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物探与化探  2022, Vol. 46 Issue (1): 78-86    DOI: 10.11720/wtyht.2022.1071
  方法研究·信息处理·仪器研制 本期目录 | 过刊浏览 | 高级检索 |
基于多级次流动单元的砂砾岩储层分类渗透率评价方法——以陆丰油田古近系文昌组W53油藏为例
石磊(), 管耀, 冯进, 高慧, 邱欣卫, 阙晓铭
中海石油(中国)有限公司深圳分公司 南海东部石油研究院,广东 深圳 518000
Multi-level division method of flow units for accurate permeability assessment of glutenite reservoirs:A case study of reservoir W53 of Paleogene Wenchang Formation in Lufeng oilfield
SHI Lei(), GUAN Yao, FENG Jin, GAO Hui, QIU Xin-Wei, QUE Xiao-Ming
Research Institute,Shenzhen Branch of CNOOC Ltd.,Shenzhen 518000,China
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摘要 

中国南海东部海域陆丰油田古近系文昌组砂砾岩储层具有岩性复杂、孔隙度低、孔隙结构非均质性较强等特征。不同类型储层渗流特征差异明显,传统的孔渗模型精度难以满足生产开发需要。流动单元能有效刻画储层内部渗流特征,但单纯依据流动单元指标进行流动单元划分就会出现错划的现象。文昌组储层非均质性由宏观到微观具有层次性,综合地质、测井、岩心资料建立多层次流动单元判别法:首先基于沉积相划分第一级流动单元,然后以岩心和成像测井标定常规测井,识别岩性并划分第二级流动单元,最后基于孔隙结构,以流动单元指标FZI为依据划分第三级流动单元,由此形成了基于沉积微相—岩性—孔隙结构的三级流动单元划分方法。应用结果表明,该方法能有效避免流动单元划分不准确的现象,提高渗透率计算精度,对寻找优质产层、实现油藏高效开发具有重大意义。

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石磊
管耀
冯进
高慧
邱欣卫
阙晓铭
关键词 陆丰油田砂砾岩储层渗透率流动单元成像测井    
Abstract

The glutenite reservoirs of the Paleogene Wenchang formation in the Lufeng oilfield in the eastern South China Sea are characterized by complex lithology,low porosity,and strongly heterogeneous pore structure.Since different types of reservoirs show greatly different seepage characteristics,traditional permeability models are difficult to meet the demand for petroleum production and development due to their low calculation precision.Flow units can effectively characterize the internal seepage characteristics of reservoirs.However,the division of flow units based only on flow unit indicators will lead to misclassification.Given the macro and micro hierarchical heterogeneity of reservoirs of the Wenchang Formation,this study establishes a multi-level division method of flow units by combining geological,logging,and core data.Specifically,the first-order flow units are determined according to sedimentary facies.Then the second-order flow units are determined according to the lithology identified by calibrating conventional logging based on core and imaging logging.Finally,the third-order flow units are determined using flow zone indicator (FZI) approaches combined with pore structure.In this manner,a three-level division method of flow units based on sedimentary microfacies-lithology-pore structure is formed.As indicated by application results,this method can effectively avoid the inaccurate classification of flow units and improve the accuracy of permeability calculation,thus having great significance for finding high-quality reservoirs and the efficient development of oil reservoirs.

Key wordsLufeng oilfield    glutenite reservoirs    permeability    flow unit    imaging logging
收稿日期: 2021-02-26      修回日期: 2021-11-26      出版日期: 2022-02-20
ZTFLH:  P631.4  
基金资助:“十三五”国家科技重大专项课题“南海东部海域勘探领域及关键技术”(2016ZX05024-004);“十三五”集团公司科技重点项目课题“珠一坳陷潜在富生烃洼陷烃源潜力及大中型油田方向研究”(CNOOC-KJ 135 ZDXM 37 SZ 02 SZ)
作者简介: 石磊(1986-),男,工程师,主要从事测井综合解释及测井方法等研究工作。Email: shilei22@cnooc.com.cn
引用本文:   
石磊, 管耀, 冯进, 高慧, 邱欣卫, 阙晓铭. 基于多级次流动单元的砂砾岩储层分类渗透率评价方法——以陆丰油田古近系文昌组W53油藏为例[J]. 物探与化探, 2022, 46(1): 78-86.
SHI Lei, GUAN Yao, FENG Jin, GAO Hui, QIU Xin-Wei, QUE Xiao-Ming. Multi-level division method of flow units for accurate permeability assessment of glutenite reservoirs:A case study of reservoir W53 of Paleogene Wenchang Formation in Lufeng oilfield. Geophysical and Geochemical Exploration, 2022, 46(1): 78-86.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2022.1071      或      https://www.wutanyuhuatan.com/CN/Y2022/V46/I1/78
Fig.1  陆丰油田位置与地层特征
沉积微相 伽马曲
线特征
岩性 岩心照片 孔隙度/% 渗透率/(10-3 μm2) 储层类型 流动单元
类别
水下分流河道 含砾砂岩、粗砂岩、
细砂岩
5.8~17.4 1.8~212.0 低孔低渗—中孔中渗
滩坝 细砂岩、粉砂岩 4.0~15.7 0.25~6.0 低孔低渗—中孔低渗
水下天然堤 泥质粉砂岩、粉
砂质泥岩
2.5~6.9 <0.01 干层
Table 1  W53油藏沉积微相类型及第一级流动单元划分标准
Fig.2  W53油藏不同岩性的常规测井与成像测井特征
Fig.3  W53油藏岩性识别图版
第一级次 第二级次 物性
沉积微相 流动单元类别 岩性 流动单元类别 孔隙度/% 渗透率/(10-3 μm2)
水下分流河道 含砾砂岩 1 10.1~17.4 11.9~212.5
粗砂岩 2 5.8~14.8 1.8~38.1
细砂岩 3 8.0~13.7 2.0~15.1
滩坝 细砂岩 1 4.0~13.3 0.3~6.0
粉砂岩 2 4.6~15.7 0.04~3.9
Table 2  W53油藏第二级流动单元划分标准
Fig.4  二级分类后孔隙度与渗透率关系
Fig.5  压汞曲线验证储层类型
Fig.6  流动单元指标累积概率分布
第一级次 第二级次 第三级次 流动单元总类型
(FZI)
沉积微相 流动单元类别 岩性 FZI 流动单元类别 FZI
水下分
流河道
含砾砂岩 3.02~5.20 1 3.02~5.20 第一类(3.0~5.2)
粗砂岩 2.31~2.90 2 1.01~2.90 第二类(2.3~3.0)
细砂岩 1.45~2.29 3 第三类(1.5~2.3)
滩坝 细砂岩 1.01~1.95 1 第四类(1.0~1.9)
粉砂岩 0.31~0.93 2 0.61~0.93 第五类(0.6~1.0)
0.31~0.60 第六类(0.3~0.6)
Table 3  W53储层流动单元三级分类标准
Fig.7  三级分类后孔隙度渗透率关系
Fig.8  well-X1井W53油藏流动单元剖面
井名 孔隙度/
%
试井渗透率/
(10-3 μm2)
流动单元
总类型
钻杆地层测试* 米采油指数/
[m3·MPa-1·d-1·m-1]
well-X1 13.4 17.2 第三类 自喷求产:油210.9 m3/d 0.53
well-2 17.0 186.0 第一类 自喷求产:油487.3 m3/d 7.75
well-8 17.9 67.5 第二类 自喷求产:油145.2 m3/d 3.03
Table 4  W53储层流动单元类型与试油结果对比
Fig.9  计算渗透率与岩心渗透率对比
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