Flow plasticity theory

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Plastic deformation of a thin metal sheet. Biegeanimation 2D.gif
Plastic deformation of a thin metal sheet.

Flow plasticity is a solid mechanics theory that is used to describe the plastic behavior of materials. [1] Flow plasticity theories are characterized by the assumption that a flow rule exists that can be used to determine the amount of plastic deformation in the material.

Contents

In flow plasticity theories it is assumed that the total strain in a body can be decomposed additively (or multiplicatively) into an elastic part and a plastic part. The elastic part of the strain can be computed from a linear elastic or hyperelastic constitutive model. However, determination of the plastic part of the strain requires a flow rule and a hardening model.

Small deformation theory

Stress-strain curve showing typical plastic behavior of materials in uniaxial compression. The strain can be decomposed into a recoverable elastic strain (
e
e
{\displaystyle \varepsilon _{e}}
) and an inelastic strain (
e
p
{\displaystyle \varepsilon _{p}}
). The stress at initial yield is
s
0
{\displaystyle \sigma _{0}}
. For strain hardening materials (as shown in the figure) the yield stress increases with increasing plastic deformation to a value of
s
y
{\displaystyle \sigma _{y}}
. Rock plasticity compression plain.svg
Stress-strain curve showing typical plastic behavior of materials in uniaxial compression. The strain can be decomposed into a recoverable elastic strain () and an inelastic strain (). The stress at initial yield is . For strain hardening materials (as shown in the figure) the yield stress increases with increasing plastic deformation to a value of .

Typical flow plasticity theories for unidirectional loading (for small deformation perfect plasticity or hardening plasticity) are developed on the basis of the following requirements:

  1. The material has a linear elastic range.
  2. The material has an elastic limit defined as the stress at which plastic deformation first takes place, i.e., .
  3. Beyond the elastic limit the stress state always remains on the yield surface, i.e., .
  4. Loading is defined as the situation under which increments of stress are greater than zero, i.e., . If loading takes the stress state to the plastic domain then the increment of plastic strain is always greater than zero, i.e., .
  5. Unloading is defined as the situation under which increments of stress are less than zero, i.e., . The material is elastic during unloading and no additional plastic strain is accumulated.
  6. The total strain is a linear combination of the elastic and plastic parts, i.e., . The plastic part cannot be recovered while the elastic part is fully recoverable.
  7. The work done of a loading-unloading cycle is positive or zero, i.e., . This is also called the Drucker stability postulate and eliminates the possibility of strain softening behavior.

The above requirements can be expressed in three dimensional states of stress and multidirectional loading as follows.

where the stiffness matrix is constant.
The above equation, when it is equal to zero, indicates a state of neutral loading where the stress state moves along the yield surface.

Flow rule

In metal plasticity, the assumption that the plastic strain increment and deviatoric stress tensor have the same principal directions is encapsulated in a relation called the flow rule. Rock plasticity theories also use a similar concept except that the requirement of pressure-dependence of the yield surface requires a relaxation of the above assumption. Instead, it is typically assumed that the plastic strain increment and the normal to the pressure-dependent yield surface have the same direction, i.e.,

where is a hardening parameter. This form of the flow rule is called an associated flow rule and the assumption of co-directionality is called the normality condition. The function is also called a plastic potential.

The above flow rule is easily justified for perfectly plastic deformations for which when , i.e., the yield surface remains constant under increasing plastic deformation. This implies that the increment of elastic strain is also zero, , because of Hooke's law. Therefore,

Hence, both the normal to the yield surface and the plastic strain tensor are perpendicular to the stress tensor and must have the same direction.

For a work hardening material, the yield surface can expand with increasing stress. We assume Drucker's second stability postulate which states that for an infinitesimal stress cycle this plastic work is positive, i.e.,

The above quantity is equal to zero for purely elastic cycles. Examination of the work done over a cycle of plastic loading-unloading can be used to justify the validity of the associated flow rule. [2]

Consistency condition

The Prager consistency condition is needed to close the set of constitutive equations and to eliminate the unknown parameter from the system of equations. The consistency condition states that at yield because , and hence

Large deformation theory

Large deformation flow theories of plasticity typically start with one of the following assumptions:

The first assumption was widely used for numerical simulations of metals but has gradually been superseded by the multiplicative theory.

Kinematics of multiplicative plasticity

The concept of multiplicative decomposition of the deformation gradient into elastic and plastic parts was first proposed independently by B. A. Bilby, [3] E. Kröner, [4] in the context of crystal plasticity and extended to continuum plasticity by Erasmus Lee. [5] The decomposition assumes that the total deformation gradient (F) can be decomposed as:

where Fe is the elastic (recoverable) part and Fp is the plastic (unrecoverable) part of the deformation. The spatial velocity gradient is given by

where a superposed dot indicates a time derivative. We can write the above as

The quantity

is called a plastic velocity gradient and is defined in an intermediate (incompatible) stress-free configuration. The symmetric part (Dp) of Lp is called the plastic rate of deformation while the skew-symmetric part (Wp) is called the plastic spin:

Typically, the plastic spin is ignored in most descriptions of finite plasticity.

Elastic regime

The elastic behavior in the finite strain regime is typically described by a hyperelastic material model. The elastic strain can be measured using an elastic right Cauchy-Green deformation tensor defined as:

The logarithmic or Hencky strain tensor may then be defined as

The symmetrized Mandel stress tensor is a convenient stress measure for finite plasticity and is defined as

where S is the second Piola-Kirchhoff stress. A possible hyperelastic model in terms of the logarithmic strain is [6]

where W is a strain energy density function, J = det(F), μ is a modulus, and "dev" indicates the deviatoric part of a tensor.

Flow rule

Application of the Clausius-Duhem inequality leads, in the absence of a plastic spin, to the finite strain flow rule

Loading-unloading conditions

The loading-unloading conditions can be shown to be equivalent to the Karush-Kuhn-Tucker conditions

Consistency condition

The consistency condition is identical to that for the small strain case,

Related Research Articles

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<span class="mw-page-title-main">Hooke's law</span> Physical law: force needed to deform a spring scales linearly with distance

In physics, Hooke's law is an empirical law which states that the force needed to extend or compress a spring by some distance scales linearly with respect to that distance—that is, Fs = kx, where k is a constant factor characteristic of the spring, and x is small compared to the total possible deformation of the spring. The law is named after 17th-century British physicist Robert Hooke. He first stated the law in 1676 as a Latin anagram. He published the solution of his anagram in 1678 as: ut tensio, sic vis. Hooke states in the 1678 work that he was aware of the law since 1660.

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<span class="mw-page-title-main">Stress–strain curve</span> Curve representing a materials response to applied forces

In engineering and materials science, a stress–strain curve for a material gives the relationship between stress and strain. It is obtained by gradually applying load to a test coupon and measuring the deformation, from which the stress and strain can be determined. These curves reveal many of the properties of a material, such as the Young's modulus, the yield strength and the ultimate tensile strength.

In physics and materials science, elasticity is the ability of a body to resist a distorting influence and to return to its original size and shape when that influence or force is removed. Solid objects will deform when adequate loads are applied to them; if the material is elastic, the object will return to its initial shape and size after removal. This is in contrast to plasticity, in which the object fails to do so and instead remains in its deformed state.

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In materials science and continuum mechanics, viscoelasticity is the property of materials that exhibit both viscous and elastic characteristics when undergoing deformation. Viscous materials, like water, resist shear flow and strain linearly with time when a stress is applied. Elastic materials strain when stretched and immediately return to their original state once the stress is removed.

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The work of a force on a particle along a virtual displacement is known as the virtual work.

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The J-integral represents a way to calculate the strain energy release rate, or work (energy) per unit fracture surface area, in a material. The theoretical concept of J-integral was developed in 1967 by G. P. Cherepanov and independently in 1968 by James R. Rice, who showed that an energetic contour path integral was independent of the path around a crack.

<span class="mw-page-title-main">Hyperelastic material</span>

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<span class="mw-page-title-main">Rock mass plasticity</span>

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<span class="mw-page-title-main">Objective stress rate</span>

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In continuum mechanics, a hypoelastic material is an elastic material that has a constitutive model independent of finite strain measures except in the linearized case. Hypoelastic material models are distinct from hyperelastic material models in that, except under special circumstances, they cannot be derived from a strain energy density function.

<span class="mw-page-title-main">Lode coordinates</span>

Lode coordinates or Haigh–Westergaard coordinates. are a set of tensor invariants that span the space of real, symmetric, second-order, 3-dimensional tensors and are isomorphic with respect to principal stress space. This right-handed orthogonal coordinate system is named in honor of the German scientist Dr. Walter Lode because of his seminal paper written in 1926 describing the effect of the middle principal stress on metal plasticity. Other examples of sets of tensor invariants are the set of principal stresses or the set of kinematic invariants . The Lode coordinate system can be described as a cylindrical coordinate system within principal stress space with a coincident origin and the z-axis parallel to the vector .

References

  1. Lubliner, Jacob (2008), Plasticity Theory, Courier Dover Publications.
  2. Anandarajah (2010).
  3. Bilby, B. A.; Bullough, R.; Smith, E. (1955), "Continuous distributions of dislocations: a new application of the methods of non-Riemannian geometry", Proceedings of the Royal Society A , 231 (1185): 263–273, Bibcode:1955RSPSA.231..263B, doi:10.1098/rspa.1955.0171
  4. Kröner, E. (1958), "Kontinuumstheorie der Versetzungen und Eigenspannungen", Erg. Angew. Math., 5: 1–179
  5. Lee, E. H. (1969), "Elastic-Plastic Deformation at Finite Strains" (PDF), Journal of Applied Mechanics, 36 (1): 1–6, Bibcode:1969JAM....36....1L, doi:10.1115/1.3564580 [ permanent dead link ]
  6. Anand, L. (1979), "On H. Hencky's approximate strain-energy function for moderate deformations", Journal of Applied Mechanics, 46 (1): 78–82, Bibcode:1979JAM....46...78A, doi:10.1115/1.3424532

See also