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A Visualization System For Mineral Elasticity

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Solve Cristoffel's equation to obtain wave velocities-direction data ... Use an icosahedron in which each vertex on the surface represents a propagation direction ... – PowerPoint PPT presentation

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Title: A Visualization System For Mineral Elasticity


1
A Visualization System For Mineral Elasticity
  • Richard Perkins

2
Introduction
  • Objectives
  • To continue development on the interactive
    elasticity visualization system
  • To interactively visualize elastic constants and
    wave velocities-direction data of crystals with
    different pressures, temperatures and
    compositional factors
  • To support remote visualization
  • Client-Server architecture approach
  • To support an online data repository

3
Visualization Algorithm
  • Use elastic constants as input
  • Solve Cristoffels equation to obtain wave
    velocities-direction data
  • Display computed velocities as continuous
    surfaces
  • Provide interactive graphic user interface

4
Definitions
  • Elasticity/Elastic
  • When a material is elastic it deforms under
    stress but return to its original state when the
    stress is removed
  • Elastic constants (Cijs)
  • The relation between stress and strain as defined
    in Hookes Law
  • Used to define the elasticity of a crystal as a
    multivariate physical quantity
  • Wave velocity-direction data
  • Calculated from the elastic constants and wave
    propagation direction using Cristoffels equation
  • Produces three sets of wave velocities-direction
    data a longitudinal wave parallel to the
    propagation direction and two shear waves
    perpendicular to the propagation direction
  • Anisotropic factors
  • Are used to compare the velocities of the
    different waves

5
Plots
  • Star plots and parallel plots
  • Used to directly represent the elastic constants
  • An-plot
  • Plots anisotropy factors for longitudinal and
    shear waves
  • Polygon-base surface rendering
  • Graphically represent the three waves (one
    longitudinal and two shear waves)

6
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7
Polygon-based surface Rendering
  • How waves are rendered
  • Use an icosahedron in which each vertex on the
    surface represents a propagation direction
  • Recursively subdivide triangles into 4 triangle
    thereby increasing the number of vertexes
  • Use the wave velocity-direction data calculated
    from Cristoffels equation to figure out each
    velocity at each vertex (propagation direction)
  • Re-position the vertices in 3D space to represent
    the velocity-direction distribution.___

8
1st Degree 80 triangles
2nd Degree 320 triangles
3rd Degree 1280 triangles
4th Degree 5120 triangles
9
Velocity-direction Features
  • Features pertaining to wave velocity-direction
    rendering
  • Views
  • 3d velocity
  • XY/YZ/ZX plane
  • Frame
  • Solid/wire
  • Shading
  • Enables/Disabled/Scaled
  • Axis
  • Degree

10
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11
Other Features
  • Personalized line color and thickness
  • Single and Multiple mode
  • Temperature and pressure
  • Zooming
  • Clear screen
  • Removal of data from screen
  • Data being visualized is selected in tree
  • Manipulation of star plot which include
  • Changing axes
  • Removing axes
  • Rotating axes
  • And many more

12
Conclusion
  • Our system allows us to visualize elastic
    constants and wave velocities as a function of
    pressure, temperature and composition
  • Our system visualizes the data through the use of
    star plots, parallel plots, an-plots, and
    polygon-based surface rendering

13
Future Prospects
  • Make remote application access more user friendly
  • Expand the database
  • Extend the visualization system to
    polycrystalline and multiphase composites
  • Make the visualization system more user
    interactive
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