地对井电磁热采监测数值模拟

Brian R Spies , Robert J Greaves
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引用次数: 11

摘要

电导率是预测油藏岩性和流体含量的重要岩石物理性质。原则上,当源或接收器(或两者)位于井中时,可以使用电或电磁(EM)技术绘制井间电导率分布。不幸的是,这些方法的分辨率相对较差。然而,在监测应用中,在不同时间记录动态储层过程的响应并进行比较,分辨率得到了提高。此类动态过程的例子包括一次生产中的流体替换、二次采收率和提高采收率(EOR)技术,如火驱、蒸汽驱和二氧化碳驱。这种测量可以用目前地球物理行业内可用的技术进行,而且成本相对较低。为了验证电磁监测推进火洪过程的可行性,对霍尔特砂土原位燃烧提高采收率实验进行了数值模型研究。通过燃烧前和燃烧后的测井数据获得了燃烧带的电阻率和几何形状。研究表明,地对井电磁法可以从最远100米的燃烧油藏层位电阻率变化中探测到清晰的特征。类似的结论也适用于蒸汽驱过程。使热采收率过程的电磁监测解释复杂化的一个重要现象是,由于热量传导到边界页岩中,在储层附近有一个电阻率降低的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical modeling of surface-to-borehole electromagnetic surveys for monitoring thermal enhanced oil recovery

Electrical conductivity is an important petrophysical property used to predict lithology and fluid content in petroleum reservoirs. Conductivity distribution between wells can, in principle, be mapped with electrical or electromagnetic (EM) techniques when sources or receivers (or both) are located in the wells. Unfortunately, the resolution of these methods is relatively poor. Resolution is improved, however, in monitoring applications where the response of a dynamic reservoir process is recorded at different times and compared. Examples of such dynamic processes are fluid replacement during primary production, secondary recovery, and enhanced oil recovery (EOR) techniques as fireflooding, steamflooding, and CO2 flooding. Such measurements can be made with technology currently available within the geophysical industry and at relatively low expense.

A numerical model study of the Holt Sand in situ combustion EOR experiment was conducted to test the feasibility of electromagnetically monitoring the progress of the advancing fire flood. The resistivity and geometry of the burn zone was obtained from pre-burn and post-burn well log data. The study shows that the surface-to-borehole electromagnetic method detects a clear signature from changes in resistivity of the burned reservoir horizon from distances as great as 100 m. Similar conclusions hold for steam flood processes. An important phenomenon which complicates interpretation of EM monitoring of thermal EOR processes is a zone of decreased resistivity adjacent to the reservoir horizon caused by conduction of heat into the bounding shales.

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