Theoretical model of parameter r distribution in the layered rock mass

Eligiusz J?drzejec

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Theoretical model of parameter r distribution in the layered rock mass

机译：层状岩体中参数r分布的理论模型

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On the basis of analysis of subsidence transitivity in the Budryk-Knothe theory the independence of this theory feature from the selection of the function r(z,H) was shown. Attention was drawn to the existence of the transformation law, to which the parameter r is subject with the change of boundary condition location.The discussion of a particular case of function r(z,H) with invariant form in relation to this location was given. The possibility of subsidence description in the layered rock mass using the Budryk-Knothe theory and the way of parameter r calculation in this case were presented.

机译：在Budryk-Knothe理论中对沉降传递性进行分析的基础上，表明了该理论特征与函数r（z，H）的选择无关。提请注意变换定律的存在，参数r随边界条件位置的变化而变化。讨论了函数r（z，H）具有与该位置有关的不变形式的特殊情况。提出了使用Budryk-Knothe理论描述层状岩体中沉陷的可能性以及这种情况下参数r的计算方法。

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《Archives of mining sciences》 |2011年第1期|共22页
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Eligiusz J?drzejec;
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中图分类矿业工程;
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Theoretical model of parameter r distribution in the layered rock mass

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