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Estimating Strain and Stress in Oriented Rock Cores Using a Diametral Deviation Method

机译:使用径向偏差法估算定向岩心的应变和应力

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A practical core-based method for estimating in situ stress was tested using 360° measurements of rock core diameter in a laboratory setting. In several mining districts across West Virginia, rock cores were recovered from exploration core holes and oriented using an acoustic televiewer (ATV) summary log. Measurements of diametral variation were performed at 0.1-foot depth intervals using a benchtop device comprised of a pair of diametrically opposed contact digital indicator gauges working in tandem. The diametral profiles were evaluated to determine strain direction and strain magnitude. Stress magnitudes were calculated when values for Young's modulus, and Poisson's ratio were available. Stress direction results are compared to other stress determination methods, including downhole overcores, drilling-induced fractures, and borehole breakouts. The testing and analytical methods used are similar to the diametrical core deformation analysis (DCDA) method (lto, Funato, and Shono, 2012), but with a number of important improvements. The diametral deviation method presented here was found to be a practical working approach for characterizing the local in situ horizontal stress field, although aspects of it are still considered to be experimental.
机译:在实验室环境中使用岩心直径的360°测量测试了一种实用的基于岩心的现场应力估算方法。在整个西弗吉尼亚州的几个矿区,岩心是从勘探岩心孔中回收的,并使用声学电视(ATV)摘要日志进行定向。直径变化的测量是使用台式设备在0.1英尺深度间隔进行的,该台式设备由一对在直径上相对的接触式数字指示器共同工作。评估径向轮廓以确定应变方向和应变大小。当杨氏模量和泊松比值可用时,计算应力大小。将应力方向结果与其他应力确定方法(包括井下上岩心,钻井引起的裂缝和井眼破裂)进行比较。所使用的测试和分析方法类似于直径岩心变形分析(DCDA)方法(lto,Funato和Shono,2012年),但有许多重要的改进。发现这里提出的直径偏差方法是表征局部原位水平应力场的一种实用的工作方法,尽管它的某些方面仍被认为是实验性的。

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