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Estimation of dynamic petrophysical properties of water-bearing sands invaded with oil-base mud from the interpretation of multiple borehole geophysical measurements

机译:从多次钻孔地球物理测量结果的解释估算含油泥浆侵入的含水砂的动态岩石物理性质

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Nonmiscible fluid displacement without salt exchange takes place when oil-base mud (OBM) invades connate water-saturated rocks. This is a favorable condition for the estimation of dynamic petrophysical properties, including saturation-dependent capillary pressure. We developed and successfully tested a new method to estimate porosity, fluid saturation, permeability, capillary pressure, and relative permeability of water-bearing sands invaded with OBM from multiple borehole geophysical measurements. The estimation method simulates the process of mud-filtrate invasion to calculate the corresponding radial distribution of water saturation. Porosity, permeability, capillary pressure, and relative permeability are iteratively adjusted in the simulation of invasion until density, photoelectric factor, neutron porosity, and apparent resistivity logs are accurately reproduced with numerical simulations that honor the postinvasion radial distribution of water saturation. Examples of application include oil- and gas-bearing reservoirs that exhibit a complete capillary fluid transition between water at the bottom and hydrocarbon at irreducible water saturation at the top. We show that the estimated dynamic petrophysical properties in the water-bearing portion of the reservoir are in agreement with vertical variations of water saturation above the free water-hydrocarbon contact, thereby validating our estimation method. Additionally, it is shown that the radial distribution of water saturation inferred from apparent resistivity and nuclear logs can be used for fluid-substitution analysis of acoustic compressional and shear logs.
机译:当油基泥浆(OBM)侵入原生含水饱和岩石时,发生了不混溶而无盐交换的流体驱替。这是评估包括饱和度相关的毛细管压力在内的动态岩石物理特性的有利条件。我们开发并成功测试了一种新方法,可通过多次钻孔地球物理测量来估算被OBM侵入的含水砂的孔隙率,流体饱和度,渗透率,毛细压力和相对渗透率。该估算方法模拟了泥浆滤液的侵入过程,以计算出相应的含水饱和度径向分布。在入侵模拟中迭代调整孔隙度,渗透率,毛细管压力和相对渗透率,直到通过数值模拟准确地再现密度,光电系数,中子孔隙度和视电阻率测井值为止,以符合入侵后水饱和度的径向分布。应用实例包括含油和含气储层,它们在底部的水和顶部无法抑制的水饱和度的烃之间表现出完全的毛细管流体过渡。我们表明,储层含水部分的动态岩石物理特性估计与游离水-烃接触上方水饱和度的垂直变化一致,从而验证了我们的估计方法。此外,还表明,从视电阻率和核测井曲线推断出的水饱和度的径向分布可用于声压测井和剪切测井的流体替代分析。

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