Mesoscopic Theory of Microcracks
نویسندگان
چکیده
The mesoscopic concept is a way to deal with complex materials with an internal structure within continuum mechanics. It consists of extending the domain of the balance equations by mesoscopic variables and of introducing a local distribution function of these variables as a statistical element. In our case microcracks are modelled as penny shaped and completely characterized by their diameter and the unit normal to the crack surface. Two examples of crack dynamics are given as well as a possible definition of a damage parameter. Orientational order parameters (fabric-alignment tensors) are defined and balance like dynamic equations for them are derived. 1. A model of microcracks Macroscopic failure of brittle materials is initiated by the propagation of micro-cracks. In a simple model the microcrack is described as a flat, rotation symmetric surface, a so called penny shaped crack. In addition we make here the following simplifying assumptions: (1) The diameter of the cracks is much smaller than the linear dimension of the continuum element. Under this assumption the cracks can be treated as an internal structure of the continuum element. The cracks are assumed small enough that there is a whole distribution of crack sizes and orientations in the volume element. (2) The cracks are fixed to the material. Therefore their motion is coupled to the motion of representative volume elements. (3) The cracks cannot rotate independently of the material, i. e. if they have a nonzero rotation velocity at all, this rotation velocity is determined by the antisymmetric part of the time derivative of the deformation gradient of the surrounding material and it does not depend on crack length and orientation. All cracks within a volume element move and rotate with the same velocity. (4) The number of cracks is fixed, there is no production of cracks, but very short cracks are preexisting in the virgin material. (5) The cracks cannot decrease area, but can only enlarge, meaning that cracks cannot heal. To summarize our model the microcrack is characterized by a unit vector n representing the orientation of the surface normal and by the radius l of the spherical crack surface. These parameters will be taken as the additional variables in the mesoscopic theory.
منابع مشابه
Griffith Cracks in the Mesoscopic Microcrack Theory
The mesoscopic concept is applied to the description of microcracked brittle materials. The mesoscopic equations are solved in a special case when the microcracks are developing according to the Rice-Griffith evolution law. The evolution of the crack distribution function is investigated in case of simple loading conditions and for two different initial crack distribution functions. The time de...
متن کاملCrack Initiation and Crack Growth as the Problem of Localized Instability in Microcrack Ensemble
Statistical theory of defect evolution allows us to obtain non-linear kinetic equations for tensor parameter of microcrack density. Investigation of non-linear properties of kinetic equation showed the existence of specific type of self-similar solution at the developed stage of damage, which is characterized by explosion-like kinetics of the microcrack growth on the spectrum of spatial scales....
متن کاملاتلاف در مدارهای الکتریکی کوانتومی مزوسکوپی RLC
The quantum theory for a mesoscopic electric circuit with charge discreteness is investigated. Taking the Caldirola-Kanai Hamiltonian in studding quantum mechanics of dissipative systems, we obtain the persistent current and the energy spectrum of a damped quantum LC-design mesoscopic circuit under the influence of a time-dependent external field.
متن کاملComparison of two different implementations of a finite-difference-method for first-order pde in mathematica and matlab
1 Physics and analytical solution The growth rate of microcracks in a brittle material can be discribed by a mesoscopic equation. Here the specialized version for uniaxial loading is presented. ∂f(l, t) ∂t = − 1 l2 ∂lvl(l, t)f(l, t) ∂l , (1) f(l, t) is the distribution function for the crack length l at time t, vl = l̇ is the growth velocity of the cracks. A Rice-Griffith-like dynamic is assumed...
متن کاملA damage-softening statistical constitutive model considering rock residual strength
Under stress, the microcracks in rock evolve (initiation, growth and coalescence) from damage to fracture with a continuous process. In order to describe this continuous process, a damage-softening statistical constitutive model for rock was proposed based on the Weibull distribution of mesoscopic element strength. This model usually adopts the Drucker–Prager criterion as its distribution param...
متن کامل