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A method for controlling stress-strain state of rocks

机译:一种控制岩石应力应变状态的方法

摘要

A method for controlling the stress-strain state of rock, comprising measuring radiation in the interior of the rock, characterized in that continuous measurement of residual gamma background in low background chambers consisting of layers of metals and / or liquid absorbing external natural radioactive radiation and placed on Earth's surface, variations in the obtained gamma-ray background is isolated anomalies DSA method of Fourier analysis and at their presence analyzed daily averages gamma background network with nizkofon ovyh sensors and their relative change in the detector count rate determine the time and place of stress-deformed state of the rock.
机译:一种用于控制岩石的应力-应变状态的方法,包括测量岩石内部的辐射,其特征在于,在低本底腔室中连续测量残留伽马本底,该本底腔室由金属层和/或吸收外部自然放射性辐射的液体组成放置在地球表面上的伽马射线背景中的变化是孤立的异常DSA傅里叶分析方法,在存在的情况下,使用nizkofon ovyh传感器分析的每日平均伽马背景网络及其在探测器计数率中的相对变化确定了时间和地点。岩石的应力变形状态。

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