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Characterization of Reservoir Heterogeneity Through Fluid Movement Monitoring With Deep Electromagnetic and Pressure Measurements

机译:通过深电磁和压力测量流体运动监测来表征储层非均质性

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This paper presents a novel technique to characterize detailed formation heterogeneity for a carbonate reservoir using measurements from electrode resistivity array (ERA), a wireline formation tester, and a permanent downhole pressure sensor. The ERA was installed on tubing in a barefoot well rather than permanently cemented outside the casing as in previous applications. This notable difference provided flexibility for device installation and operation but also introduced particular issues in the ERA data acquisition and interpretation. Furthermore, the ERA measurements were carried out in conjunction with low-salinity water injection and oil and water production in the same well. The primary finding presented in this paper is that the time-lapse ERA voltages near a source electrode showed unique characteristics that represented local formation heterogeneity. This localized sensitivity of ERA data allows detailed characterization of the formation heterogeneity within the length of the ERA string in the vertical direction and about 100 ft laterally around the wellbore. The scale size of the investigated formation heterogeneity is comparable to typical grid sizes used in current reservoir simulations. Models were developed to identify stratified permeability heterogeneities from the time-lapse ERA voltages. The stratified heterogeneity estimated from the ERA measurements was compared to and verified by openhole logs and core analyses data. The final heterogeneous reservoir model from the ERA was subsequently applied to a numerical simulation that integrated the dynamic fluid flow, salt transport, and electrode array responses for monitoring water-front movement and estimating multiphase formation properties. The history matching of the time-lapse ERA data confirmed the first pass estimates of the identified heterogeneities.
机译:本文提出了一种新技术,可利用电极电阻率阵列(ERA),电缆地层测试仪和永久性井下压力传感器的测量来表征碳酸盐岩储层的详细地层非均质性。 ERA安装在赤脚井的油管上,而不是像以前的应用一样永久地胶粘在套管外。这一显着差异为设备安装和操作提供了灵活性,但同时也带来了ERA数据采集和解释中的特殊问题。此外,ERA测量是在同一口井中结合低盐度注水以及油和水生产进行的。本文提出的主要发现是源电极附近的延时ERA电压表现出独特的特性,代表局部形成异质性。 ERA数据的这种局部敏感性允许对ERA柱长度范围内的垂直方向和井眼周围约100 ft的地层非均质性进行详细描述。研究的地层非均质性的尺度大小可与当前储层模拟中使用的典型网格大小相媲美。开发了一些模型,以从延时ERA电压中识别分层的渗透率异质性。通过ERA测量估算出的分层异质性与裸眼测井和岩心分析数据进行了比较和验证。随后将来自ERA的最终非均质储层模型应用于数值模拟,该数值模拟将动态流体流动,盐分传输和电极阵列响应集成在一起,以监控水边运动并估算多相地层性质。延时ERA数据的历史记录匹配确认了所识别异质性的首次通过估计。

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