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Deformation of a continuum

When the displacement gradient is split into its symmetric and skew symmetric portions, the infinitesimal strain tensor of Eq. (3.18) is identified to be the former, while the latter represents infinitesimal rotations that do not [Pg.26]

So the infinitesimal strain tensor is established as a symmetric tensor of second order. With provision for the engineering shear-strain measures aside the diagonal, the components can be assigned as given by the left-hand side of Eqs. (3.20). An alternative representation may be gained by resorting the six independent components into a vector as shown on the right-hand side of Eqs. (3.20)  [Pg.26]

The transformation of a tensor is accomplished by changing its base vector system. Such a change from the orthonormal base vectors 61,62,63 to the [Pg.26]

These transformation coefficients may be summarized in the transformation matrix T for the subsequent transformation of stresses, respectively strains, in matrix representation  [Pg.27]

As it is dealt with second-order tensors, the associated base vector pairs need to be considered, and thus products of the transformation coefficients appear [Pg.27]


The plastic deformation patterns can be revealed by etch-pit and/or X-ray scattering studies of indentations in crystals. These show that the deformation around indentations (in crystals) consists of heterogeneous rosettes which are qualitatively different from the homogeneous deformation fields expected from the deformation of a continuum (Chaudhri, 2004). This is, of course, because plastic deformation itself is (a) an atomically heterogeneous process mediated by the motion of dislocations and (b) mesoscopically heterogeneous because dislocation motion occurs in bands of plastic shear (Figure 2.2). In other words, plastic deformation is discontinuous at not one, but two, levels of the states of aggregation in solids. It is by no means continuous. And, it is by no means time independent it is a flow process. [Pg.12]

From the preceding seven paragraphs we learn to see the mechanical deformation of a continuum as being driven by a difference between the chemical potential for one direction and the chemical potential for a second direction. This potential difference makes the material behave as if wafers migrated along short curved paths of an identifiable length Lq. [Pg.7]

Figure 11.4 Deformation of a continuum. Lengths / and SI are identified as small finite quantities then the ratio is kept constant as the quantities tend to zero. Figure 11.4 Deformation of a continuum. Lengths / and SI are identified as small finite quantities then the ratio is kept constant as the quantities tend to zero.
Of course, eventually, particles will reappear, through the equation = Po + RTln the existence of R depends on the existence of particles. But a theory of stress-driven deformation of a continuum does not require particles, even with stress-driven self-diffusion coefficients for viscosity and self-diffusion are the only things required. [Pg.91]

The QC method which presents a relationship between the deformations of a continuum with that of its crystal lattice uses the classical Cau-chy-Bom rule and representative atoms. The quasi-continuum method mixes atomistic-continuum formulation and is based on a finite element discretization of a continuum mechanics variation principle. [Pg.239]

Fig. 3.2. Deformation of a continuum—(a) reference configuration with particle position X and (b) momentary configuration with particle position x in the inertial frame of reference. Fig. 3.2. Deformation of a continuum—(a) reference configuration with particle position X and (b) momentary configuration with particle position x in the inertial frame of reference.
The large deformability as shown in Figure 21.2, one of the main features of rubber, can be discussed in the category of continuum mechanics, which itself is complete theoretical framework. However, in the textbooks on rubber, we have to explain this feature with molecular theory. This would be the statistical mechanics of network structure where we encounter another serious pitfall and this is what we are concerned with in this chapter the assumption of affine deformation. The assumption is the core idea that appeared both in Gaussian network that treats infinitesimal deformation and in Mooney-Rivlin equation that treats large deformation. The microscopic deformation of a single polymer chain must be proportional to the macroscopic rubber deformation. However, the assumption is merely hypothesis and there is no experimental support. In summary, the theory of rubbery materials is built like a two-storied house of cards, without any experimental evidence on a single polymer chain entropic elasticity and affine deformation. [Pg.581]

Low-porosity mass of soluble grains. The situation discussed by Fletcher differs from the above in important ways. Again we have two phases, a mechanically robust host-material and a small volume-fraction of an interstitial fluid but here the host-material is viscous rather than elastic (with extremely high viscosity), and the interstitial fluid has no ability to move from place to place— it is more like a stationary surface film that functions only as a solvent and a channelway for the diffusion of solute. Under a load such as is shown in Figure 8.3a, effects are (i) the viscous host deforms as a continuum (see Figure 10.2), and also (ii) host material... [Pg.78]

The box stress-driven interdiffusion is the one on which attention centers, which can be treated in either of two ways. We envisage here a crystalline material that, despite its crystallinity, can be made to creep (like a glacier) if it is squeezed in a nonuniform way, its composition changes—it deforms as a continuum and changes composition by particle exchange to the one act of squeezing, the material responds mechanically and chemically. [Pg.177]

Polyhedral deformation can result in unusual, open pseudocloso) structures, which, although not represented on the Wade-Williams matrix, appear structurally to lie between closo and hypercloso forms. The further discovery of partially deformed (semipseudocloso) species supports the idea of a continuum of structure type, which can, at least in part, be controlled by judicious use of substituents with differing steric demands. [Pg.139]

When fluids can seep through pores, interacting mechanically with the solid skeleton, the material is composed of more than one constituent thus we need to use a mixture theory in which we could clearly make out each part filled by different constituents on a scale which is rather large in comparison with molecular dimensions so we put forward a new continuum theory of an immiscible mixture consisting both of a continuum with ellipsoidal microstructure (the porous elastic solid) and of two classical media (see, also, the conservative case examined by Giovine (2000)). In accordance with Biot (1956), we consider virtual mass effects due to diffusion we also introduce the microinertia associated with the rates of change of the constituents local densities, as well as the one due to the deformation of the pores close to their boundaries. [Pg.535]

In the continuum limit the local deformation of a crystal can be described by the gradient of the displacement field (/, t) = Ri(t) - Ri where Ji, and JJ, are the temporary and equilibrium lattice positions, respectively. The gradient tensor is given by = dUi (i)ldR with k, l = x, y, z. The general deformation can be described as a pure strain deformation tj followed by a rotation D... [Pg.235]

These laws provide the basis for the continuum model and must be coupled with the appropriate constitutive equations and the equations of state to provide all the equations necessary for solving a continuum problem. The continuum method relates the deformation of a continuous medium to... [Pg.221]

It is therefore common to assume that the state variables that describe the rapid deformation response of granular materials would border on the parameters that describe the behavior of fluids and Coulomb type dissipation of energy (static). In view of the above it is common to find that the theories governing granular flow are formulated around the assumption of a continuum similar in some regard to viscous fluids however, the equilibrium states of the theories are not states of hydrostatic pressure, as would be in the case of fluids, but are rather states that are specified by the Mohr-Coulomb criterion (Cowin, 1974). The advantage of continuum formulations over alternative particulate (stochastic) formulations is that use of continuum is more capable of generating predictive results. Mathematically one... [Pg.62]

A review of the literature reveals that previous finite-element analyses of adhesive joints were either based on simplified theoretical models or the analyses themselves did not exploit the full potential of the finite-element method. Also, several investigations involving finite-element analyses of the same adhesive joint have reported apparent contradictory conclusions about the variations of stresses in the joint.(24,36) while the computer program VISTA looks promising (see Table 1), its nonlinear viscoelastic capability is limited to Knauss and Emri.(28) Recently, Reddy and Roy(E2) (see also References 37 and 38) developed a computer program, called NOVA, based on the updated Lagrangian formulation of the kinematics of deformation of a two-dimensional continuum and Schapery s(26) nonlinear viscoelastic model. The free-volume model of Knauss and Emri(28) can be obtained as a degenerate model from Schapery s model. [Pg.364]

In the continuum theory of liquid crystals, the free energy density (per unit volume) is derived for infinitesimal elastic deformations of the continuum and characterized by changes in the director. To do this we introduce a local right-handed coordinate x, y, z) system with (z) at the origin parallel to the unit vector n (r) and x and y at right angles to each other in a plane perpendicular to z. We may then expand n (r) in a Taylor series in powers of x, y, z, such that the infinitesimal change in n (r) varies only slowly with position. In which case... [Pg.1350]

After the deformation force is removed from the liquid crystal material, it will relax back to the equilibrium state. This behavior is analogous to the elastic properties of continuous solids. Therefore, it has been possible to describe the deformation of liquid crystals in terms of a continuum elastic theory. When we consider the elastic properties of a solid, we think of Hookes law ... [Pg.51]

Lin et al. [60, 61] have meshed a planar, intermediate-temperature three-cell stack based on anode supported-cells and a glass-ceramic sealant, with linear continuum shell elements (see Fig. 11). The maximum principal stress in the PEN reaches 170 MPa at room temperature and decreases to 70 MPa in operation, because of the smaller temperature difference with the reference state. The MIC undergoes significant plastic deformation. In operation, the elastic modulus of the glass-ceramic sealant has been reduced by two thirds for a first assessment of the effects of the viscous behaviour. It results in a decrease of the stress of 10 % in the cell. Few studies have been carried out on the overall deformation of a SRU embedded in a functional stack. In the conditions of their simulations, a limited influence of the stack support conditions and position in the stack on the stress profile has been highlighted (see Fig. 11). [Pg.147]

Another chapter deals with the physical mechanisms of deformation on a microscopic scale and the development of micromechanical theories to describe the continuum response of shocked materials. These methods have been an important part of the theoretical tools of shock compression for the past 25 years. Although it is extremely difficult to correlate atomistic behaviors to continuum response, considerable progress has been made in this area. The chapter on micromechanical deformation lays out the basic approaches of micromechanical theories and provides examples for several important problems. [Pg.357]


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