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Technical Papers
Oct 13, 2015

Interfacial Micromechanics Assessment of Classical Rheological Models. I: Single Interface Size and Viscosity

Publication: Journal of Engineering Mechanics
Volume 142, Issue 3

Abstract

Creep functions are often represented by “rheological models” consisting of springs and dashpots, while the actual microscopic origins of creep, such as micro-sliding along interfaces, has only recently been explicitly considered in a continuum mechanics framework. The question arises whether formal analogies between the former and the latter can be derived: This question is answered here for the rheological models of the Kelvin-Voigt and Maxwell type. Thereby, it appears a full analogy between shear stresses and strains acting on the rheological models, and those acting on a micromechanical representative volume element consisting of an elastic solid matrix with embedded viscous interfaces, whereby the respective viscosity arises from layered polar fluids absorbed at these interfaces. The corresponding Kelvin-Voigt parameters are much simpler and more intuitively related to the micromechanical quantities, when compared to the Maxwell parameters. More specifically, rheological spring parameters are always related to the shear stiffness of the elastic solid matrix, while they may additionally depend on the Poisson’s ratio of the elastic solid matrix, and on the interface density. On the other hand, dashpot viscosities are always related to interface viscosities, interface radii, and interface densities; and they may even depend on the Poisson’s ratio of the elastic solid matrix.

Introduction

In 1874, Boltzmann introduced the concept of creep functions as well as the associated superposition principle, and he confirmed these groundbreaking ideas by an initial experimental campaign (Boltzmann 1874). Ever since, these ideas have remained the fundament of the theory of viscoelasticity, which has been developed up to high mathematical maturity (Gurtin and Sternberg 1962; Salençon 1983; Leitman and Fisher 1973). In order to keep things simple, exponential creep functions are often considered, and they are standardly related to the simple rheolgical models composed of linear springs and dashpots. Their simplest versions exhibit a parallel arrangement of one spring and one dashpot (the so-called Kelvin-Voigt model) (Thomson 1865; Voigt 1890), or a serial arrangement of one spring and one dashpot (the so-called Maxwell model) (Maxwell 1867). Slightly more complex arrangements of spring and dashpots are normally called standard linear solid models. They can be either represented as a serial arrangement of a Kelvin-Voigt unit and an additional spring [Kelvin-Voigt representation or Zehner model (Zener 1948)], or as a parallel arrangement of a Maxwell unit and an additional spring (Maxwell representation). However, such simple models do not contain any direct information on the microstructural origin of creep, such as the flow of water along thin layers within the texture of hydrated bio- or geomaterials (Morrow et al. 2000; Stipp et al. 2006; Tullis and Yund 1991; Arnold and Venditti 2001; Bažant et al. 1997; Alizadeh et al. 2010; Kalinichev et al. 2007; Vlahinić et al. 2012; Youssef et al. 2011; Németh et al. 1998; Cordobés et al. 1997; Eberhardsteiner et al. 2014; Sasaki et al. 1993). These layers typically exhibit areal dimensions in the micrometer range, and nanoscopic thicknesses. Aiming exactly at the aforementioned direct consideration of viscous “micro-”interfaces when mathematically describing macroscopic creep behaviors, we recently developed a micromechanical formulation for matrix-interface composites consisting: (1) of a continuous isotropic linear elastic solid matrix; and (2) of embedded parallel interfaces filled by a liquid crystal exhibiting a linear viscous behavior (Shahidi et al. 2014), see also Fig. 1. The obvious question arising then is: How does such a micromechanical formulation and the microstructural quantities appearing therein relate to the classical rheological models made up of springs and of dashpots? As an answer to this question, we here aim at establishing relations between microstructural quantities, such as interface size, interface density, interface viscosity, as well as elastic properties of the solid material phase (Fig. 1), on the one hand, and spring stiffnesses and dashpot viscosities of macroscopic rheological models (as illustrated in Figs. 2 and 3), on the other hand. Therefore, it suffices to consider macroscopic pure shear strains in planes orthogonal to the viscous interfaces (with normals e̲z), i.e., in the x,z-plane or in the y,z-plane of Fig. 1. Namely, in the chosen base frame e̲x, e̲y, e̲z, only the aforementioned shear strain components are related to creep deformation, and hence, we here focus on relations between macroscopic strains
E̲̲=Exz(e̲xe̲z+e̲ze̲x)
(1)
and corresponding stresses
Σ̲̲=Σxz(e̲xe̲z+e̲ze̲x)
(2)
When it comes to the rheological models as depicted in Figs. 2 and 3, it is noteworthy that they refer to the behavior of a unit cube of a tested material, i.e., the “force” acting on the rheological model is equal to the shear traction acting on the material unit cube, and the “elongation” of the spring-dashpot model is equal to the engineering shear strain of the material unit cube.
Fig. 1. Matrix-interface composite consisting of continuous isotropic solid matrix and parallel 2D interfaces; 2D sketch of 3D representative volume elements
Fig. 2. Kelvin-Voigt representation of standard linear solid, used to model time-dependent behavior under pure shear according to Eq. (4): (a) complete arrangement of spring and dashpot elements; (b) section through Kelvin-Voigt unit, for illustration of shear stress contributions
Fig. 3. Maxwell representation of standard linear solid, used to model time-dependent behavior under pure shear according to Eq. (4): (a) complete arrangement of spring and damper elements; (b) section through the rheological model, for illustration of shear stress contributions
In order to establish the aforementioned link between micromechanics and classical rheology, we will, in the remainder of this paper: (1) derive differential equations describing the material behavior in terms of overall stresses and strains defined on representative volume elements; and (2) carry out a dissipation analysis, where we will consider the fundamental thermodynamics definition of the dissipation D, which is equal to the rate of work of the external forces, Σ̲̲:E˙̲̲, minus the rate of elastic or free “Helmholtz” energy Ψ˙
D=Σ̲̲:E˙̲̲Ψ˙
(3)
This will be developed, in three consecutive sections, for (1) the Kelvin-Voigt representation of the standard linear solid model, for (2) the Maxwell representation of the standard linear solid model, and for (3) a matrix-interface composite. Corresponding analytical formulations will allow us to relate rheological spring stiffnesses and the dashpot viscosities of standard linear solid models, to microstructural features of a matrix-interface composite. This composite, as seen in Fig. 1, is not modelled up to each and every detail of the microstructure (which, in reality, is not known anyway), but follows the tradition of continuum micromechanics (Zaoui 2002), in reflecting only the mechanically most relevant microstructural features. Even more so, we introduce the very minimum of such features, which results in a highly “idealized” system as seen in Fig. 1, so as to relate standard material parameter of classical rheological models, to the nature of different objects found in many creep-active material systems such as clay, concrete, or bone, where interfaces filled with viscously behaving matter, are embedded into elastic domains. This explicitly reductionist vision includes the introduction of only one (average) interface size [extension to several such sizes is discussed in the companion paper, Part II (Shahidi et al. 2015)], of the 2D planar geometry of the interfaces, and of only one interface density per interface size, i.e., leaving aside explicit consideration of fluctuations of such densities within the considered RVE. Nevertheless, as often encountered in science (Popper 1935), such as reductionist approach will lead to surprisingly general and helpful results. In particular, it will allow for a micromechanical interpretation of the stresses and strains which are formally associated with the rheological springs and dashpots, and for a micromechanical illustration of the energy dissipating in the dashpots. Implications for preferential choices of rheological parameters, and their relation to experiments, will be covered, thereafter, in the Discussion section.

Review of Rheological “Spring-Dashpot” Models

Kelvin-Voigt Representation of Standard Linear Solid

The Kelvin-Voigt representation of the standard linear solid consists of a Kelvin-Voigt unit (i.e., parallelly set spring and dashpot elements) in series with an additional elastic spring (Fig. 2). Here, we focus on pure shear deformation, so that rheological shear stresses τ and strains γ are related to the following stress and strain tensors by analogy to Eqs. (1) and (2)
Σ̲̲=τ(e̲xe̲z+e̲ze̲x)andE̲̲=12γ(e̲xe̲z+e̲ze̲x)
(4)
The overall shear deformation of the rheological model, γ, can be decomposed into a dissipative portion related to the Kelvin-Voigt unit (γ1) and an elastic portion related to the single spring (γe)
γ=γ1+γe
(5)
The overall shear stress τ, in turn, is transferred both through the Kelvin-Voigt unit (τ1=τ) and through the elastic spring (τe=τ)
τ=τ1=τe
(6)
The shear stress acting on the Kelvin-Voigt unit, τ1, can be decomposed into the shear stress acting on the spring, τ1μ, and into the one acting on the dashpot, τ1η
τ1=τ1μ+τ1η
(7)
where indexes μ and η refer to the spring and to the dashpot, respectively.
Derivation of a differential equation in τ and γ describing the constitutive behavior of the rheological model requires individual constitutive laws for all three rheological devices. Denoting the stiffness of the additional elastic spring as μe, and the one of the Kelvin-Voigt spring as μ1, as well as the dashpot viscosity as η1, Fig. 2, the individual constitutive laws read as
τ1μ=μ1γ1,τ1η=η1γ˙1,τe=μeγe
(8)
where a dot is standing for the time derivative ˙=/t. The sought differential equation is obtained by combining Eqs. (58), with the aim to eliminate the individual stress combinations τ1μ and τ1η as well as the individual strain combinations γ1 and γe. To this end, Eq. (7) is specified for (6) and (8), and the resulting expression is divided by η1
τη1=μ1η1γ1+γ˙1
(9)
Next, the last Eq. (8) is specified for (6) and solved for γe, yielding τ/μe=γe. The equality is modified in two different directions: firstly, we consider its time derivative
τ˙μe=γ˙e
(10)
and secondly, we consider it multiplied by μ1/η1
τμ1μeη1=μ1η1γe
(11)
The differential equation describing the constitutive behavior of the rheological model follows from summing up Eqs. (9)(11), as well as from consideration of (5) and of its time derivative, γ˙=γ˙1+γ˙e, as
τ˙μe+τμ1η1(1μ1+1μe)=γ˙+μ1η1γ
(12)
Eq. (12) is a first-order ordinary differential equation in the overall shear stress τ and the overall shear strain γ.
Specification of the dissipation D according to Eq. (3), for the Kelvin-Voigt representation of the standard linear solid model requires expressions for the rate of work of the external forces, Σ̲̲:E˙̲̲, and the rate of elastic internal energy Ψ˙. According to Eq. (4), the former is simply equal to “force” τ acting on the rheological model times the “elongation rate” γ˙, i.e., the shear stress τ times the rate of the engineering strain, γ˙
Σ̲̲:E˙̲̲=τγ˙
(13)
Elastic internal energy Ψ, in turn, is stored in the two springs. In both cases the energy is equal to 1/2 times the spring’s force multiplied with its elongation; under consideration of (8) we obtain
Ψ=12τ1μγ1+12τeγe=12γ1μ1γ1+12γeμeγe
(14)
Taking the time derivative of (14), and consideration of (8), delivers the sought rate of elastic internal energy as
Ψ˙=μ1γ1γ˙1+μeγeγ˙e=τ1μγ˙1+τeγ˙e
(15)
The dissipation finally follows from specification of (3) for (13) and (15). This yields, under consideration of (6), of (5) in the form γ˙γ˙e=γ˙1, and of (7) in the form ττ1μ=τ1η
D=τ(γ˙γ˙e)τ1μγ˙1=(ττ1μ)γ˙1=τ1ηγ˙1
(16)
Eq. (16) underlines that energy dissipates exclusively in the dashpot.

Maxwell Representation of Standard Linear Solid

The Maxwell representation of the standard linear solid consists of a Maxwell unit (i.e., serially set spring and dashpot elements) in parallel with an additional elastic spring (see Fig. 3). Here, it is considered to represent a piece of material under pure shear, see (4). The overall shear stress of the rheological model, τ, can be decomposed into the shear stress of the Maxwell unit (τI) and into the one of the elastic spring (τE)
τ=τI+τE
(17)
The overall shear deformation γ, in turn, is equal to the deformation of the Maxwell unit (γI=γ) and to the deformation of the elastic spring (γE=γ)
γ=γI=γE
(18)
The shear deformation of the Maxwell unit, γI, can be decomposed into the shear deformation of the spring, γIμ, and into the one of the dashpot, γIη
γI=γIμ+γIη
(19)
where indexes μ and η refer to the spring and to the dashpot, respectively.
Derivation of a differential equation in τ and γ, describing the constitutive behavior of the rheological model, requires individual constitutive laws for all three rheological devices. Denoting the stiffness of the additional elastic spring as μE, and the one of the Maxwell spring as μI, as well as the dashpot viscosity as ηI, the individual constitutive laws read by analogy to (8) as
τI=μIγIμ,τI=ηIγ˙Iη,τE=μEγE
(20)
The sought differential equation is obtained by combining Eqs. (1720), with the aim to eliminate the individual strain components γIμ and γIη, as well as the individual stress components τI and τE. To this end, the time derivative of (19) is specified for γ˙Iμ and γ˙Iη from (20), delivering under consideration of (18)
τ˙IμI+τIηI=γ˙
(21)
Next, the last Eq. (20) is specified for (18), and the resulting equality, τE=μEγ, is modified in two different directions: firstly, we consider it multiplied with 1/ηI
τEηI=μEγηI
(22)
and, secondly, we consider its time derivative, multiplied with 1/μI
τ˙EμI=μEγ˙μI
(23)
The differential equation describing the constitutive behavior of the rheological model follows from summing up Eqs. (2123) and from consideration of (17) as well as of its time derivative, τ˙=τ˙I+τ˙E, as
1μIτ˙+1ηIτ=γ˙(1+μEμI)+μEηIγ
(24)
Eq. (24) is a first-order ordinary differential equation in the overall shear stress τ and the overall shear strain γ.
Specification of the dissipation D according to Eq. (3), for the Maxwell representation of the standard linear solid model requires expressions for the rate of work of the external forces, Σ̲̲:E˙̲̲, and the rate of elastic internal energy Ψ˙. The former reads by analogy to (13) as
Σ̲̲:E˙̲̲=τγ˙
(25)
Elastic internal energy Ψ, in turn, is stored in the two springs. In both cases the energy is equal to 1/2 times the spring’s force multiplied with its elongation; under consideration of (20) we obtain
Ψ=12τIγIμ+12τEγE=12γIμμIγIμ+12γEμEγE
(26)
Taking the time derivative of (26), and consideration of (20), delivers the sought rate of elastic internal energy as
Ψ˙=μIγIμγ˙Iμ+μEγEγ˙E=τIγ˙Iμ+τEγ˙E
(27)
The dissipation finally follows from specification of (3) for (25) and (27). This yields, under consideration of (18), of (17) in the form of ττE=τI, and of (19) in the form γ˙Iγ˙Iμ=γ˙Iη
D=γ˙I(ττE)τIγ˙Iμ=τI(γ˙Iγ˙Iμ)=τIγ˙Iη
(28)
Eq. (28) underlines that energy dissipates exclusively in the dashpot.

Matrix-Interface Micromechanics

Materials Representation and Constitutive Relations

Consider matrix-interface composites consisting of one solid phase and of one interface phase comprising the entity of all viscous fluid layers (Fig. 1). The solid matrix phase exhibits linear elastic behavior characterized by an isotropic stiffness tensor C̲̲̲̲s
σ̲̲(x̲)=C̲̲̲̲s:ε̲̲(x̲)
(29)
with σ̲̲(x̲) and ε̲̲(x̲) as Cauchy microstresses and linear microstrains at any position x̲ in the solid phase. As regards the interfaces, we consider that molecular ordering-related joining forces prevent the interfaces from opening, hence dislocations in interface normal direction e̲z vanish ξz=0. The component of the traction vector acting in the interface plane, Tx, is related by a linear viscous law to the dislocation rate ξ˙x
Tx=ηintξ˙x
(30)
where ηint denotes a viscosity constant with physical dimension [stress×time/length], and where index x stands for the in-plane tangential direction aligned with the macroscopic loading, see Eqs. (2) and (1).
In order to derive a differential equation describing the constitutive behavior of the studied composite in terms of macroscopic stress Σxz and macroscopic strain Exz, we recall two fundamental interfacial micromechanics relations (Shahidi et al. 2014), derived in the framework of homogenization schemes for eigenstressed micro-heterogeneous materials (Pichler and Hellmich 2010):
The macroscopic state equation, expressing the macrostress Σ̲̲ as a function of the macrostrain E̲̲ and of the interface traction vector T̲ reads as (Shahidi et al. 2014)
Σ̲̲=C̲̲̲̲hom:E̲̲+B̲̲̲·T̲
(31)
where C̲̲̲̲hom denotes the homogenized stiffness tensor of the studied composite, and B̲̲̲ denotes a Biot-type tensor quantifying the influence of interface traction vector T̲ on the macrostress Σ̲̲ provided that the macrostrain E̲̲ is equal to zero. Specifying (31) for the matrix-interface composite shown in Fig. 1, and for loading in terms of pure macroscopic shear according to (1), allows for extracting the following scalar equation linking shear stress Σxz, shear strain Exz, and the in-plane interface traction vector component Tx (Shahidi et al. 2014)
Σxz=μs3(2νs)3(2νs)+16d(1νs)2Exz+16d(1νs)3(2νs)+16d(1νs)Tx
(32)
In (32), μs and νs stand for the shear modulus and for Poisson’s ratio of the isotropic solid matrix, and d denotes the interface density parameter (Budiansky and O’Connell 1976)
d=Na3
(33)
with N and a standing for the number of the interfaces per unit volume of the composite, and for the radius of the interfaces, respectively.
The concentration-influence relation expressing the dislocation vector ξ̲ as a function of the macrostrain E̲̲ and of the interface traction vector T̲, reads as (Shahidi et al. 2014)
ξ̲=A̲̲̲:E̲̲+D̲̲·T̲
(34)
where A̲̲̲ denotes a concentration tensor quantifying the influence of macrostrain E̲̲ on the dislocation vector ξ̲ provided that the interface traction vector T̲ vanishes, and D̲̲ stands for an influence tensor quantifying the influence of the interface traction vector T̲ on the dislocation vector ξ̲ provided that macrostrain E̲̲ vanishes. Specifying (34) for the matrix-interface composite shown in Fig. 1 and for loading in terms of pure macroscopic shear according to (1), allows for extracting the following scalar equation linking in-plane dislocation ξx, the shear strain Exz, and the in-plane interface traction vector component Tx (Shahidi et al. 2014)
ξx=8(1νs)aπ[3(2νs)+16d(1νs)][2ExzTxμs]
(35)
In order to derive the sought differential equation linking Σxz and Exz, as well as their time derivatives Σ˙xz and E˙xz, we solve the concentration-influence relation (35) for the interface traction Tx, and we insert the resulting expression into (32), delivering
Σxz=2μsExzμs2πdaξx
(36)
Taking the time derivative of (36), multiplying ξ˙x by 1 in form of ηint/ηint yields, under consideration of (30)
Σ˙xz=2μsE˙xzμs2πdaηintTx
(37)
Solving (37) for Tx and inserting the resulting expression into (32), delivers the sought differential equation describing the constitutive behavior of the studied composite as
Σ˙xz1μs+Σxzπ[3(2νs)+16d(1νs)]8aηint(1νs)=2E˙xz+2Exz3(2νs)πμs8(1νs)aηint
(38)
Eq. (38) is a first-order ordinary differential equation in the overall shear stress Σxz and the overall shear strain Exz.

Elastic Energy and Dissipation

In order to quantify the elastic energy stored in the elastic solid matrix, it is convenient to replace the “eigentractions” T̲ of the interface phase, by eigenstresses σ̲̲iE of a flat spheroidal phase (whereby the limit case of the spheroid’s thickness going to zero would again relate to the two-dimensional interface). For such a system, state equations analogous to (31) and (34) read as (Pichler and Dormieux 2010; Pichler and Hellmich 2010)
Σ̲̲=C̲̲̲̲hom:E̲̲+σ̲̲iE:B̲̲̲̲
(39)
and
Φ̲̲=ϕiε̲̲i=B̲̲̲̲:E̲̲N̲̲̲̲1:σ̲̲iE
(40)
with ϕi and ε̲̲i as volume fraction and the strains of the spheroidal phase, with Φ̲̲ as the product of the latter two quantities, with C̲̲̲̲hom as the homogenized stiffness tensor, B̲̲̲̲ as the tensor of Biot coefficients, and N̲̲̲̲1 as the inverse of the tensor of Biot moduli. The latter quantities are defined as (Pichler and Dormieux 2010)
C̲̲̲̲hom=C̲̲̲̲s:[I̲̲̲̲+4πd3T̲̲̲̲i]1B̲̲̲̲=I̲̲̲̲C̲̲̲̲s1:C̲̲̲̲homN̲̲̲̲1=B̲̲̲̲:C̲̲̲̲s1
(41)
see also the Appendix for more details, in particular as concern the morphology tensor T̲̲̲̲i. The portion of elastic energy ψs stored per time increment in the purely elastically behaving solid matrix is equal to the external power Lsext supplied to this elastic matrix. This reads mathematically as (Pichler and Dormieux 2010)
ψ˙s=Lsext=Vsσ̲̲:ε˙̲̲dV=VRVEσ̲̲:ε˙̲̲dVViσ̲̲:ε˙̲̲dV=Σ̲̲:E˙̲̲σ̲̲iE:Φ˙̲̲
(42)
with σ̲̲ and ε̲̲ denoting the microscopic stress and strain fields within a representative volume element hosting an elastic matrix with spheroidal inclusions; and VRVE, Vs, and Vi, respectively, denoting the volume of such an RVE, and of its subvolumes hosting solid matrix and spheroidal inclusions, respectively.
In order to quantify the dissipation in matrix-interface composites, it is noteworthy that the elastic energy stored in the composite, Ψ, is equal to the elastic energy stored in the solid matrix, ψs, because the viscous interfaces do neither exhibit any elastic properties, nor do they, due to their 2D nature, occupy any significant volume within the RVE. Specification of the dissipation inequality (3) for Ψ˙=ψ˙s according to (42), yields the dissipation of the matrix-interface composite as
D=Σ̲̲:E˙̲̲ψ˙s=σ̲̲iE:Φ˙̲̲
(43)
The aim is now to transform (43) into a function of the variables characterizing the dissipative interfaces, namely T̲ and ξ̲. Therefore, Φ˙̲̲ follows from temporal derivation of (40):
Φ˙̲̲=B̲̲̲̲:E˙̲̲N̲̲̲̲1:σ˙̲̲iE
(44)
When additionally considering the actual two-dimensional nature of the interface phase, the eigenstress tensor degenerates to
σ̲̲iE=Tx(e̲xe̲z+e̲ze̲x)
(45)
and Φ˙̲̲ simplifies to
Φ˙̲̲=Φ˙xz(e̲xe̲z+e̲ze̲x)
(46)
Φ˙xz in (46) follows from specification of (44) for (1) and (45), resulting in:
Φ˙xz=16d(1νs)3(2νs)+16d(1νs)E˙xz8d(1νs)[3(2νs)+16d(1νs)]μsT˙x
(47)
whereby T˙x, through consideration of (35), can be expressed in terms of E˙xz and ξ˙x as
T˙x=2μsE˙xzμsπ[3(2νs)+16d(1νs)]8a(1νs)ξ˙x
(48)
Accordingly, insertion of (48) into (47) yields
Φ˙̲̲=ξ˙xdπa(e̲xe̲z+e̲ze̲x)
(49)
Finally, use of (49) and of (45) for transforming the expression (43), allows us to identify the dissipation as
D=2dπaξ˙xTx
(50)
Eq. (50) expresses explicitly that the energy dissipates exclusively in the viscous interfaces.

Interfacial Micromechanics Assessment of Classical Rheological Models

Micromechanical Explanation of Rheological Parameters

In the preceding sections we have derived equations describing, in terms of the overall shear stress and the overall shear strain, the constitutive behavior of the Kelvin-Voigt representation of the standard linear solid model, see (12), of the Maxwell representation of the standard linear solid model, see (24), and of a matrix-interface composite, see (38). These differential equations are valid for any type of prescribed loading history, including the special cases of a creep scenario (vanishing shear stress rate) and of a relaxation scenario (vanishing shear strain rate), see also the Appendix. Notably, the structure of the three differential equations is the same, i.e., an analogy can be established through comparison of (2), (1), and (4), by setting equal
τ=Σxzandγ=2Exz
(51)
In order to complete the analogy, also the factors of the stress and strain variables, as appearing in (12), (24), and (38), need to be set equal. In other words, comparison of these coefficients delivers the sought relations between spring stiffnesses and dashpot viscosities, on the one hand, and micromechanical quantities, such as interface density, size, and viscosity, as well as shear modulus and Poisson’s ratio of the solid matrix, on the other hand; see Table 1 for the result of this comparison and Figs. 46 for further illustration of relations between viscosities and stiffnesses.
Fig. 4. Dimensionless dashpot viscosities of Kelvin-Voigt and Maxwell models, η1 and ηI, over the dimensionless interface density parameter d, see also Table 1
Fig. 5. Dimensionless representation of interface-micromechanical origins of Kelvin-Voigt springs: instantaneous elasticity μe and delayed elasticity μ1 (both normalized with respect to the shear modulus of the solid elastic matrix μs), as functions of the interface density parameter d, depending on the magnitude of the Poisson’s ratio νs of the solid matrix, see graph labels; μe and μ1 are defined in Table 1
Fig. 6. Dimensionless representation of interface-micromechanical origins of Maxwell springs: stiffness μE of spring parallel to dashpot and stiffness μI in series with dashpot (both normalized with respect to the shear modulus of the solid elastic matrix μs), as functions of the interface density d, depending on the magnitude of the Poisson’s ratio νs of the solid matrix, see graph labels; μE and μI are defined in Table 1
Table 1. Relations between Spring Stiffnesses and Dashpot Viscosities of the Kelvin-Voigt and Maxwell Representations of the Standard Linear Solid Model and Micromechanical Quantities of a Matrix-Interface Composite, for Illustrations See Figs. 46
ModelsMaxwellKelvin-VoigtMicromechanics
According to Fig. 3According to Fig. 2According to Fig. 1
MaxwellμE=μEμE=μ1[1+(μ1)/(μe)]1μE=μs[3(2νs)]/[3(2νs)+16d(1νs)]
According to Fig. 3μI=μIμI=μe[1+(μ1)/(μe)]1μI=μs[16d(1νs)]/[3(2νs)+16d(1νs)]
ηI=ηIηI=η1[1+(μ1)/(μe)]2ηI=[aηint128d(1νs)2]/{π[3(2νs)+16d(1νs)]2}
Kelvin-Voigtμe=μI+μEμe=μeμe=μs
According to Fig. 2μ1=[(μE)/(μI)](μI+μE)μ1=μ1μ1=μs[3(2νs)]/[16d(1νs)]
η1=ηI[(μI+μE)/(μI)]2η1=η1η1=(aηint)/(2πd)

Micromechanical Interpretation of Stress and Strain Contributions of Individual Springs and Dashpots of the Rheological Models

The established relations between the rheological models and the micromechanical description of the matrix-interface composite, see (51) and Table 1, open the door to a novel, micromechanics-based interpretation of the rheological models. Accordingly, we will now express the stresses and strains acting in individual springs and dashpots, as functions of micromechanical quantities.
As for the Kelvin-Voigt representation of the standard linear solid model, such expressions concern the strain in the Kelvin-Voigt unit, γ1, the strain in the additional spring, γe, the stress acting on the Kelvin-Voigt spring, τ1μ, and the stress acting on the dashpot, τ1η. As for the expression for γ1 and γe, we specify the constitutive law of the additional spring, τ=μeγe, see (8), for γe=γγ1, see (5), yielding τ=μe(γγe), and we compare this relation with (36). Under consideration of (51) and the relations listed in Table 1, we then obtain
γ1=2πdaξxandγe=2Exz2πdaξx=Σxzμs
(52)
Next, we relate τ1μ=μ1γ1 to micromechanical quantities, by specifying this equality for μ1 according to Table 1, and for γ1 from (52)
τ1μ=3μsπ(2νs)8a(1νs)ξx
(53)
Finally, the micromechanical analogon for τ1η follows from first solving both (32) and (35) with respect to Exz, and from setting equal the corresponding results, yielding
Σxz=Tx+3μsπ(2νs)8a(1νs)ξx
(54)
Then this relation (54) is compared to τ=τ1η+τ1μ. Under consideration of (51) and (53), it follows that:
τ1η=Tx
(55)
As for the Maxwell representation of the standard linear solid model, we seek micromechanical analogons for the stress acting on the Maxwell unit, τI, the stress acting on the additional spring, τE, the strain in the Maxwell spring, γIμ, and the strain in the dashpot, γIη. As for a micromechanics-based expression for τE, we first specify the spring law τE=μEγ for μE=μE(μs,νs,d) according to Table 1, and for γ=2Exz, see (51)
τE=μEγ=μs3(2νs)3(2νs)+16d(1νs)2Exz
(56)
As for expressing τI, we first solve (32) for Exz, and we then insert the resulting expression into (56); this yields
τE=Σxz16d(1νs)3(2νs)+16d(1νs)Tx
(57)
Comparing this relation with τE=ττI, yields, under consideration of (51)
τI=16d(1νs)3(2νs)+16d(1νs)Tx
(58)
In order to provide a micromechanical analogon for γIμ, we specify the spring law γIμ=τI/μI, see (20), for τI from (58), and for μI from Table 1, yielding
γIμ=Txμs
(59)
Similarly, we specify the dashpot law γ˙Iη=τI/ηI, see (20), for τI from (58), and for ηI from Table 1, leading to
γ˙Iη=π[3(2νs)+16d(1νs)]8a(1νs)Txηint
(60)
Specifying (60) for Tx/ηint=ξ˙x, see (30), and omitting the dots indicating time derivatives, i.e. integrating over time, finally yields
γIη=π[3(2νs)+16d(1νs)]8a(1νs)ξx
(61)

Micromechanical Illustration of Energy Dissipating in Dashpots of the Rheological Models

The relation between rheological parameters and micromechanical quantities, as derived in the previous two subsections, allow us to illustrate the dashpot-associated dissipation in terms of micromechanical quantities. Specification of the Kelvin-Voigt-related dissipation according to (16), for τ1η according to (55), and for γ˙1 according to the time derivative of (52), delivers
D=τ1ηγ˙1=2dπaξ˙xTx
(62)
Similarly, specification of the Maxwell-related dissipation according to (28), for τI according to (58), and for γ˙Iη according to the time derivative of (61), delivers
D=τIγ˙Iη=2dπaξ˙xTx
(63)
Notably, both (62) and (63) result in the same expression for the dissipation of the matrix-interface composite. This clearly illustrates that the dissipation happening in the daspots of the two rheological models is related to the dissipation happening in the viscous interfaces of the micromechanical representation. In addition, the analogy-derived micromechanical expressions (62) and (63) are identical to the directly derived dissipation relation (50). This proves that all our derivations are correct, because the analogy-defining formulas for τ1η, γ˙1, τI and γ˙Iη were obtained from comparison of the differential equations (12), (24), as well as (38), and hence their derivation was independent of the derivation of dissipation relations (16), (28), and (50).

Discussion

The standard linear solid models, both in the Kelvin-Voigt and in the Maxwell representations, can perfectly describe the rheological behavior of a matrix-interface composite whose time-dependent material properties result from the linear viscosity of the interfaces behavior, i.e., they are compatible with traction-dislocation relations originating from liquid crystal interface physics, and multiscale homogenization of eigenstressed interfaces. The relations listed in Table 1 establish the links between spring stiffnesses as well as dashpot viscosities, on the one hand, and micromechanical quantities of the matrix-interface composite, on the other hand, the latter ones being interface size, density, and viscosity, as well as shear modulus and Poisson’s ratio of the isotropic solid matrix material.
When subjecting the matrix-interface composite to sudden loading, either in terms of stresses or of strains, the effective stiffness of the material is equal to the stiffness of the solid matrix, because, according to (30), dislocations would need time to develop, so that, without time passing, the interfaces are locked, which results in an uniform microscopic stress field (Shahidi et al. 2014). The same is true for the dashpot in the rheological models, being blocked upon sudden loading. Accordingly, the then observed effective stiffness of the Kelvin-Voigt model is equal to the additional spring stiffness, and the effective stiffness of the Maxwell model is equal to the sum of the spring stiffnesses. These effective stiffnesses are directly related to how the stiffness of the solid matrix manifests itself in the two rheological models: In the Kelvin-Voigt representation, the additional elastic spring simply represents the solid matrix material, while in the Maxwell representation, the sum of the two spring stiffnesses is equal to the one of the solid matrix, see Table 1.
The time-dependent evolution of interfacial dislocations increases the effective compliance of the matrix-interface composite. Given a constant (time-independent) loading, the stiffness-reducing effect is fully developed, once the asymptotic state of the material is reached, i.e., once the interface tractions have decayed to zero and the interface dislocations have grown to their maximum (Shahidi et al. 2014). The additional time-dependent material compliance is the larger, the larger the interface density. As for the Kelvin-Voigt model, the additional compliance is simply equal to the compliance of the Kelvin-Voigt spring, see Table 1. In the Maxwell representation, in turn, the interface density appears in the expressions of both spring constants, and the compliance of the additional spring is equal to the compliance of the solid matrix plus the additional compliance stemming from the interfacial dislocations, see Table 1.
The characteristic time of the rheological processes inherent to a matrix-interface composite are triggered, in general, by interface size a, viscosity ηint, and density d. This becomes apparent from the fact that the dashpot viscosities of both rheological models are directly proportional to interface size and viscosity, but the role of interface density deserves special attention, see Table 1. The Kelvin-Voigt dashpot viscosity is simply indirectly proportional to the interface density, see Table 1. Due to a more intricate mode of spring-dashpot interaction, however, the Maxwell dashpot viscosity depends in a non-trivial fashion on the interface density, and the dashpot viscosity is the smaller, the larger the Poisson’s ratio of the solid matrix, see Table 1 and Fig. 4.
When it comes to discussing the rheological counterparts of interface tractions and interface dislocations, the Kelvin-Voigt model again allows for a more straightforward mode of interpretation of the underlying interface-micromechanics: the interface traction is simply equal to the stress acting on the Kelvin-Voigt dashpot, see (55), and the strain in the Kelvin-Voigt unit is directly proportional to both the interfacial dislocations and the interface density, while it is indirectly proportional to the interface size, see (52). In the Maxwell model, in turn, the stress acting on the Maxwell unit is also proportional to the interface tractions, but the proportionality factor depends, again in a non-trivial fashion, on both the interface density and on the Poisson’s ratio of the solid matrix, see (58). Also the relation between interfacial dislocations and the strain of the Maxwell dashpot is of increased mathematical complexity, with the interface density not any more exhibiting the nature of a simple proportionality factor, and also the Poisson’s ratio of the solid entering the picture, see (61).
The Kelvin Voigt model also reveals a surprising feature of the investigated material system. As the characteristic creep time of a Kelvin-Voigt model reads as τKV=η1/μ1, it follows from Table 2 that the characteristic creep time reads as
τcreep=8aηint(1νs)3πμs(2νs)
(64)
Table 2. Shear Stress and Strain in Rheological Models, As Functions of Interface Tractions in Relation to Interface Traction and Dislocation in Micromechanical Representation of Matrix-Interface Composite
ModelsMicromechanics
According to Fig. 1
Kelvin-Voigtτ1η=Tx
According to Fig. 2γ1=[(2πd)/(a)]ξx
MaxwellτI=[16d(1νs)]/[3(2νs)+16d(1νs)]Tx
According to Fig. 3γIη=π[3(2νs)+16d(1νs)]/[8a(1νs)]ξx
It becomes obvious that the characteristic creep time is independent of the interface density, and only depends on interface viscosity and radius, as well as on the elastic properties of the solid matrix. This confirms our statements given in (Shahidi et al. 2014). On the other hand, the relaxation time of the studied micromechanical material system does depend on the interface density as well, see again (Shahidi et al. 2014) for further details.
When it comes to applications of the developed formulations to real-life material systems, particular attention needs be paid to the identification of the interface viscosity, in light of different experimental or computational sources for material creep and interface physics, respectively. More precisely, the comparison of top-down and bottom-up approaches has proven as quite instructive recently in the context of bone (Qu et al. 2015): Downscaling of creep experiments on bone (Sasaki et al. 1993; Iyo et al. 2004) by means of a multiscale continuum micromechanics model (Eberhardsteiner et al. 2014) delivered Kelvin-Voigt-type creep properties at the level of hydrated extrafibrillar crystal clusters, which when used in the relations of Table 2, provided top-down-access to the interface viscosity. Alternatively, explicit molecular modeling (Dubey and Tomar 2009) of the shear forces acting between two mutually sliding mineral crystals, with water or organic molecules filling the 1 nm thick gap between them, provided a bottom-up approach. It turned out that the huge difference in velocity magnitudes between these two approaches (the molecular approach entailing more than ten orders of magnitude larger velocities than those experienced under quasi-physiological conditions) resulted in bottom-up interface viscosities exceeding their top-down counterparts by orders of magnitudes. This is fully consistent with the well-known phenomenon of thixotropy or shear thinning (Barnes 1997), i.e. the strong dependence of viscous properties of the investigated material system, on the applied shear rates, in contrast to rate-independent elastic properties (Salençon 2001). Similar phenomena are also expected in the ongoing research work on multiscale creep mechanics of concrete, based on the aging viscoelasticity formulation of Scheiner and Hellmich (2009).

Conclusion

We conclude that the Kelvin-Voigt representation of the standard linear solid model, when compared to its Maxwell counterpart, is a more natural and elegant choice for modeling a hydrated matrix-interface composite containing viscous interfaces of identical size and viscosity, because the relations between spring-dashpot properties and micromechanical quantities turn out as very simple. Nonetheless, exactly the same model features can be achieved through a Maxwell-type representation, based on an appropriate choice of the spring stiffnesses and dashpot viscosities; their relations to micromechanics quantities, however, are significantly less intuitive when compared to the Kelvin-Voigt model. It is interesting to generalize this conclusion towards consideration of multiple interface sizes and viscosities, and corresponding chain models of the Kelvin-Voigt or Maxwell type. This is the topic of the companion paper (Shahidi et al. 2015).

Notation

The following symbols are used in this paper:
a
radius of the interfaces;
A̲̲̲
third-order concentration tensor;
B̲̲̲
third-order Biot-type influence tensor;
B̲̲̲̲
fourth-order Biot tensor;
C
integration constant;
C̲̲̲̲s
fourth-order stiffness tensor of solid;
C̲̲̲̲s1
inverse of fourth-order stiffness tensor of solid;
C̲̲̲̲hom
fourth-order homogenized stiffness tensor;
d
interface density parameter;
D̲̲
second-order influence tensor;
D
dissipation;
e̲x, e̲y, e̲z
unit base vectors of Cartesian coordinate system;
E̲̲
second-order tensor of macroscopic strain;
Exz
shear component of macroscopic strain;
Exz,h
solution of homogeneous differential equation for Exz;
Exz,p
particular solution for Exz;
i
index for interface phase;
1̲̲
second-order identity tensor;
I̲̲̲̲
symmetric fourth-order identity tensor;
I̲̲̲̲dev
deviatoric part of I̲̲̲̲;
I̲̲̲̲vol
volumetric part of I̲̲̲̲;
ks
bulk modulus of solid phase;
characteristic size of RVE;
sext
external power supplied to elastic matrix;
N̲̲̲̲1
inverse of fourth-order tensor of Biot moduli;
N
number of interfaces per unit volume of the composite;
RVE
representative volume element;
s
index for solid phase;
t
time;
T̲
interface traction vector;
T̲̲̲̲i
fourth-order morphology tensor for 2D interface inclusion (shape of a “sharp crack”);
Tx
shear component of interface traction vector;
Vi
volume of inclusion;
Vs
volume of solid;
VRVE
volume of RVE;
x, y, z
Cartesian coordinates;
x̲
position vector;
γ
shear strain;
γe
shear strain of elastic spring of Kelvin-Voigt representation of standard linear solid (Zener model);
γE
shear strain of elastic spring of Maxwell representation of standard linear solid;
γh
solution of homogeneous differential equation for γ;
γI
shear strain of Maxwell unit;
γIμ
shear strain of spring in Maxwell unit;
γIη
shear strain of dashpot in Maxwell unit;
γp
particulate solution for γ;
γ1
shear strain of Kelvin-Voigt unit;
δ
Kronecker delta;
ε̲̲
second-order tensor of microscopic linear strain;
ε̲̲i
second-order tensor of microscopic linear strain in spheroidal inclusion;
ηint
viscosity of the interfaces;
η1
viscosity constant of dashpot in Kelvin-Voigt unit;
ηI
viscosity constant of dashpot in Maxwell unit;
μe
shear modulus of elastic spring in Kelvin-Voigt representation of standard linear solid (Zener model);
μE
shear modulus of spring in Maxwell representation of standard linear solid;
μ1
shear modulus of spring in Kelvin-Voigt unit;
μI
shear modulus of spring in Maxwell unit;
μs
shear modulus of isotropic solid matrix;
νs
Poisson’s ratio of isotropic solid matrix;
ξ̲
displacement vector;
ξ̲
interfacial dislocation vector;
ξx
in-plane component of interfacial dislocation vector;
ξz
out-of-plane component of interfacial dislocation vector;
σ̲̲
second-order tensor of microscopic stress;
σ̲̲iE
second-order tensor of interface eigenstress;
Σ̲̲
second-order tensor of macroscopic stress;
Σxz
shear component of macroscopic stress;
Σxz,h
solution of homogeneous differential equation for Σxz;
Σxz,p
particular solution for Σxz;
τ
shear stress;
τe
shear stress in elastic spring in Kelvin-Voigt representation of standard linear solid (Zener model);
τE
shear stress in elastic spring in Maxwell representation of standard linear solid;
τh
solution of homogeneous differential equation for shear stress;
τI
shear stress acting on Maxwell unit;
τp
particulate integral;
τ1
shear stress acting on Kelvin-Voigt unit;
τ1μ
shear stress in spring of Kelvin-Voigt unit;
τ1η
shear stress in dashpot of Kelvin-Voigt unit;
ϕi
volume fraction of spheroidal inclusions;
Φ̲̲
second-order tensor accounting for interfacial geometry changes;
Φxz
shear component of Φ̲̲;
Ψ
elastic energy of matrix-interface composites;
ψs
elastic internal energy of solid;
partial derivative;
:
second-order tensor contraction;
˙
partial derivative with respect to time (“rate”) of quantity “”; and
dyadic product.

Appendix. Tensor Components, As Well As Details on Creep and Relaxation Studies

Defintion of Elastic Stiffness of Solid, Identity Tensor, and Interface Morphology Tensor

The isotropic elastic stiffness of solid in matrix-interface composite read as
C̲̲̲̲s=3ksI̲̲̲̲vol+2μsI̲̲̲̲dev
(65)
where I̲̲̲̲vol=(1)/(3)1̲̲1̲̲ and I̲̲̲̲dev=I̲̲̲̲I̲̲̲̲vol, respectively, denote the volumetric and the deviatoric part of the symmetric fourth-order identity tensor I̲̲̲̲, with components Iijkl=(1)/(2)(δikδjl+δilδkj), and with δij denoting the Kronecker delta being equal to 1 if i=j and 0 otherwise. In addition, 1̲̲ is the second-order identity tensor with components being equal to the Kronecker delta. In (65), ks and μs denote the bulk modulus and the shear modulus of the solid phase, respectively. Bulk modulus ks is related to Poisson’s ratio νs and the shear modulus μs as
ks=2μs(1+νs)3(12νs)
(66)
The non-vanishing components of interface morphology tensor T̲̲̲̲i are functions of Poisson’s ratio of the solid, and they read as (Dormieux and Kondo 2004)
Ti,xzxz=Ti,zxxz=Ti,xzzx=Ti,zxzxTi,yzyz=Ti,zyyz=Ti,yzzy=Ti,zyzy}=2(1νs)π(2νs)
(67)
Ti,zzxxTi,zzyy}=4νs(1νs)π(12νs)
(68)
Ti,zzzz=4(1νs)2π(12νs)
(69)

Kelvin-Voigt Formulation: Creep and Relaxation Study

Creep Test
In a creep study, the system is suddenly subjected to a force τ which is kept constant afterwards:
τ(t)=constant=τ,τ˙=0
(70)
Specification of (12) for (70) delivers the governing differential equation for creep as
τ(1μe+1μ1)μ1η1=μ1η1γ(t)+γ˙(t)
(71)
The solution of (71) contains two parts: the solution of the homogeneous differential equation, called complementary function γh, and one particulate integral γp
γ(t)=γh(t)+γp
(72)
The particulate solution turns out to be constant and reads as
γp=τ(1μe+1μ1)
(73)
The sought complementary function follows as:
γh(t)=Cexp(μ1η1t)
(74)
The total solution is obtained from specification of (72) for (73) and for (74), reading as
γ(t)=Cexp(μ1η1t)+τμe+τμ1
(75)
The integration constant C follows from the initial condition γ(t=0)=(τ)/(μe) as
C=τμ1
(76)
Backsubstitution of (76) into (75), and simplifying the corresponding result, finally yields
γ(t)=τμe+τμ1[1exp(μ1η1t)]
(77)
Relaxation Test
In a relaxation study, the system is suddenly subjected to an elongation γ which is kept constant afterwards
γ(t)=constant=γ,γ˙=0
(78)
Specifying Eq. (12) for (78) delivers the governing differential equation for relaxation as
τ˙(t)+τ(t)μeη1(1+μ1μe)=γ(μeμ1η1)
(79)
The solution of (79) contains two parts: the solution of the homogeneous differential equation, called complementary function τh(t), and one particulate integral τp
τ(t)=τh(t)+τp
(80)
The particulate solution turns out to be time-independent, and reads as
τp=γμ1(1+μ1μe)=γ(1μ1+1μe)
(81)
The sought complementary function reads as
τh(t)=Cexp[μeη1(1+μ1μe)t]
(82)
Specifying (80) for (81) and (82), yields the force history
τ(t)=Cexp[μeη1(1+μ1μe)t]+γ(1μ1+1μe)
(83)
The integration constant C is identified from the initial condition τ(t=0)=γμe as
C=γμe(1+μ1μe)
(84)
Backsubstitution of (84) into (83) gives access to the final solution which reads as
τ(t)=γμe(1+μ1μe)exp[μeη1(1+μ1μe)t]+γ(1μ1+1μe)
(85)

Maxwell Formulation: Creep and Relaxation Study

Creep Study
In a creep study, the system is suddenly subjected to a force τ which is kept constant afterwards: see (70). Specification of (24) for (70) delivers the governing differential equation for creep as
γ˙(t)+μIμE(μI+μE)ηIγ(t)=μI(μI+μE)ηIτ
(86)
The solution of (86) contains two parts: the solution of the homogeneous differential equation, called complementary function γh, and one particulate integral γp
γ(t)=γh(t)+γp
(87)
The particulate solution turns out to be constant and reads as
γp=τμE
(88)
The sought complementary function follows as:
γh(t)=Cexp(μIμEμI+μEtηI)
(89)
The total solution is obtained from specification of (87) for (88) and for (89), as
γ(t)=Cexp(μIμEμI+μEtηI)+τμE
(90)
In order to solve for the integration constant C, we consider the initial condition γ(t=0)=(τ)/(μI+μE), yielding
C=μIτμE(μI+μE)
(91)
Specifying (90) for (91), delivers the deformation history of the system as
γ(t)=τμEμIτμE(μI+μE)exp(μIμEμI+μEtηI)
(92)
Relaxation Study
In a relaxation study, the system is suddenly subjected to an elongation γ which is kept constant afterwards, see (78). Specification of (24) for (78) delivers the governing differential equation for relaxation as
τ˙(t)+μIηIτ(t)=μIμEηIγ
(93)
The solution of (93) contains two parts: the solution of the homogeneous differential equation, called complementary function τh(t), and one particulate integral τp
τ(t)=τh(t)+τp
(94)
where the particulate solution turns out to be time-independent, and reads as
τp=γμE
(95)
The sought complementary function follows as:
τh(t)=Cexp[μIηIt]
(96)
Specification of (94) for (95) and for (96), yields
τ(t)=Cexp[μIηIt]+γμE
(97)
In order to solve for the integration constant C, we apply the initial condition τ(t=0)=γ(μE+μI), which yields
C=γμI
(98)
Specification of (97) for (98) delivers the stress history of the system as
τ(t)=γμE+γμIexp[μIηIt]
(99)

Micromechanics Formulation: Creep and Relation Study

Creep Test
In a creep study, the RVE is suddenly subjected to a shear stress Σxz which is kept constant afterwards
Σxz(t)=constant=Σxz,Σ˙xz=0
(100)
Specification of the governing differential equation of interface micromechanics (38) for (100), yields the governing equation for the macrostrain reads as
E˙xz+μs3(2νs)π8(1νs)aηintExz=π[3(2νs)+16d(1νs)]16aηint(1νs)Σxz
(101)
The solution of (101) contains two parts: the solution of homogeneous differential equation, called complementary function Exz,h(t), and one particular integral Exz,p
Exz(t)=Exz,h(t)+Exz,p
(102)
The particular solution turns out to be time-independent, and reads as
Exz,p=3(2νs)+16d(1νs)2μs3(2νs)Σxz
(103)
The sought complementary function reads as
Exz,h(t)=Cexp[μs3(2νs)π8(1νs)taηint]
(104)
The total solution is obtained from specification of (102) for (103) and for (104), yielding
Exz(t)=C[exp(μs3(2νs)π8(1νs)taηint]+3(2νs)+16d(1νs)2μs3(2νs)Σxz
(105)
In order to solve for the integration constant C, we consider the initial condition Exz(t=0)=(1)/(2μs)Σxz, yielding
C=16d(1νs)2μs3(2νs)Σxz
(106)
Specifying (105) for the integration constant (106) allows us to write the time evolution of the macroscopic strain as
Exz(t)=Σxz2μs3(2νs)+16d(1νs)[1exp(3π(2νs)8(1νs)μstaηint)]3(2νs)
(107)
Relaxation Test
In a relaxation study, the RVE is suddenly subjected to a shear deformation Exz which is kept constant afterwards
Exz(t)=constant=Exz,E˙xz=0
(108)
Specification of the governing differential equation of interface micromechanics (38) for (108), yields the following differential equation in Σxz:
Σ˙xz+μsπ[3(2νs)+16d(1νs)]8aηint(1νs)Σxz=2μs23(2νs)π8aηint(1νs)Exz
(109)
The solution of (109) contains two parts: the solution of homogeneous differential equation, called complementary function Σxz,h(t), and one particular integral Σxz,p
Σxz(t)=Σxz,h(t)+Σxz,p
(110)
The particular solution turns out to be time-independent, and reads as
Σxz,p=2μs3(2νs)3(2νs)+16d(1νs)Exz
(111)
The sought complementary function reads as
Σxz,h(t)=Cexp(μsπ[3(2νs)+16d(1νs)]8(1νs)taηint)
(112)
Specification of (110) for the particular solution (111) and for the complementary function (112), yields
Σxz(t)=Cexp(μsπ[3(2νs)+16d(1νs)]8(1νs)taηint)+2μs3(2νs)3(2νs)+16d(1νs)Exz
(113)
In order to solve for the integration constant C, we consider the initial condition [Σxz(t=0)=2μsExz], delivering
C=2μs16d(1νs)3(2νs)+16d(1νs)Exz
(114)
Specification of (113) for (114), yields the stress history as
Σxz(t)=2μsExz3(2νs)+16d(1νs)exp[π[3(2νs)+16d(1νs)]8(1νs)μstaηint]3(2νs)+16d(1νs)
(115)

Acknowledgments

Financial support of this work through the European Research Council (ERC) under project ERC-2010-StG-257032-MICROBONE is gratefully acknowledged.

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Information & Authors

Information

Published In

Go to Journal of Engineering Mechanics
Journal of Engineering Mechanics
Volume 142Issue 3March 2016

History

Received: Dec 24, 2014
Accepted: Aug 11, 2015
Published online: Oct 13, 2015
Published in print: Mar 1, 2016
Discussion open until: Mar 13, 2016

Authors

Affiliations

Research Assistant, Institute for Mechanics of Materials and Structures, TU Wien-Vienna Univ. of Technology, Karlsplatz 13/202, A-1040 Vienna, Austria. E-mail: [email protected]
B. Pichler, Aff.M.ASCE [email protected]
Associate Professor, Institute for Mechanics of Materials and Structures, TU Wien-Vienna Univ. of Technology, Karlsplatz 13/202, A-1040 Vienna, Austria. E-mail: [email protected]
Ch. Hellmich, M.ASCE [email protected]
Full Professor, Institute for Mechanics of Materials and Structures, TU Wien-Vienna Univ. of Technology, Karlsplatz 13/202, A-1040 Vienna, Austria (corresponding author). E-mail: [email protected]

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