%%% This file is part of PlanetMath snapshot of 2009-01-12 %%% Primary Title: surface of revolution %%% Primary Category Code: 51M04 %%% Filename: SurfaceOfRevolution2.tex %%% Version: 9 %%% Owner: pahio %%% Author(s): pahio %%% PlanetMath is released under the GNU Free Documentation License. %%% You should have received a file called fdl.txt along with this file. %%% If not, please write to gnu@gnu.org. \documentclass[12pt]{article} \pagestyle{empty} \setlength{\paperwidth}{8.5in} \setlength{\paperheight}{11in} \setlength{\topmargin}{0.00in} \setlength{\headsep}{0.00in} \setlength{\headheight}{0.00in} \setlength{\evensidemargin}{0.00in} \setlength{\oddsidemargin}{0.00in} \setlength{\textwidth}{6.5in} \setlength{\textheight}{9.00in} \setlength{\voffset}{0.00in} \setlength{\hoffset}{0.00in} \setlength{\marginparwidth}{0.00in} \setlength{\marginparsep}{0.00in} \setlength{\parindent}{0.00in} \setlength{\parskip}{0.15in} \usepackage{html} % this is the default PlanetMath preamble. as your knowledge % of TeX increases, you will probably want to edit this, but % it should be fine as is for beginners. % almost certainly you want these \usepackage{amssymb} \usepackage{amsmath} \usepackage{amsfonts} % used for TeXing text within eps files %\usepackage{psfrag} % need this for including graphics (\includegraphics) %\usepackage{graphicx} % for neatly defining theorems and propositions \usepackage{amsthm} % making logically defined graphics %\usepackage{xypic} % there are many more packages, add them here as you need them % define commands here \theoremstyle{definition} \newtheorem*{thmplain}{Theorem} \begin{document} If a \htmladdnormallink{curve}{http://planetmath.org/encyclopedia/LocalMultiplicity.html} in $\mathbb{R}^3$ \htmladdnormallink{rotates}{http://planetmath.org/encyclopedia/Rotate.html} about a \htmladdnormallink{line}{http://planetmath.org/encyclopedia/Incident2.html}, it \htmladdnormallink{generates}{http://planetmath.org/encyclopedia/SubgroupGeneratedBy.html} a {\em surface of revolution}. The line is called the {\em axis of revolution}. Every \htmladdnormallink{point}{http://planetmath.org/encyclopedia/Point.html} of the curve generates a {\em circle of latitude}. If the \htmladdnormallink{surface}{http://planetmath.org/encyclopedia/Surface.html} is intersected by a half-plane beginning from the axis of revolution, the \htmladdnormallink{intersection}{http://planetmath.org/encyclopedia/Meets.html} curve is a {\em meridian curve}. One can always think that the surface of revolution is \htmladdnormallink{generated by}{http://planetmath.org/encyclopedia/SubgroupGeneratedBy.html} the \htmladdnormallink{rotation}{http://planetmath.org/encyclopedia/Rotate.html} of a certain meridian, which may be called the {\em 0-meridian}. Let\, $y = f(x)$\, be a curve of the $xy$-plane rotating about the $x$-axis. Then any point \,$(x,\,y)$\, of this 0-meridian draws a circle of latitude, \htmladdnormallink{parallel}{http://planetmath.org/encyclopedia/ParallelLines.html} to the $yz$-plane, with \htmladdnormallink{centre}{http://planetmath.org/encyclopedia/Centre4.html} on the $x$-axis and with the \htmladdnormallink{radius}{http://planetmath.org/encyclopedia/NSphere2.html} $|f(x)|$. So the $y$- and $z$-coordinates of each point on this \htmladdnormallink{circle}{http://planetmath.org/encyclopedia/InteriorPoint2.html} satisfy the \htmladdnormallink{equation}{http://planetmath.org/encyclopedia/MultipleRoot.html} $$y^2+z^2 = [f(x)]^2.$$ This equation is thus satisfied by all points\, $(x,\,y,\,z)$\, of the surface of revolution and therefore it is the equation of the whole surface of revolution. More generally, if the equation of the meridian curve in the $xy$-plane is given in the implicit form \,$F(x,\,y) = 0$,\, then the equation of the surface of revolution may be written $$F(x,\,\sqrt{y^2\!+\!z^2}) = 0.$$ \textbf{Examples.} When the \htmladdnormallink{catenary}{http://planetmath.org/encyclopedia/Catenary2.html} \,$y = a\cosh\frac{x}{a}$\, rotates about the $x$-axis, it generates the {\em catenoid} $$y^2+z^2 = a^2\cosh^2\frac{x}{a}.$$ The catenoid is the only surface of revolution being also a \htmladdnormallink{minimal surface}{http://planetmath.org/encyclopedia/MinimalSurface.html}. The \htmladdnormallink{quadratic surfaces}{http://planetmath.org/encyclopedia/ConeSurface.html} of revolution: \begin{itemize} \item When the \htmladdnormallink{ellipse}{http://planetmath.org/encyclopedia/DandelinSphere.html} \,$\displaystyle\frac{x^2}{a^2}+\frac{y^2}{b^2} = 1$\, rotates about the $x$-axis, we get the \htmladdnormallink{ellipsoid}{http://planetmath.org/encyclopedia/Ellipsoid.html} $$\frac{x^2}{a^2}+\frac{y^2+z^2}{b^2} = 1.$$ This is a {\em stretched ellipsoid}, if\, $a > b$,\, and a {\em flattened ellipsoid}, if\, $a < b$, and a \htmladdnormallink{sphere}{http://planetmath.org/encyclopedia/NSphere2.html} of radius $a$, if\, $a = b$. \item When the \htmladdnormallink{parabola}{http://planetmath.org/encyclopedia/Focus4.html} \,$y^2 = 2px$ (with $p$ the {\em \htmladdnormallink{latus rectum}{http://planetmath.org/encyclopedia/DandelinSphere.html}} or the \htmladdnormallink{parameter of parabola}{http://planetmath.org/encyclopedia/ParametricPresentation.html}) rotates about the $x$-axis, we get the {\em paraboloid of revolution} $$y^2+z^2 = 2px.$$ \item When we let the \htmladdnormallink{conjugate hyperbolas}{http://planetmath.org/encyclopedia/ConjugateHyperbola.html} and their common \htmladdnormallink{asymptotes}{http://planetmath.org/encyclopedia/Asymptote.html} \,$\displaystyle\frac{x^2}{a^2}-\frac{y^2}{b^2} = s$\, (with\, $s = 1,\,-1,\,0$) rotate about the $x$-axis, we obtain the {\em \htmladdnormallink{two-sheeted hyperboloid}{http://planetmath.org/encyclopedia/ConeSurface.html}} $$\frac{x^2}{a^2}-\frac{y^2+z^2}{b^2} = 1,$$ the {\em \htmladdnormallink{one-sheeted hyperboloid}{http://planetmath.org/encyclopedia/ConeSurface.html}} $$\frac{x^2}{a^2}-\frac{y^2+z^2}{b^2} = -1$$ and the {\em cone of revolution} $$\frac{x^2}{a^2}-\frac{y^2+z^2}{b^2} = 0,$$ which apparently is the common {\em asymptote cone} of both hyperboloids. \end{itemize} \begin{thebibliography}{8} \bibitem{LP}{\sc Lauri Pimi\"a}: {\em Analyyttinen geometria}.\, Werner S\"oderstr\"om Osakeyhti\"o, Porvoo and Helsinki (1958). \end{thebibliography} \end{document}