Page 192 - Schaum's Outline of Theory and Problems of Advanced Calculus
P. 192

Applications of Partial




                                                                 Derivatives













                     APPLICATIONS TO GEOMETRY
                        The theoretical study of curves and surfaces began
                     more than two thousand years ago when Greek phi-
                     losopher-mathematicians explored the properties of
                     conic sections, helixes, spirals, and surfaces of revolu-
                     tion generated from them.  While applications were
                     not on their minds, many practical consequences
                     evolved. These included representation of the ellipti-
                     cal paths of planets about the sun, employment of the
                     focal properties of paraboloids, and use of the special
                     properties of helixes to construct the double helical
                     model of DNA.
                        The analytic tool for studying functions of more
                     than one variable is the partial derivative. Surfaces are
                     a geometric starting point, since they are represented
                     by functions of two independent variables.  Vector
                     forms of many of these these concepts were introduced
                     in the previous chapter.  In this one, corresponding
                     coordinate equations are exhibited.                          Fig. 8-1

                     1.  Tangent Plane to a Surface.  Let Fðx; y; zÞ¼ 0be the equation of a surface S such as shown in
                     Fig. 8-1. We shall assume that F, and all other functions in this chapter, is continuously differentiable
                     unless otherwise indicated. Suppose we wish to find the equation of a tangent plane to S at the point
                     Pðx 0 ; y 0 ; z 0 Þ.  A vector normal to S at this point is N 0 ¼rFj , the subscript P indicating that the
                                                                         P
                     gradient is to be evaluated at the point Pðx 0 ; y 0 ; z 0 Þ.
                        If r 0 and r are the vectors drawn respectively from O to Pðx 0 ; y 0 ; z 0 Þ and Qðx; y; zÞ on the plane, the
                     equation of the plane is
                                                 ðr   r 0 Þ  N 0 ¼ðr   r 0 Þ rFj P ¼ 0               ð1Þ
                     since r   r 0 is perpendicular to N 0 .
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