| 节理岩体分形描述 |
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| 引用本文： | 黄国明,黄润秋.节理岩体分形描述[J].中国煤田地质,1998,10(3):45-48. |
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| 作者姓名： | 黄国明 黄润秋 |
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| 作者单位： | 成都理工学院 |
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| 摘 要： | 研究了岩体节理产状、迹长、间距和节理数目对岩体节理网络分维的影响和节理几何参数的分维特征。结果表明，随节理发育方向、迹长、间距和节理数目的变化，岩体节理网络分维发生变化，节理间距和迹长的空间分布具有较好的分维特性，岩体节理网络分维可以作为岩体节理几何特征的定量描述指标。
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| 关 键 词： | 节理岩体 分形 描述 |
FRACTAL DISCRIPTION OF JOINTED ROCK MASS |
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| Huang Huoming Huang Runqiu.FRACTAL DISCRIPTION OF JOINTED ROCK MASS[J].Coal Geology of China,1998,10(3):45-48. |
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| Authors: | Huang Huoming Huang Runqiu |
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| Abstract: | The influences on fractal of jointed rock mass induced by orientation,trace length,spacing and number of discontinuities and fractal features of joint geometrical parameter are studied in this paper.It shows that the variation of jointde rock mass fractal is induced by orientation,trace length,spacing and number of discontinuities.The spatial distrbutions of trace length and spacing of discontinuities have better fractal features,whose fractal can be used as a quantative index for discribing geometry character of jointed rock mass. |
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| Keywords: | jointed mass fractal discrption |
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