Monitoring Water Flood Front Movement by Propagating High Frequency Pulses Through Subsurface Transmission Lines

J. M. Felix Servin
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引用次数: 2

Abstract

This manuscript describes a novel approach to monitor water flood front movement using Proximity Sensing in conjunction with contrast agents. Our technique exploits the presence of resistive layers between reservoirs, which act as a transmission line for electromagnetic signals, to achieve increased propagation range. This work focuses on numerical simulations to evaluate the potential of this approach to monitor water movement in the reservoir under different conditions. A series of 2D axisymmetric numerical simulations were conducted to assess the potential of Proximity Sensing to monitor moving fronts of labeled brine as well as to detect isolated pockets of brine labeled with contrast agents. The study was conducted using layered models that resemble a resistive seal bounded by reservoirs saturated with brine or brine and contrast agents. The effect of magnetic permeability (μ) on signal travel time and amplitude is reported and compared to the effect of electric permittivity (ε). The results show that Proximity Sensing is a suitable technique to detect changes in the μ of reservoirs adjacent to resistive seals. Therefore, our approach can be used in combination with contrast agents, such as Magnetic NanoMappers, to monitor water flood front movement in the reservoir. In addition, this technique can be used to detect isolated pockets of labeled brine, which suggests that injection of slugs of labeled water would be enough for field applications. The observed effect of μ on signal travel time is similar to the trend observed when the electric permittivity of the bounding reservoirs is changed. A significant difference is that increasing μ of the bounding reservoirs appears to reduce signal amplitude while increasing ε has the opposite effect. This result was unexpected and requires further simulations and experimentation to validate this behavior. Proximity Sensing offers a novel approach to address the challenge of electromagnetic propagation in conductive media and paves the way for the development of refined techniques that provide reservoir saturation and water flood front monitoring capabilities with greater resolution.
通过地下传输线传播高频脉冲监测洪水锋面运动
这篇手稿描述了一种新的方法来监测水洪水前沿运动使用接近感测结合造影剂。我们的技术利用储层之间的电阻层,作为电磁信号的传输线,以增加传播范围。本文主要通过数值模拟来评估该方法在不同条件下监测水库水运动的潜力。研究人员进行了一系列二维轴对称数值模拟,以评估近距离传感技术在监测标记盐水移动锋面以及检测用造影剂标记的盐水孤立袋方面的潜力。该研究采用层状模型,类似于由饱和盐水或盐水和对比剂包围的储层的电阻密封。报道了磁导率(μ)对信号走时和幅值的影响,并与介电常数(ε)的影响进行了比较。结果表明,近距离传感技术是一种适合探测邻近阻性密封的储层μ变化的技术。因此,我们的方法可以与造影剂(如磁性纳米地图)结合使用,以监测储层中的水驱锋面运动。此外,该技术可用于检测标记盐水的孤立袋,这表明注入标记水段塞足以用于现场应用。μ对信号走时的影响与边界储层介电常数变化时的趋势相似。显著不同的是,增加边界储层的μ会降低信号幅度,而增加ε则会降低信号幅度。这个结果是出乎意料的,需要进一步的模拟和实验来验证这种行为。近距离传感技术为解决电磁在导电介质中传播的挑战提供了一种新方法,并为开发更精细的技术铺平了道路,从而提供更高分辨率的油藏饱和度和水洪前沿监测能力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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