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Donaldson, Roger David (2008-05-02) Discrete geometric homogenisation and inverse homogenisation of an elliptic operator. http://resolver.caltech.edu/CaltechETD:etd-05212008-164705


Type of Document Dissertation
Author Donaldson, Roger David
Author's Email Address rdonald@acm.caltech.edu
URN etd-05212008-164705
Persistent URL http://resolver.caltech.edu/CaltechETD:etd-05212008-164705
Title Discrete geometric homogenisation and inverse homogenisation of an elliptic operator
Degree PhD
Option Applied and Computational Mathematics
Advisory Committee
Advisor Name Title
Houman Owhadi Committee Chair
Jerrold Marsden Committee Member
Mathieu Desbrun Committee Member
Peter Schroeder Committee Member
Thomas Hou Committee Member
Keywords
  • FEM
  • upscaling
  • metric-based up-scaling
  • inverse problems
  • discrete differential geometry
  • electric impedance tomography
  • conductivity
  • homogenization
  • finite element method
  • metric
  • convexity
  • variational mesh generation
  • anisotropy
  • anisotropic
  • weighted Delaunay triangulation
  • Dirichlet Neumann map
  • multiscale
  • multi-scale
Date of Defense 2008-05-02
Availability mixed
Abstract
We show how to parameterise a homogenised conductivity in $R^2$ by a scalar function $s(x)$, despite the fact that the conductivity parameter in the related up-scaled elliptic operator is typically tensor valued. Ellipticity of the operator is equivalent to strict convexity of $s(x)$, and with consideration to mesh connectivity, this equivalence extends to discrete parameterisations over triangulated domains. We apply the parameterisation in three contexts: (i) sampling $s(x)$ produces a family of stiffness matrices representing the elliptic operator over a hierarchy of scales; (ii) the curvature of $s(x)$ directs the construction of meshes well-adapted to the anisotropy of the operator, improving the conditioning of the stiffness matrix and interpolation properties of the mesh; and (iii) using electric impedance tomography to reconstruct $s(x)$ recovers the up-scaled conductivity, which while anisotropic, is unique. Extensions of the parameterisation to $R^3$ are introduced.
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