Didi Chekwube Nnamdi, Osinowo Olawale Olakunle, Akpunonu Okey Eliseus
Pan African University Life and Earth Sciences Institute, University of Ibadan, Ibadan, Nigeria.
Department of Geology, University of Ibadan, Ibadan, Nigeria.
Sci Rep. 2025 Jul 1;15(1):20742. doi: 10.1038/s41598-025-94592-z.
The reservoir characterization of the Yolde Formation was conducted to assess the hydrocarbon potential of the Kolmani field in the Gongola Basin, Upper Benue Trough. This evaluation utilized Pressure, Temperature, PVT, mobility, and well log data. Data from repeated formation testers (RFT), modular formation testers (MDT), PVT laboratory results, and well logs were analyzed to achieve a comprehensive understanding of the Yolde Formation reservoir. The pressure data and PVT analysis revealed the presence of gas and water in the Yolde Formation at depths of 6916 ft and 6997 ft, respectively. This led to the identification of the gas-water contact at 6997 ft. Further analysis of the gas type using PVT analysis and the Soave-Redlich-Kwong (SRK) equation of state (EOS) model indicated that 80% of the gas in the reservoir was condensate gas. Temperature data ranged from 104 to 270 °F at the bottom hole and 109 °F to 281 °F in the formation. The calculated geothermal gradients of 0.0228 deg F/ft (52.49 °C/Km) and 0.0234 deg F/ft (42.62 °C/Km) suggested favorable conditions for gas reservoirs and hydrocarbon generation. The highest fluid mobility was observed at depths of 6916 ft, 7116.5 ft, and 7186.9 ft, indicating the presence of gas. The gamma ray log and resistivity log of the Kowell-1 well characterized the Yolde Formation as a substantial system of thin to medium sand/shale laminae. This research provides valuable insights into the hydrocarbon potential of the area, supporting future exploration and development efforts.
对约尔德组进行储层表征,以评估上贝努埃槽地贡戈拉盆地科尔马尼油田的油气潜力。该评估利用了压力、温度、PVT、流度和测井数据。分析了重复地层测试器(RFT)、模块地层测试器(MDT)的数据、PVT实验室结果以及测井数据,以全面了解约尔德组储层。压力数据和PVT分析表明,约尔德组在深度6916英尺和6997英尺处分别存在天然气和水。由此确定了气水界面在6997英尺处。利用PVT分析和Soave-Redlich-Kwong(SRK)状态方程(EOS)模型对气体类型进行的进一步分析表明,储层中80%的气体为凝析气。井底温度数据范围为104至270°F,地层温度范围为109°F至281°F。计算得出的地温梯度分别为0.0228°F/英尺(52.49°C/公里)和0.0234°F/英尺(42.62°C/公里),表明有利于气藏和气烃生成。在深度6916英尺、7116.5英尺和7186.9英尺处观察到最高流体流度,表明存在天然气。科韦尔-1井的自然伽马测井和电阻率测井将约尔德组表征为一个由薄至中砂岩/页岩层组成的大型系统。这项研究为该地区的油气潜力提供了有价值的见解,为未来的勘探和开发工作提供了支持。