Relay-Version: version B 2.10 5/3/83; site utzoo.UUCP Path: utzoo!watmath!clyde!burl!ulysses!mhuxr!mhuxn!ihnp4!hplabs!turtlevax!ken From: ken@turtlevax.UUCP (Ken Turkowski) Newsgroups: net.graphics,net.math Subject: Re: parametric equations Message-ID: <1149@turtlevax.UUCP> Date: Tue, 29-Apr-86 13:09:06 EDT Article-I.D.: turtleva.1149 Posted: Tue Apr 29 13:09:06 1986 Date-Received: Fri, 2-May-86 07:30:15 EDT References: <1450@nlm-mcs.ARPA> Reply-To: ken@turtlevax.UUCP (Ken Turkowski) Distribution: net Organization: CIMLINC, Inc. @ Menlo Park, CA Lines: 19 Xref: watmath net.graphics:1616 net.math:3132 In article <1450@nlm-mcs.ARPA> garl@nlm-mcs.ARPA (Gary Letourneau) writes: > If given an equation of a 3-dimensional surface in the form > f(x, y, z) = ... > and a range of values for x, y, and z > x1 < x < x2, y1 < y < y2, z1 < z < z2 > is there an algorith for determining the parametric equations for the > same surface > fx(t) = ... , fy(t) = ... , fz(t) = ... , 0 <= t <= 1 First, you'll never get a full surface from a univariate function; you need two variables: fx(u,v), fy(u,v), fz(u,v), 0 <= u <= 1, 0 <= v <= 1 Otherwise, you'll get a curve instead of a surface. -- Ken Turkowski @ CIMLINC, Menlo Park, CA UUCP: {amd,decwrl,hplabs,seismo}!turtlevax!ken ARPA: turtlevax!ken@DECWRL.DEC.COM