Analysis of the Influence of the Vertical Coaxiality of the Pillars on the Stability of the Resistance Structures, from the Ocnele Mari Saline

D. Marian, I. Onica, Ovidiu Marina
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Abstract

Abstract The Ocnele Mari rock salt deposit is exploited with small rooms and square pillars, on the horizons +226 m and 210 m. Following the exploitation of the lower horizon +210 m, the floor between the two horizons suffered instability phenomena, marked by fractures and cracks and local degradation of the pillars.Since the pillars at the two horizons have certain deviations from the coaxiality, the question was raised whether the instability phenomena were generated by the deviations from the coaxiality.This article presents the stability analysis of bearing structures, taking into account the actual geometry of pillars, 3D finite element analysis and analysis of safety factors at the ceiling level, calculated from 2D finite element models. The final conclusion is that the instability phenomena that occurred at the Ocnele Mari Saline were generated by the state of stresses and strains, produced by the spatial distribution of the underground voids and the geomechanical characteristics of the rock salt and insignificantly, by the deviation from the coaxiality of the pillars.
矿柱垂直同轴度对阻力结构稳定性的影响分析——以海星岩为例
Ocnele Mari岩盐矿床在+226 m和210 m的层位上以小室和方柱开采。在下一层+210 m开采后,两层之间的底板出现了不稳定现象,主要表现为裂缝和裂缝以及矿柱的局部退化。由于两个地平线上的矿柱有一定的同轴度偏差,因此提出了不稳定现象是否由偏离同轴度引起的问题。本文介绍了考虑柱的实际几何形状、三维有限元分析和顶板安全系数分析的承载结构的稳定性分析,采用二维有限元模型计算。最后得出结论:Ocnele Mari Saline发生的失稳现象主要由地下空洞的空间分布和岩盐的地质力学特征引起的应力应变状态引起,与矿柱同轴度的偏离无关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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