Le Ngoc Son, Nguyen The Duc, Sumihiko Murata, Phan Ngoc Trung
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Several other reparameterization techniques have attempted to preserve geological consistency by incorporating 4D seismic data; however, these techniques cannot be applied to our fractured basement reservoirs (FBRs) as they do not have 4D seismic data. Taking into account these challenges, in this study, an AHM methodology and workflow have been developed using a new reparameterization technique. This approach attempts to minimize the potential for geological nonconsistency of the calibrated results by linking the permeability to geophysical data. The proposed methodology can be applied to fields with only traditional geophysical data (3D seismic and conventional well logs). In the proposed workflow, the spatial distributions of seismic attributes and geomechanical properties were calculated and estimated from 3D seismic data and well logs, respectively. After that, a feed-forward artificial neural network (ANN) model trained by the back-propagation algorithm of the relationship between initial permeability with seismic attributes and geomechanical properties of their grid cell values is developed. Then, the calibration of the permeability distribution is performed by adjustment of the ANN model. Modification of the ANN model is performed using the simultaneous perturbation stochastic approximation (SPSA) algorithm to calibrate transmission coefficients in the ANN model to minimize the discrepancy between the simulated results and observed data. The developed methodology is applied to calibrate the permeability distribution of a simulation model of Bach Ho FBR in Vietnam. The effectiveness of the methodology is evident by comparing the historical matches with an available manually history-matched simulation model. 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引用次数: 0
摘要
许多学者研究了开发自动历史匹配(AHM)方法,以取代传统的手动历史匹配(MHM)方法来调整储层模拟模型的渗透率分布。由于在典型的储层模拟模型中,需要对成百上千个网格单元的渗透率值进行评估,因此有必要采用重新参数化技术,以便用更少的变量实现优化算法。在基本的重新参数化技术(包括分区法和先导点法)中,校准通常仅基于生产数据,与地质和地球物理数据没有系统的联系,因此得到的渗透率分布可能与地质不一致。其他一些重新参数化技术试图通过结合四维地震数据来保持地质一致性;然而,这些技术无法应用于我们的断裂基底储层(FBRs),因为它们没有四维地震数据。考虑到这些挑战,本研究采用一种新的重新参数化技术,开发了一种 AHM 方法和工作流程。这种方法试图通过将渗透率与地球物理数据联系起来,将校准结果的地质不一致性降至最低。建议的方法可应用于只有传统地球物理数据(三维地震和常规测井)的油田。在建议的工作流程中,地震属性和地质力学属性的空间分布分别由三维地震数据和测井记录计算和估算。然后,根据初始渗透率与地震属性及其网格单元值的地质力学属性之间的关系,建立一个由反向传播算法训练的前馈人工神经网络(ANN)模型。然后,通过调整 ANN 模型对渗透率分布进行校准。利用同步扰动随机近似(SPSA)算法对 ANN 模型进行修改,以校准 ANN 模型中的传输系数,从而最大限度地减少模拟结果与观测数据之间的差异。所开发的方法被用于校准越南 Bach Ho FBR 模拟模型的渗透率分布。通过将历史匹配结果与现有的人工历史匹配模拟模型进行比较,可以明显看出该方法的有效性。应用结果表明,所提出的方法可被视为调整 FBR 储层模拟模型渗透率分布的一种合适的实用方法。
Automatic History Matching for Adjusting Permeability Field of Fractured Basement Reservoir Simulation Model Using Seismic, Well Log, and Production Data
Developing automatic history matching (AHM) methods to replace the traditional manual history matching (MHM) approach in adjusting the permeability distribution of the reservoir simulation model has been studied by many authors. Because permeability values need to be evaluated at hundreds of thousands of grid cells in a typical reservoir simulation model, it is necessary to apply a reparameterization technique to allow the optimization algorithms to be implemented with fewer variables. In basic reparameterization techniques including zonation and pilot point methods, the calibrations are usually based solely on the production data with no systematic link to the geological and geophysical data, and therefore, the obtained permeability distribution may be not geologically consistent. Several other reparameterization techniques have attempted to preserve geological consistency by incorporating 4D seismic data; however, these techniques cannot be applied to our fractured basement reservoirs (FBRs) as they do not have 4D seismic data. Taking into account these challenges, in this study, an AHM methodology and workflow have been developed using a new reparameterization technique. This approach attempts to minimize the potential for geological nonconsistency of the calibrated results by linking the permeability to geophysical data. The proposed methodology can be applied to fields with only traditional geophysical data (3D seismic and conventional well logs). In the proposed workflow, the spatial distributions of seismic attributes and geomechanical properties were calculated and estimated from 3D seismic data and well logs, respectively. After that, a feed-forward artificial neural network (ANN) model trained by the back-propagation algorithm of the relationship between initial permeability with seismic attributes and geomechanical properties of their grid cell values is developed. Then, the calibration of the permeability distribution is performed by adjustment of the ANN model. Modification of the ANN model is performed using the simultaneous perturbation stochastic approximation (SPSA) algorithm to calibrate transmission coefficients in the ANN model to minimize the discrepancy between the simulated results and observed data. The developed methodology is applied to calibrate the permeability distribution of a simulation model of Bach Ho FBR in Vietnam. The effectiveness of the methodology is evident by comparing the historical matches with an available manually history-matched simulation model. The application shows that the proposed methodology could be considered as a suitable practical approach for adjusting the permeability distribution for FBR reservoir simulation models.
期刊介绍:
Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines.
Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.