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Measurements of electrical resistivity and seismic velocity of drill cores

机译:钻孔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:对于科学的深度钻探项目,如综合海洋钻井计划(IODP),基于核心的电阻率和地震速度的实验室测量对于在原位条件下估计岩石的物理性质并检查物理性质与物理性质之间的关系条件,因为物理性质的数据和关系是对地球物理探索的调查结果的解释,因为在钻孔中的广域和测井数据的地球物理探索的调查结果的解释。四种砂岩,三个牙龈和两个花岗岩的电阻率,在各种测量条件下测量Inada花岗岩和Tako砂岩的速度,例如体积水含量(孔隙水饱和度),孔隙水电阻率,限制压力,差动应力,高 - 温度等。结果表明,这些条件对物理性质的影响是不同的,不能被忽略。此外,我们强调必须考虑测量条件,以便在原位条件下正确估计岩石的物理性质。

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