隐式表面上的山脊和沟壑

A. Belyaev, A. Pasko, T. Kunii
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引用次数: 55

摘要

表面折痕为我们提供了关于物体形状的重要信息,可以直观地定义为表面上的曲线,表面沿着这些曲线急剧弯曲。我们对这种表面折痕的数学描述是基于对沿其曲率线的主曲率的极值的研究。在光滑的一般曲面上,我们将脊定义为沿其相关曲率线的最大主曲率的局部正最大值,将沟定义为沿其相关曲率线的最小主曲率的局部负最小值。山脊和沟壑是形状分析的重要组成部分,具有显著的数学性质。例如,它们对应于形状骨架的端点。本文导出了在隐式曲面上检测山脊和沟壑的公式。我们还提出了一种以两个隐式曲面的交点曲线求脊沟分段线性逼近的算法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Ridges and ravines on implicit surfaces
Surface creases provide us with important information about the shapes of objects and can be intuitively defined as curves on a surface along which the surface bends sharply. Our mathematical description of such surface creases is based on a study of extrema of the principal curvatures along their curvature lines. On a smooth generic surface we define ridges to be the local positive maxima of the maximal principal curvature along its associated curvature line and ravines to be the local negative minima of the minimal principal curvature along its associated curvature line. The ridges and ravines are important for shape analysis and possess remarkable mathematical properties. For example, they correspond to the end points of shape skeletons. In this paper we derive formulas to detect the ridges and ravines on a surface given in implicit form. We also propose an algorithm for obtaining piecewise linear approximation of ridges and ravines as intersection curves of two implicit surfaces.
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