利用尼日利亚尼日尔三角洲岩石物理模型进行时移孔隙度和速度分析

E. Aniwetalu, Akudo Ernest, J. Ilechukwu, O. Ikegwuonu, U. Omoja
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引用次数: 0

摘要

通过对Isomu油田三维和时移地震资料的分析,提供了储层变化的动态表征。利用流体替代模型和地震速度模型分析了这些变化。结果表明,储层初始孔隙度为29.50%,含水饱和度为12%。油气饱和度保持在40%和48%,平均纵波速度2905m/s,平均横波速度1634m/s。然而,在流体替代模型中,结果反映了流体性质的变化,平均气饱和度和油饱和度分别为34%和24%,分别下降了14%和16%。平均含水饱和度提高30%,平均值为42%。含油饱和度降低,地层含水增加,影响孔隙度。孔隙率降低了4.16%,这可能是由于压力增大导致长径比裂纹闭合所致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
TIME-LAPSE POROSITY AND VELOCITY ANALYSIS USING ROCK PHYSICS MODELS IN NIGER DELTA, NIGERIA
The analysis of 3-D and time-lapse seismic data in Isomu Field has offered the dynamic characterization of the reservoir changes. The changes were analyzed using fluid substitution and seismic velocity models. The results of the initial porosity of the reservoirs was 29.50% with water saturation value of12%.The oil and gas maintained saturation values of 40% and 48% with average compressional and shear wave velocities of 2905m/s and 1634m/s respectfully. However, in fluid substitution modelling, the results reflect a change in fluid properties where average gas and oil saturation assume a new status of 34% and 24% which indicates a decrease by 14% and 16% respectively. The average water saturation increases by 30% with an average value of 42%. The decrease in hydrocarbon saturation and increase in formation water influence the porosity. Thus, porosity decreased by 4.16% which probably arose from the closure of the aspect ratio crack due to pressure increase.
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