Three-axis borehole gravity monitoring for CO2 storage using machine learning coupled to fluid flow simulator

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geophysical Prospecting Pub Date : 2023-08-13 DOI:10.1111/1365-2478.13413
Taqi Alyousuf, Yaoguo Li, Richard Krahenbuhl, Dario Grana
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Abstract

The field of geophysics faces the daunting task of monitoring complex reservoir dynamics and imaging carbon dioxide storage up to several decades into the future. This presents numerous challenges, including sensitivity to parameter changes, resolution of obtained results and the cost of long-term deployment. To effectively store CO2 subsurface, it is necessary to monitor and account for the injected CO2. The gravity method provides several advantages for CO2 monitoring, as changes in fluid saturation correspond directly and uniquely to observed density changes. Three-axis borehole gravity has demonstrated significant promise as a next-generation tool for reliably monitoring reservoir dynamics across a range of depths and sizes. However, the gravity inverse problem is highly ill-posed, necessitating regularization that incorporates prior knowledge. To address this issue, we propose using a feed-forward neural network, a machine learning method, to invert time-lapse three-axis borehole gravity data and monitor CO2 movement within a reservoir. By training the neural network on models that analyse changes in density and corresponding gravity responses resulting from perturbations made to the reservoir model, we can create scenarios that train the algorithm to identify unexpected CO2 migration in addition to the normal movement of CO2. Our method is demonstrated using reservoir models for the Johansen formation in offshore Norway. We convert reservoir saturation models into density changes and generate their corresponding three-axis gravity data in a set of boreholes. Our results show that the developed machine learning inversion algorithm has high reliability and resolution for imaging density change associated with CO2 plumes, as demonstrated in the Johansen reservoir models utilized by the simulator. We also investigate machine learning inversion using regularization parameters and show that it is robust, with a strong tolerance for higher levels of noise. Our study demonstrates that the developed machine learning algorithm is a powerful tool for inverting three-axis borehole gravity data and monitoring the migration and long-term storage of injected CO2.

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利用机器学习与流体流动模拟器相结合的三轴井眼重力监测co2储存
地球物理学领域面临着在未来几十年内监测复杂储层动力学和成像二氧化碳储存的艰巨任务。这带来了许多挑战,包括对参数变化的敏感性、获得结果的分辨率以及长期部署的成本。为了有效地在地下储存二氧化碳,有必要监测和说明注入的二氧化碳。重力法为CO2监测提供了几个优点,因为流体饱和度的变化与观测到的密度变化直接且唯一地对应。三轴井眼重力已被证明是下一代可靠监测各种深度和尺寸储层动态的工具。然而,重力反问题是高度不适定的,需要结合先验知识的正则化。为了解决这个问题,我们建议使用前馈神经网络,一种机器学习(ML)方法,来反演时移三轴钻孔重力数据,并监测储层内的二氧化碳运动。通过在分析储层模型扰动引起的密度变化和相应重力响应的模型上训练神经网络,我们可以创建训练算法的场景,以识别除CO2正常移动外的意外CO2迁移。使用挪威近海Johansen组的储层模型证明了我们的方法。我们将储层饱和度模型转换为密度变化,并在一组钻孔中生成相应的三轴重力数据。我们的结果表明,如模拟器使用的Johansen储层模型所示,所开发的ML反演算法对与CO2羽流相关的密度变化成像具有较高的可靠性和分辨率。我们还研究了使用正则化参数的ML反演,并表明它是稳健的,对更高级别的噪声具有很强的容忍度。我们的研究表明,所开发的ML算法是反演三轴钻孔重力数据、监测注入二氧化碳迁移和长期储存的强大工具。本文受版权保护。保留所有权利
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
期刊介绍: Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.
期刊最新文献
Issue Information Simultaneous inversion of four physical parameters of hydrate reservoir for high accuracy porosity estimation A mollifier approach to seismic data representation Analytic solutions for effective elastic moduli of isotropic solids containing oblate spheroid pores with critical porosity An efficient pseudoelastic pure P-mode wave equation and the implementation of the free surface boundary condition
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