Geophysical Measurements Performed at Targu Ocna Salt Mine to Evaluate Subsurface Homogeneity

A. Anghel, A. Badescu, Valentin Dedu, N. Rotar
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Abstract

This paper presents the results of an experimental campaign performed in a mine gallery from Targu Ocna salt mine (Bacau county, Romania) that aimed to assess the potential of various geophysical measurement methods to evaluate the homogeneity of salt layers. The test site contained two different subsurface layer structures: one that has a 7 m layer of rock salt followed by a cavity corresponding to the next exploitation level of the mine, and one that is formed only by solid layers. The specific purpose of the measurements was to emphasize the presence of this cavity. The investigations were performed using the following methods: ground-penetrating radar, electromagnetic ground conductivity analysis and seismic refraction. For each method we present the measurement configurations and the main results. The long term goal of the measurement campaign was to identify a reliable geophysical measurement technique that can be used as reference for future muon tomography-based measurements in salt mines or other types of soil/geological layers.
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Targu Ocna盐矿地下均匀性评价的地球物理测量
本文介绍了在Targu Ocna盐矿(罗马尼亚Bacau县)的一个矿库中进行的一项实验活动的结果,该实验旨在评估各种地球物理测量方法在评估盐层均匀性方面的潜力。试验场包含两种不同的地下层结构:一种是7米的岩盐层,后面是一个与矿山下一个开采水平相对应的空腔,另一种是只由固体层形成的。测量的具体目的是强调这个空洞的存在。利用探地雷达、电磁地面电导率分析和地震折射等方法进行了调查。对于每种方法,我们都给出了测量配置和主要结果。测量活动的长期目标是确定一种可靠的地球物理测量技术,可作为将来在盐矿或其他类型的土壤/地质层中基于介子层析成像的测量的参考。
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