陈枫, 孙宗颀. 1998: 岩体不连续间距数学模型的一个修正函数. 工程地质学报, 6(2): 150-154.
    引用本文: 陈枫, 孙宗颀. 1998: 岩体不连续间距数学模型的一个修正函数. 工程地质学报, 6(2): 150-154.
    Chen Feng, Sun Zonqi. 1998: A FUNCTION FOR MODIFYING MATHEMATICAL MODEL OF ROCK DISCONTINUITY SPACING. JOURNAL OF ENGINEERING GEOLOGY, 6(2): 150-154.
    Citation: Chen Feng, Sun Zonqi. 1998: A FUNCTION FOR MODIFYING MATHEMATICAL MODEL OF ROCK DISCONTINUITY SPACING. JOURNAL OF ENGINEERING GEOLOGY, 6(2): 150-154.

    岩体不连续间距数学模型的一个修正函数

    A FUNCTION FOR MODIFYING MATHEMATICAL MODEL OF ROCK DISCONTINUITY SPACING

    • 摘要: 不连续间距对岩体性质具有十分重要的意义。基于无限长测量线得到的岩体不连续间距的负幂指数分布是最重要的一种概率分布密度, 为纠正因用有限长测量线而带来的不连续间距的分布误差, 本文提出了一个封闭形式的修正函数。结果表明, 该法可显著减少不连续间距的相对误差, 从而可以采用较短的测量线来测量岩体的不连续间距。

       

      Abstract: iscontinuity spacing in rockmass is very important for prediction of rock behaviour. The negative exponential probability distribution density of rock discontinuity spacing based on infinite length scanline measurement is the most important distribution function. A closed form function is proposed for correction of sampling base caused by finite length scanline in this paper. The result shows that the suggested method is quite effective in decreasing relative error percentage, this makes it possible to estimate discontinuity spacing of rockmase using short scanline. It is also of great importance for decreasing the measurement cost.

       

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