2021-06-07 18:54:36 +02:00
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\documentclass[8pt,landscape]{article}
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\usepackage{calc}
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% \usepackage{ccicons}
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\usepackage{amsmath, amsfonts, amssymb, amsthm}
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\usepackage[
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type={CC},
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modifier={by-sa},
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version={3.0}
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]{doclicense}
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% To make this come out properly in landscape mode, do one of the following
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% 1.
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% pdflatex latexsheet.tex
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%
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% 2.
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% latex latexsheet.tex
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% dvips -P pdf -t landscape latexsheet.dvi
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% ps2pdf latexsheet.ps
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% If you're reading this, be prepared for confusion. Making this was
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% a learning experience for me, and it shows. Much of the placement
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% was hacked in; if you make it better, let me know...
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% 2008-04
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% Changed page margin code to use the geometry package. Also added code for
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% conditional page margins, depending on paper size. Thanks to Uwe Ziegenhagen
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% for the suggestions.
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% 2006-08
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% Made changes based on suggestions from Gene Cooperman. <gene at ccs.neu.edu>
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% To Do:
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% This sets page margins to .5 inch if using letter paper, and to 1cm
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% if using A4 paper. (This probably isn't strictly necessary.)
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% If using another size paper, use default 1cm margins.
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{ \geometry{top=.5in,left=.5in,right=.5in,bottom=.5in} }
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{\ifthenelse{ \lengthtest{ \paperwidth = 297mm}}
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{-1ex plus -.5ex minus -.2ex}%
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T\kern-.1667em\lower.7ex\hbox{E}\kern-.125emX}}
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% -----------------------------------------------------------------------
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\begin{document}
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\raggedright
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\footnotesize
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2021-06-24 11:57:16 +02:00
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\begin{multicols*}{3}
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2021-06-07 18:54:36 +02:00
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% multicol parameters
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% These lengths are set only within the two main columns
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\begin{center}
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\Large{ZF Mathematik V} \\
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\small{701-0106-00L Mathematik V, bei M. A. Sprenger} \\
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\small{Jannis Portmann \the\year}
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\end{center}
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\begin{center}
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\rule{\linewidth}{0.25pt}
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\end{center}
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2021-06-24 09:08:56 +02:00
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\section{Gewöhnliche Differentialgleichungen}
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\subsection{1. Ordnung}
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$$\frac{dH}{dt} = v_0 - \frac{H(t)}{\tau}$$
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Eine Lösung davon
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$$H(t) = (H_0 - v_0\tau)^{\frac{-t}{\tau}} + v_0 \tau$$
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2021-06-24 14:12:16 +02:00
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\subsection{Fliessgleichgewicht}
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Für eine Funktion $F$, bei
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$$\frac{dF}{dt} = 0$$
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2021-06-24 18:05:47 +02:00
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\subsection{Satz von Gauss}
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$$\iint_A \mathrm{div} \, v \, dA = \oint_C \, v \, dr$$
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Flächenintegral der Divergenz von $v$ = Fluss von $v$ durch Rand $C$
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\subsection{Satz von Stokes}
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$$\iint_A \mathrm{rot} \, v \, dA = \iint_A \zeta \, dA = \oint_C \, v \, ds$$
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Flächenintegral der Rotation von $v$ = Linienintegral von $v$ entlang $C$ (Zirkulation)
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2021-06-24 09:08:56 +02:00
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\section{Taylor-Reihe}
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2021-06-24 11:56:45 +02:00
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An der stelle $a$ einer Funtkion $f(x)$
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2021-06-24 11:58:06 +02:00
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$$f(a) + \frac{f'(a)}{1!}(x-a) + \frac{f''(a)}{2!}(x-a)^2 + \frac{f'''(a)}{3!}(x-a)^3 + ...$$
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2021-06-24 09:08:56 +02:00
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2021-06-07 19:11:26 +02:00
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\section{Operators}
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2021-06-24 18:10:26 +02:00
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$$\mathrm{div} \, \vec{u} = \frac{\partial u}{\partial x} + \frac{\partial v}{\partial y}$$
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$$\mathrm{rot} \, \vec{u} = \nabla \times \vec{u} = -\frac{\partial u}{\partial y} + \frac{\partial v}{\partial x}$$
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2021-06-07 19:11:26 +02:00
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$$\nabla = \begin{pmatrix}
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\frac{\partial}{\partial x},
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\frac{\partial}{\partial y},
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\frac{\partial}{\partial z}
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\end{pmatrix}$$
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2021-06-07 18:54:36 +02:00
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\scriptsize
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\section{Copyleft}
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\doclicenseImage \\
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Dieses Dokument ist unter (CC BY-SA 3.0) freigegeben \\
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\faGlobeEurope \kern 1em \url{https://n.ethz.ch/~jannisp} \\
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\faGit \kern 0.88em \url{https://git.thisfro.ch/thisfro/wettersysteme-zf} \\
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Jannis Portmann, HS20
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\section{Referenzen}
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\begin{enumerate}
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\item Skript zur Vorlesung
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\end{enumerate}
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\end{multicols*}
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\end{document}
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