成功圈定砂体以改善碳捕获和储存储层模型,以泰国湾北马来盆地为例

O. Limpornpipat, R. Uttareun, A. Satitpittakul, Takonporn Kunpitaktakun, P. Henglai, Khuananong Wongpaet
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摘要

本研究的目的是利用地震反演技术对砂岩储层进行表征,并利用反演结果支持CO2储存潜力识别和储层建模工作(储存量计算)。主要的储集目标是含盐含水层和衰竭储层。这些主要目标被解释为中新世古Chao Praya三角洲平原的分流河道沉积。该项目的结果有助于更准确地计算CO2储存容量的体积。为了了解观测到的地震反应与岩石性质之间的联系,进行了岩石物理可行性分析。基于岩石物理分析得出的结论,p阻抗可以用于页岩砂储层的圈定,因此选择叠后确定性地震反演进行储层表征。贝叶斯岩性分类方法通过p -阻抗的概率密度函数(PDF)来确定岩性类型,然后将结果PDF应用于倒置的相对p -阻抗,以创建砂概率和岩性(最可能)体积。然后,通过研究实际升级后的岩性测井曲线与贝叶斯分类得到的伪岩性测井曲线的匹配度,对岩性分类结果进行后验验证。此外,目标储层砂体概率图对下海岸平原环境分流河道的砂体分布响应较好,与实测结果一致。这项工作的结果表明,定量解释(QI)可以成功地提高砂储层填图的信心,在一个复杂的断层储层区段。本文的研究结果有利于储层潜力识别和储层建模,可以更精确地估算CO2的储存量。QI研究的最终结果提供了高质量的地震反演产品和岩性立方体,从而实现了目标CO2储层的砂岩圈定。关键因素是确保最佳的地震输入数据,在这种情况下,通过使用PSDM地震处理技术,对地震反演过程进行仔细的参数化,以及利用贝叶斯分类方法进行岩性分类来实现。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Successful Delineation of Sand Bodies to Improve Carbon Capture and Storage Reservoir Modelling, A Case Study from the North Malay Basin, Gulf of Thailand
The objective of this study is to characterize sand reservoirs by using seismic inversion technique, the results were used to support CO2 storage potential identification and reservoir modeling works (storage volume calculation). The key storage targets are the saline aquifers and depleted reservoirs. These main targets were interpreted as a deposition of distributary channels occurring in the Paleo Chao Praya delta plain during Miocene. The results of this project contribute to a more accurate volume calculation for CO2 storage capacity. A rock physics feasibility analysis was carried out to understand a link between the observed seismic responses and the rock properties. Based on conclusions made in the rock physics analysis, P-Impedance could be used to delineate sand reservoir from shale, thus, a post-stack deterministic seismic inversion was selected for this reservoir characterization. Bayesian litho-classification method justifies lithology types by Probability Density Function (PDF) of P-Impedance, the resulting PDF was then applied to the inverted relative P-Impedance to create sand probability and lithology (most probable) volumes. Then, posterior validation of the lithology classification results was performed by investigating the match between the actual upscaled lithology log and pseudo lithology log from the Bayesian classification. Furthermore, the sand probability maps of the target reservoirs show an acceptable sand distribution response to the distributary channels in lower coastal plain environment that is consistent with the well results. The results of this work demonstrate how quantitative interpretation (QI) can successfully improve confidence in sand reservoirs mapping, in an area of complex faulted reservoir interval. The results presented here are beneficial for storage potential identification and reservoir modeling part, which can provide a more precise estimation of CO2 storage volume. The final results of the QI study provide good quality seismic inversion products and lithology cube, which enabled sand delineation at the target CO2 storage level. The key contributors have been ensuring optimal seismic input data, being in this case achieved through using a PSDM seismic processing technology, careful parameterization of seismic inversion process, and utilization of Bayesian classification method for lithology classification.
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