首页> 外文会议>International Symposium of the Society of Core Analysts >SCA2003-03: CARBONATE ROCK WETTABILITY INTERPRETED FROM CAPILLARY PRESSURE AND IMBIBITION RESISTIVITY INDEX ANALYSES
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SCA2003-03: CARBONATE ROCK WETTABILITY INTERPRETED FROM CAPILLARY PRESSURE AND IMBIBITION RESISTIVITY INDEX ANALYSES

机译:SCA2003-03:碳酸盐岩石润湿性从毛细管压力和吸收电阻率指数分析中解释

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The wettability of rock samples from 5 carbonate reservoirs in Western Canada varies from weakly water wet to mixed wet to mildly oil wet.Wettability was determined by USBM and Amott analyses on 17 aged rock samples.Evidence supporting these interpretations was provided in one case by a contact angle measurement of the live oil,and in other instances by relations between un-restored primary drainage and restored secondary drainage capillary pressure curves.Imbibition resistivity index(IRI)measurements were performed on 9 aged sister-plug samples to determine a restored Archie saturation exponent”n”.The saturation exponent measured at the onset of the IRI test provides the most reliable”n”value as it is determined on a restored sample prior to any hysteresis that occurs during increasing Sw.Values for the restored”n”vary from 1.2 to 3.1.Although the imbibition RI tests provide a reliable measure of the saturation exponent,this number cannot be used alone as a valid indicator of wettability.Wettability and pore geometry principally control the shape of the RI profile during imbibition.Comparisons of imbibition RI profiles and water relative permeability curves were made between an oil wet and water wet reservoir with similar pore geometry.The water wet samples generally exhibit suppressed electrical and hydraulic behaviour during imbibition consistent with a more water wet pore system.In contrast,the oil wet samples exhibit an instantaneous flow of water and electric current with increasing Sw that is consistent with a more oil wet pore system.The wettability interpretations and saturation exponent measurements made for these 5 carbonate reservoirs were used to refine expectations of reservoir performance and enhance petrophysical interpretations.
机译:加拿大西部5个碳酸盐储层的岩石样品的润湿性因弱水而变化,湿润湿润至温和的油湿法。通过USBM和17岁老年的岩石样品的Amott分析确定。 Live油的接触角测量,以及通过未恢复的初级排水和恢复的二次排水毛细管压力曲线关系的其他情况。在9岁老年的姊妹插头样本上进行了测量电阻率指数(IRI)测量以确定恢复的ARCHIE饱和度指数“n”。在IRI测试开始时测量的饱和度指数提供了最可靠的“n”值,因为在恢复的“n”变化期间发生的任何滞后之前在恢复的样本上确定了恢复的样本。从1.2到3.1。虽然吸收RI测试提供了饱和度指数的可靠度量,但该数字不能单独使用,作为Wettabil的有效指标Ity。填充性和孔几何形状主要控制IMBIBITING期间的RI谱的形状。在具有类似孔隙几何形状的油湿和水湿储存器之间进行了利用型材和水相对渗透曲线。水湿样品通常表现出抑制电力在吸收过程中的液压行为一致,与更多的水湿孔系统一致。对比,油湿样品具有瞬时流动的水和电流,随着更多的湿孔系统一致,普通的速度符合。润湿性解释和饱和度指数一致为这5种碳酸盐储层制备的测量用于改进储层性能的预期,提高岩石物理解释。

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