分形维数确定方法中的边界计算

Sh. A. Anarova, Saidkulov Elyor Abdullaevich
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摘要

本文介绍了自然界中的分形及其特征,并对分形维数提出了自己的看法。说明了分形几何形状的地球物理起源现象和描述复杂形状的潜在有用工具。尽管如此,分形被广泛应用于地理区域;对不同分形计算算法导致结果不一致的观点进行了阐述。分形维数最初是作为描述几何复杂形状的系数引入的,它被认为细节比绘制完整的图形更重要。描述简单几何形状的集合的理论分形维数等于通常的欧几里得维数或拓扑维数。描述点的集合的理论分形维数为0,描述只有长度的直线的集合的理论分形维数为1,描述曲面的集合的理论分形维数为2,描述体积的集合的理论分形维数为3。
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Calculating Boundaries in Methods of Determination of Fractal Dimension
The fractal shapes in the nature, their characteristics, also, opinions about fractal dimension are given in this article. The phenomena of geophysical origin of fractal geometric shapes and potential useful tools for describing complex shapes are illustrated. Despite, the fractals are widely used in geographical areas; the opinions which cause inconsistent results from different fractal computational algorithms have been expressed.Fractal dimension was firstly introduced as the coefficient which describes geometrically complex shapes, the details are considered more important than a completely drawen picture. The theoretical fractal dimension for sets which describes simple geometric shapes is equal to the usual Euclidean or topological dimension. The theoretical fractal dimension for sets which describe points, is equal to 0, the fractal dimension for sets which describe straight line with only length, is equal to 1, the fractal dimension for sets which describe surface, is equal to 2, and the fractal dimension for sets which describe volume, is equal to 3.
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