Abstract

Diffuse interface models are widely used to describe the evolution of multi-phase systems of various natures. Dispersed inclusions described by these models are usually three-dimensional (3D) objects characterized by phase field distribution. When employed to describe elastic fracture evolution, the dispersed phase elements are effectively two-dimensional (2D) objects. An example of the model with effectively one-dimensional (1D) dispersed inclusions is a phase field model for electric breakdown in solids. Any diffuse interface field model is defined by an appropriate free energy functional, which depends on a phase field and its derivatives. In this work we show that codimension of the dispersed inclusions significantly restricts the functional dependency of the free energy on the derivatives of the problem state variables. It is shown that to describe codimension 2 diffuse objects, the free energy of the model necessarily depends on higher order derivatives of the phase field or needs an additional smoothness of the solution, i.e., its first derivatives should be integrable with a power greater than two. Numerical experiments are presented to support our theoretical discussion.

Highlights

  • Phase field models form a theoretically sound framework for analysis of a broad class of problems in multiphase hydrodynamics [1], solid mechanics and fracture [2,3], material science, solidification and phase transitions, crystal structures [4,5,6]and many others research fields

  • Any diffuse interface field model is defined by an appropriate free energy functional, which depends on a phase field and its derivatives

  • In this paper we study a problem with “inclusions” of higher codimension whose evolution is described by the diffuse interface models

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Summary

Introduction

Phase field (or order parameter) models form a theoretically sound framework for analysis of a broad class of problems in multiphase hydrodynamics [1], solid mechanics and fracture [2,3], material science, solidification and phase transitions, crystal structures [4,5,6]. These models are employed to describe dynamics of certain inclusions, i.e., elementary macroscopic constituents (such as droplets), of the dispersed phase immersed into a homogeneous medium. Spatial distribution of the dispersed phase is described by the so-called phase field or order parameter field which is a smooth function of time and spatial coordinates. In the context of multiphase hydrodynamics, two or more immiscible fluids are separated by a diffuse interface. The models have to provide an internal mechanism preventing excessive sharpening or spreading of the diffuse interface during the system evolution

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