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  1. 85
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      dox/book.tex
  2. 269
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      dox/chapters/derivation.tex
  3. 58
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      dox/chapters/examples.tex
  4. 9
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      dox/chapters/magnetics.tex
  5. 189
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      dox/chapters/mesh.tex
  6. 5
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      dox/chapters/usage.tex
  7. 0
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      examples/magnet/toroid.geo

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dox/book.tex 查看文件

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+%\documentclass[11pt]{article}
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+%\documentclass[a4paper,11pt]{report}
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+%\documentclass[11pt]{report}
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+%\documentclass[a4paper,11pt]{scrartcl}
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+\documentclass[a4paper,11pt]{scrreprt} %book}
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+%\usepackage{times}
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+\usepackage{fullpage,amsmath,placeins,graphicx,color,amssymb,setspace,listings,tikz,amsthm,yfonts,subfigure}
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+\usepackage{natbib}
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+
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+\usepackage[linkbordercolor=white,citecolor={1 1 1}]{hyperref}
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+
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+\usepackage{amsthm} % theorem
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+	
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+\newcounter{proof}
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+\stepcounter{proof}	
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+\newtheorem{corollary}{Corollary}[proof]
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+
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+\definecolor{dkgreen}{rgb}{0,0.6,0}
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+\definecolor{gray}{rgb}{0.5,0.5,0.5}
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+
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+%\lstset{language=c++,numbers=left,numberstyle=\tiny,showstringspaces=false,color=true}
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+\lstset{language=c++,
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+   keywords={real, VectorXd, SparseMatrix, string, this, default, exit, float, double,int, break, case,
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+             catch,continue,else,elseif,end,for,function,Real,Complex,
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+             global,if,otherwise,persistent,return,switch,try,while,long, unsigned, vector},
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+   basicstyle=\ttfamily,
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+   keywordstyle=\color{blue},
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+   commentstyle=\color{red},
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+   stringstyle=\color{dkgreen},
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+   numbers=left,
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+   numberstyle=\tiny\color{gray},
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+   stepnumber=1,
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+   numbersep=10pt,
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+   backgroundcolor=\color{white},
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+   tabsize=4,
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+   showspaces=false,
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+   showstringspaces=false}
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+
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+
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+\def\LAPL#1{\nabla^2 {#1}}
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+\def\VEC#1{\mathbf{#1}}
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+\def\LBM{ \mathcal{L} ( \mathbb{R}^n ) }
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+\def\LBO{ \mathcal{L} ( \mathbb{R}^1 ) }
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+\def\LBT{ \mathcal{L} ( \mathbb{R}^2 ) }
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+\def\REB{ \mathbb{R} }
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+\def\REBN{ \mathbb{R}^n }
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+\def\CENSECA{\alpha(U_{n+1}^m-2U_n^m+U_{n-1}^m)}
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+%\def\DD#1{\frac{\partial}{\partial #1}}
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+\def\DD#1{\frac{d}{d #1}}
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+
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+\author{Trevor Irons \\  
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+        XRI Geophysics, LLC \\ 
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+        Trevor.Irons@xrigeo.com   }
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+
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+\title{FEM4EllipticPDE}
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+\subtitle{Lemma module v1.0}
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+
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+\begin{document}
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+
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+\maketitle
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+
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+\tableofcontents
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+
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+\renewcommand{\labelenumi}{(\Roman{enumi})}
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+\renewcommand{\labelenumii}{(\arabic{enumii})}
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+\renewcommand{\labelenumiii}{(\roman{enumiii})}
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+
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+\abstract
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+	This Lemma module provides a Galerkin-style finite element solution to general elliptic problems. 
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+	Lemma is an open source geophysical programming API that supports modular plug-ins, such as this one. 
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+	Lemma may be freely downloaded from \href{http://lemmasoftware.org}{http://lemmasoftware.org}.
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+	This module is currently closed source. Development of FEM4EllipticPDE started at the 
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+	Center for Gravity Electrical and Magnetic Studies (CGEM) at the Colorado School of Mines. The modules  
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+	was completed by XRI Geophysics, LLC. 
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+
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+\input{chapters/derivation}
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+\input{chapters/usage}
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+
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+\input{chapters/magnetics}
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+\input{chapters/examples}
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+
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+\bibliographystyle{seg}
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+\bibliography{nmr}
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+
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+\end{document}

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dox/chapters/derivation.tex 查看文件

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+\chapter{Derivation}
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+
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+\section{Problem Statement}
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+FEM4EllipticPDE is a Lemma module implementing a Galerkin finite element solution to a family of commonly encountered 
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+elliptic  problems taking the form
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+%Considering the uniformly elliptic Dirichlet BVP: 
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+\begin{eqnarray}
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+	\label{eq:scheme}
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+	-\nabla \cdot \left( \sigma(\mathbf{r}) \nabla u(\mathbf{r}) \right) = g(\mathbf{r}) & \mathop{\forall}_{u \in \Omega} \\
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+	u = 0                                            & \mathop{\forall}_{u \in \partial \Omega} 
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+\end{eqnarray}
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+
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+Where $0 < \sigma_{min} \leq \sigma(\mathbf{r}) \leq \sigma_{max} \ll \infty $  and $\Omega \in \mathbb{R}^3$. When $\sigma \equiv 1$, this 
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+reduces to Poisson's equation $\left( \nabla^2 u  = g \right)$. These types of problem arises in several areas of geophysics: gravitational or magnetic potentials 
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+obey Poisson's equation, while the more general form can be used to solve electrostatic (DC and SP) problems. 
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+
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+\begin{enumerate}
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+	\item The Galerkin finite element method is defined by reposing the global problem in terms of numerous local ones through the use of 
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+	appropriate test functions. 
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+	\begin{itemize}
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+
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+		\item Test functions $v$ must be from a suitable subspace. 
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+		In this case, due to the Dirichlet boundary conditions,
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+		\[
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+			v  \in H^a_b(\Omega)
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+		\]
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+		meet our requirements. $H^a_b$ represents the subspace of weakly differentiable functions that are zero valued at $a$, and $b$
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+		and $\textgoth{V}$ represents the actual functions. % Hilbert space.
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+
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+		The 3D variational problem may be written
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+
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+%		\[
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+%				-\nabla \cdot \left( \sigma(\mathbf{r}) \nabla u(\mathbf{r}) \right) = g(\mathbf{r}) & \mathop{\forall}_{u \in \Omega} \\
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+%	u = 0                                            & \mathop{\forall}_{u \in \partial \Omega} 
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+%
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+		%\] 
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+		\[
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+		  \int	-v \nabla \cdot \sigma  \nabla u = v g.
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+		\]
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+		This can be simplified 
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+		\[
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+			\int_a^b \sigma \frac{du}{dx} \frac{dv}{dx} dx = v g
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+		\]
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+		The proof of which follows below. 
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+		%\item The variational form may be found by multiplying the elliptic PDE by any arbitrary
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+		%\[ 
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+		%	v \in H_a^b(\Omega) 
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+		%\]
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+		
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+		%In 1D ($\Omega \in \mathbb{R}^1$) \autoref{eq:scheme} reduces to:
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+		%\begin{equation} \label{eq:oned}
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+		%	- \DD{x} \sigma \DD{x} u = g
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+		%\end{equation}
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+		%Using the variational (weak) formulation for any arbitrary $v \in \textgoth{V} 
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+	
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+		\item In any arbitrary dimension $x$, if the boundaries in that dimension of $\partial \Omega = [a,b]$ the variational problem using 
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+		test functions can be constructed 
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+		\begin{equation} \label{eq:oned}
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+			-\int_a^b v(x) \DD{x} \sigma(x) \DD{x} u(x)  dx = \int_a^b v(x) g(x) dx ,  
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+		\end{equation}
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+
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+				
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+		The variation problem can be reduced to a simplified version, if appropriate test functions we may instead write the 
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+		variational problem as 
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+		\[
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+			\int_a^b  \sigma \frac{du}{dx} \frac{dv}{dx} dx = \int_a^b v(x) g(x) dx
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+		\]
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+		
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+
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+		In one dimension this resolves to
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+		\[
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+			%	-\int_a^b v \frac{d}{dx} \left[ \sigma \frac{du}{dx} \right] dx = 
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+			\int_a^b  \sigma \frac{du}{dx} \frac{dv}{dx} dx = \int_a^b v(x) g(x) dx
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+		\]
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+
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+		
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+				
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+
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+		\begin{corollary}
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+		\[
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+		\frac{d}{dx} \left[ v \sigma \frac{du}{dx}  \right] = v \frac{d}{dx} \left[ \sigma \frac{du}{dx} \right] +
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+		 \sigma \frac{du}{dx} \frac{dv}{dx}  
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+		\]	
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+		\end{corollary}
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+
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+		
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+
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+		\begin{proof}
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+		and the integration by parts on the left hand side yields
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+		\begin{eqnarray*}
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+		\int_a^b v \frac{d}{dx} \left[ v \sigma \frac{du}{dx} \right] dx &=&  \int_a^b v \frac{d}{dx} 
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+		\left[ \sigma \frac{du}{dx} \right] dx + 
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+		\int_a^b \sigma \frac{du}{dx} \frac{dv}{dx} dx  \\
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+		\Rightarrow & & \\
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+		\left[ v \sigma \frac{du}{dx} \right]_a^b &=& \int_a^b v \frac{d}{dx} \left[ 
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+		\sigma \frac{du}{dx} \right]  + \int_a^b \sigma \frac{dv}{dx}\frac{du}{dx} dx \\
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+		\Rightarrow & & \\\
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+			-\int_a^b v \frac{d}{dx} \left[ \sigma \frac{du}{dx} \right] dx &=& \left[ v \sigma 
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+			\frac{du}{dx} \right]_a^b + \int_a^b \sigma \frac{du}{dx} \frac{dv}{dx} dx
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+		\end{eqnarray*}
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+		\[
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+				-\int_a^b v \frac{d}{dx} \left[ \sigma \frac{du}{dx} \right] dx = \int_a^b 
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+		\sigma \frac{du}{dx} \frac{dv}{dx} dx
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+		\]
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+		\end{proof}
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+
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+		Because $v\in H^1_0$ the solution vanishes at the boundaries $\left[ v \sigma \frac{du}{dx} \right]_a^b =0 $.
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+		Therefore the scheme reduces to:
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+
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+% 		Which can be rewritten as
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+% 		\[
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+% 			a(u,v) = <g,v>
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+% 		\] 
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+		
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+		The Galerkin FEM method uses triangle (hat) functions for $v$, which are renamed $\phi$ as 
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+		they are specific. I will occasionally use these interchangeably.  
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+
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+		Through induction it can be shown then that the 3D problem can similarity be posed 
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+		So that Equation \ref{eq:scheme} may be rewritten
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+		\[
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+			-v \nabla \cdot \sigma  \nabla u = g v.
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+		\]
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+
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+		\FloatBarrier
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+	
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+		\item \FloatBarrier Define mesh. Since $\Omega = (0,\pi)$ is an uncountable subset of $\mathbb{R}^1$ a 
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+		countable subset of $\Omega$ must be defined. A mesh is defined over the interval $(0,\pi)$.
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+		This mesh is defined and shown in Figure \ref{fig:mesh}.	
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+
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+		\begin{figure}[ht]
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+		\begin{center}
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+		\input{chapters/mesh}
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+		\caption{A 1D FEM mesh is defined. $N$ nodes ($n$) are defined over the interval. Between the 
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+		nodes an element is defined. The mesh is general and the spacing between nodes is defined by 
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+		$N-1$ discritisation parameters $h$.}
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+		\label{fig:mesh}
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+		\end{center}
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+		\end{figure}
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+
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+		\item Define a finite dimensional subspace based on the mesh and a particular test function.  
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+		A subspace  $\textgoth{V}_h \subset \textgoth{V}$ is sought such that $ \textgoth{V}_h$ is finite 
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+		dimensional. 
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+		Particular linearity independent test functions $\phi$ are defined on $\textgoth{V}_h$ such that 
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+		$\textgoth{V}_h = \mathrm{span}(\phi_i)$. The test functions form a basis of this space. 
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+		If the weak formulation of the derivative is used these
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+		test functions may be constructed such as they are only piecewise differentiable. We may define test 
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+		functions as Kronecker delta $\delta$ functions taking values of unity at a particular node of the mesh. 		
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+		The linear spline Galerkin method of FEM interpolates these $\delta$ functions. They are zero valued at the 
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+		neighbouring nodes. In 1D this interpolation yields hat functions.
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+		Therefore the test functions  $\phi_i$  are defined as:
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+
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+		\begin{equation}
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+		\phi_i(x) = \left\{ \begin{array}{ccl} 
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+		0 & \textrm{if}  & x\in[\alpha, x_{i-1}]  \\
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+		\frac{x - x_{i-1}}{h_i} & \textrm{if}  & x\in[x_{i-1}, x_i]  \\
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+		\frac{x_{i+1}-x}{h_{i+1}} & \textrm{if}  & x\in[x_i, x_{i+1}]  \\
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+		0 & \textrm{if}  & x\in[x_{i+1}, \beta ]  \\
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+		\end{array} \right.
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+		\end{equation} 
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+
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+		Define the variational form of the solution solution 
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+
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+		\begin{equation} \label{eq:sol1}
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+		a(u, v) = <g,v> 
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+		\end{equation}
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+
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+		A is a symmetric bilinear form such that $a(u,v) = a(v,u)   \forall v \in \textgoth{V}_h$.
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+		
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+	\end{itemize}
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+
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+	In 3D things are a little different. For a given element (tetrahedra) comprised of 4 points we construct the 
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+	location matrix
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+	\[ \mathbf{C}  = 
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+		\left[ \begin{matrix}
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+			1 & x_1 & y_1 & z_1  \\
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+			1 & x_2 & y_2 & z_2  \\
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+			1 & x_3 & y_3 & z_3  \\
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+			1 & x_4 & y_4 & z_4
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+		       \end{matrix} \right]
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+	\]
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+
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+	We can then fill the stiffness matrix
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+	\[
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+		K_{ij} = \sum_{i=0}^{N} \int_{Tet_k} = c \nabla \phi_i \cdot \phi_j
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+	\]
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+
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+	\item The solution may be written in matrix(stiffness matrix) vector (load vector) notation. 
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+
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+	We approximate the solution (Equation \ref{eq:sol1}) using the trial and test functions $\phi$ discussed 
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+	previously. Let 
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+	\begin{eqnarray*}
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+		\sigma(x) &=& x + 1 \\
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+		u(x) &=& \sin(x) 
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+	\end{eqnarray*}
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+
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+	At each node $u_h \in \textgoth{V}_h : a(u_h, v) = <g,v>$ the stiffness matrix $A$
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+	\begin{eqnarray*}
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+		A_{ij} &=& a(\phi_i, \phi_j) = \int_0^\pi \sigma(x) \phi'_i \phi'_j \\
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+		       &=&  \int_0^\pi (x+1) \phi'_i \phi'_j 
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+	\end{eqnarray*}
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+	
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+	%//Since $\phi$ is a triangle, $\phi'$ becomes a step function.
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+
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+	We have for $i= 1,\cdots , n$
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+	\[
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+		\phi'(x) = \left\{ \begin{array}{ccl}
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+			0 & \textrm{if}  & x\in[\alpha, x_{i-1}]  \\
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+			\frac{1}{h_i} & \textrm{if}  & x\in[x_{i-1}, x_i]  \\
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+			-\frac{1}{h_{i+1}} & \textrm{if}  & x\in[x_i, x_{i+1}]  \\
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+			0 & \textrm{if}  & x\in[x_{i+1}, \beta ]  \\
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+		\end{array} \right.
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+	\]
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+
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+	The product $\phi_i'(x) \phi_j(x)$ vanishes when $|i - j| > 1$. So that in a 1D case, A becomes tri-diagonal. 
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+	Following the general equation:
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+	\begin{eqnarray*}
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+		A_{ij} &=&  \int_{i-1}^{i+1} (x+1) \phi'_i(x) \phi'_j(x) \\ 
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+	\end{eqnarray*}
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+
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+	The load vector $g$ is given:
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+	\[
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+		[g]_i = <g, \phi_i> = \int_0^\pi g \phi_i
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+	\]
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+
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+	Using $ g = [g]$, the linear system becomes:
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+	\[
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+		Au = g
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+	\]
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+
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+	\item For this case the entries of the stiffness matrix  and load vector are
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+	
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+	For the three non-zero cases of $A$:
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+	\begin{eqnarray*}
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+		A_{ii} &=&  \int_{i-1}^{i+1} (x+1) \phi'_i(x) \phi'_i(x) \\ 
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+		A_{ii} &=& \int_{{i-1}}^{i} (x+1) \phi_i'^2 dx + \int_{i}^{x_{i+1}} (x+1)\phi_i'^2 \\ 
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+		A_{ii} &=& \frac{1}{h_i^2}\int_{{i-1}}^{i} (x+1)  dx + \frac{1}{h_{i+1}^2} \int_{i}^{{i+1}} (x+1) dx 
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+	\end{eqnarray*}
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+
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+	\begin{eqnarray*}
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+		A_{i,i+1} &=& \int_{i}^{i+1} (x+1) \phi'_i(x) \phi'_{i+1}(x) \\ 
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+		A_{i,i+1} &=& \int_{i}^{i+1} (x+1) \phi_i' \phi_{i+1}' dx \\ %+ \int_{i}^{x_{i+1}} (x+1)\phi_i' \phi_{i+1}'  \\ 
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+		A_{i,i+1} &=& \frac{1}{h_i + h_{i+1}}\int_{i}^{i+1} (x+1)  dx %+ \frac{1}{h_{i+1}^2} \int_{i}^{{i+1}} (x+1) dx 
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+	\end{eqnarray*}
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+
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+	\begin{eqnarray*}
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+		A_{i,i-1} &=&  \int_{i-1}^{i} (x+1) \phi'_i(x) \phi'_{i-1}(x) \\ 
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+		A_{i,i-1} &=&  \int_{i-1}^{i} (x+1) \phi_i' \phi_{i-1}' dx \\%+ \int_{i}^{x_{i+1}} (x+1)\phi_i' \phi_{i-1}' \\ 
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+		A_{i,i-1} &=& \frac{1}{h_i + h_{i-1}}\int_{{i-1}}^{i} (x+1) dx % dx + \frac{1}{h_{i+1}^2} \int_{i}^{{i+1}} (x+1) dx 
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+	\end{eqnarray*}
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+	
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+	These integrals are evaluated numerically in my program \textit{gfemddn} using Simpson's Rule.
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+
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+	Solving for the forcing function $g$ in  \autoref{eq:scheme}
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+	\begin{eqnarray*}
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+		-\nabla \cdot \sigma(x) \nabla u(x) &=& g(x) \\
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+		-\frac{\partial}{\partial x} \cdot (x+1) \frac{\partial }{\partial x} \sin(x) &=& g(x) \\
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+		-\frac{\partial}{\partial x} \cdot (x+1) \cos(x) &=& g(x) \\
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+		 \sin(x) + x\sin(x) - \cos(x) &=& g(x) \\
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+		 \sin(x) (x+1) - \cos(x) &=& g(x) \\
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+	\end{eqnarray*}	 
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+
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+	The load vector $g$ is then:
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+	\[
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+		g_i = <g, \phi_i> = \int_0^\pi \left(  \sin(x) (x+1) - \cos(x) \right) \phi_i
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+	\]
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+	In \textit{gfemddn} this integral is again evaluated using Simpson's Rule.
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+
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+	\end{enumerate}
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+

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dox/chapters/examples.tex 查看文件

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+\chapter{Examples and Verification}
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+
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+\section{Coulombic Magnetic Potential}
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+		In the absence of external current densities, we may write $\nabla \times \mathbf{H} = 0$.
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+		This allows the $H$ field to be represented using a scalar potential term  
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+		\begin{align} 
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+			\mathbf{H} = \nabla \phi_M.
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+		\end{align}
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+		Static magnetics problems (in linear media) can be solved using a scalar potential term obeying the 
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+		following relationship \cite[e.g.,][]{Jackson1998}
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+		\begin{align} \label{eq:permMagnet}
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+			%-\nabla \cdot \mu(\mathbf{r}) \nabla \phi_M(\mathbf{r}) = \mu(\mathbf{r}) M_0(\mathbf{r}).
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+			-\LAPL{\phi_M} = \rho_M(\mathbf{r}).
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+		\end{align}
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+		Where $\phi_M$ represents the Coulomb magnetic potential (appropriate for static magnetics problems) 
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+		and $\rho_M$ is the effective magnetic charge density (=$\nabla \cdot \mathbf{M}$).
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+		This formulation is particularity useful in calculating the fields of permanent magnets, where the 
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+		magnetisation of the magnet is given by $\mathbf{M}(\mathbf{r})$.
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+		The left hand side of (\ref{eq:permMagnet}) can easily be solved using {\bf{FEM4EllipticPDE}}, however 
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+		the right hand side requires some special care. 
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+
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+	\subsection{Calculation of Charge Density}
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+		For uniformly magnetised media $\rho_M$ vanishes everywhere except at the boundaries of the magnet.  
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+		In truth, $\mathbf{M}$ is well behaved and there are no truly uniformly magnetized magnets, but the 
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+		true nature of $\mathbf{M}$ is rarely known, and the assumption of uniform magnetisation becomes necessary. 
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+		Practical permanent magnets are \emph{effectively} uniformly magnetised, and this assumption is completely 
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+		reasonable, and even necessary. 
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+
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+		We can therefore apply the divergence theorem to to the boundaries to calculate the surface charge density
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+		$\sigma_M = \hat{\mathbf{n}} \cdot \mathbf{M}$ which exists on the 2D surface of the media and has zero 
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+		Riemann measure, formally necessitating a Lebesgue integral. 
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+		We may then let $\rho_M \rightarrow \sigma_M$ in 
33
+		(\ref{eq:permMagnet}). 
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+		The FEM variational formulation for an particular element in the load vector $g$ that spans 
35
+		the boundary of the media at point $\mathbf{r}_0$  can be written
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+		\begin{align}
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+			[g]_i & = \left< \rho_M, \phi_i \right> = \int \rho_M \phi_i \\
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+			      %//& = \int_L \delta\{\hat{\mathbf{r}_0}\} \sigma_M \phi_i \\ 
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+			      & = \int_L \sigma_M \phi_i \\ 
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+			      & = \sigma_M \phi_i(\mathbf{r}_0). 
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+		\end{align}
42
+
43
+	\subsection{Uniformly Charged Sphere}
44
+	The scalar potential of a uniformly charged sphere is given \cite[p. 198, ][]{Jackson1998} 
45
+	\begin{align}
46
+		\phi_M(\rho, \theta) = \frac{1}{3} M_0 a^2 \frac{r_<}{r_>^2} \cos(\theta).
47
+	\end{align}
48
+	Where the notation $r_<, r_>$ represents the smaller or larger of the distance $\rho$ and sphere radius $a$.
49
+
50
+	Inside the sphere
51
+	\begin{align}
52
+		%\phi_M &= \frac{1}{3} M_0 \rho \cos \theta  & \text{inside the sphere} \\
53
+		\phi_M &= \frac{1}{3} M_0 z  & \text{inside the sphere} \\
54
+		\phi_M &= \frac{1}{3} M_0 a^3 \frac{\cos \theta}{\rho^2}  & \text{outside the sphere} 
55
+	\end{align}
56
+	
57
+
58
+ 

+ 9
- 0
dox/chapters/magnetics.tex 查看文件

@@ -0,0 +1,9 @@
1
+\chapter{Magnetics}
2
+
3
+\section{Linear approximation}
4
+
5
+Linear induced magnetism. For low values of $\kappa$, the induced field can be approximated. For higher suceptibilities for for 
6
+remanance furthur corrections are needed, see section \
7
+\[
8
+	\nabla^2 u = \nabla \cdot \kappa \mathbf{H}
9
+\]

+ 189
- 0
dox/chapters/mesh.tex 查看文件

@@ -0,0 +1,189 @@
1
+% Graphic for TeX using PGF
2
+% Title: /home/tirons/CGEM/tirons/Class/npde/ass2/report/mesh.dia
3
+% Creator: Dia v0.96.1
4
+% CreationDate: Sun Mar 29 11:45:22 2009
5
+% For: tirons
6
+% \usepackage{tikz}
7
+% The following commands are not supported in PSTricks at present
8
+% We define them conditionally, so when they are implemented,
9
+% this pgf file will use them.
10
+\ifx\du\undefined
11
+  \newlength{\du}
12
+\fi
13
+\setlength{\du}{15\unitlength}
14
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15
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+% was here!!!
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+\pgfsetstrokecolor{dialinecolor}
31
+\draw (12.012500\du,10.037500\du)--(27.337500\du,10.062500\du);
32
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+\node[anchor=west] at (26.820000\du,12.410000\du){$\pi$};
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148
+}
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150
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151
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152
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154
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155
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156
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158
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159
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160
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163
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188
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189
+\end{tikzpicture}

+ 5
- 0
dox/chapters/usage.tex 查看文件

@@ -0,0 +1,5 @@
1
+\chapter{Usage}
2
+
3
+The main resource for using FEM4EllipticPDE is the Doxygen generated man pages. However, in this document 
4
+a more high level, simplified and incomplete, but also practical description of the API is presented for 
5
+those just wanting to use, and not extend the module. 

+ 0
- 106
examples/magnet/toroid.geo 查看文件

@@ -1,106 +0,0 @@
1
-/* This file is part of Lemma, a geophysical modelling and inversion API.
2
- * More information is available at http://lemmasoftware.org
3
- */
4
-
5
-/* This Source Code Form is subject to the terms of the Mozilla Public
6
- * License, v. 2.0. If a copy of the MPL was not distributed with this
7
- * file, You can obtain one at http://mozilla.org/MPL/2.0/.
8
- */
9
-
10
-/**
11
- * @file
12
- * @date      02/04/2016 02:58:54 PM
13
- * @version   $Id$
14
- * @author    Trevor Irons (ti)
15
- * @email     tirons@egi.utah.edu
16
- * @copyright Copyright (c) 2016, University of Utah
17
- * @copyright Copyright (c) 2016, Lemma Software, LLC
18
- */
19
-
20
-radius = 3.25;   // Radius of the damn thing
21
-blc = radius/2;  //  0.25;   // Target element size
22
-Box = 3*radius;  // The down side of potential
23
-lc = radius/2;        // toroid characteristic length
24
-
25
-
26
-tpp = newp;
27
-ts = 1;         // height of toroid
28
-tx = radius;  // radial width of toroid, measured in centre of ring
29
-tl = 0;         // centre of rotation
30
-
31
-Point(tpp  ) = {    tx,    0, 0,  lc};
32
-Point(tpp+1) = { ts+tx,    0, 0,  lc};
33
-Point(tpp+2) = {    tx,   ts, 0,  lc};
34
-Point(tpp+3) = {    tx,  -ts, 0,  lc};
35
-Point(tpp+4) = {-ts+tx,    0, 0,  lc};
36
-
37
-cc = newc;
38
-Circle(cc  ) = {tpp+1, tpp, tpp+2};
39
-Circle(cc+1) = {tpp+2, tpp, tpp+4};
40
-Circle(cc+2) = {tpp+4, tpp, tpp+3};
41
-Circle(cc+3) = {tpp+3, tpp, tpp+1};
42
-
43
-ll = newll;
44
-Line Loop(ll) = {cc, cc+1, cc+2, cc+3};
45
-
46
-ps = news;
47
-pio2=Pi/2;
48
-Plane Surface(ps) = {ll};
49
-tv1[] = Extrude {{0, 1, 0},{-tl,0,0}, 2*Pi/3} { Surface{ps}; };
50
-tv2[] = Extrude {{0, 1, 0},{-tl,0,0}, 2*Pi/3} { Surface{28}; };
51
-tv3[] = Extrude {{0, 1, 0},{-tl,0,0}, 2*Pi/3} { Surface{50}; };
52
-//t1[] = Rotate {{0,0,1},{0,0,0},pio2  } {Duplicata{Surface{ps};}};
53
-//Extrude Surface {ps, {0,1,0}, {-tl,0,0}, 2*Pi/3} { Recombine ;};
54
-//Extrude Surface {28, {0,1,0}, {-tl,0,0}, 2*Pi/3}; //{Layers{10,73,1};};
55
-//Extrude Surface {50, {0,1,0}, {-tl,0,0}, 2*Pi/3}; //{Layers{10,73,1};};
56
-
57
-/* Make a list of a ring (annulus) of surfaces around the hole */
58
-//allParts[] = {tv1[1], tv2[1], tv3[1]};
59
-
60
-/* Make surfaces to be meshed by transfinite algorithm */
61
-//Transfinite Surface {allParts[]};
62
-
63
-/* The "Recombine Surface" command is issued in order to
64
- * crate quadrilateral elements.
65
- */
66
-//Recombine Surface {allParts[]};
67
-
68
-// Extrude Surface {12, {0,0,1}, {0,0,0}, 2*Pi/3} {
69
-//   Recombine ; Layers { 6, 54, 1 } ;
70
-// } ;
71
-
72
-// Total Solution Space
73
-X0 = -Box;
74
-X1 =  Box;
75
-Y0 = -Box;
76
-Y1 =  Box;
77
-Z0 = -Box;
78
-Z1 =  Box;
79
-/////////////////////////////////////
80
-// Large Bounding box
81
-pp = newp;
82
-Point(pp)    = {X0, Y0, Z0, blc};
83
-Point(pp+1)  = {X1, Y0, Z0, blc};
84
-Point(pp+2)  = {X1, Y1, Z0, blc};
85
-Point(pp+3)  = {X0, Y1, Z0, blc};
86
-//
87
-lv = newl;
88
-Line(lv) = {pp,pp+1};
89
-Line(lv+1) = {pp+1,pp+2};
90
-Line(lv+2) = {pp+2,pp+3};
91
-Line(lv+3) = {pp+3,pp};
92
-Line Loop(lv+4) = {lv, lv+1, lv+2, lv+3};
93
-//
94
-// Hard coded doom
95
-bs = news;
96
-Plane Surface(bs) = {lv+4};
97
-//
98
-//v = newv;
99
-v[] = Extrude {0, 0, Z1-Z0} { Surface{bs}; };
100
-
101
-/* This is GOOD */
102
-//Surface{ allParts[1] } In Volume{v[1]};
103
-Surface{ ps } In Volume{v[1]};
104
-//Surface{t1[0]} In Volume{v[1]};
105
-//Surface{t2[0]} In Volume{v[1]};
106
-//Surface{t3[0]} In Volume{v[1]};

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