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Measurements of electrical resistivity and seismic velocity of drill cores

机译:钻芯电阻率和地震速度的测量

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摘要

For scientific deep drilling projects such as the integrated ocean drilling program (IODP), core-based laboratory measurements of electrical resistivity and seismic velocity are important to estimate the physical properties of rocks under in-situ conditions and to examine relations between the physical properties and the conditions, because the data of physical properties and the relations are indispensable for the interpretations of survey results of geophysical explorations on a wide area and logging data in boreholes. The resistivity of four sandstones, three tuffs and two granites, the velocities of Inada granite and Tako sandstone were measured under various measurement conditions such as volumetric water content (saturation degree of pore water), pore water resistivity, confining pressure, differential stress, high-temperature etc. The results showed that the effects of these conditions on the physical properties were distinct and cannot be neglected. In addition, we emphasize that measurement conditions must be taken into consideration for the correct estimation of physical properties of rocks under in-situ conditions.
机译:对于诸如综合海洋钻探计划(IODP)之类的科学深度钻探项目,基于岩心的电阻率和地震速度实验室测量对于估算原位条件下岩石的物理特性以及检查物理特性与强度之间的关系非常重要。这些条件是因为物理性质和关系的数据对于解释大范围地球物理勘探的测量结果和钻孔测井数据是必不可少的。在体积水分含量(孔隙水饱和度),孔隙水电阻率,围压,微分应力,高应力等不同的测量条件下,测量了四种砂岩,三种凝灰岩和两种花岗岩的电阻率,稻田花岗岩和Tako砂岩的速度。结果表明,这些条件对物理性能的影响是明显的,不能忽略。此外,我们强调必须正确考虑测量条件,才能正确估算原位条件下岩石的物理性质。

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