Thermodynamically and Mathematically Consistent Linear Micromorphic Microcontinuum Theory for Solid Continua ()
1. Introduction
The polar nature of solids, in particular crystalline solids, was observed by Voigt in 1887 [1]. He presented equations of equilibrium for such solids, including moment equilibrium. In 1909, E. Cosserat and F. Cosserat presented a theory of elasticity by considering rotations about rigid directors using the principle of virtual work [2]. They derived the balance of momenta for the dynamic case. This work lacked conservation and balance laws and had no infrastructure for constitutive theories, hence it remained dormant till 1960. Grad in 1952 [3], Gunther in 1958 [4] and Schaefer in 1967 [5] revisited the Cosserat theory and established its connection to dislocation physics. Eringen in 1967 [6]-[8] presented the linear theory of micromorphic elastic solids and the theory of micropolar plates. In 1964, Eringen and Suhibi [9] presented a nonlinear theory for microelastic solids. Various works of Eringen [10]-[16] consider various aspects of micropolar continuum theories. The mechanics of micromorphic continua were introduced by Eringen in 1968 [17]. This was followed by subsequent works of Eringen: conditions for the theory of micromorphic solids in 1969 [18], balance laws for micromorphic mechanics in 1970 [19], micromorphic materials with memory in 1972 [20], balance laws for micromorphic continua revisited in 1992 [20], application of micromorphic theory to dislocation physics in 1970 [21].
A compilation of Eringen’s work on 3M theories was published in the two books by Eringen [22] [23]. Since the publication of micromorphic theory and more generally 3M microcontinuum theories, many papers have appeared on micropolar theories, but not so many on micromorphic theory. Most published works on micropolar theory are largely following the balance laws and the constitutive theories derived by Eringen. We cite some more recent works in the following.
Vernerey, Liu and Moran in 2007 [24] presented a multiscale micromorphic theory for hierarchical materials. The authors employed the method of virtual power to derive the mathematical model for a particular scale, with its interaction with the macroscale. Chen, Lee and Xiong in 2009 [25] considered the concept of deformable material point, thus not taking a crystal as structureless and hence not idealizing it as a mass point. The paper considers classical, micromorphic and generalized field theories and their applicability. Finite strain micromorphic elastoplasticity theory was presented by Regueiro in 2010 [26]. The basic foundations of the conservation and the balance laws and the constitutive theories in this work follow the approach presented by Eringen for micromorphic continua with extension to finite strain plasticity. Wang and Lee in 2010 presented micromorphic theory as a gateway to the nano world [27]. This work uses the basic micromorphic theory of Eringen but additionally introduces objective Eringen tensors in the kinematics and the balance laws are derived by requiring the energy equations to be form-invariant under generalized Galilean transformation. Lee and Wang in 2011 [28] presented a generalized micromorphic theory for solids and fluids based on Eringen’s micromorphic theory with adjustments similar to those in Lee’s work in reference [27]. Isbuga and Regueiro in 2011 [29] presented a three-dimensional finite element analysis of finite deformation micromorphic linear elasticity. The conservation and balance laws and the constitutive theories used in this work are the same as those due to Eringen. Reges, Petangueira and Silva in 2024 [30] presented a modeling of micromorphic continua based on a heterogeneous microscale. In ref. [31], McAvoy presented a consistent linearization technique for micromorphic continuum theories and presented its applicability to 3M theories. They advocated that this linearization technique yields tractable linear theories for nonlinear elastic microstructured materials.
From the literature review, it is clear that most published works on micromorphic microcontinuum theories follow the conservation and the balance laws and the constitutive theories derived and presented by Eringen (papers are cited here).
2. Scope of Work
In this paper, we undertake the derivation of the conservation and the balance laws and the constitutive theories for a linear elastic micromorphic continua in which: 1) the deformation/strain measures derived by Surana et al. [32] 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 the laws of thermodynamics of classical continuum mechanics, yielding micro conservation and balances. From micro conservation and balance laws, “integral-average” definitions are introduced that permit the derivation of macro conservation and balance laws and the constitutive theories using principles of thermodynamics and well-established concepts in applied mathematics. 3) In deriving conservation and balance laws and the 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, etc. introduced and used by Surana et al. [32]-[54] in conjunction with linear and nonlinear micropolar theories for solid and fluent continua. This is necessary because the physics of rigid rotations of microconstituents exists in all 3M theories as it arises from the skew-symmetric part of the micro deformation gradient tensor. Thus, we must have the exact same mathematical treatment of rigid rotation physics in 3M theories, requiring that we maintain the micropolar theory as a subset of micromorphic theory.
We first present 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 the balance laws at the macro level. This is followed by constitutive theories for the macro Cauchy stress tensor, the microconstituent Cauchy stress tensor, the macro Cauchy moment tensor and the heat vector. Constitutive theories are initiated using conjugate pairs in the entropy inequality, establishing constitutive tensors and their argument tensors. Constitutive tensors and argument tensors are adjusted or augmented as required by the desired physics that may not have been considered while deriving the entropy inequality. In all three constitutive theories (microconstituent Cauchy stress tensor, macro Cauchy stress tensor and macro Cauchy moment tensor), we consider mechanisms of elasticity for microconstituent Cauchy stress tensor (
) as well as the macro stress tensor
(symmetric part) and the interaction of microconstituent in the elastic medium, Cauchy moment tensor
.
All constitutive theories are derived using the representation theorem [55]-[66], hence are always thermodynamically (not in violation of entropy inequality) and mathematically consistent. Constitutive theories and material coefficients are first derived for the constitutive theories based on integrity (complete basis) and then their simplified forms are presented, which are linear in the components of the argument tensors.
The micromorphic theory derived here is shown to be thermodynamically and mathematically consistent, hence it is a valid and physical linear micromorphic theory. The linear micromorphic theory derived here is compared with Eringen’s micromorphic theory. The differences in the two theories are identified, discussed and evaluated for their validity based on thermodynamic principles and well accepted mathematical concepts to establish their validity or lack of validity, hence the validity of the resulting micromorphic theory.
3. Preliminary Considerations and Definitions
3.1. Classical Rotations (
), Deformation Gradient Tensor, Classical Rotation Gradient Tensor, and Micro Deformation
In classical continuum mechanics, the macro deformation gradient tensor
is given in the Lagrangian description as
(1)
in which
and
are the deformed and undeformed coordinates of a material point in a fixed
-frame and
are displacements of the material point also in
-frame. The additive decomposition of
into symmetric
and skew-symmetric
tensor gives
(2)
We also note that
(3)
(4)
where
are the classical rotations. The skew-symmetric matrix
contains
.
are the rotations about the axes of a triad located at the material point with axes parallel to the axes of the
-frame.
In classical continuum mechanics,
constitutes a free field. Thus, even though it is present in every deforming solid, the classical continuum theory is not influenced by its presence because it is a free field. In the presence of microconstituents causing obstruction to the free field
, the rotation field due to
is no longer a free field and in fact describes the 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 constitute a free field that has no effect 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 displacement 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. Secondly, the free field has no influence on 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
is in fact the rigid rotations of the microconstituents. Thus, in micropolar theory, in which microconstituents only experience rigid rotations referred to as
(defined by skew symmetric part of microconstituent deformation gradient tensor
),
suffices to be the rigid rotations of the microconstituents as known degrees of freedom. Thus,
serves as rigid rotations of the microconstituents in all three 3M theories, hence not requiring
as unknown rigid rotational degrees of freedom.
For classical rotations
, we also note the following:
(5)
(6)
in which
is the gradient tensor of classical rotations and
and
are its symmetric and skew-symmetric decompositions.
Next, we consider the concept of a deformable material point, rationalized through deformable directors contained in a material point. Consider a volume of matter
enclosed by surface
in the reference configuration. Upon deformation,
and
change to
and
at time
. Let the volume
contain microconstituents uniformly dispersed in the volume. Let the volume
of a material particle
contain N microconstituents. Let
and
be the volume and its closure for the
microconstituent with mass density
.
The center of mass of
has the position coordinate
in
. Let
be the location of the microconstituent
with respect to the center of mass of
and let
be its position coordinate in the
-frame. Upon deformation, in the current configuration,
changes to
,
to
and
to
(see Figure 1).
At this stage, we can possibly entertain two different methodologies in deriving the deformation/strain measures.
1) In the first case, we assume that each microconstituent located at a different position in
has its own deformation physics, implying that there are N different deformation physics within the volume
of the material point
. We then assume that the material point
only sees the homogenized response of N microconstituents. Since the homogenization yields surrogate behavior, homogenization must include boundary conditions and the load so that the homogenized model with surrogate material properties is representative of the true physics. It is obvious that homogenization is not practical for the volume
of the material point.
2) In the second approach, we assume that the material point
only sees the statistically averaged deformation physics of N microconstituents. This is a more practical viewpoint of considering complex physics within the volume
. To simplify the consideration of varied deformation physics of microconstituents in this approach, we assume that there is a surrogate configuration of microconstituents in
in which each of the N microconstituents has identical deformation physics. Thus, the average of the N microconstituent deformation physics in this case is the same as the deformation physics of one microconstituent, which is assumed to be the same as the statistically averaged deformation physics due to the original configuration of microconstituents in volume
. Thus referring to Figure 1,
is the director in the undeformed configuration and
is the director in the deformed configuration
. The deformation of
is assumed to represent the micro deformation of the microconstituents within the volume
of the material point with the director
. In the following, we only present essential relations that are helpful in the derivation of the conservation and balance laws and the constitutive theories for linear micromorphic solids. With this, we can proceed with the details of the derivations of deformation measures presented in ref. [32]. Referring to Figure 1, the following relations hold:
(7)
If we consider Lagrangian description, then
depends upon
and
and we can write:
And we can write:
(8)
Figure 1. Undeformed and deformed configurations of material point volume.
We note that
and
are undeformed and deformed coordinates. Hence,
(9)
Substituting (9) into (7)
(10)
in which
is the micro deformation gradient tensor (similar to
in macro physics). Additive decomposition of
gives
(11)
Symmetric tensor
contains the deformation physics of the microconstituent and
contains
,
being the rigid rotations of the microconstituents. Using (8), (9) and (10) the rest of the details regarding various micro deformation measures follow. For example, velocity
, velocity gradient tensor
and
in the Lagrangian description are given by:
(12)
(13)
(14)
and
(15)
In Eulerian description, we have the following:
(16)
(17)
(18)
(19)
(20)
We also note the following useful relations.
(21)
(22)
(23)
(24)
(25)
(26)
The relations (12) - (26) are helpful when deriving conservation and balance laws and the constitutive theories.
3.2. Microconstituent Stress Tensor
Due to Micro Cauchy Stress Tensor
In the derivation of the conservation and balance laws, we use the following integral-average definition
in which
is the total stress tensor. Thus,
is the total microconstituent stress tensor. In this process, there is no concept of additive decomposition of
into equilibrium and deviatoric stress tensors, hence volumetric and distortional physics are not considered explicitly. Secondly, microconstituent density is eliminated through integral-average definitions. But
is needed if we are to consider a constitutive theory for the equilibrium stress for the microconstituents. Both of these considerations help us conclude that the stress tensor
or
is due to mechanical loading, hence it is a function of the work conjugate strain tensor and the elastic properties of the microconstituents. Henceforth, we do not consider any additive decomposition of
, but instead consider the work conjugate strain tensor and temperature as its argument tensors of
in deriving the constitutive theory for it.
4. Degrees of Freedom in Micro Deformation Physics
Determination of the degrees of freedom necessary to describe micro deformation physics is crucial. Since the deformation of microconstituents can be described by classical continuum mechanics, i.e., by the micro displacement gradient tensor
. Additive decomposition of
into symmetric (
) and skew symmetric (
) tensor separates rigid rotation of microconstituents (
) and the deformation of the microconstituents (
).
is completely defined by the gradients of the microconstituent displacements. Thus, in principle
, three translational degrees of freedom are necessary to define
. But this requires the position coordinates of the microconstituents with respect to the center of mass of the material point, which we do not have. Thus, instead of three displacements of the microconstituents, we need to consider six independent components of
as degrees of freedom for the micro constituents. Thus, in the linear micromorphic theory presented here, a microconstituents has nine degrees of freedom: three rigid rotations
, which are same as classical rotations
(hence do not add to unknown degrees of freedom), and six deformational degrees of freedom, which are six independent components of the symmetric part of the displacement gradient tensor
. We point out that this approach is totally different from that used by Eringen and those following Eringen’s work. In Eringen’s work, all nine components of
are treated as microconstituent degrees of freedom. It is clear that this consideration does not permit the separation of rigid rotations from deformations, which is essential in the development of the conservation and balance laws and the constitutive theories.
5. Conservation and Balance Laws for Linear Micromorphic Continua
In the following, we present the derivation of the conservation and balance laws: conservation of mass, balance of linear momenta, balance of angular momenta, balance of moment of moments and the first and second laws of thermodynamics, in both Eulerian and Lagrangian description for linear micromorphic solid continua. The two descriptions can be derived from each other when displacements are kinematic variables in both. We always begin with the conservation or the balance laws derivation for micro deformation of the microconstituent and show that valid thermodynamic laws are possible to derive using classical continuum theory. This is followed by the introduction of “integral-average” definitions that hold at the macro level and are used to derive valid conservation and balance laws for macro physics. The conservation and balance laws of classical continuum mechanics are used in the micro deformation physics. Due to use of integral-average definitions at macro level, the conservation and balance laws of classical continuum mechanics are modified for macro physics. Introduction of a new kinematic conjugate pair, rotations and moments in addition to already existing displacements and forces requires an additional balance law, balance of moment of moments at the macro level [44] [54] [67].
5.1. Conservation of Mass
5.1.1. Conservation of Micro Mass
For the microconstituent in the reference and the deformed configurations, conservation of mass can be expressed as:
(27)
If micro constituent mass is conserved, then
(28)
Using transport theorem [68] [69], we can write the following for (28)
(29)
Using localization theorem, we obtain the following from (29)
(30)
Equation (30) is the differential form of the conservation of mass in Eulerian description for the micro constituent based on classical continuum mechanics.
In Lagrangian description, using (27)
(31)
Equation (31) implies that
(32)
Equation (32) is conservation of mass for microconstituent in Lagrangian description based on classical continuum mechanics.
5.1.2. Conservation of Macro Mass
Consider Eulerian description in (27) and integration over
to obtain
(33)
Define
(34)
Substituting (34) in (33) and setting its material derivative to zero (as mass in conserved for volume
)
(35)
Using transport theorem [68] [69], we obtain the following from (35)
(36)
using localization theorem
(37)
Equation (37) is continuity equation at macro level in Eulerian description. Thus, conservation of mass holds at micro as well as macro level. In Lagrangian description, using (27) we can write the following:
(38)
Thus,
(39)
Equation (39) is the continuity equation at macro level in Lagrangian description.
5.2. Balance of Linear Momenta
5.2.1. Balance of Micro Linear Momenta
If and
are microconstituent acceleration, body forces per unit mass and Cauchy stress tensor, then using balance of linear momenta of classical continuum mechanics, we can write the following:
(40)
or
(41)
Using localization theorem [69]
(42)
Equation (42) is balance of linear momenta for micro constituent based on classical continuum mechanics in Eulerian description. Micro balance of linear momenta in Lagrangian description can be directly written using (42).
(43)
5.2.2. Balance of Macro Linear Momenta
Consider the following integral-average definitions:
(44)
(45)
(46)
Using (44) - (46) in (40) and integrating over
and
(47)
or (48)
Using localization theorem [69]
(49)
5.3. Balance of Macro Angular Momenta
The simplified way to derive this is to consider the micro balance of linear momenta for
and
and multiply it by
, and integrate over
and
and then integrate over
and
and including
acting on
. This can be written in three different forms, all three forms are conceptually identical, but there are some differences. We label these three forms as Case 1, Case 2 and Case 3.
Case 1
(50)
Case 2
(51)
Case 3
We consider the following identity
(52)
(53)
We substitute from (53) in the second term of (51) to obtain
(54)
Equation (54) is the third possible form that can be used to derive macro balance of angular momenta.
Integral terms that are common in Case 1, Case 2 and Case 3
In all three forms (50), (51) and (54), the first and the third terms are identically the same.
Thus, we consider the first and third terms appearing in (50), (51) and (54) first, and then provide individual details of the second term in (50), (51) and (54).
Consider the first term (say T1) in (50) or (51) or (54).
(55)
Let
(56)
Substituting from (56) in (55)
(57)
(58)
Define
(59)
Using (59) in (57), we can write (59) as follows
(60)
In Lagrangian description
(61)
Consider the third term (say T3) in (50) or (51) or (54)
(62)
(63)
Define
(64)
Using (64) in (63)
(65)
This is the final form of T3 in Eulerian description. In Lagrangian description, (65) can be written as
(66)
Integral terms that are not common in Case 1, Case 2 and Case 3
Case 1: Consider second term (say T2C1) and (58)
(67)
Substitute
from (56) in (67)
(68)
Define
(69)
Substituting (69) in (68)
(70)
Define
(71)
Using (71) in (70)
(72)
This is the final form of the second term in (58) (T2C1) for Case 1 in the Eulerian description. In the Lagrangian description, we can write T2C1 as follows:
(73)
Case 2: Consider second term (say T2C2) in (51)
(74)
Substitute (56) in (74)
(75)
Define
(76)
Substituting (76) in (75), we obtain the following.
(77)
Define
(78)
Using (78) in (77)
(79)
This is the final form of T2C2 in the Eulerian description. T2C2 in the Lagrangian description can be written directly from (79)
(80)
As expected, T2C2 in (79) for Case 2 is exactly same as T2C1 in (72) for Case 1 and (80) is same as (73).
Case 3: Consider second term (T2C2) in (54)
(81)
Substitute for
from (56) in (81)
(82)
Define
(83)
(84)
Substituting (83) and (84) in (82)
(85)
or
(86)
This is the final form of T2C3 in the Eulerian description. T2C3 in the Lagrangian description can be written directly using (86), given below
(87)
Differential forms of balance of angular momenta for Case 1, Case 2 and Case 3
We note that T2C3, i.e., (87), is exactly same as in T2C1 and T2C2, except here in (86),
has a negative sign. This, of course, is due to introducing an identity to replace
term by the terms obtained due to identity. By using T2C1, T2C2 and T2C3 in Case 1, Case 2 and Case 3, and also using (61) and (65), we can derive the final expression for the balance of angular momenta for Case 1, Case 2 and Case 3, first in the Eulerian descriptions followed by Lagrangian description.
Balance of linear momenta: Case 1
Consider Eulerian description
(88)
Grouping terms in (88)
(89)
The first and the second terms in (89) are zero due to the macro and micro balance of linear momenta, thus (89) reduces to
(90)
Using localization theorem (90) yields
(91)
Equation (91) is the final form of the balance of macro angular momenta for Case 1 in the Eulerian description. Equation (91) in the Lagrangian description can be written as:
(92)
Balance of linear momenta: Case 2
Consider the Eulerian description. Since the final form resulting for T2C2 for Case 2 (Equation (79)) is the same as the final form resulting for Case 1 for T2C1 (Equation (64)), the final form of the balance of macro angular momenta for this case is the same as that for Case 1, and we can write the following in the Eulerian description
(93)
In the Lagrangian description, (93) becomes
(94)
Balance of linear momenta: Case 3
Consider the Eulerian description.
(95)
Collecting terms in (95)
(96)
The first term in (96) is zero due to balance of macro and micro linear momenta. Thus, (96) reduces to
(97)
Using localization theorem (97) yields
(98)
This is the final form of the balance of macro angular momenta for Case 3 in the Eulerian description. In the Lagrangian description, (98) can be written as:
(99)
We note that Case 1 and Case 2 use the actual balance of micro linear momenta in the derivation, whereas in Case 3, the micro gradient stress term in the balance of micro linear momenta is altered using an identity. The result of this change is a negative sign for
term in the balance of angular momenta (Equation (98)). Equation (98) is what was derived by Eringen using a weighting function
for the balance of microlinear momenta.
The derivation presented here for Case 3 shows that a weighting function is not needed. The end result of using the weight function is the same as what we have presented in this paper. The answer to the question of whether the correct form of the balance of angular momenta is (91) (or (93)) or (97) is important. Based on the derivation presented in Case 1 and Case 2 from the first principles, straight forward use of balance of angular momenta at this point we lean towards the forms (91) or (93). However, the use of identity resulting in change of sign for
term may be meritorious of further consideration if supported by physics. Thus, at this stage we consider the following forms of balance of angular momenta in Eulerian and Lagrangian description that provides alternative to either forms with plus or minus sign with
or
tensors.
(100)
(101)
We note that since
and
, in (100) and (101), we have
and
, thus (100) and (101) reduce to the following.
(102)
(103)
Equations (102) and (103) are balance of angular momenta in Eulerian and Lagrangian descriptions. We keep (100) and (101) for further considerations.
Balance of angular momenta (102) or (103) is the same as balance of angular momenta for the micropolar microcontinum theory, as it should be, because the rigid rotation physics of a micro constituent is identical in micropolar and micromorphic microcontinuum theories. Equation (102) or (103) defines three balance of angular momenta equations about
-axes. Balance of angular momenta in the forms (100) and (101) is more informative. We use this in a later section.
5.4. First Law of Thermodynamics
Since the conservation and the balance laws of classical continuum mechanics hold for the micro deformation of the microconstituents, we can begin with the energy equation for the micro constituents over the volume
and its surface
and integrate it over
.
(104)
in which
is the specific internal energy,
is the heat flux and
are classical rotation rates (due to
). We consider each term in (104) (say t1).
Consider first term in (104)
(105)
Let
(106)
Using (106) in (105)
(107)
Consider second term in (104) (say t2)
(108)
We note that
(109)
and
(110)
Substituting (109) and (110) in (108)
(111)
Define
(112)
(113)
Substituting (112) and (113) in (111)
(114)
We note that
(115)
and
(116)
Define
(117)
Using (117) in (116)
(118)
Substituting (115) and (118) in (114)
(119)
Collecting coefficients in (119)
(120)
The second and the third terms in (120) are zero due to the balance of macro linear momentum and the balance of micro linear momentum, and we can write (120) as follows
(121)
Consider the third term in (104) (say t3)
(122)
Let
(123)
Using (123) in (122)
(124)
Consider the fourth term in (104) (say t4)
(125)
Define
(126)
Substituting (126) in (125), we can write (125) as follows
(127)
We can show that [49] [53]
(128)
Using (128) in (127)
(129)
in which are the gradients of the rotation rates.
Substituting (107), (121), (124) and (129) into (104), we can write the following for (104).
(130)
or
(131)
using localization theorem
(132)
This is the final form of the macro energy equation in the Eulerian description. The energy equation in the Lagrangian description can be written directly from (132) and is given by
(133)
We note that
(134)
and
(135)
5.5. Second Law of Thermodynamics: Macro
Let
be entropy density in microconstituent volume
,
be the entropy flux imparted to volume
by surrounding medium and
be the source of entropy in
due to noncontacting sources (or bodies), then the rate of increase of entropy in volume
of the microconstituent from all contacting and noncontacting sources is given by
(136)
Integrating (136) over
and
(137)
Using
(138)
(139)
(140)
and
(141)
Using (140) and (141) in (137)
(142)
Define
(143)
(144)
(145)
Using (143), (144) and (145) in (142)
(146)
or
(147)
or
(148)
Using localization theorem
(149)
Multiply throughout by
(150)
Let
(151)
(152)
(153)
Substituting from (153) into (150)
(154)
Substituting
from the energy Equation (133) in (154) after inserting
in the energy equation
(155)
term and
terms cancel and we can write the following after changing the sign.
(156)
This is the final form of the macro entropy inequality in the Eulerian description. In the Lagrangian description, we can write the following directly from (156).
(157)
5.6. Balance of Moment of Moments: Macro
Since in all 3M microcontinuum theories the classical rotations
and conjugate moment
form an additional kinematically conjugate pair, in addition to displacements and forces, it follows that, based on Yang et al. [67] and Surana et al. [44] [54], the balance of moment of moments balance law is essential in all 3M theories. Using the macro definition of Cauchy stress tensor and Cauchy moment tensor, and following [44] [54], we can derive the following for this balance law:
(158)
That is Cauchy moment tensor is symmetric in all 3M microcontinuum theories.
6. Summary of Macro Conservation and Balance Laws in Eulerian Description
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:
(159)
(160)
(161)
(162)
(163)
(164)
This mathematical model in the Eulerian description consists of eight equations: conservation of mass (1), balance of linear momenta (3), balance of angular momenta (3) and energy Equation (1) in thirty five dependent variables:
and . Thus, we need twenty-seven more equations for closure of the mathematical model. Constitutive theories yield twenty-one equations:
. Thus, we need an additional six equations for closure. These are discussed in Section 6.2.
6.1. Summary of Macro Conservation and Balance Laws in Lagrangian Description
Conservation of mass, balance of linear momenta, balance of angular momenta, first and second laws of thermodynamics and balance of moment of moments are given in the following:
(165)
(166)
(167)
(168)
(169)
(170)
This mathematical model consists of seven partial differential equations: balance of linear momenta (3), balance of angular momenta (3) and energy Equation (1) in thirty four dependent variables:
. Thus, an additional twenty-seven equations are needed for closure. Constitutive theories provide twenty-one equations:
. Thus, an additional six equations are needed for closure. These are discussed in Section 6.2.
6.2. 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). Eringen [6]-[23] [70] and those following his work suggest that in the derivations 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 [6]-[23] [70], it is stated that the three equations in (4) and the six equations in (5) 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 [54]. 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 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 (101) (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 (101) 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 (101) must be eliminated. This of course can be done by premultiplying Equation (101) or (167) with
, the inverse of
. Symbolically, we can write
(171)
or
(172)
But inverse of
(for values of 1, 2, 3 for
) is
, thus we can write (172) as
(173)
or
(174)
Since
(175)
is balance of angular momenta, (174) reduces to the following.
(176)
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 (176) with only negative sign.
(177)
Equations (177) are additional six equations that provide closure of the mathematical model.
Remarks
1) First, we note that (102) and (103) (balance of angular momenta) only contains nonclassical physics, both
and
are due to nonclassical physics, whereas (177) 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 (177) must hold. When the microconstituents and the medium are of different material, (177) 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 nonclassical physics.
6.3. Constitutive Theories for Linear Elastic Micromorphic Solid Continua
We assume that the medium and microconstituents are linear elastic. Thus, in the derivation of the constitutive theories for
and
, we consider only linear elasticity in this paper.
6.3.1. Determination of Constitutive Tensors and Their Argument Tensors
In deriving constitutive theories, we always begin with the rate of work or otherwise conjugate pairs in the entropy inequality, for determination of the constitutive tensors based on the causality axiom of constitutive theory and their possible argument tensors. The choice of constitutive tensors can be altered or changed if the physics requires it, and the argument tensors of the constitutive tensors can be augmented with additional tensors if the physics requiring this has not been considered while deriving the entropy inequality. We follow the details and the guidelines presented in references [68] [69]. Once the constitutive tensors and their argument tensors are established, we follow the theory of isotropic tensors or representation theorem for deriving the constitutive theories and the standard procedure of Taylor series expansion of the coefficients in the linear combination of the basis of the space of constitutive tensor for determining the material coefficients [68] [69].
Consider the entropy inequality (169).
(178)
The macro stress tensor
is nonsymmetric, and hence cannot be a constitutive tensor due to representation theorem [55]-[66]. Thus, we need additive decomposition of
into symmetric tensor
and skew symmetric tensor
. There cannot be constitutive theory for
, as it is defined by the balance of angular momenta. Thus,
is the constitutive tensor, and not
or
.
(179)
Secondly
(180)
in which
is the displacement gradient tensor, and
and
are symmetric and skew-symmetric tensors obtained by additive decomposition of
.
(181)
Likewise, additive decomposition of (
) and
into symmetric and skew-symmetric tensors gives:
(182)
Also
(183)
and
(184)
in which
is micro displacement gradient tensor and
and
are symmetric and skew-symmetric tensors due to additive decomposition of
. Furthermore,
(185)
Also
(186)
Substituting (179) - (186) as needed in the entropy inequality (169) and noting that
(187)
We can write (169) as follows:
(188)
From balance of angular momenta
(189)
Substituting (189) in (188)
(190)
A simple calculation shows that
(191)
Using (191) in (190), (191) reduces to
(192)
Further additive decomposition of
into equilibrium and deviatoric stresses,
and
, is used to derive the constitutive theory for volumetric and distortional deformation physics, which are mutually exclusive
(193)
Substituting (193) in (192)
(194)
The rate of work conjugate pairs and the last term in (194) suggest, in conjunction with the axiom of causality [69], that
, and
are valid choices of constitutive tensors. The initial choice of argument tensors is as follows (
is included as an argument tensor in all constitutive tensors because of non-isothermal physics):
(195)
(196)
(197)
(198)
(199)
Even though we do not need a constitutive theory for
, its argument tensors are essential to establish as it is used to simplify entropy inequality (194) as well as to derive constitutive theory for
. The presence of
in (194) must be addressed as well. Clearly,
and
must be argument tensors of both
and
. Other argument tensors of
and
are chosen based on principle of equipresence. However, the principle of equipresence is not used in (195) - (199), since the conjugate pairs appearing in the entropy inequality (194) directly dictate their selection.
(200)
(201)
The energy Equation (168) can be simplified in the same manner as the entropy inequality to obtain the following (similar to (194))
(202)
6.3.2. Constitutive Theory for Equilibrium Cauchy Stress Tensor
In Lagrangian description, density
is determined directly from the conservation of mass
, once the deformation gradient tensor
is known. Therefore, density
cannot be an argument tensor of the constitutive tensors [69]. However, compressibility and incompressibility physics is related to density and temperature. Consequently, the constitutive theory for
cannot be derived from the entropy inequality (194) in the Lagrangian description. Instead, we must begin with the entropy inequality similar to (194) in the Eulerian description to derive constitutive theory for
first.
(203)
In this case,
is unknown and therefore treated 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:
(204)
(205)
(206)
(207)
(208)
(209)
(210)
Using (209), we can write
(211)
From conservation of mass in the Eulerian description
(212)
Substituting from (212) for
in (211) and then substituting (211) in (203), we obtain the following after regrouping the terms
(213)
The entropy inequality (213) holds for arbitrary but admissible choices of and
if the following conditions hold:
(214)
(215)
(216)
(217)
(218)
Equations (214) - (218) imply that
is not a function of and
. Equation (218) implies that
is deterministic from
; hence,
is not a constitutive or dependent variable. Using (214) - (218), the constitutive tensors and their argument tensors in (204) - (208) remain the same, but the argument tensors of
and
can be modified:
(219)
(220)
and the entropy inequality (213) reduces to
(221)
Constitutive theory for
for compressible matter can be obtained by setting coefficient of
in the first term of (221) to zero.
(222)
(223)
in which
is thermodynamic pressure, the equation of state for 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, the conservation of mass gives:
(224)
and
(225)
Hence, for incompressible solid, the constitutive theory for
cannot be derived using (222) and (223). First, using (225), the entropy inequality (221) reduces to
(226)
In order to derive constitutive theory for
for incompressible solid matter, we must introduce incompressibility condition in (226). From the continuity equation, the velocity field for incompressible matter is divergence free, i.e.,
(227)
If (227) holds, then the following holds too:
(228)
in which,
is a Lagrange multiplier. Adding (228) to (226) and regrouping terms
(229)
Entropy inequality (229) holds for arbitrary but admissible
, if the coefficient of
in the first term in (229) is set to zero, giving:
(230)
The reduced form of entropy inequality is given by:
(231)
In the Lagrangian description, the constitutive theory for
can be obtained directly from (222), (223) and (230).
(232)
(233)
The reduced form of entropy inequality in the Lagrangian description follows directly from (231).
(234)
In the following, we present the derivation of constitutive theories for
and
using representation theorem [55]-[66]. The tensors
are symmetric tensors of rank two and their work 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 the representation theorem.
6.3.3. 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 (234). This conjugate pair, in conjunction with axiom of causality, suggests that
is the constitutive tensor and
as its argument tensor. Thus, we can write (with
included in the argument tensors due to non-isothermal physics)
(235)
Equation (235) suffices for thermoelastic deformation physics.
Let
be the combined generators of the argument tensors of
in (235), which are symmetric tensors of rank two. Then,
together with
constitute the basis of the space of tensor
, referred to as integrity basis. Now,
can be expressed as a linear combination of the basis in the current configuration.
(236)
in which
are combined invariants of the argument tensors of
in (235). The material coefficients in (236) are determined by expanding
in the invariants
and the temperature
about a known configuration
and only retaining up to linear terms in
and temperature
.
(237)
We substitute
from (237) into (236)
(238)
Collecting coefficients of
and
, we can write (238) as follows:
(239)
The material coefficients
and
are defined in the following:
(240)
The constitutive theory (239), together with material coefficients (240), is based on integrity, i.e., the complete basis of the space of constitutive tensor
. Simplified forms of (239) can be obtained from (239) by retaining specific generators and invariants. A simplified yet sufficiently general constitutive theory for
is one in which
is expressed as a linear function of the components of its argument tensors. By redefining the material coefficients and rearranging terms in (239), we can write the following:
(241)
6.3.4. Constitutive Theory for Stress Tensor
Consider (197), i.e.,
(242)
Let
be the combined generators of the argument tensors of
in (242), which are symmetric tensors of rank two and let
be the combined invariants of the same argument tensors of
in (242). Then,
constitute the basis of the space of constitutive tensor
, and we can write the following expression for
.
(243)
in which
(244)
Following the procedure described in Section 6.3.3 (Taylor series expansion and collecting coefficients) we can derive the following constitutive theory for
(245)
in which material coefficients are given by (240) 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 that is linear in the components of the argument tensors is given by (after redefining material coefficients)
(246)
6.3.5. Constitutive Theory for Moment Tensor
Rigid rotations and rotation rates of the microconstituents in the medium require consideration of elasticity due to rotation gradient tensor.
is the constitutive tensor and its argument tensors are given by:
(247)
Let
and
be the combined generators and combined invariants of the argument tensors of
in (247) in which
are symmetric tensors of rank two. Then based on the representation theorem,
constitute basis of the space of constitutive tensor
(integrity). Thus, we can represent
as a linear combination of the basis in the current configuration.
(248)
in which coefficients
(249)
Following the procedure described in Section 6.3.3 (Taylor series expansion) we can derive the following constitutive theory for
:
(250)
in which material coefficients are given by after replacing
and
with
and
. The material coefficients can be functions of
and
in a known configuration
.
A constitutive theory that is linear in the components of the argument tensors is given by:
(251)
6.4. Constitutive Theory for
Consider
(252)
Following references [68] [69], we can derive the following constitutive theory for
using representation theorem.
(253)
where
and
are material coefficients. These can be functions of
and
. In (253),
is invariant of argument tensor
. Simplified form of (253), the Fourier heat conduction law is given by
(254)
7. Thermodynamic and Mathematical Consistency of the Micromorphic Theory Presented in the Paper
This requires that we establish that while deriving conservation and the balance laws and the constitutive theories the principles of thermodynamics and well established mathematical concepts have not been violated. The following list of what has been used in deriving the linear micromorphic theory establishes its thermodynamic and mathematical consistency.
1) Conservation and balance laws of classical continuum mechanics are applied and hold for microconstituent deformation.
2) Integral-average definitions derived from the microconstituents’ conservation and balance laws permit the use of conservation and balance laws of classical continuum mechanics at micro level with appropriate modifications due to new microconstituent deformation physics.
3) Separation of micro constituent strains and rigid rotations by additive decomposition of the microconstituent deformation gradient tensor is essential for a thermodynamically correct and consistent treatment of the deformation physics and the rigid rotation physics. The constitutive theory for the microconstituent stress tensor obviously requires the use of strain measure (and not the rigid rotations or the micro deformation gradient tensor) while the rigid rotations are part of the constitutive theory for the moment tensor.
4) The rigid rotations of the microconstituents (present in all three 3M theories) and the conjugate moment constitute a new kinematically conjugate pairs in 3M theories in addition to displacements and forces already present (classical continuum mechanics). Each conjugate pair requires two balance laws: balance of forces and balance of moment of forces due to displacement and force kinematic pair and balance of moments and balance of moment of moments due to the new kinematically conjugate pair of rotations and moments. The balance of moment of moments balance law has been shown to be essential [44] [54] [67] in 3M theories. In its absence, incorrect conjugate pairs appear in the entropy inequality that yield nonphysical and invalid constitutive theories, resulting in violation of thermodynamic consistency of the resulting theory.
5) Inequality restrictions imposed on the conjugate pairs in the entropy inequality are satisfied by the constitutive theories derived in the paper.
6) Choice of constitutive tensors and their argument tensors are decided from the conjugate pairs in the entropy inequality in conjunction with axiom of causality.
7) All constitutive tensors of rank two are symmetric tensors with symmetric tensors of rank two, tensors of rank zero and one as their argument tensors. This is supported by representation theorem, hence the resulting constitutive theories are mathematically consistent.
8) Deformation/strain measures derived in ref. [32] by Surana et al. are found to be valid for linear micromorphic theory, and hence are used in the present work.
9) All constitutive theories are derived using the complete basis (integrity) of the spaces of constitutive tensors first, followed by derivation of material coefficients. This is followed by simplified constitutive theories supported by the one derived using integrity.
10) Appropriate additive decomposition of the constitutive tensors is done to ensure that the physics of deformation is correctly described by the constitutive theories. Additive decomposition of
,
are examples that help in determination of correct constitutive tensors for specific physics.
11) In summary all derivations presented in the paper for conservation and balance laws and specifically the constitutive theories are supported both thermodynamically and mathematically.
8. Linear Micromorphic Theory of Eringen
The linear micromorphic microcontinuum theory presented by Eringen [17]-[22] [70] is used almost exclusively in all published works related to micromorphic theories. We list important features and details of the linear micromorphic theory of Eringen and compare them with the corresponding details of the micromorphic theory presented in this paper. This is followed by an evaluation of their admissibility based on thermodynamic principles and the well established mathematical concepts.
1) In Eringen’s linear micromorphic theory a microconstituent has nine degrees of freedom defined by the nine components of the microconstituent deformation gradient tensor
. Additive decomposition of
shows that its skew-symmetric component contains rigid rotations of microconstituents. Thus, components of
contain deformation as well as rigid rotations hence
cannot be used as a strain measure.
In the present work, we consider additive decomposition of
into
and
tensors. The three rigid rotations in
are in fact classical rotations
in the present work, hence these are not unknown degrees of freedom. Six components of
constitute unknown degrees of freedom for the microconstituents. In this approach rigid rotations of the microconstituents are
that remain the same in all three 3M theories and their treatment in the development of the theories also remains the same.
In the works of Surana et al. on micropolar theories [24]-[55] and in the micromorphic theory presented here, rigid rotations
result in the Cauchy moment tensor. In Eringen’s work, the moment tensor definition is in error as it cannot be due to classical continuum physics of the microconstituent Cauchy stress tensor.
2) Micro and macro conservation of mass presented in this paper is exactly the same as in references [17]-[22] [70] presented by Eringen.
3) The balance of linear momenta, balance of angular momenta and the balance of first moment of momenta (in Eringen’s works [17]-[22] [70]) are derived by considering weighted integral of the balance of microlinear momenta using a weight function
.
(255)
in which
.
Using
(256)
Equation (255) can be written as:
(257)
or
(258)
a) Macrobalance of linear momenta is derived using
in which case
and Equation (258) reduces back to (255) with
but with the substitution (256). This form is the same as the standard approach for balance of macro linear momenta, hence yields the same balance of macro linear momenta equations as we have in this paper.
b) In Eringen’s work balance of angular momenta is derived using
in (258).
c) Balance of first moment of momentum is derived using
.
There are many issues, inconsistencies and possible errors in this approach. We discuss these in the following:
i) There is no basis for using
as a weight function in (255).
ii) Introduction of (256) due to
in (255) changes the original physics in (255) which is the correct physics of the balance of microlinear momenta. Hence, the derivation that follows is of concern.
iii) Introduction of a third rank moment tensor through
(259)
is not valid due to the fact that
is a symmetric Cauchy stress tensor for the microconstituents (classical continuum mechanics), hence cannot possibly yield something that is purely related to nonclassical microcontinuum physics, i.e.,
tensor.
iv) The fundamental mistake is that balance of angular momenta is the sum of the rate of change of moment of linear momenta, the moment of all other forces and the moments. Thus, the permutation tensor can only appear with the rate of change of moment of momenta and moment of forces and not with the Cauchy moment tensor as it is already a moment tensor. Due to this error, definition (259) is in error and the balance of angular momenta and balance of first moment of momentum are in error as well. Since, balance of angular momenta is used in the energy equation and the entropy inequality, these are in error also.
v) Due to i) - iv), the balance laws have incorrect definitions of “integral-average” moment tensor and as a consequence their derivations have errors and are in violation of thermodynamic consistency.
4) Constitutive tensors are nonsymmetric tensors of rank two and their argument tensors are also nonsymmetric tensors of rank two. This is not supported by the theory of isotropic tensors (representation theorem) [55]-[66]. For nonsymmetric tensors, the basis of the space of the constitutive tensors cannot be established. Thus, all constitutive theories for nonsymmetric constitutive tensors are in violation of mathematical consistency, as these cannot be supported by well established mathematical concepts of the representation theorem. For the most part, the derivation of constitutive theories presented by Eringen for nonsymmetric constitutive tensors using potentials or using the polynomial approach has no mathematical foundation either, hence it is ad hoc or phenomenological in our view.
5) The principle of equipresence used almost in all works of Eringen including micromorphic theories introduces nonphysical coupling between classical and nonclassical physics, hence results in many nonphysical material coefficients that either need to be justified or whose elimination needs to be proved.
6) Various additive decompositions shown to be essential in our work in deriving physical and valid constitutive theories are entirely missing in Eringen’s work.
7) The constitutive theory for the nonsymmetric stress tensor, of course, violates the representation theorem, but additionally it contains
for which there cannot be a constitutive theory as it is completely defined by the balance of angular momenta in terms of gradients of the Cauchy moment tensor.
8) Eringen’s work does not use the balance of moment of moments balance law; as a consequence Cauchy moment tensor is nonsymmetric, further leading to a nonphysical constitutive theory for nonsymmetric moment tensor and resulting in thermodynamic inconsistency of the resulting micromorprhic theory.
9) It is instructive to check the closure in our linear micromorphic theory and the linear micromorphic theory of Eringen. In the linear micromorphic theory presented in this paper, we have: 34 dependent variables
and 34 equations: balance of linear momenta(3), balance of angular momenta(3), balance of moment of symmetric stresses (6), energy Equation (1), and constitutive theories for
. Hence, the mathematical model has closure.
In Eringen’s linear micromorphic theory, there are 43 dependent variables:
and 40 equations: balance of linear momenta (3), balance of angular momenta (3), balance of moment of momentum (6), energy Equation (1), and constitutive theories for:
, thus additional three equations are needed for closure. Eringen advocates these to be due to conservation of micro inertia.
We remark that in Eringen’s work
and
have nine independent components each requiring nine constitutive equations. In our theory,
and
have six and nine independent components but only six constitutive equations for each are required as
(three components) are balanced by the balance of angular momenta hence cannot be part of the constitutive theory. In Eringen’s theory
has nine independent components all of which are considered degrees of freedom in Eringen’s theory. In our case
has only six independent components and
are in fact
, hence are not unknown degrees of freedom. Thus, a microconstituent only has six unknown degrees of freedom. These significant differences are necessary to note so that we can see why our micromorphic theory is quite different from that of Eringen.
10) The conservation of micro inertia law is proposed by Eringen to obtain the additional three equations needed for closure of Eringen’s mathematical model. The laws of thermodynamic have no such conservation law. In our work presented in the paper, which is strictly based on the laws of thermodynamics and well-established mathematical principles, the need for an additional conservation or balance law does not arise. These equations proposed by Eringen are not part of the thermodynamic framework and laws. We keep in mind that we are not discarding the conservation of microinertia. This conservation law is not part of the laws of thermodynamics, and hence its need never arises in our micromorphic theory that is strictly based on the thermodynamic framework.
11) All issues and concerns regarding Eringen’s work have been discussed and illustrated using the well-established laws of thermodynamics and well-established principles of applied mathematics; hence, our remarks and comments in the paper regarding Eringen’s work are not to be misconstrued as speculative.
In summary, we have presented ample evidence that the linear micromorphic theory of Eringen is both thermodynamically and mathematically inconsistent as a microcontinuum theory, hence cannot be considered a valid micromorphic microcontinuum theory.
9. Summary and Conclusions
A linear micromorphic continuum theory has been presented in which the mechanism of elasticity is considered for the microconstituents, for the solid medium and for the interaction of the microconstituents with the solid medium. In the following, we summarize the work presented in the paper and draw some conclusions.
1) In the present micromorphic theory, a microconstituent also has nine degrees of freedom, as in the case of Eringen’s theory, but the degrees of freedom are completely different. In our work, rotations of the microconstituents (described by
, hence known) and the six independent components of the symmetric part of the micro displacement gradient tensor (unknown) constitute nine degrees of freedom, out of which
are known; thus, we have only six unknown degrees of freedom for microconstituents. In Eringen’s work, all nine components of the micro deformation gradient tensor are considered unknown degrees of freedom. In these degrees of freedom, rigid rotations and deformations are not separated, leading to incorrect considerations in the derivation of the theory compared to the theory we have presented in this paper.
2) In the theory presented here, care is taken to ensure that the rigid body rotation physics of the microconstituent, which is common to all three 3M theories, is incorporated in an identical manner in all three 3M theories.
3) Our work recognizes that rotations
and the Cauchy moment tensor form a new kinematically conjugate pair in all three 3M theories, and hence will require two balance laws just as the displacement-force kinematic pair does in classical continuum mechanics. This necessitates a new balance law in all 3M theories [38] [54] [67]: the balance of moment of moments. This balance law is never used in Eringen’s work, the consequence of this is spurious constitutive theories.
4) Varying rotations
in the deforming solid medium, when resisted, create moments. Our derivation shows that the Cauchy moment tensor and the symmetric part of the gradients of
are work conjugate. This physics is purely due to nonclassical mechanics, hence it has no interaction or any connection to classical continuum theory. Based on this, the “integral-average” definition of moment tensor (259) by Eringen is incorrect as it is based on
which is purely due to classical continuum mechanics.
5) Our derivation in this paper shows that the use of weight function
in Eringen’s work in the derivation of the macro balance of linear momenta, balance of angular momenta and moment of moment has no thermodynamic basis. Our work shows that the use of
as advocated by Eringen is not justified based on the physics considered in the balance laws and leads to balance laws different from those obtained without using it.
6) All constitutive tensors of rank two are symmetric tensors and their argument tensors of rank two are also symmetric tensors, hence permitting the use of representation theorem in deriving constitutive theories that are naturally mathematically consistent. This is in contrast with published works in which the constitutive tensors of rank two are mostly nonsymmetric tensors with nonsymmetric argument tensors. Such constitutive theories derived using assumed potentials are nonphysical and cannot be justified based on representation theorem.
7) Conservation of micro inertia, advocated by Eringen to be necessary in 3M theories, is neither needed in the present work nor used. These additional equations are required primarily due to
being unknown degrees of freedom, whereas in our work,
are in fact
, hence known. Other significant differences are that in Eringen’s work,
and
are nonsymmetric and nine constitutive equations are considered for
, as well as
. In our work,
decomposition is used and there are only six constitutive equations needed for
.
is symmetric due to the balance of moment of moments balance law, hence only six constitutive equations are needed for
as well. It is shown in Section 8 why Eringen’s micromorphic theory does not have closure without the conservation of micro inertia conservation law.
8) The thermodynamic and mathematical consistency of the linear micromorphic theory presented in this paper has been established in Section 7. The lack of thermodynamic and mathematical consistency of Eringen’s linear micromorphic theory has been discussed and illustrated in Section 8.
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 while he was a graduate student in the Department of Mechanical Engineering. The computational facilities provided by the Computational Mechanics Laboratory of the mechanical engineering departments are also acknowledged.