A Nonlinear Micropolar Continuum Theory for Thermoviscoelastic Solid Medium Based on Classical Rotations ()
1. Introduction, Literature Review
In the comprehensive works published by Eringen and Eringen et al. [3]-[21] and references [22]-[24] on 3M nonclassical continuum theories, it is relatively easy to conclude that whatever needs to be done regarding the theoretical foundations of 3M linear and nonlinear nonclassical continuum theories has already been done and that what remains are probably the applications. However, upon closer examination, we find that this indeed is not the case. In the works published by Eringen and Eringen et al., as well as by many other researchers who follow the approaches introduced by Eringen and Eringen et al., there are some serious shortcomings, omissions, and the use of mathematically unjustifiable approaches that have led to linear and nonlinear micropolar nonclassical continuum theories that are thermodynamically and/or mathematically inconsistent; hence, they are not valid nonclassical micropolar continuum theories. We will list some of the concerns and issues below and discuss their consequences on the resulting nonclassical continuum theories.
(a) Yang et al. [25] and Surana et al. [26] [27] have shown that balance of moment of moments is an essential balance law in all micropolar nonclassical continuum theories. When this balance law is used, the Cauchy moment tensor becomes symmetric. The constitutive theory for the nonsymmetric moment tensor has been addressed using two approaches: (1) in the first approach, the nonsymmetric tensor is considered as a constitutive tensor with nonsymmetric tensors as its argument tensors (amongst others). This approach is used almost exclusively in all published works of Eringen and Eringen et al. and by those that follow Eringen. It is now well established due to works of Zhang, Wang, Spencer and Smith [28]-[39], that for a nonsymmetric constitutive tensor, the basis of the space of the constitutive tensor cannot be established. Thus, nonsymmetric constitutive tensors lead to constitutive theories (derived in published works by using potentials or polynomial approach) that are in violation of basic principles of mathematics, hence cannot be valid constitutive theories. (2) In the second approach, the nonsymmetric Cauchy moment tensor is additively decomposed into symmetric and skew symmetric tensors (Surana et al. [26] [27]) followed by derivation of constitutive theories for each using representation theorem. This approach is mathematically consistent based on the works of Zhang, Wang, Spencer and Smith [28]-[39]. Surana et al. [26] [27] have shown using simple 2D micropolar physics that this approach leads to nonphysical constitutive theories. Thus, in the absence of balance of moment of moments balance law, there are no valid means of deriving constitutive theory for the Cauchy moment tensor. This is a major problem in all 3M nonclassical continuum theories of Eringen and Eringen et al. This is significant enough to question the validity of the published works on 3M.
(b) The strain measures presented by Eringen [8] are in fact deformation measures. These are derived using expressions that are not dimensionless and hence fail to yield the simple linear strain measure (change in length per unit length) for 1D case. These measures in their original form or in the modified form may be viewed as strain measures if they appear in the rate of work conjugate pairs in the entropy inequality.
(c) In any deforming solid continua, the deformation consists of elongation of the material lines and change in angle between them and rigid rotation of the material lines. Additive decomposition of the displacement gradient tensor
(linear elasticity) into symmetric
and skew symmetric tensors
allows us to separate strains (
) and the rotations
. Energy equation and the entropy inequality establish rate of work conjugate pairs that enable determination of constitutive tensors and their argument tensors. We remark that choice of
or
as argument tensors of the stress tensor is invalid. Important point to note is that rigid rotations (as in
) or strain plus rigid rotations (as in
) cannot be argument tensor of the stress constitutive tensor. The deformation measures [1] clearly show the strain measure for rigid microconstituents in micropolar nonclassical continuum theory to be zero. Thus, equations (20.1) and (20.6) in ref. [8], which consider strain measure as
plus rotations of microconstituents and then use this measure as an argument of stress tensor, have no meaning. A constitutive theory for stress tensor based on this strain measure is obviously in violation of thermodynamics (second law) and is bound to be erroneous.
(d) In micropolar nonclassical continuum theory, balance of angular momenta defines antisymmetric Cauchy stress tensor in terms of the gradients of the Cauchy moment tensor. If we have constitutive theory for Cauchy moment tensor (which we do), then the antisymmetric Cauchy stress tensor is defined, hence cannot be part of the constitutive theory in the stress tensor. This requires additive decomposition of
i.e.,
in which only
, the symmetric part of contravariant Cauchy stress tensor
, can be a constitutive tensor. A single constitutive theory for
must address volumetric as well as distortional deformation that are mutually exclusive; this is obviously not possible. Further additive decomposition of
is needed to describe volumetric (constitutive theory for equilibrium tensor,
) and distortional (constitutive theory for deviatoric
tensor) deformation physics that are mutually exclusive. None of these aspects are discussed in the literature on micropolar nonclassical continuum theories. In our view, the published work in this area lacks clarity, consistent use of concepts related to physics, and of course, the derivations of the constitutive theories are in total violation of the representation theorem.
(e) In case of linear micropolar nonclassical continuum theory, the deformation measures of references [1] clearly show that the theory must only consider rigid rotations of the microconstituents. If we assume that rigid rotations
of the microconstituents are unknown degrees of freedom at a material point (Eringen, Eringen et al. and others), then a material point has
classical rotations (known in terms of displacement gradients) and unknown rotations
. In the published works, linear micropolar nonclassical continuum theory based on
and
(neglecting
) have been reported by many researchers. Surana et al. [40] [41] have shown that linear micropolar nonclassical continuum theory based on these two rotation considerations lead to spurious conjugate pairs in the entropy inequality that necessitate constitutive theory for
, which of course is not physical as
are defined by balance of angular momentum equations. In our view [1], all published works on linear micropolar nonclassical continuum theory based on
and
are in violation of physics, hence result in invalid micropolar nonclassical continuum theory.
(f) Principle of equipresence used almost exclusively in published micropolar nonclassical continuum theory is not supported by second law of thermodynamics. It creates nonphysical coupling between classical and nonclassical physics in the micropolar nonclassical continuum theory.
In view of (a)-(f), the published works on 3M nonclassical continuum theory, whether linear or nonlinear, there are many concerns, hence, the theories are questionable. In published work on micropolar nonclassical continuum theory, the thermodynamic and mathematical details use many questionable and unfounded approaches that cannot be supported by thermodynamic principles or mathematics. Thus, the natural question arises: Do we have any valid linear and nonlinear micropolar nonclassical continuum theory at present that is thermodynamically and mathematically consistent? We discuss answer to this question below. Surana et al. [1] [2] [26] [27] [40]-[43] have shown the following in these works:
(1) Classical rotations (
) constitute a free field in classical continuum mechanics. It is always present undisturbed, hence has no effect on the development of classical continuum theory. This implies that each material point in the deformed solid medium has rotations
at the material points about the axes of triad, axes being parallel to
-frame. The presence of microconstituents offers resistance to the free field; as a consequence, the free field is no longer a free field, but instead defines the rigid rotations of the microconstituents i.e.,
are the rotations of the rigid microconstituents (see [1] for explanation). Thus, we see that classical rotations
are sufficient to account for the rigid rotations of the microconstituents. This eliminates the need for
as additional unknown dofs at a material point, hence the need for spurious and nonphysical constitutive theory for
necessitated due to presence of
as unknown degrees of freedom at a material point.
(2) Balance of moment of moments must always be used as a balance law in all nonclassical continuum theory (Yang et al., [25], Surana et al. [26] [27]). When this balance law is used, Cauchy moment tensor is symmetric and the problems associated with the constitutive theory for nonsymmetric moment tensor are eliminated.
(3) Based on (1) and (2), Surana et al. [1] [40] [41] have presented thermodynamically and mathematically consistent linear micropolar nonclassical continuum theory for solid and fluent media with successful model problem studies. To our knowledge, works of Surana et al. are the only works that contain valid linear micropolar nonclassical continuum theory that are supported by thermodynamics and mathematics. Model problem studies confirm that the micropolar nonclassical continuum theory based on
contain correct micropolar physics. Thermodynamic and mathematical consistency of linear micropolar nonclassical continuum theory based on
is assurance of its validity.
(4) Surana et al. [40] [41] addressed thermodynamic and mathematical consistency of linear micropolar theories based on rotations
,
and
with the conclusion that the only linear micropolar theory based on rotations
is a valid linear micropolar theory.
(5) In references [44]-[46] authors derived conservation and balance laws for micropolar medium for finite deformation/finite strain physics using first Piola-Kirchhoff stress
, first Piola-Kirchhoff moment
, rate of deformation gradient tensor
and the rate of classical rotation gradient tensor, , use of these measures is convenient in the derivation, but the final form of the conservation and balance laws can always be expressed in terms of contravariant second Piola-Kirchhoff stress tensor
and contravariant second Piola-Kirchhoff moment tensor
and their conjugate rates as shown in this paper. These are valid measures for finite deformation/finite strain physics. Additive decomposition of
and
are used. The constitutive theory for
in terms of thermodynamic pressure is derived using entropy inequality in Eulerian description. The final reduced form of the entropy inequality contains constitutive tensors
and
with conjugate tensors
and , where
and
being tensors of rank one, and all others are symmetric tensors of rank two. Constitutive theories for
,
and
are derived using representation theorem. This nonlinear micropolar nonclassical continuum theory is thermodynamically and mathematically consistent, and the mathematical model consisting of conservation and balance laws and the constitutive theories has closure. To our knowledge, this is the only thermodynamically and mathematically consistent nonlinear micropolar nonclassical continuum theory for thermoviscoelastic solid matter available in the published literature.
2. Scope of Work
In this paper, we present finite deformation/finite strain nonlinear micropolar nonclassical continuum theory for compressible thermoviscoelastic solids. This nonlinear micropolar nonclassical continuum theory incorporates the finite deformation/finite strain deformation physics for thermoelastic solid, but also incorporates mechanisms of dissipation that are absent in the nonlinear micropolar nonclassical continuum theory for thermoelastic solids. We begin with the conservation and balance laws in references [1] [26] [41] for finite deformation/finite strain micropolar physics expressed in terms of
,
and their rate of work conjugates
and .
are convenient to use in the derivation of the conservation and balance laws but these are not valid measures for finite deformation/finite strain physics. Expressing
and
in terms of
and
, contravariant second Piola-Kirchhoff stress and moment tensors and establishing their rate of work conjugate is not straight forward due to micropolar physics. This is an important aspect of the derivation presented in this paper. Of course, without the valid rate of work conjugate, the constitutive theories cannot be derived. Thus, there are two important aspects of the work presented in this paper: (1) conservation and balance laws expressed in terms of
and
with thermodynamically valid rate of work conjugates (2) the second aspect of the work is derivation of ordered rate constitutive theories for
and
based on the conjugate pair in the entropy inequality and theory of isotropic tensors, thus ensuring thermodynamic and mathematical consistency of the resulting mathematical model. Theories incorporate micro as well as macro ordered rate nonlinear deformation mechanism. The additive decomposition of
;
;
is necessary to consider various aspects of deformation physics. The constitutive theory for equilibrium stress tensor
describing volumetric deformation physics remains the same as in ref. [42] [43]; hence, only the final forms of the equations related to the constitutive theory for equilibrium stress tensor are presented. Constitutive theories for
and
address distortional deformation physics as well as dissipation mechanisms. The rate of work conjugate pair
in the reduced form of the entropy inequality suggests that elasticity must be due to
and dissipation mechanism is due to
i.e., Green’s strain rate of order one. In the present work, we generalize this nonlinear dissipation mechanism to be a function of Green’s strain rates of up to order
i.e., dependent on
. Thus, we have ordered rate theory for the dissipation of the medium, which is entirely due to viscous drag forces between the particles of the medium. The second nonlinear mechanism of dissipation is due to microconstituents and the viscosity of the medium, micro viscous dissipation or micro dissipation. The rigid rotations of the microconstituents must overcome the viscous drag forces due to surrounding viscous medium. This mechanism is naturally a function of the rotation rates of the microconstituents. Based on this line of reasoning and using classical rotations
, we have a free field
and associated rotation rate
field in the absence of microconstituents. Due to the presence of microconstituents, the rotations
and their rates
are in fact rotations and rotation rates of the microconstituents. The mechanical work expended due to the rotations of the microconstituents in overcoming viscous drag results in additional entropy generation that influences thermal field. This mechanism of dissipation, micro dissipation or micro viscous dissipation, is also incorporated in the present work as an ordered rate theory of up to order
. The constitutive theories for
and
are derived using integrity (complete basis) in conjunction with representation theorem. In each case, material coefficients are derived. The material coefficients can be a function of the combined invariants of the argument tensors of each constitutive tensor and temperature
. Simplified constitutive theories that are linear in the components of the argument tensor are also presented. Linear micropolar nonclassical continuum theory is shown to be a complete subset of nonlinear micropolar nonclassical continuum theory presented in this paper. Also, the nonlinear finite deformation/finite strain classical continuum theory remains intact when micropolar physics is discarded. It is shown that the nonlinear micropolar nonclassical continuum theory for thermoviscoelastic solid presented in this paper is thermodynamically and mathematically consistent, and that the mathematical model consisting of conservation and balance laws and constitutive theories has closure.
3. Consideration of Various Measures
In the following, we present a short summary of various measures considered in deriving the conservation and balance law and the constitutive theories for nonlinear micropolar nonclassical continuum theory for compressible thermoviscoelastic solid matter. In finite deformation physics, use of contravariant Cauchy stress tensor and derivation of corresponding first and second Piola-Kirchhoff stress tensors using correspondence rules is commonly used in classical continuum mechanics [42] [43]. In the case of nonlinear micropolar nonclassical continuum theory, these measures also remain valid. Additionally, we have contravariant Cauchy moment tensors and derivations of corresponding first and second Piola-Kircchoff moment tensors. The Cauchy principle holds for co- and contra-variant stress and moment tensors [42]-[46], and interrelationships between Cauchy, first and second Piola-Kirchhoff stress tensors as well as moment tensors provide flexibility in terms of a suitable choice of measure that maintains simplicity in the details of the derivations. Following references [42] [43] [45] [46], we have the following (for compressible matter):
Cauchy principle:
(1)
(2)
Correspondence rules for first, second Piola-Kirchhoff stress and moment tensors:
(3)
(4)
We note that since
is not symmetric.
and
are nonsymmetric as well. When balance of moment of moments is used as a balance law,
is symmetric, hence
is symmetric but
remains not symmetric.
4. Classical Rotations, Their Gradients and Other Considerations
In reference [1], authors have discussed that in the absence of microconstituents, the classical rotation field is a free field, hence the classical continuum theories are not affected by its presence. Based on classical continuum mechanics in every deforming solid matter, the classical rotation field exists as a free field. In the presence of microconstituents, the classical rotation field is no longer a free field, instead it describes the rigid rotations of the microconstituents. A simple example illustrates this quite well. Consider 1D axial deformation of an unconstrained rod subjected to a force at the right end. The rigid body translations of the rod is a free field that has no affect on the deformation of the rod as all points of the rod are moving in the same direction by the same amount. If we constrain the left end of the rod from moving, then the deformation field is no longer a free field and is in fact the actual deformation field of the constrained rod with load on the right end. Thus, we see that the obstruction (constrained left end in this case) changes the free field to the actual deformation field of the constrained rod. Our situation of
as a free field and the microconstituents obstructing this free field is exactly similar to the axial rod. That is the free field
in the presence of microconstituents becomes a rotation field
describing the rotations of the microconstituents, meaning
are in fact the rotations of the microconstituents.
Thus, in micropolar theory requiring rigid rotations of the microconstituents, classical rotations serve as their rigid rotations. Furthermore, it has been shown in references [40] [41] that if we consider rigid rotations of the microconstituents as additional unknown degrees of freedom at the material points, a valid linear micropolar theory that is thermodynamically and mathematically consistent is not possible. In case of linear micropolar theories [40] [41], authors have shown that a micropolar theory based on classical rotations as rigid rotations of the microconstituents is always thermodynamically and mathematically consistent provided balance of moment of moments is used as a balance law and the constitutive theories are derived using representation theorem. The work presented in this paper for nonlinear micropolar continuum theory for thermoviscoelastic solids is strictly based on classical rotations as rigid rotations of the microconstituents, thus in this micropolar theory a material point only has three translational degrees of freedom. Some details of classical rotations
, their gradients, stress and moment tensors are given below:
(5)
(6)
(7)
(8)
(9)
(1)-(9) are basic measures, definitions and relations that are used in deriving the conservation and balance laws and the constitutive theories.
We note that
appears in
. In the conservation and balance laws, we must use
,
and
as these are valid measures for finite deformation/finite strain physics. However, since this is a relationship between
,
,
and
,
and
, for the sake of simplicity in the derivation of the conservation and the balance laws, we can use
,
and
and finally express this in
,
and
using relationship between them. The deformation measures for nonlinear 3M theories derived in ref. [1] are utilized in conjunction with entropy inequality.
5. Conservation and Balance Laws
Consider conservation and the balance laws derived in references [1] [41] for finite deformation/finite strain physics of micropolar medium using
and . Conservation of mass, balance of linear momenta, balance of angular momenta, first and the second law of thermodynamics are given below:
(10)
(11)
(12)
(13)
(14)
(15)
This mathematical model contains:
, a total of 22 dependent variables, but has only balance of linear momenta (3), balance of angular momenta (3) and first law of thermodynamics (1), seven partial differential equations in total. Thus, an additional 15 equations are needed for closure. These are provided by the constitutive theories for stress tensor (6), moment tensor (6), and heat vector (3).
6. Constitutive Theories
In the derivation of the constitutive theories, the first important step is to establish constitutive tensors and their argument tensors. The entropy inequality and axioms of constitutive theory suffice for this purpose. Based on the conjugate pairs
,
and and axioms of constitutive theory,
are likely the initial choice for the constitutive theories.
and
are all nonsymmetric tensors of rank two, hence cannot be utilized in deriving constitutive theories using representation theorem. Thus, at this stage, we have:
(16)
Through additive decompositions, all nonsymmetric second rank tensors must be expressed as symmetric and skew-symmetric tensors. Additionally, the last term in (15) must also be addressed i.e., either eliminated by substitution or quantified otherwise, so that entropy inequality is not effected by its arbitrary but admissible value. We present details below:
From balance of angular momenta, we have:
(17)
Using (17), the last term in (15) can be written as:
(18)
A simple calculation shows that
(19)
Therefore,
(20)
Using (20), the entropy inequality (15) can be written as:
(21)
Consider
term in (21)
(22)
Consider term in (22)
(23)
We consider each term in (23)
(24)
(25)
(26)
(27)
(28)
(29)
(30)
(31)
Substituting (24)-(31) in (23), we obtain
(32)
Substituting from (32) into (22) we obtain
(33)
Substituting from (33) into (21), and noting that terms cancel, we obtain the following form of entropy inequality:
(34)
We substitute
in the last term of (34):
(35)
Substituting (35) in (34), we obtain the final form of entropy inequality:
(36)
From the entropy inequality (36), we observe that
and are rate of work conjugate to
and
(symmetric).
We must check the validity of these rate terms in (36) by comparing them with the nonlinear deformation measures given by:
(37)
in which
is the micro deformation gradient tensor. Its additive decomposition into symmetric and skew symmetric components contains microconstituent rigid rotations
in the skew symmetric part of tensor. Since microconstituent rigid rotations are in fact classical rotations
(due to free field in the absence of microconstituents), in (37) we can replace
by
i.e., in place of
by
and
by
.
(38)
These measures in the form listed in (38) or with some minor modifications must be utilized in the nonlinear micropolar nonclassical continuum theory for compressible thermoviscoelastic solid without memory. From entropy inequality (36), we note
and
as constitutive tensors and
and
as their argument tensors are valid based on axiom of constitutive theory in the nonlinear micropolar nonclassical continuum theory for thermoviscoelastic solid. Thus, we see that
is a deformation measure in (37) and not a strain measure. We need to multiply by
to obtain strain measure
, then it is valid argument tensor of
. Likewise,
is not conjugate to
either, we need to multiply by
to obtain a measure conjugate to
. We remark that as pointed out in ref. [1] and substantiated here, the derivations of strain measure initiated using
only yield deformation measures and not strain measures as we have seen here. Last term in (36) requires further considerations. We note that work conjugate pair is , in which
is symmetric, thus we must consider:
(39)
We substitute (39) in (36)
(40)
We can also substitute
in the conservation and balance laws. Thus, the conservation and balance laws (10)-(15) now have the following form:
(41)
(42)
(43)
(44)
(45)
(46)
in which
(47)
Remarks
(1)
is the strain rate conjugate to
.
(2) The linear micropolar nonclassical continuum theory for infinitesimal deformation is a complete subset of the nonlinear micropolar nonclassical continuum theory described by conservation and balance laws (41)-(47). In this case,
(48)
in which
is linear strain measure and
is the symmetric part of the classical rotation gradient tensor. Thus, (41)-(47) reduce to the linear micropolar nonclassical continuum theory for infinitesimal deformation.
(3) When
is not considered, the conservation and balance laws (41)-(47) reduce to finite deformation/finite strain classical continuum physics.
(4) When
is a free field (i.e.,
is not considered) and the deformation is infinitesimal, the conservation and balance laws (41)-(47) reduce to infinitesimal deformation classical continuum mechanics.
(5) All conjugate pairs in the entropy inequality define constitutive tensors and their argument tensors that are supported by the representation theorem; hence, they would yield thermodynamically and mathematically consistent constitutive theories.
6.1. Constitutive Theory for Equilibrium Stress
Recall that the additive decomposition
is necessary because
cannot be part of the constitutive theories, as it is defined by balance of angular momenta through gradients of moment tensor. To address volumetric and distortional deformation physics (mutually exclusive) in nonlinear micropolar nonclassical continuum theory, we must further additively decompose
into equilibrium
and deviatoric
components. Volumetric deformation physics is associated with
, while distortion deformation physics is described by
. As discussed in ref. [1], compressibility in solids in Lagrangian description is controlled by
, and the density in the current configuration is deterministic through conservation of mass if
is known. Thus, density is not a dependent variable in the conservation and balance laws in Lagrangian description for solid matter. The equation of state in solids is a consequence of density change i.e., for a density change caused due by
, there is a pressure field associated with it. The presence of this pressure field through equilibrium stress in balance of linear momenta is essential for correct force balance. We further elaborate that in compressible solids, one could determine solution for compressible case without using equation of state, but such solutions would be erroneous due to incorrect force balance in the balance of linear momenta. Since compressibility physics depends upon density and temperature, the constitutive theory for
must be obtained using the constitutive theory for
. Details of the derivation of the constitutive theory for
can be found in recent papers [40] [41] by the authors, including references [42] [43]. The final form of the constitutive theory for
for compressible and incompressible cases are given by:
(49)
(50)
in which,
and
are thermodynamic and mechanical pressures.
In (50), we could have used
and
, but we leave the expression as it is in (50). Reduced form of entropy inequality (after considering constitutive theory for
) in Lagrangian description is given by:
(51)
Constitutive Theory for
The constitutive theory for
must address: (1) distortional deformation physics and (2) the macrodissipation mechanism due to viscosity of the medium. From the rate of work conjugate pairs
in the reduced form of the entropy inequality,
is the work conjugate pair, suggesting that
as argument tensor of
is a valid choice. From viscous fluid physics, we know that dissipation is a function of convected time derivative of the Green or Almansi strain tensor. Symmetric part of the velocity gradient tensor
(where viscous stress is proportional to
) is the first convected time derivative of the Green and Almansi strain tensors. This holds for any viscous medium. Thus, at the very minimum, the dissipation mechanism will require
to be a function of
or
, the first convected time derivative of the Green’s strain tensor (same as ordinary time derivative in this case). We can generalize this by assuming that viscous dissipation mechanism depends on strain rates
of up to order
. This is macro dissipation. This provides ordered rate dissipation mechanism.
is naturally an argument tensor of
. Thus, we can write:
(52)
Now we can derive constitutive theory for
using representation theorem. Let
be the combined generators of the argument tensors of
in (52), that are symmetric tensors of rank two. Then,
constitute the basis of the space of tensor
, referred to as integrity. Hence, we can express
as a linear combination of
in the current configuration.
(53)
in which
are the combined invariants of the same argument tensor of
in (52).
The material coefficients in (53) are determined by expanding
in Taylor series in
and the temperature
about a known configuration
(based on principle of smooth neighborhood) and retaining only up to linear terms in
and temperature
(for simplicity of the resulting constitutive theory).
(54)
Substituting for
and
from (54) into (53)
(55)
Collecting coefficients of
and
in (55)
(56)
If we define
(57)
then, using (57) in (56), we can write (56) in a more compact form.
(58)
Equation (58) defines material coefficients, that can be functions of
and
.
This constitutive theory is based on integrity (complete basis) and requires
material coefficients. Various simplified forms of the constitutive theory for
can be obtained from (58) by choosing desired generators and invariants. The most simplified yet some what general constitutive theory for
is the one in which
is a linear function of the components of the argument tensor in (52). This is given by, after redefining material coefficients:
(59)
in which
and
are similar to Lames coefficients in linear elasticity.
and
are damping material coefficients associated with strain rate
. This constitutive theory is nonlinear in the components of the displacement gradient tensor. The dissipation mechanism is nonlinear and is defined by strain rates
of up to order
.
6.2. Constitutive Theory for
Just like the constitutive theory for
that addresses macro elasticity and macro dissipation due to viscosity of the medium, the constitutive theory for
must also address: (1) the macro distortional deformation physics (macro elasticity) and (2) the dissipation mechanism between the microconstituents and the viscosity of the medium, micro dissipation or micro viscous dissipation mechanism. From the reduced form of the entropy inequality, we consider the rate of work conjugate pair
in which:
(60)
Thus, we can write
(61)
Generalizing (61) to include rates of
and
up to orders
, we can write:
(62)
and
(63)
Thus, based on rate of work conjugate pair
,
in (63) must be an argument tensor of
. If we assume that dissipation between the microconstituents and the viscous medium (micro viscous dissipation or microdissipation mechanism) depends on rate of
, then
in (62) must also be argument tensors of
. Choice of
as an argument tensor of
is obvious. Thus, we have:
(64)
in which
and
are defined by (63) and (62). Now, we can derive constitutive theory for
using representation theorem [28]-[39]. Let
and
be the combined generators and combined invariants of the argument tensors of
in (64) that are symmetric tensors of rank two. Then
constitute the basis of the space of constitutive tensor
(integrity), hence we can express
as a linear combination of the basis in the current configuration.
(65)
The coefficients
in the linear combination can be functions of
and
. We remark that coefficients
are not material coefficients. Material coefficients in (65) are determined by considering Taylor series expansion of
(based on axioms of smooth neighborhood [42] [43]) in
and
about a known configuration
and retaining only up to linear terms in
and
(for simplicity)
(66)
Substituting
and
from (66) in (65), we get:
(67)
Collecting coefficients (defined in
) of
,
,
,
,
,
in (67), we can write (67) as follow:
(68)
If we define
(69)
then, using (69) in (68), we can write (68) in more compact form.
(70)
In this constitutive theory (70) for
, the material coefficients are defined in (69). The material coefficients can be functions of
, and
. This constitutive theory requires
material coefficients. Simplified forms of the constitutive theories for
can be obtained from (70) by choosing only the desired generators and invariants. The most simplified, yet general constitutive theory for
is one in which
is a linear function of the components of the argument tensors.
(71)
in which
and
are similar to Lame’s coefficients and the terms containing these are causing distortion of the matter.
are damping coefficients corresponding to the rate
for the
rate of the rotation gradients.
6.3. Constitutive Theory for q
Considering
(72)
and following references [42] [43] we can derive the following constitutive theory for
using representation theorem.
(73)
and
are material coefficients. These can be functions of
and
.
is invariant of argument tensor
. Simplified form of (73), the Fourier heat conduction law is given by
(74)
7. Complete Mathematical Model
In the following, we present complete mathematical model consisting of conservation and balance laws of nonclassical continuum mechanics and the constitutive theories for finite deformation/finite strain nonlinear micropolar nonclassical continuum theory based on classical rotation
for thermoviscoelastic compressible solid medium. The mathematical model consists of (41)-(47), (59), (71) and (74). We have the following (using non-reduced forms of first law of thermodynamics and second law of thermodynamics)
(75)
(76)
(77)
(78)
(79)
(80)
(81)
(82)
(83)
in which
(84)
(85)
(86)
(87)
(88)
(89)
in which
and
. The mathematical model (75)-(89) consists of 22 equations: balance of linear momenta(3), balance of angular momenta(3), first law of thermodynamics(1), constitutive theories for
,
,
in twenty two variables:
,
,
,
,
and
. Thus, this mathematical model consisting of conservation and balance laws for nonlinear micropolar nonclassical continuum theory and constitutive theories for compressible thermoviscoelastic solid without memory has closure.
8. Summary and Conclusions
We have presented a finite deformation/finite strain nonlinear micropolar nonclassical continuum theory for compressible thermoviscoelastic solid continua without rheology based on classical rotations
of the microconstituents. This theory consists of conservation and balance laws including balance of moment of moments, which is a new necessary balance law in all 3M nonclassical continuum theories. The constitutive theories are derived using representation theorem. A summary of the work presented in the paper and some conclusions drawn from it are given below.
(1) Finite deformation/finite strain measures have been utilized in the derivation of the theory based on the conjugate pairs in the entropy inequality.
(2) We distinguish between the strain measures and the rigid rotations in the derivation of the constitutive theories. In micropolar theories, the microconstituents can only experience rigid rotations. These rotations cannot be added to the strain measures as done in ref. [8]. This approach leads to incorrect definitions of strain tensor and consequently, erroneous constitutive theories that are based on this measure.
(3) The importance of additive stress decompositions:
;
are necessary to ensure that
is not part of constitutive tensors and to ensure that mutually exclusive volumetric and distortional deformations are addressed correctly in the constitutive theories.
(4) In micropolar theories, rigid rotations of the microconstituents must be incorporated in the development of the theory. We must keep in mind that classical rotations
already exist at the material and constitute a free field in the absence of microconstituents. In the presence of microconstituents, classical rotations in fact are the rotations of the microconstituents. Thus,
is a measure of rigid rotations of the microconstituents. This theory allows rigid rotations of microconstituents without considering
as additional unknown rotations of the microconstituents at the material points. The micropolar theory that uses unknown
at the material points is thermodynamically and mathematically consistent and the mathematical model lacks closure. (b) The linear micropolar theories based on rotations (
) at the material points and the linear micropolar theories based on
at the material point (ignoring
) have been shown to be thermodynamically and mathematically inconsistent and suffer from lack of closure.
(5) Use of balance of moment of moments balance law (Yang et al. [25], Surana et al. [26] [27] [41]) is shown to be essential in linear micropolar theories. This is also true in the case of nonlinear micropolar theories. In the absence of this balance law, the nonlinear micropolar theories are also nonphysical and the mathematical model suffers from lack of closure.
(6) In the derivation of the conservation and balance laws,
,
, and
, , are used for simplicity. However, in the final form of the conservation and balance laws, as well as in the constitutive theories, these are substituted in terms of
,
and
,
as they are the true measures for finite deformation/finite strain.
and
and their conjugates are supported by theory of isotropic tensors. Determination of these conjugate pairs is an important aspect of the work presented in the paper.
(7) All constitutive theories are derived using representation theorem to ensure that they are mathematically consistent.
(8) The nonlinear micropolar nonclassical continuum theory for thermoviscoelastic solid presented here incorporates two nonlinear mechanisms of dissipation, micro dissipation and macro dissipation. Both mechanisms use ordered rates of work conjugate quantities that appear in the entropy inequality. This is also an important and unique aspect of the work presented in this paper.
(i) The first viscous dissipation mechanism is due to
and Green’s strain rates
, standard nonlinear viscous drag forces between the material particles.
(ii) The second mechanism of nonlinear viscous dissipation mechanism is due to rotation rates of the microconstituents in the viscous medium, hence due to viscous drag forces between the microconstituents and the viscous medium. This mechanism depends upon the rotation rates of the gradients of microconstituent rotations
up to order
, hence is also an ordered rate mechanism. Both nonlinear dissipation mechanisms reduce to linear dissipation for linear micropolar theories in which
and
.
(iii) The linear micropolar theory for small deformation, small strain physics for thermoviscoelastic solid is a complete subset of the nonlinear micropolar theory for thermoviscoelastic solid matter presented in this paper.
(iv) Model problem studies using this nonlinear micropolar theories and comparison with finite deformation/finite strain classical continuum theory will be presented in a follow up paper.
Acknowledgements
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.
Appendix
Nomenclature
,
,
|
deformed Coordinates |
,
,
|
undeformed Coordinates |
|
reference density |
|
density in Lagrangian description |
|
density in Eulerian description |
|
specific entropy in Lagrangian description |
|
specific entropy in Eulerian description |
|
specific internal energy in Lagrangian description |
|
specific internal energy in Eulerian description |
,
,
|
internal or classical rotations in Lagrangian description |
,
,
|
rigid rotations of the microconstituents |
,
,
|
total rotations in Lagrangian description |
|
deformation gradient tensor in Lagrangian description |
|
symmetric part of deformation gradient tensor in
Lagrangian description |
|
skew-symmetric part of deformation gradient tensor in
Lagrangian description |
|
displacement gradient tensor in Lagrangian description |
|
symmetric part of displacement gradient tensor in
Lagrangian description |
|
skew-symmetric part of displacement gradient tensor in
Lagrangian description |
|
rotation gradient tensor in Lagrangian description |
|
symmetric part of classical rotation gradient tensor in
Lagrangian description |
|
skew-symmetric part of classical rotation gradient tensor in Lagrangian description |
|
symmetric part of gradient of classical rotation rate tensor in Eulerian description |
|
rate of symmetric part of gradient of classical rotation
tensor in Lagrangian description |
|
classical rotation rate tensor in Eulerian description |
|
classical rotation rate tensor in Lagrangian description |
,
, |
heat vector in Lagrangian description |
,
,
|
heat vector in Eulerian description |
,
,
|
velocities in Lagrangian description |
,
,
|
velocities in Eulerian description |
,
,
|
displacements in Lagrangian description |
,
,
|
displacements in Eulerian description |
|
average stress in Lagrangian description on the oblique plane of elementary tetrahedron |
|
average stress in Eulerian description on the oblique plane of elementary tetrahedron |
|
average moment in Lagrangian description on the oblique plane of elementary tetrahedron |
|
average moment in Eulerian description on the oblique plane of elementary tetrahedron |
,
,
|
Contravariant Cauchy stress tensor in Lagrangian description |
,
,
|
Contravariant Cauchy stress tensor in Eulerian description |
|
symmetric part of Contravariant Cauchy stress tensor
tensor |
|
anti-symmetric part of Contravariant Cauchy stress tensor tensor |
|
deviatoric part of the symmetric Contravariant Cauchy
stress tensor tensor |
|
equilibrium part of the symmetric Contravariant Cauchy
stress tensor tensor |
|
temperature in Lagrangian description |
|
temperature in Eulerian description |
|
thermal conductivity in Lagrangian |
|
thermodynamic or Mechanical Pressure in Lagrangian
description |
|
thermodynamic or Mechanical Pressure in Eulerian
description |
,
,
|
temperature gradient tensor in Lagrangian description |
,
,
|
temperature gradient tensor in Eulerian description |
|
velocity gradient tensor in Eulerian description |
|
symmetric part of the velocity gradient tensor in Eulerian description |
|
Skew symmetric part of the velocity gradient tensor in
Eulerian description |