首页> 外文会议>International Symposium of the Society of Core Analysts >A NEW APPROACH TO CORRECT FOR ROCK CONDUCTIVITY IN CONJUNCTION WITH CORE PLUG RESISTIVITY MEASUREMENT AND INTERPRETATION OF RESISTIVITY LOGS
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A NEW APPROACH TO CORRECT FOR ROCK CONDUCTIVITY IN CONJUNCTION WITH CORE PLUG RESISTIVITY MEASUREMENT AND INTERPRETATION OF RESISTIVITY LOGS

机译:一种新的岩石电导率与核心插头电阻率测量和电阻率日志的解释来校正岩石电导率的新方法

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An empirical equation has been developed to correct resistivity data from core plugs and logs. A combination of rock conductivity dependent on water salinity, conductivity as a result of the interaction between cations in brine and shale, and conductivity of the rock itself may occur in reservoir sediments. The commonly used Waxman and Smits equation incorporates a rock conductivity which is result of the cation exchange between the brine and the rock, i. e. the clay portion of the rock matrix. A new model has been established by introducing the possibility of the rock itself to conduct electrical current, combined with the Waxman and Smits model. For reservoir rocks with high matrix conductivity, it is shown that the conventional Waxman and Smits correction indicates abnormally high water saturation in oil zones. The introduction of this new concept has proved its usefulness in a case study. The study presents resistivity data of core plugs from porous plate drainage including multiple salinity measurements (C_OC_W). The saturation n-exponents have been corrected to values applicable for log interpretation. Secondary log evaluation, using the new method for resistivity correction, show a increase in net-pay for the reservoir.
机译:已经开发了一种经验方程来校正来自核心插头和日志的电阻率数据。岩土传导率的组合依赖于水盐度,导电性作为盐水和页岩中的阳离子之间的相互作用以及岩石本身的电导率可能发生在储层沉积物中。常用的蜡烛和Smits方程包含岩石电导率,这是盐水和岩石之间的阳离子交换的结果。 e。岩石基质的粘土部分。通过引入岩石本身进行电流的可能性,结合蜡烛和SMITS模型来建立一个新的模型。对于具有高矩阵电导率的储库岩石,示出了传统的蜡烛和SMITS校正表明油区中的异常饱和度异常高。在案例研究中证明了这一新概念的引入证明了其有用性。该研究呈现来自多孔板排水的芯塞的电阻率数据,包括多个盐度测量(C_OC_W)。饱和N-指数已经校正为适用于日志解释的值。二级日志评估,使用新方法进行电阻率校正,显示储层的Net-Pay增加。

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