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<html>
<title>multicomponent</title><body bgcolor="FFFFFF">
<h2>multicomponent</h2>
<menu>
<LI><A HREF="../../../src/snes/examples/tutorials/ex19.c.html"><CONCEPT>ex19.c</CONCEPT></A>
<menu>
Nonlinear driven cavity with multigrid in 2d.<BR>  <BR>
The 2D driven cavity problem is solved in a velocity-vorticity formulation.<BR>
The flow can be driven with the lid or with bouyancy or both:<BR>
  -lidvelocity &lt;lid&gt;, where &lt;lid&gt; = dimensionless velocity of lid<BR>
  -grashof &lt;gr&gt;, where &lt;gr&gt; = dimensionless temperature gradent<BR>
  -prandtl &lt;pr&gt;, where &lt;pr&gt; = dimensionless thermal/momentum diffusity ratio<BR>
  -contours : draw contour plots of solution<BR>
</menu>
<LI><A HREF="../../../src/snes/examples/tutorials/ex27.c.html"><CONCEPT>ex27.c</CONCEPT></A>
<menu>
Nonlinear driven cavity with multigrid and pusedo timestepping 2d.<BR>  <BR>
The 2D driven cavity problem is solved in a velocity-vorticity formulation.<BR>
The flow can be driven with the lid or with bouyancy or both:<BR>
  -lidvelocity &lt;lid&gt;, where &lt;lid&gt; = dimensionless velocity of lid<BR>
  -grashof &lt;gr&gt;, where &lt;gr&gt; = dimensionless temperature gradent<BR>
  -prandtl &lt;pr&gt;, where &lt;pr&gt; = dimensionless thermal/momentum diffusity ratio<BR>
  -contours : draw contour plots of solution<BR>
</menu>
<LI><A HREF="../../../src/snes/examples/tutorials/ex29.c.html"><CONCEPT>ex29.c</CONCEPT></A>
<menu>
Hall MHD with in two dimensions with time stepping and multigrid.<BR>-options_file ex29.options<BR>
other PETSc options<BR>
-resistivity &lt;eta&gt;<BR>
-viscosity &lt;nu&gt;<BR>
-skin_depth &lt;d_e&gt;<BR>
-larmor_radius &lt;rho_s&gt;<BR>
-contours : draw contour plots of solution<BR>
</menu>
<LI><A HREF="../../../src/snes/examples/tutorials/ex30.c.html"><CONCEPT>ex30.c</CONCEPT></A>
<menu>
Steady-state 2D subduction flow, pressure and temperature solver.<BR>\\nThe flow is driven by the subducting slab.<BR>
  -ivisc &lt;#&gt; = rheology option.<BR>
      0 --- constant viscosity.<BR>
      1 --- olivine diffusion creep rheology (T-dependent, newtonian).<BR>
      2 --- weak temperature dependent rheology (1200/T, newtonian).<BR>
  -ibound &lt;#&gt; = boundary condition <BR>
      0 --- isoviscous analytic.<BR>
      1 --- stress free. <BR>
      2 --- stress is von neumann. <BR>
  -icorner &lt;#&gt; = i index of wedge corner point.<BR>
  -jcorner &lt;#&gt; = j index of wedge corner point.<BR>
  -slab_dip &lt;#&gt; = dip of the subducting slab in DEGREES.<BR>
  -back_arc &lt;#&gt; = distance from trench to back-arc in KM.(if unspecified then no back-arc). <BR>
  -u_back_arcocity &lt;#&gt; = full spreading rate of back arc as a factor of slab velocity. <BR>
  -width &lt;#&gt; = width of domain in KM.<BR>
  -depth &lt;#&gt; = depth of domain in KM.<BR>
  -lid_depth &lt;#&gt; = depth to the base of the lithosphere in KM.<BR>
  -slab_dip &lt;#&gt; = dip of the subducting slab in DEGREES.<BR>
  -slab_velocity &lt;#&gt; = velocity of slab in CM/YEAR.<BR>
  -slab_age &lt;#&gt; = age of slab in MILLIONS OF YEARS. <BR>
  -potentialT &lt;#&gt; = mantle potential temperature in degrees CENTIGRADE.<BR>
  -kappa &lt;#&gt; = thermal diffusivity in M^2/SEC. <BR>
  -peclet &lt;#&gt; = dimensionless Peclet number (default 111.691)<BR>\
</menu>
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</body>
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