
be the combined invariants of the same argument tensors, then
forms the basis of the space (integrity) of constitutive tensor
and we can write the following for
:
(87)
in which coefficients
(88)
Following the procedure described in section 7.3 (Taylor series expansion), we can derive the following constitutive theory for
:
(89)
in which material coefficients are given by after replacing
and
with
and
and
by
. The material coefficients can be functions of
and
in a known configuration
.
A constitutive theory that is linear in the components of the argument tensor is given by:
(90)
When
, we have the simplest possible constitutive theory for
:
(91)
7.6. Constitutive Theory for
In this derivation, we consider (based on conjugate pairs in the reduced entropy inequality)
Considering
(92)
Tensors
and
are tensors of rank one and
is a tensor of rank zero. The only combined generator of rank one of the argument tensor
and
is
, hence based on representation theorem, we can write:
(93)
The coefficient
is a function of the combined invariants of
i.e.,
and temperature
. Let us define
to simplify the details of further derivation. We note that (93) holds in the current configuration in which the deformation is not known. Hence, in (93),
is not yet deterministic and it is not a material coefficient. To determine material coefficients in (93), we expand
in Taylor series about a known configuration
in
and
and retain only up to linear terms in
and
(for simplicity)
(94)
Substituting (94) into (93)
(95)
We note that
and
are functions of
and
, whereas
in (93) is a function of
and
in the current configuration. From (95), we can write the following, noting that
(96)
or
(97)
Let
(98)
(99)
(100)
Then,
(101)
This is the simplest possible constitutive theory based on conjugate pairs in the entropy inequality, representation theorem and (92). This constitutive theory uses integrity, the complete basis of the space of
. The only assumption in this theory beyond (92) is the truncation of the Taylor series in (94) beyond linear terms in
and
. The constitutive theory for
in (101) is cubic in
. It contains linear and cubic terms in
, but does not contain a quadratic term in
. Simplified linear theory is given by (101) by retaining only the first term on the right hand side of (101) (Fourier heat conduction law).
8. Thermodynamic and Mathematical Consistency of the Linear Micromorphic Theory Presented in the Paper
Surana et al. have shown in their earlier paper that the linear micromorphic microcontinuum theory presented for thermoelastic solids is thermodynamically and mathematically consistent. This is also the case for thermoviscoelastic solids. Significant aspects of the linear micromorphic theory presented in ref [1] are: strict use of classical continuum mechanics for microconstituents, valid integral-average definitions and their use in the derivation of macro conservation and balance laws, additively separating microconstituent deformation and its rigid rotations, use of classical rotations
to define microconstituent rigid rotations, use of conjugate pairs in the entropy inequality to determine constitutive tensors and the initial choice of their argument tensors in conjunction with the axiom of causality, ensuring that constitutive tensors of rank two are symmetric tensors and their argument tensors of rank two are also symmetric tensors of rank two, strict adherence to the representation theorem in deriving constitutive theories, use of valid deformation measures derived in ref [33], appropriate additive decomposition of stress tensors to accommodate correct physics and to obtain valid constitutive tensors. Additionally, derivations of the constitutive theories presented in this paper for thermoviscoelastic solids with dissipation are carried out strictly using the theory of isotropic tensors and the entropy inequality, and are therefore thermodynamically and mathematically consistent. Thus, the complete mathematical model including the constitutive theories is thermodynamically and mathematically consistent.
9. Linear Micromorphic Theory of Eringen
Surana et al. in a recent paper have also presented an extensive discussion of Eringen’s micromorphic theory including various issues, inconsistencies, incorrect definitions, questionable derivations of some balance laws and constitutive theories, which suggest that the micromorphic theory presented by Eringen may have serious concerns. Some of these, reported in ref [1], are summarized here: the microconstituents have nine deformational degrees of freedom, six due to
and three unknown rigid rotations
; use of a weighted integral of balance of micro linear momenta has no physical or mathematical basis and yields balance of angular momenta that cannot be derived using well known conventional approach; introduction of a third rank moment tensor for nonclassical physics using
which is due to classical continuum mechanics, is invalid; use of the permutation tensor with the moment tensor in the balance of linear momenta is in error, use of nonsymmetric constitutive tensors (of rank two) and their nonsymmetric argument tensors is not supported by the theory of isotropic tensors, necessity of an additional balance due to a new kinematically conjugate pair of rotations and moments is completely ignored, leading to spurious constitutive theories; use of phenomenologically constructed potentials containing nonsymmetric tensors of rank two to derive constitutive theories for nonsymmetric tensors of rank two has no basis based on the representation theorem; additive decomposition of
is not employed to separate
, which cannot be part of a constitutive tensor as it is defined by the balance of angular momenta; the principle of equipresence introduces non physical coupling between classical and nonclassical physics; conservation of micro inertia as a conservation law introduced to obtain additional equations for closure of the mathematical model is neither needed nor used in the theory presented in ref [1]. It is thus conclusive, based on the points discussed in ref [1] and summarized above, that Eringen’s micromorphic theory has many serious concerns and lacks thermodynamic and mathematical consistency.
10. Summary and Conclusions
The thermodynamically and mathematically consistent linear micromorphic microcontinuum theory derived by Surana Sting of conservation and balance laws is utilized in the present work to derive constitutive theories for a linear micromorphic elastic continuum with dissipation. The significant aspects of the constitutive theories are:
1) Classical rotations
describing rigid rotations of the microconstituents are separated from the argument tensor of the constitutive stress tensors.
2) Appropriate additive decomposition of the stress tensor
is considered to separate volumetric and distortional physics and to ensure that
is not part of the constitutive tensor as it is defined by the balance of angular momenta.
3) All constitutive tensors of rank two are symmetric with symmetric argument tensors of rank two, as necessitated by the representation theorem.
4) The constitutive theories naturally provide a mechanism of elasticity for the microconstituent, for the medium of the volume of matter as well as for the interaction of the microconstituent with the medium (due to rigid rotations
). The dissipation mechanisms for microconstituents (due to
), for the volume of the medium (due to
) and due to interaction of the microconstituents with the medium (function of rates of the symmetric part of the rotation gradient tensor) are all ordered rate mechanisms. That is each dissipation physics can be considered to be dependent on up to the desired orders of the conjugate rates. Thus, in these constitutive theories there is a spectrum of dissipation coefficients for each of the three dissipation mechanisms.
5) All constitutive theories are initiated using conjugate pairs in the entropy inequality and are derived using the representation theorem, and are therefore thermodynamically and mathematically consistent.
Acknowledgements
The first author is grateful for his endowed professorships and the department of mechanical engineering of the University of Kansas for providing financial support to the second author. The computational facilities provided by the Computational Mechanics Laboratory of the mechanical engineering departments are also acknowledged.