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In situ rock stress measurement using an improved Downward Compact Conical-ended Borehole Overcoring technique

机译:使用改进的向下紧凑锥形端钻孔过芯技术进行原位岩石应力测量

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Rock stress was measured in situ by an improved Downward Compact Conical-ended Borehole Overcoring (DCCBO) technique, which is a type of overcoring method, at Kamaishi mine to further promote the practical use of this technique. Prior to in situ stress measurement, a measuring apparatus (special conical bit, strain cell installation tool and data-logger with a built-in tilt/azimuth sensor) for an HQ-size borehole was developed by improving the apparatus used for a PQ-size borehole.A measurement method based on the determination of strain coefficients depending on the estimated elastic properties of an adhesive under the temperature measured in situ was then proposed. Through the use of in situ tests, we verified that this improved measuring apparatus for a HQ-size borehole works well in a water-filled vertical borehole. Moreover, the proposed measurement method could estimate in situ stresses relatively consistent with those obtained by other measurement methods near this test site. The results show that in situ stresses measured by the proposed measurement method are sufficiently reliable.
机译:岩石应力是通过在Kamaishi矿井中使用一种改进的向下压紧锥形端钻孔过芯(DCCBO)技术现场测量的,该技术是一种过芯方法,旨在进一步促进该技术的实际应用。在现场应力测量之前,针对HQ尺寸的井眼开发了用于HQ尺寸井眼的测量设备(特殊的锥形钻头,应变盒安装工具和带有内置倾斜/方位角传感器的数据记录仪),提出了一种基于应变系数确定的测量方法,该方法取决于在现场测量的温度下粘合剂的估计弹性性能。通过现场测试,我们验证了这种改进的HQ尺寸测量仪器在充满水的垂直钻孔中能很好地工作。而且,提出的测量方法可以估计与在该测试地点附近通过其他测量方法获得的应力相对一致的原地应力。结果表明,通过所提出的测量方法测量的原位应力是足够可靠的。

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