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基于三维激光扫描仪的岩石破裂面粗糙度研究 被引量:2
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作者 王学宁 闫帅 +2 位作者 宋远霸 张涛 徐博彪 《煤矿安全》 CAS 北大核心 2019年第1期62-66,共5页
为更深层地认识岩石的破裂机制。通过压、剪试验测取2组24个圆柱形岩样的破坏载荷,采用高精度三维激光扫描仪扫描岩样破裂面,得到了顶板砂岩在压、剪破坏后,破裂面的起伏粗糙特征分布规律,并采用统计分析方法得到破裂面粗糙曲线曲率半径... 为更深层地认识岩石的破裂机制。通过压、剪试验测取2组24个圆柱形岩样的破坏载荷,采用高精度三维激光扫描仪扫描岩样破裂面,得到了顶板砂岩在压、剪破坏后,破裂面的起伏粗糙特征分布规律,并采用统计分析方法得到破裂面粗糙曲线曲率半径,从而揭示了砂岩受剪切破坏后粗糙曲线曲率半径分别与粗糙度系数JRC、破坏载荷的相关关系。结果表明:单轴抗压试验中,离加载中心越远,JRC越小;抗剪试验中,粗糙度曲线的曲率半径统计值分别与JRC和抗剪强度呈线性正相关。 展开更多
关键词 三维激光扫描仪 剪切强度 岩石破裂面 粗糙度曲线 曲率半径
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岩石破裂面的摩擦特性研究
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作者 袁果 胡江春 《矿冶工程》 CAS CSCD 北大核心 2010年第2期25-27,共3页
研究了自然状态和接触面掺泥两种情况下的砂岩、泥岩破裂面及其互层接触的摩擦特性。结果表明,在自然状态下,砂岩、泥岩的接触面的力-位移曲线具有相同形态,都能很快达到峰值强度;当接触面掺泥时,砂岩和泥岩的粘聚力和内摩擦角都有不同... 研究了自然状态和接触面掺泥两种情况下的砂岩、泥岩破裂面及其互层接触的摩擦特性。结果表明,在自然状态下,砂岩、泥岩的接触面的力-位移曲线具有相同形态,都能很快达到峰值强度;当接触面掺泥时,砂岩和泥岩的粘聚力和内摩擦角都有不同程度的降低,其中粘聚力下降尤其明显,与自然状态下相比,其剪切应力和摩擦位移关系曲线发生了变化,剪应力与摩擦位移关系曲线也有不同,但是粘滑现象明显渐弱。 展开更多
关键词 岩石破裂面 摩擦性能 强度指标
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Time difference correlation between earthquake lights and seismic ground accelerations
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作者 Juan Antonio Lira Maurizio Mulas 《Applied Geophysics》 SCIE CSCD 2021年第1期9-16,128,共9页
Although earthquake lights have been known since ancient times,it has not been easy to study them.It was not until the 60s that the first photographs of them were taken.During the Peruvian earthquake in 2007,it was po... Although earthquake lights have been known since ancient times,it has not been easy to study them.It was not until the 60s that the first photographs of them were taken.During the Peruvian earthquake in 2007,it was possible to obtain the fi rst fi lm recording on earthquake lights.Likewise,during the earthquakes in Ecuador in 2016 and in Mexico in 2017,two fi lms of the earthquake lights were recorded.These fi lm recordings have helped in the study of earthquake lights,both for their objectivity and for their informational content.Several causal mechanisms have been proposed to explain earthquake lights:piezoelectricity,radon emanation,fluid diffusion,friction-vaporization,positive holes and dipole currents,among others.In this work a time difference correlation between earthquake lights and seismic ground accelerations was found and we use both seismic data and fi lm recordings of earthquake lights to explain its origin.In the discussion section it is suggested that fracturing of rocks manifest itself to some extent in the form of static electricity producing earthquake lights through induction The induction model proposed is new and it can explain the formation of EQL,even if the earth’s crust has layers of large electrical resistivity.The model also explains the formation of seismic lights without the need for special conditions on the earth’s surface or in the atmosphere.A better understanding of the earthquake lights generation process can improve our understanding of seismicity and help in the prediction of earthquakes. 展开更多
关键词 time diff erence correlation earthquake lights seismic ground accelerations rock fracturing
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