非均质气砂岩储层渗透率神经网络预测。第九届中东地球科学会议,2010。

G. Hamada
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引用次数: 0

摘要

非均质气砂岩储层分析是油气勘探中的难点问题之一。这些储层通常由不同渗透率和复杂地层的多层组成,通常通过自然压裂来提高储层的渗透率。因此,使用新的测井技术,如核磁共振(NMR)或核磁共振与常规裸眼测井的结合,以及开发新的解释方法,对于改善储层表征至关重要。核磁共振测井不同于传统的中子、密度、声波和电阻率测井,因为核磁共振测量主要提供与岩性无关的详细孔隙度,并能很好地评估油气潜力。核磁共振测井也可以用来确定地层渗透率和毛管压力。本研究的重点是利用核磁共振测井参数估算渗透率。利用核磁共振计算渗透率的模型有Kenyon模型、coats - timer模型和Bulk Gas Magnetic Resonance模型。根据储层物性的不同,这些模型各有优缺点。本文讨论了由大体积气体磁共振模型推导出的渗透率,并引入神经网络模型,利用核磁共振和其他裸眼测井数据推导出地层渗透率。通过研究井的岩心渗透率验证了神经网络模型和其他模型的渗透率结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neural permeability prediction of heterogeneous gas sand reservoirs. 9th Middle East Geosciences Conference, GEO 2010.
Analysis of heterogeneous gas sand reservoirs is one of the most difficult problems. These reservoirs are usually produced from multiple layers with different permeability and complex formation, which is often enhanced by natural fracturing. Therefore, using new well logging techniques like nuclear magnetic resonance (NMR) or a combination of NMR and conventional open-hole logs, as well as developing new interpretation methodologies are essential for improved reservoir characterization. NMR logs differ from conventional neutron, density, sonic and resistivity logs because the NMR measurements provide mainly lithology-independent detailed porosity and offer a good evaluation of the hydrocarbon potential. NMR logs can also be used to determine formation permeability and capillary pressure. This study concentrates on permeability estimation from NMR logging parameters. Three models used to derive permeability from NMR are Kenyon model, Coates-Timer model and Bulk Gas Magnetic Resonance model. These models have their advantages and limitations depending on the nature of reservoir properties. This study discusses permeability derived from Bulk Gas Magnetic Resonance model and introduces neural network model to derive formation permeability using data from NMR and other open hole log data. The permeability results of neural network model and other models were validated by core permeability for the studied wells.
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