首页> 外文会议>International Symposium of the Society of Core Analysts >HETEROGENEITY OF FRACTURED GRANITE: EFFECTS ON PETROPHYSICAL PROPERTIES AND WATER SATURATION OF PRESERVED CORES
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HETEROGENEITY OF FRACTURED GRANITE: EFFECTS ON PETROPHYSICAL PROPERTIES AND WATER SATURATION OF PRESERVED CORES

机译:裂缝花岗岩的异质性:保存芯的岩石物理性质和水饱和度的影响

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Heterogeneity of oil-bearing fractured granite of the Bach Ho oil field has been studied through petrophysical measurement.Full-size and plug core data of permeability and porosity were compared to show the scale of macroscopic heterogeneity of the rocks.An attempt to evaluate the content of connate water was made on preserved cores(taken by using water-based mud).Excessive water(invaded into the macropores)was removed by capillary extraction using chalk powder.The regime of this process has been calibrated with porous plate technique.The percentage of invaded water was found close to the partition coefficient of rnacrofractures.Electrical properties have been studied on preserved,”preserved afier chalk”and cleaned cores.Scatter in resistivity index vs.water saturation cross-plots for these states was observed whereas a satisfactory relationship of formation factor vs.porosity was obtained.Rock matrix was found to obey Archie's law with certain cementation and saturation exponents.For samples with dual porosity(containing macrofractures)the slope”n”of RI-Sw curves changed from high a value of water saturation to low values.Electrical anisotropy was also investigated by measurements in perpendicular directions.The results show that electrical anisotropy exists due to the orientation of macrofractures while RI-Sw curves have the same characteristics.Explanations of these irregularities of electrical properties can be found by reconstructing the theoretical model of fractured media with dual porosity.Fair agreement between the characteristics of electrical parameters of actual cores and reconstructed model shows the essential role of macrofractures in the behavior of fractured granite.
机译:通过岩石物理测量研究了BACH Ho油田的耐油骨折花岗岩的异质性。相比,透磁性和孔隙率的尺寸和插头核心数据显示出岩石的宏观异质性等级。试图评估含量的试图评估含量在保存的芯上制造了合成水(通过使用水基泥浆捕获)。使用粉笔粉通过毛细管萃取除去毛细血管萃取除去水(侵入麦克脂)。该方法的制度用多孔板技术校准。百分比发现侵入水贴近rnacrofractures的分区系数。已经研究了在保存的“保存的粉笔”和清洁的核上研究了电性能。在电阻率指数中散射,而这些状态的饱和横向图是令人满意的形成形成因子vs。发现矩阵被发现遵守某些胶泥和饱和指数的原则。具有双孔隙率的样品(含有Macrofracture)的斜率“N”的RI-SW曲线的斜率从高度的水饱和值变为低值。通过垂直方向的测量还通过测量来研究电子各向异性。结果表明由于宏观的取向,而RI-SW曲线具有相同的特征。通过使用双孔隙度重建裂缝介质的理论模型,可以找到这些不规则的电特性的开发。实际核心电气参数的特征与重建模型之间的达成协议。显示Macrofractures在裂缝花岗岩行为中的基本作用。

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