特种油气藏 ›› 2025, Vol. 32 ›› Issue (1): 88-97.DOI: 10.3969/j.issn.1006-6535.2025.01.010

• 地质勘探 • 上一篇    下一篇

鄂尔多斯盆地庆阳气田上古生界气藏气水分布主控因素

夏辉1,2, 王龙1,2, 李娅1,2, 张道锋1,2, 张园园1,2, 朱望明3, 张伟1,2, 刘平1,2   

  1. 1.中国石油长庆油田分公司, 陕西 西安 710018;
    2.低渗透油气田勘探开发国家工程实验室, 陕西 西安 710018;
    3.中国石油集团东方地球物理勘探有限责任公司,陕西 西安 710021
  • 收稿日期:2024-03-06 修回日期:2024-12-10 出版日期:2025-02-25 发布日期:2025-05-13
  • 通讯作者: 王龙(1982—),男,高级工程师,2006年毕业于成都理工大学资源勘查专业,现主要从事天然气开发与储层精细描述研究工作。
  • 作者简介:夏辉(1991—),男,工程师,2013年毕业于西安石油大学地质学专业,2020年毕业于中国地质大学(北京)矿产普查与勘探专业,获博士学位,现主要从事天然气开发与沉积储层研究工作。
  • 基金资助:
    中国石油重大科技专项“致密砂岩气藏提高采收率关键技术研究”(2023ZZ25)

Main control factors of gas-water distribution in the Upper Paleozoic gas reservoirs of the Qingyang Gasfield in the Ordos Basin

XIA Hui1,2, WANG Long1,2, LI Ya1,2, ZHANG Daofeng1,2, ZHANG Yuanyuan1,2, ZHU Wangming3, ZHANG Wei1,2, LIU Ping1,2   

  1. 1. PetroChina Changqing Oilfield Company, Xi′an, Shaanxi 710018, China;
    2. National Engineering Laboratory for Exploration and Development of Low-Permeability Oil and Gas Fields, Xi′an, Shaanxi 710018, China;
    3. BGP INC., China National Petroleum Corporation, Xi′an, Shaanxi 710021, China
  • Received:2024-03-06 Revised:2024-12-10 Online:2025-02-25 Published:2025-05-13

摘要: 庆阳气田上古生界气藏气水分布复杂,制约了气田的高效开发。针对这一问题,综合利用钻测井、三维地震、试气及生产数据等资料,系统开展地层水类型划分、气水分布规律及控制因素研究,明确气水分布主控因素。结果表明:研究区地层水主要赋存于山1段,盒8段产水层较局限,平面上可划分出中部高含水区以及西部、东部中含水区;地层水可划分为构造低部位滞留水、断裂破坏层间水及孤立透镜体水。构造低部位滞留水分布于研究区西部,受区域构造特征和生烃强度影响;断裂破坏层间水主要分布于研究区中部,受断裂体系控制;孤立透镜体水分布于研究区东部,主要受控于储层非均质性及运移距离。该研究成果为复杂构造背景致密砂岩气藏气水分布及天然气成藏研究提供了理论借鉴,也为后续气田效益开发提供了地质依据。

关键词: 气水分布, 控制因素, 致密砂岩气藏, 上古生界, 庆阳气田, 鄂尔多斯盆地

Abstract: The complex distribution of gas and water in the Upper Paleozoic gas reservoirs of Qingyang Gasfield restricts the efficient development of the gas field. To solve this problem, we comprehensively utilized data from drilling and logging wells, 3D seismic, gas testing and production to systematically carry out study on the classification of formation water types, the distribution pattern of gas and water and the controlling factors, so as to clarify the main control factors for the distribution of gas and water. The results show that:the formation water in the study area is primarily distributed in the Shan 1 Member, with the water-producing layers in the He 8 Member being relatively limited.On a plane, a high water-bearing area in the center and medium water-bearing areas in the west and east can be delineated. The formation water can be categorized into structural low-lying trapped water,interlayer fracture water, and isolated lens-body water. Structural low-lying trapped water is distributed in the western part of the study area,influenced by regional tectonic characteristics and the intensity of hydrocarbon generation; interlayer fracture water is primarily found in the central part of the study area, controlled by the fault system;isolated lens body water is distributed in the eastern part of the study area, mainly controlled by the heterogeneity of the reservoir and the migration distance.This achievement provides theoretical reference for the study of gas-water distribution in tight sandstone gas reservoirs under complex structural backgrounds, as well as for the study of natural gas accumulation. It also offers geological basis for the subsequent efficient development of gas fields.

Key words: gas-water distribution, control factors, tight sandstone gas reservoir, Upper Paleozoic, Qingyang Gasfield, Ordos Basin

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