Prediction of reservoir properties and fluids using rock physics techniques in the Rio Del Rey Basin, Cameroon

IF 2.2 4区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Journal of African Earth Sciences Pub Date : 2024-07-16 DOI:10.1016/j.jafrearsci.2024.105346
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Abstract

The application of rock physics modeling has been a breakthrough in oil and gas industry and has greatly managed exploration and interpretation risk. In the Rio del Rey Basin, the rock physics method was used to ascertain the reservoir's characteristics and relate them to the elastic characteristics. Using conventional techniques to connect to the elastic properties and assess various rock physics diagnostics, the estimated petrophysical parameters were water saturations, porosity, and shale volume. By connecting the saturated bulk modulus to its porosity, the bulk modulus of the porous frame, the bulk modulus of the mineral matrix, and the bulk modulus of the pore filling fluids, the Gassmann fluid replacement modeling was used to simulate various fluid scenarios. Finally, an evaluation was conducted on rock physics boundaries and cement models. The reservoirs are rated as extremely good based on the results. The rock physics model generated showed the friable sand model is a suitable model for the said basin and the rock physics bounds that were evaluated indicated that the sediments are deposited below the critical porosity and less compacted thereby depicting a soft sand model. Conventional petrophysical study would not be able to reveal the clustering of the gas sands from the brine sand and the shale zone in connection to the geologic trend as demonstrated by the rock physics template. The anticipated model will be useful to extrapolate the study to other sedimentary basins in Cameroon and estimate porosity from the impedance acquired from seismic data throughout the basin.

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利用岩石物理技术预测喀麦隆里奥德尔雷盆地的储层特性和流体
岩石物理模型的应用是油气行业的一项突破,极大地控制了勘探和解释风险。在里奥德尔雷盆地,岩石物理方法被用来确定储层的特征,并将其与弹性特征联系起来。利用常规技术连接弹性特性并评估各种岩石物理诊断,估算出的岩石物理参数包括含水饱和度、孔隙度和页岩体积。通过将饱和容积模量与孔隙度、多孔框架的容积模量、矿物基质的容积模量以及孔隙填充流体的容积模量联系起来,利用加斯曼流体置换模型模拟了各种流体情况。最后,对岩石物理边界和水泥模型进行了评估。根据结果,储层被评为极好。生成的岩石物理模型显示,易碎砂模型适合上述盆地,评估的岩石物理边界显示,沉积物沉积在临界孔隙度以下,压实程度较低,因此描述了软砂模型。传统的岩石物理研究无法揭示卤水砂和页岩带中的气砂聚集与岩石物理模板所显示的地质趋势之间的联系。预期的模型将有助于将研究推广到喀麦隆的其他沉积盆地,并根据从整个盆地的地震数据中获得的阻抗估算孔隙度。
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来源期刊
Journal of African Earth Sciences
Journal of African Earth Sciences 地学-地球科学综合
CiteScore
4.70
自引率
4.30%
发文量
240
审稿时长
12 months
期刊介绍: The Journal of African Earth Sciences sees itself as the prime geological journal for all aspects of the Earth Sciences about the African plate. Papers dealing with peripheral areas are welcome if they demonstrate a tight link with Africa. The Journal publishes high quality, peer-reviewed scientific papers. It is devoted primarily to research papers but short communications relating to new developments of broad interest, reviews and book reviews will also be considered. Papers must have international appeal and should present work of more regional than local significance and dealing with well identified and justified scientific questions. Specialised technical papers, analytical or exploration reports must be avoided. Papers on applied geology should preferably be linked to such core disciplines and must be addressed to a more general geoscientific audience.
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