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物探与化探  2024, Vol. 48 Issue (1): 142-150    DOI: 10.11720/wtyht.2024.1146
  方法研究·信息处理·仪器研制 本期目录 | 过刊浏览 | 高级检索 |
牛东地区砂砾岩储层测井层内非均质性评价
周军1(), 边会媛1(), 陈文安2, 张迪2, 刘国良2, 王飞3
1.西安科技大学 地质与环境学院,陕西 西安 710054
2.青海油田勘探开发研究院,甘肃 敦煌 736202
3.长安大学 地质工程与测绘学院,陕西 西安 710064
Log-based evaluation of intralayer heterogeneity of glutenite reservoirs in the Niudong area
ZHOU Jun1(), BIAN Hui-Yuan1(), CHEN Wen-An2, ZHANG Di2, LIU Guo-Liang2, WANG Fei3
1. College of Geology and Environment, Xi'an University of Science and Technology, Xi'an 710054, China
2. Research Institute of Exploration and Development, Qinghai Oilfield Company, PetroChina, Dunhuang 736202, China
3. College of Geology Engineering and Geomatics, Chang'an University, Xi'an 710064, China
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摘要 

牛东地区砂砾岩储层具有低孔、低渗等特征,储层结构复杂,非均质性较强,常规测井对储层类型划分困难,影响了储层评价精度。岩心孔渗、薄片分析、X衍射等测试资料表明,牛东地区砂砾岩储层具有较强的非均质性,且根据毛管压力形态可将储层分为3个类别。本次研究利用电成像测井资料对储层层内非均质性进行评价:首先对电成像测井资料进行处理得到储层孔隙度谱,再对随深度变化的孔隙度谱进行研究,分别计算不同深度上孔隙度谱的均值、方差、洛伦兹系数和集中程度函数;根据综合概率模型,利用层次分析法确定评价指标的权重,得到储层非均质性综合指数,据此对储层进行划分,并建立储层非均质性的评价标准。应用该方法得到的研究结果与压汞实验结果一致,说明利用该方法能够有效地评价储层非均质性,可丰富现有的储层非均质性评价方法,为储层的精细评价提供一定的理论支撑。

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周军
边会媛
陈文安
张迪
刘国良
王飞
关键词 电成像测井非均质性评价压汞曲线洛伦兹系数储层分类    
Abstract

Glutenite reservoirs in the Niudong area exhibit low porosity and permeability, intricate reservoir structures, and pronounced heterogeneity, making it difficult to classify the reservoirs using conventional logs and further impairing reservoir evaluation accuracy. As indicated by the data from core porosity and permeability tests, thin-section analysis, and X-ray diffraction tests, the glutenite reservoirs in the Niudong area feature high heterogeneity and can be classified into three types based on capillary pressure morphologies. This study evaluated the intralayer heterogeneity of the reservoirs using electrical imaging logs. First, reservoir porosity spectra were derived from the electrical imaging logs. Then, the averages, variances, Lorenz coefficients, and concentration functions of the porosity spectra of different depths were calculated by analyzing these depth-varying porosity spectra. Based on the integrated probability model, the weights of evaluation indices were determined through hierarchical analysis, obtaining the composite index of reservoir heterogeneity. Accordingly, the reservoirs were classified, and the evaluation criteria for reservoir heterogeneity were established. The results of this study were consistent with the results of mercury injection experiments. The method used in this study proves effective in reservoir heterogeneity evaluation, enriching current methods for reservoir heterogeneity evaluation and providing theoretical support for fine-scale reservoir evaluation.

Key wordselectrical imaging log    heterogeneity evaluation    mercury injection curve    Lorentz coefficient    reservoir classification
收稿日期: 2023-04-10      修回日期: 2023-06-09      出版日期: 2024-02-20
ZTFLH:  P631.84  
基金资助:国家自然科学基金项目(42304143);陕西省自然科学基础研究计划(2022JM-147)
通讯作者: 边会媛(1986-),女,副教授,主要从事复杂储层测井精细解释及岩石物理研究的教学与研究工作。Email:smilebianhuiyuan@126.com
作者简介: 周军(2000-),男,硕士研究生,研究方向:测井评价与岩石物理研究。Email:akzhoujun@126.com
引用本文:   
周军, 边会媛, 陈文安, 张迪, 刘国良, 王飞. 牛东地区砂砾岩储层测井层内非均质性评价[J]. 物探与化探, 2024, 48(1): 142-150.
ZHOU Jun, BIAN Hui-Yuan, CHEN Wen-An, ZHANG Di, LIU Guo-Liang, WANG Fei. Log-based evaluation of intralayer heterogeneity of glutenite reservoirs in the Niudong area. Geophysical and Geochemical Exploration, 2024, 48(1): 142-150.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2024.1146      或      https://www.wutanyuhuatan.com/CN/Y2024/V48/I1/142
Fig.1  柴达木盆地牛东地区侏罗系构造位置及岩性柱状图
Fig.2  侏罗纪储层岩性特征
Fig.3  侏罗纪储层孔隙类型特征
Fig.4  侏罗纪储层孔渗分布
Fig.5  孔隙度谱形态结构
Fig.6  牛东地区牛X井3340~3370 m砂砾岩孔隙度谱
Fig.7  洛伦兹系数计算示意
标度 含义
1 两个参数相比,具有相同重要性
3 两个参数相比,前者比后者稍重要
5 两个参数相比,前者比后者明显重要
7 两个参数相比,前者比后者强烈重要
9 两个参数相比,前者比后者极端重要
2,4,6,8 表示上述相邻标度的中间值
倒数 与上述情况相反
Table 1  判断矩阵标度定义
参数 均值 方差 洛伦兹
系数
集中程
度函数
权重
均值 1 1/3 1/8 1/7 0.0461
方差 3 1 1/7 1/5 0.0898
洛伦兹系数 8 7 1 2 0.5319
集中程度函数 7 5 1/2 1 0.3322
Table 2  参数权重的配对比较矩阵
Fig.8  牛X井侏罗纪储层非均质性评价结果
Fig.9  牛X井岩心压汞毛管压力曲线
储层类型 岩性 / % / 10 - 3 μ m 2 洛伦兹系数 集中程度函数 综合概率函数 非均质性程度
I 泥质长石岩屑砂岩 7.9 ~ 9.8 8.3 0.3 ~ 0.8 0.6 ≤0.1 ≤0.001 ≤0.07
砾质长石岩屑砂岩 7.1 ~ 8.2 7.5 0.28 ~ 0.7 0.42 0.1~0.15 0.001~0.002 0.07~0.2 一般
含泥砾不等粒砂岩 5.3 ~ 7.2 6.6 0.04 ~ 0.3 0.2 >0.15 >0.002 >0.2
Table 3  综合概率值划分储层类型
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