油气藏评价与开发 ›› 2024, Vol. 14 ›› Issue (1): 138-150.doi: 10.13809/j.cnki.cn32-1825/te.2024.01.019
郭智栋1(),康毅力2(),王玉斌1,古霖蛟3,游利军2,陈明君2,颜茂凌2
收稿日期:
2023-07-12
出版日期:
2024-02-26
发布日期:
2024-03-05
通讯作者:
康毅力(1964—),男,博士,教授,博士生导师,本刊第二届编委会委员,主要从事储层保护理论及技术、非常规天然气、油气田开发地质研究与教学方面的工作。地址:四川省成都市新都区新都大道8号,邮政编码:610500。E-mail: 作者简介:
郭智栋(1985—),男,硕士,高级工程师,主要从事煤层气等非常规油气的开发工作。地址:陕西省西安市莲湖区劳动路115号,邮政编码:710082。E-mail:基金资助:
GUO Zhidong1(),KANG Yili2(),WANG Yubin1,GU Linjiao3,YOU Lijun2,CHEN Mingjun2,YAN Maoling2
Received:
2023-07-12
Online:
2024-02-26
Published:
2024-03-05
摘要:
气-水相渗曲线反映储层综合物性特征,明确致密砂岩气-水相渗行为与气井生产动态的关系,有利于致密气藏高效开发。以鄂尔多斯盆地东缘典型致密砂岩气藏为研究对象,将储层分为3类并开展气-水相渗实验,结合X射线衍射、扫描电镜和核磁共振等岩心分析手段,揭示气-水相渗与气井生产动态曲线的关系。结果表明:①Ⅰ类相渗曲线两相过渡区较宽,孔隙类型以粒间孔为主,Ⅱ类相渗曲线两相过渡区较窄,孔隙类型以粒间孔和晶间孔为主,Ⅲ类储层相渗曲线两相过渡区极窄,孔隙类型以晶间孔为主;②储层黏土矿物含量高,高岭石和绿泥石有利于气水两相流动,伊利石不利于气水两相流动;③孔喉差异大,大致分为3类:中—粗孔喉(大于1.0 μm)、细孔喉(0.1~1.0 μm)和微孔喉(小于0.1 μm),Ⅰ类、Ⅱ类和Ⅲ类储层的中—粗孔喉占比分别约为40%、10%和4%;④根据上述3类储层的气-水相渗特征,可将气井分为3类,其生产动态特征与相渗曲线预测结果均相符,Ⅰ类井主要产层为Ⅰ类储层,有效厚度约为7 m,平均日产气量约为2×104 m3,稳产时间长,Ⅱ类井主要产层为Ⅱ类储层,有效厚度约为5 m,平均日产气量约为1×104 m3,Ⅲ类井主要产层为Ⅲ类储层,有效厚度约为6 m,平均日产气量约为0.5×104 m3,稳产时间极短。通过分析致密砂岩气-水相渗特征预测气井生产动态,揭示了孔隙结构和黏土矿物对气水流动行为的影响,可为制定低压高含水致密气开发过程降阻提效措施提供理论支撑。
中图分类号:
郭智栋, 康毅力, 王玉斌, 古霖蛟, 游利军, 陈明君, 颜茂凌. 低压高含水致密气藏气-水相渗特征及生产动态响应[J]. 油气藏评价与开发, 2024, 14(1): 138-150.
GUO Zhidong, KANG Yili, WANG Yubin, GU Linjiao, YOU Lijun, CHEN Mingjun, YAN Maoling. Gas-water relative permeability characteristics and production dynamic response of low pressure and high water cut tight gas reservoirs[J]. Petroleum Reservoir Evaluation and Development, 2024, 14(1): 138-150.
表3
DJ区块实验岩心束缚水饱和度对应的特征参数变化情况"
样号 | 孔隙度/ % | 渗透率/ 10-3 μm2 | 束缚水 饱和度/% | 束缚水气相 相对渗透率 |
---|---|---|---|---|
DJ-1 | 8.39 | 9.52 | 33.30 | 0.67 |
DJ-2 | 9.90 | 1.38 | 40.46 | 0.57 |
DJ-3 | 11.73 | 1.85 | 39.26 | 0.52 |
DJ-4 | 15.90 | 0.33 | 57.32 | 0.21 |
DJ-5 | 8.69 | 0.44 | 58.11 | 0.18 |
DJ-6 | 8.07 | 0.45 | 69.65 | 0.28 |
DJ-7 | 7.56 | 0.15 | 78.01 | 0.10 |
DJ-8 | 5.81 | 0.19 | 69.65 | 0.28 |
DJ-9 | 5.80 | 0.15 | 70.17 | 0.04 |
表4
DJ区块气-水相渗实验岩心XRD结果"
样号 | 石英含量 | 斜长石含量 | 方解石含量 | 菱铁矿含量 | 黏土矿物含量 | 伊利石含量 | 高岭石含量 | 绿泥石含量 | 类型 |
---|---|---|---|---|---|---|---|---|---|
DJ-1 | 81 | 5 | 1 | 0 | 13 | 14 | 10 | 30 | Ⅰ |
DJ-2 | 59 | 35 | 1 | 0 | 5 | 23 | 49 | 17 | |
DJ-3 | 90 | 2 | 1 | 0 | 7 | 34 | 49 | 17 | |
DJ-4 | 76 | 0 | 8 | 3 | 13 | 56 | 28 | 10 | Ⅱ |
DJ-5 | 59 | 4 | 1 | 0 | 21 | 45 | 17 | 8 | |
DJ-6 | 62 | 0 | 1 | 2 | 17 | 70 | 23 | 7 | |
DJ-7 | 39 | 10 | 2 | 6 | 43 | 29 | 3 | 5 | Ⅲ |
DJ-8 | 30 | 3 | 0 | 14 | 53 | 76 | 19 | 5 | |
DJ-9 | 59 | 6 | 10 | 0 | 20 | 60 | 24 | 7 |
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