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首页> 外文期刊>American Journal of Geoscience >Subsidence Inferred from a Time Lapse Reservoir Study in a Niger Delta Field, Nigeria
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Subsidence Inferred from a Time Lapse Reservoir Study in a Niger Delta Field, Nigeria

机译:根据尼日利亚尼日尔三角洲油田的延时油藏研究推断出的沉降

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Production-induced subsidence due to compressibility and fluid property changes in a Niger delta field has been investigated using well log and 4D seismic data sets. The objective of the study is to evaluate changes in time lapse seismic attributes due to hydrocarbon production and infer to probable ground subsidence. Petrophysical modeling and analysis of well data revealed that Density ("), Lambda rho (&") and Acoustic impedance (Ip) are highly responsive to changes in reservoir properties. These properties and water saturation attribute were subsequently, extracted from time-lapse seismic volumes in the immediate vicinity of well locations. Result show that monitor horizon slices exhibit appreciable increases in ", &", Ip and water saturation values compared to the base data, especially around the well locations. These increases in relative values of rock/attribute properties between the time-lapse surveys for a constant overburden stress are obvious indications of pore pressure and fluid depletion in the reservoir. Depletion in these properties increases the effective stress (pressure) and the grain-to-grain contact of the reservoir matrix, with a corresponding decrease in compressibility. Consequently, pore and matrix volume decreases, the reservoir compacts and the ground subsides. However, this is suspected to be small and at the reservoir scale due to low initial reservoir porosity and the relatively large lateral dimension compared to the thickness of the reservoir.
机译:已经使用测井和4D地震数据集研究了由于尼日尔三角洲油田中的可压缩性和流体性质变化而导致的生产引起的沉降。这项研究的目的是评估由于油气生产而引起的时移地震属性的变化,并推断可能的地面沉降。岩石物理模型和井眼数据分析表明,密度(“),Lambda rho(&”)和声阻抗(Ip)对储层特性的变化有很高的响应能力。随后从井位置附近的延时地震体积中提取这些属性和含水饱和度属性。结果表明,与基础数据相比,监控层的水平切片在“,”,Ip和水饱和度值上显示出明显的增加,尤其是在井眼周围。对于恒定的上覆应力,随时间推移测量之间岩石/属性属性的相对值的这些增加是储层中孔隙压力和流体耗竭的明显指示。这些特性的减少会增加有效应力(压力)和储层基质的颗粒间接触,从而相应降低可压缩性。因此,孔隙和基质体积减小,储层致密,地面沉降。但是,由于储层的初始孔隙度低,并且与储层的厚度相比,侧向尺寸相对较大,这被怀疑是很小的,并且处于储层规模。

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