岩性油气藏 ›› 2024, Vol. 36 ›› Issue (3): 3139.doi: 10.12108/yxyqc.20240303
程静1,2, 闫建平1,2, 宋东江3, 廖茂杰4, 郭伟5, 丁明海6, 罗光东6, 刘延梅7
CHENG Jing1,2, YAN Jianping1,2, SONG Dongjiang3, LIAO Maojie4, GUO Wei5, DING Minghai6, LUO Guangdong6, LIU Yanmei7
摘要: 以川南长宁地区 NX22 井五峰组—龙马溪组低电阻率页岩气储层为例,利用岩心矿物组分、扫描电镜、总有机碳(TOC)含量、含水饱和度测试及测井曲线等资料,确立了低电阻率页岩气储层岩石体积物理模型,采用随机法构建了三维数字岩心模型,进而利用有限元数值模拟方法模拟计算各矿物组分含量、含水饱和度及有机质石墨化的电阻率响应特征,并分析其主控因素。研究结果表明:①长宁地区五峰组—龙马溪组低电阻率页岩气储层岩石体积物理模型由骨架(石英、长石、方解石和白云石等)、黏土矿物、黄铁矿、未石墨化有机质以及石墨化有机质、孔隙 6 个部分组成。②三维数字岩心模型的长、宽、高分别为 100×100×100 像素,融入了上述物理模型中的 6 个部分,并采用不同的颜色对导电组分进行标识,可以显示不同方向上的切片,表征低电阻率页岩气储层的组分特性。③黏土矿物含量、黄铁矿含量、含水饱和度以及有机质石墨化程度等 4 个参数增大都会造成页岩气储层的电阻率下降,而有机质的高石墨化程度(25%)和高含水饱和度(88.0%)使页岩气储层的电阻率从正常电阻率(大于 15 Ω·m)降到低阻甚至超低阻(小于 5 Ω·m),是导致研究区页岩气储层超低阻响应的 2 个核心因素。
中图分类号:
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