维多利亚和坎塔库西诺矿地表变形监测与预报

I. Onica, D. Marian, Ovidiu Marina
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引用次数: 0

摘要

斯利奇尼克岩盐矿床的地下开采始于1665年,有老矿,1970年有维多利亚矿,1993年有坎塔库津诺矿。Victoria和Cantacuzino矿场采用的采矿方法是小房间和方形柱子,开采了970多万立方米的岩盐。这一巨大的地下开采空洞量导致地下开挖的收敛,从而导致地表的变形。本文对地表位移的测量结果进行了分析,并对其随时间的沉降进行了预测。分析了造成地表变形的主要因素,即地下空洞的尺寸、开采深度、地质力学特征、矿床的构造和微构造、水文地质和爆破作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Monitoring and Forecasting of Surface Deformation at Victoria and Cantacuzino Mines
Abstract The underground mining of the rock salt deposit from Slănic started in 1665, with the Old Mines and continued in 1970, with Victoria Mine, then in 1993, with Cantacuzino Mine. The mining method applied at Victoria and Cantacuzino mines was the one with small rooms and square pillars, with which over 9.7 million m3 of rock salt were extracted. This very large volume of underground mining voids led to the convergence of the underground excavations and thus to the deformation of the surface. This article presents the analysis of the measurements of surface displacement and the prediction of its subsidence over time. Also, the main factors that contributed to the deformation of the surface are analyzed, namely: the dimensions of the underground voids, the mining depth, the geomechanical characteristics, the tectonics and microtectonics of the deposit, the hydrogeology and the effect of blasting.
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