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diff --git a/texmf-dist/doc/latex/siam/ptexconf.all b/texmf-dist/doc/latex/siam/ptexconf.all new file mode 100644 index 00000000..06e2a7f3 --- /dev/null +++ b/texmf-dist/doc/latex/siam/ptexconf.all @@ -0,0 +1,102 @@ + +Please answer the following: + +1. Name of conference +2. Type of Presentation + Contributed: Lecture form or Poster form + Minisymposium: + +3. Equipment for Visual Support + Lecture form/Minisymposium: Overhead Projector or + 2" x 2" Slide Projector (35mm) + + Poster form: Easel or Poster Board + +4. If you are a speaker in a minisymposium, who is the organizer? + +5. What is the minisymposium title? + +6. If more than one author, who will present the paper? + + +%This is a macro file for creating a SIAM Conference abstract in +% Plain Tex. +% +% If you have any questions regarding these macros contact: +% Lillian Hunt +% SIAM +% 3600 University City Center Center +% Philadelphia, PA 19104-2688 +% USA +% (215) 382-9800 +% e-mail:meetings@siam.org + + +\hsize=25.5pc +\vsize=50pc +\parskip=3pt +\parindent=0pt +\overfullrule=0pt +\nopagenumbers + +\def\title#1\\{\bf{#1}\vskip6pt} +\def\abstract#1\\{\rm {#1}} +\def\author#1\\{\vskip6pt\rm {#1}\vfill\eject} +\def\eol{\hfill\break} + +% end of style file + +% This is ptexconf.tex. Use this file as an example of a SIAM +% Conference abstract in plain TeX. + +\input ptexconf.sty + +\title Numerical Analysis of a 1-Dimensional +Immersed-Boundary Method\\ + +\abstract We present the numerical analysis of a simplified, +one-dimensional version +of Peskin's immersed boundary method, which has been used to +solve +the two- and three-dimensional Navier-Stokes equations in the +presence of immersed boundaries. We consider the heat +equation + in a finite domain with a moving source term. +We denote the solution as $u(x,t)$ and the location of the +source + term as $X(t)$. The source term is a moving delta function +whose strength is a function of u at the location of the +delta function. +The p.d.e. is coupled to an ordinary differential equation +whose +solution gives the location of the source term. + The o.d.e. is $X'(t) = u(X(t),t)$, which can be interpreted as +saying the source term moves at the local velocity. +The accuracy the numerical method of solution depends on how +the +delta function is discretized when the delta function is not +at +a grid point and on how the solution, u, is represented + at locations between grid points. We present results showing +the effect of different choices of spreading the source to +the grid and +of restricting the solution to the source location. +The problem we analyze is also similar to the Stefan problem +and +the immersed-boundary method has features in common with +particle-in-cell + methods.\\ +\author\underbar{Richard P. Beyer, Jr.}\eol +University of Washington, Seattle, WA\eol +%\vskip3pt +Randall J. LeVeque\eol +University of Washington, Seattle, WA\\ +\bye + +% end of example file + + +Please furnish complete addresses for all co-authors. + + +PLEASE BE SURE TO INDICATE WHAT CONFERENCE THE ABSTRACT IS FOR.
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