新疆石油地质 ›› 2025, Vol. 46 ›› Issue (5): 582-590.doi: 10.7657/XJPG20250508

• 油藏工程 • 上一篇    下一篇

HQ1区块齐古组稠油油藏倾斜油水界面主控因素

颜永何1(), 李海波1, 朱爱国1, 张无忌1, 张晶1, 刘刚2, 陈燕辉1, 汪彪1   

  1. 1.中国石油 新疆油田分公司 勘探开发研究院,新疆 克拉玛依 834000
    2.陕西延长石油(集团)有限责任公司 研究院,西安 710065
  • 收稿日期:2024-12-02 修回日期:2025-01-03 出版日期:2025-10-01 发布日期:2025-09-30
  • 作者简介:颜永何(1989-),男,四川达州人,工程师,硕士,油藏开发地质,(Tel)15009901341(Email)fcyyhe@petrochina.com.cn
  • 基金资助:
    中国石油科技项目(2023ZZ23YJ03)

Main Controlling Factors of Tilted Oil-Water Contact of Shallow Heavy Oil Reservoirs of Qigu Formation in Block HQ1,Karamay Oilfield

YAN Yonghe1(), LI Haibo1, ZHU Aiguo1, ZHANG Wuji1, ZHANG Jing1, LIU Gang2, CHEN Yanhui1, WANG Biao1   

  1. 1. Research Institute of Exploration and Development, Xinjiang Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
    2. Research Institute, Shaanxi Yanchang Petroleum (Group) Co. Ltd., Xi'an, Shaanxi 710065, China
  • Received:2024-12-02 Revised:2025-01-03 Online:2025-10-01 Published:2025-09-30

摘要:

为确定克拉玛依油田HQ1区块齐古组浅层稠油油藏油水关系及其主控因素,以油藏边部油水关系矛盾突出的h-4井区为例,利用密集井网资料及测试分析资料,探讨了砂体展布、水动力、储集层物性、油藏充注压力和构造作用对油藏油水界面的影响。研究区h-4井区油水界面特征明显,东部含水边界线与构造线平行,西部含水边界线与构造线斜交且油水界面倾斜。形成倾斜油水界面的主要原因为构造作用影响下的断裂阶段性开启、原油黏度变化导致的油水界面调整滞后,油藏具构造活动与非稳态耦合的成藏机制。研究区西部断裂开启形成原油的运移通道,原油在齐古组聚集成藏。西部断裂封闭后再次开启,油藏被破坏,原油溢散形成西高东低油水界面;同时,原油遭受降解,形成原油黏度西高东低的特征。在构造作用以及原油黏度影响下,油水界面的水平调整明显滞后,油藏属于非稳态油气藏。

关键词: 克拉玛依油田, HQ1区块, 齐古组, 稠油油藏, 油水界面, 原油黏度, 非稳态油藏

Abstract:

In order to determine the oil-water relationship and its controlling factors in the shallow heavy oil reservoirs of the Qigu formation in Block HQ1, Karamay oilfield, the study focuses on the h-4 well area, which exhibits significant oil-water distribution complexities at the reservoir margins. Using the data of dense well pattern and test analysis, the influences of sand body distribution, hydrodynamic conditions, reservoir properties, hydrocarbon charging pressure, and tectonic activities on the oil-water contact (OWC) are identified. The h-4 well area demonstrates distinctive OWC characteristics, where the water boundary is parallel with the structural line in the east, and the water boundary obliquely intersects the structural line in the west, resulting in a tilted OWC. This tilted OWC is believed to have been resulted from the periodical fracture opening due to tectonic activities and the OWC adjustment hysteresis is caused by oil viscosity variation, indicating a coupled mechanism of tectonism and unsteady reservoir formation. The fracture opening in the western part of the study area provided oil migration pathways, facilitating oil accumulation in the Qigu formation. Subsequent fracture sealing and reactivation events led to reservoir compartmentalization, creating a OWC that is high in west and low in east. Oil biodegradation shaped a similar viscosity feature. The combined effects of tectonic activities and viscosity variations significantly retard horizontal adjustments of OWC, characterizing the reservoir as a unsteady hydrocarbon accumulation system.

Key words: Karamay oilfield, Block HQ1, Qigu formation, heavy oil reservoir, oil-water contact, oil viscosity, unsteady reservoir

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