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Curves and surfaces

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On the Problem of Plateau

Part of the book series: Ergebnisse der Mathematik und Ihrer Grenƶgebiete ((MATHE2,volume 2))

Abstract

If x = x(t), y = y(t), z = z(t), a≤ t ≤ b are the equations of a curve C, then under the usual classroom assumptions the length l(C) of C is given by the formula

$$l\left( C \right) = \int\limits_a^b {{{\left[ {{{\left( {\frac{{dx}}{{dt}}} \right)}^2} + {{\left( {\frac{{dy}}{{dt}}} \right)}^2} + {{\left({\frac{{dz}}{{dt}}} \right)}^2}} \right]}^{\frac{1}{2}}}dt.} $$
((1.1))

If C reduces to a straight segment of length /, then the formula (1.1) reduces to l = \(l = \left( {l_1^2 + l_2^2 + l_3^2} \right)\frac{1}{2}\) where l 1, l 2, l 3 denote the lengths of the orthogonal projections of the segment upon the axes x, y, z (the coordinate system will always be supposed to be rectangular). The formula (1.1) is equally evident geometrically if C is a polygon. It is then clear that for a general curve C the formula results by approximating C by polygons1. As a matter of fact, (1.1) follows immediately by approximating C by an inscribed polygon.

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References

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Radó, T. (1933). Curves and surfaces. In: On the Problem of Plateau. Ergebnisse der Mathematik und Ihrer Grenƶgebiete, vol 2. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-99118-9_2

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  • DOI: https://doi.org/10.1007/978-3-642-99118-9_2

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-98307-8

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