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Evaluation of a resistivity model derived from time-lapse well logging of a pilot-scale CO_2 injection site, Nagaoka, Japan

机译:来自日本长冈市中试规模CO_2注入地点随时间推移测井得到的电阻率模型的评估

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This paper presents a rock physics model describing the relationship between resistivity and CO_2 saturation at the Nagaoka CCS test site in Japan. 10.4 kt CO2 were injected at Nagaoka between July 2003 and January 2005, with repeated logging performed both during and after the injection period. The target reservoir at Nagaoka is shaly sandstone, in which the conductance of clay minerals has a significant effect on log resistivity. We analyzed open-hole log data in order to estimate shale volume anddistribution, and applied Waxman-Smits model to fit the data. For the known observables in the model we used the resistivity log and water saturation derived from the neutron log, with the saturation exponent and the correction value for shale conductionthen obtained using the time-lapse logging data. According to the modeled results, the area characterized by smaller saturation exponents corresponded to that with minor changes in resistivity. Dissolved CO_2 was also found to reduce the resistivity offormation water. Model modification taking this effect into account was thus carried out, although the essence of the original Waxman-Smits model was retained. The performed analyses provide evidences of successful residual and solubility trapping currently in progress at Nagaoka.
机译:本文提出了一个岩石物理学模型,描述了日本长冈CCS测试现场电阻率与CO_2饱和度之间的关系。 2003年7月至2005年1月,在长冈注入了10.4 kt CO2,在注入期间和注入之后都进行了重复测井。长冈的目标储层是泥质砂岩,其中粘土矿物的电导率对测井电阻率有重要影响。我们分析了裸眼测井数据以估算页岩的体积和分布,并应用Waxman-Smits模型拟合数据。对于模型中已知的可观测值,我们使用了电阻率测井和中子测井得到的水饱和度,并使用了随时间推移的测井数据获得了饱和指数和页岩传导的校正值。根据模型结果,以较小的饱和指数为特征的区域对应于电阻率的微小变化的区域。还发现溶解的CO_2降低了地层水的电阻率。因此,尽管保留了原始Waxman-Smits模型的本质,但还是考虑了这种影响进行了模型修改。进行的分析提供了长冈市目前成功进行的残留物和溶解度捕集的证据。

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