吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (1): 35-51.doi: 10.13278/j.cnki.jjuese.20190272
• 地质与资源 • 上一篇
吴蒙1,2, 秦勇1, 王晓青3, 李国璋1, 朱超1, 朱士飞2
Wu Meng1,2, Qin Yong1, Wang Xiaoqing3, Li Guozhang1, Zhu Chao1, Zhu Shifei2
摘要: 致密砂岩储层流体可动性对油气开发、预测和评价具有重要意义。查阅国内近十年相关成果,对致密储层流体可动性的相关参数、测试方法、分布特征及其影响因素进行了分析。发现致密砂岩储层的弛豫时间T2谱截止值为0.540~41.600 ms,可动流体孔隙度为0.12%~14.35%,可动流体饱和度为2.16%~90.30%,Ⅲ—Ⅳ类储层是致密砂岩储层的主要类型,致密储层可动流体的孔喉半径下限为0.013~0.110 μm,高压压汞、核磁共振、恒速压汞识别的孔喉半径下限分别为0.037 5、0.070 0~0.200 0、0.120 0 μm,水膜厚度为0.05~1.00 μm。统计分析显示,核磁共振、恒速压汞测得致密储层可动流体饱和度偏低;水膜厚度是影响致密砂岩储层流体渗流的主要因素;低煤阶煤层可动流体饱和度最高,致密砂岩储层次之,页岩储层最低;致密砂岩储层约是页岩储层、低煤阶煤层可动流体孔隙度的10倍;砂岩储层可动流体赋存于孔隙和喉道中,受孔隙和喉道共同控制;致密砂岩具有喉道分布集中,有效孔隙发育差,孔隙大部分为喉道半径小于1.000 μm的微细孔;喉道半径越集中、孔喉半径比越小、有效喉道半径越大,越有利于储层流体的渗流;砂岩渗透率(<2×10-3 μm2)越低,可动流体参数衰减越快;渗透率(>2×10-3 μm2)越高,可动流体参数升高越缓慢;喉道半径是控制致密砂岩储层流体可动性的主要因素。
中图分类号:
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