Abstract
Generalized continuum theories for materials and processes have been introduced in order to account in a phenomenological manner for microstructural effects. Their drawback mainly rests in the determination of the extra phenomenological coefficients through experiments and simulations. It is shown here that a graphical representation of the local topology describing deformation models can be used to deduce restrictions on the phenomenological coefficients of the gradient elasticity continuum theories.
1 Introduction
The purpose of the present article is to consider the implications of a graphical representation to models of gradient elasticity [1–3], proposed to generalize the classical Hooke’s law. Starting with a discrete version of “dual” elasticity models and assuming a specific topology for the two elastic chains, we can obtain certain algebraic restrictions for the phenomenological coefficients of the continuum counterparts of the discrete models.
It is shown that, depending on the assumed topology and interaction of the two elastic chains, the sign of the new phenomenological coefficients may be positive or negative with direct implications on uniqueness and stability of the solution of related boundary value problems.
While the foundations of graph theory can be traced back to L. Euler and his “Königsberg bridge problem” [4], its growth in recent years has been explosive, covering a large number of disciplines ranging from mathematical foundations of computer science [5] to physical chemistry [6] and natural language processing [7]; only recently such developments have been applied to physics, engineering sciences and current technology problems [8], including elastic networks in manmade structures [9], and biological systems [10].
2 Graphical description of dual elasticity
We consider a one-dimensional medium composed of two interpenetrating elastic chains. The displacement of chain (or path) 1 is designated by u, the displacement of chain (or path) 2 is designated by v, and the overall average displacement by w, with all three of these quantities being measured (in general) with respect to different coordinate systems. For the representation of the average displacement w in terms of the two displacements u and v, we will employ mean square displacement relation, i.e., w2=c1u2+c2v2 with c1+c2=1. When c1=c2 we obtain the ordinary mean square displacement. Now let x be the variable of the coordinate system of the average displacement w. Then, by taking the derivative of the mean square displacement relation with respect to x, we obtain:
where
In the particular case that the quotients r1 and r2 are constants, we have
In a discretized version of such dual elasticity medium, we designate the corresponding particle displacements by un and vn, n∈ℤ, and the associated spring stiffness by Ki (i=1, 2). It is also assumed that there exists an interaction force between the particles of the two superimposed lattice chains given by fint=a(u-v), where a∈ℝ is a material coefficient. Assuming Hooke’s law, for each elastic chain, the spring-like forces acting on a particle with displacement un, because of the short-range interactions of particles on the same chain, are f1=K1(un-1-un), f2=K1(un-un+1) and, in combination, f1-f2=K1(un+1-2un+un-1). Similarly the elastic forces acting on particle vn are f3=K2(vn-1-vn), f4=K2(vn-vn+1) which gives f3-f4=K2(vn+1-2vn+vn-1). Equilibrium requires f1-f2=∂σ1/∂x and f3-f4=∂σ2/∂x, where σ1 and σ2 denote the stresses in each chain. Hence, for the interacting forces between particles un and vn, we have ∂σ1/∂x=fint=a(un-vn) and ∂σ2/∂x=-fint=a(vn-un). By combining the previous equations we obtain K1(un+1-2un+un-1)=a(un-vn) and K2(vn+1-2vn+vn-1)=a(vn-un). To continualize these equations, un is replaced by the displacement of the continuum u(x), whereas the displacements of the neighboring particles un±1 are replaced by un±d, and the same is done for vn. By using a Taylor series expansions for u(x±d) and v(x±d) and neglecting terms of order d3 and higher we obtain K1d2uxx=a(u-v) and
In order to derive a corresponding governing equation for the average displacement w introduced previously, and in particular for the case that the coefficients r1 and r2 of Eq. (1) are constants, we use the last equations to obtain
we see that the two equations become identical for a=-12K1K2/(K1+K2). In the case that we consider also terms of order d3 and d4, by continualization we obtain
and similarly for v. The sign of u4x is positive if and only if (K1+K2)a>12K1K2, hence if K1 and K2 are linearly increasing then the value of a over which the sign of u4x is positive is also linearly increasing. Below that value the sign is negative and when the equality a=12K1K2/(K1+K2) holds, then the higher order term u4x vanishes. Now if we assume that the coefficients r1 and r2 of Eq. (1) are constants, by Eq. (4) and by neglecting terms of order d4 and higher we obtain
where w is the average displacement. For the coefficient of the fourth order term we have
where
The potential energies for the two elastic springs as a result of the short-range interaction forces between particles of the same chain are
Macroscopically, if we assume an average Young’s modulus E and an average strain ε, the elastic potential energy per unit volume is given by
where the average strain for the unit cell is taken as
Now, in order to relate the apparent macroscopic strain with the partial strains of the two elastic chains we apply Hooke’s law for the forces FA and FB acting on the chains, i.e.,
By comparing it with Eq. (7), we obtain K=K1+K2 and a=(K1+K2)/8. As a result of the above exercise, we may conclude that various relations on phenomenological coefficients of continuum macroscopic constitutive models are possible when particular assumptions are made for the local topology of their discrete counterparts. Graph theory may be a useful tool to employ in relation to three-dimensional constitutive models. The assumption of mean square displacement adopted herein is a bit unusual but it was made specifically to illustrate the various possibilities that can be explored.
3 Conclusion
An outline on the use of discrete modeling procedures, employing special assumptions on local topology, for deducing microscopic relations for the phenomenological coefficients of generalized continuum elasticity models is given. As the examples treated are of gradient type, a somewhat unusual definition of mean particle displacement, resembling that commonly utilized in discrete diffusion models, is adopted. The approach is not sensitive to that definition and corresponding results for more conventional expressions for the mean particle displacements for both deformation and diffusion problems will be given elsewhere. It is shown that the sign of the gradient coefficient in Aifantis gradient elasticity model (GRADELA) may be positive or negative, depending on the microscopic configuration and the interaction laws between particles of the same chain, as well as particles of different chains.
Acknowledgments
The authors acknowledge support of the Hellenic ERC-13 (IL-GradMech-ASM/Project No. 88257) by the General Secretariat of Research and Technology (GSRT) of the Greek Ministry of Education.
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- Surface effects at the nanoscale based on Gurtin’s theory: a review
- On the application of the partition of unity method for nonlocal response of low-dimensional structures
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