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基于有限元方法的储层地应力修正研究

王金铎 孙鲁宁 王军 王敏 李静 刘旭亮 刘晨

王金铎, 孙鲁宁, 王军, 等, 2019. 基于有限元方法的储层地应力修正研究. 地质力学学报, 25 (3): 349-356. DOI: 10.12090/j.issn.1006-6616.2019.25.03.032
引用本文: 王金铎, 孙鲁宁, 王军, 等, 2019. 基于有限元方法的储层地应力修正研究. 地质力学学报, 25 (3): 349-356. DOI: 10.12090/j.issn.1006-6616.2019.25.03.032
WANG Jinduo, SUN Luning, WANG Jun, et al., 2019. RESEARCH ON THE GROUND STRESS CORRECTION OF RESERVOIRS BASED ON THE FINITE ELEMENT METHOD. Journal of Geomechanics, 25 (3): 349-356. DOI: 10.12090/j.issn.1006-6616.2019.25.03.032
Citation: WANG Jinduo, SUN Luning, WANG Jun, et al., 2019. RESEARCH ON THE GROUND STRESS CORRECTION OF RESERVOIRS BASED ON THE FINITE ELEMENT METHOD. Journal of Geomechanics, 25 (3): 349-356. DOI: 10.12090/j.issn.1006-6616.2019.25.03.032

基于有限元方法的储层地应力修正研究

doi: 10.12090/j.issn.1006-6616.2019.25.03.032
基金项目: 

国家科技重大专项 2016ZX05002-002

国家自然科学基金 41272141

详细信息
    作者简介:

    王金铎(1967-), 男, 博士, 高级工程师, 从事油气地质勘探研究与管理工作。E-mail:wangjinduo.slyt@sinopec.com

  • 中图分类号: TE311;P554

RESEARCH ON THE GROUND STRESS CORRECTION OF RESERVOIRS BASED ON THE FINITE ELEMENT METHOD

  • 摘要: 地应力是油气储层评价的基础参数,传统常用的单井地应力求解往往只依托于测井数据及岩石力学实验,未考虑整体力学模型中地层岩石非均质性对地应力的影响。研究以准噶尔盆地中部4区块董11井为例,采用整体力学模型分析的方法对目的储层地应力进行修正。根据地层岩石的物理性质及岩石力学参数对井场周围地区进行划分及整体三维建模,并用ANSYS有限元软件对其整体模型进行力学分析,从而对地应力计算结果进行修正,得出研究区目的层地应力分布情况。研究结果表明,修正后的地应力值与修正前的地应力值在地层薄弱(坚硬)层段水平最小主应力值相差16%~17%左右,水平最大主应力值相差22%~23%左右。修正后的地应力可以很好地体现地层在沉积过程中造成的岩石物理性质非均质性对地应力非均质性的影响,反映了储层地应力的真实变化特征。

     

  • 图  1  研究区位置图

    Figure  1.  Location map of the research area

    图  2  董11井4050~4100 m井段的测井数据

    Figure  2.  Logging data of well section at 4050 m~4100 m of the well Dong 11

    图  3  计算模型

    Figure  3.  Computational model

    图  4  计算模型最小主应力分布云图

    MN—应力最小值点;MX—应力最大值点

    Figure  4.  Nephogram of minimum principal stress distribution in the computational model

    图  5  计算模型最大主应力分布云图

    MN—应力最小值点;MX—应力最大值点

    Figure  5.  Nephogram of maximum principal stress distribution in the computational model

    图  6  井场内部最小主应力分布云图

    MN—应力最小值点;MX—应力最大值点

    Figure  6.  Nephogram of minimum principal stress distribution in the well site

    图  7  井场内部最大主应力分布云图

    MN—应力最小值点;MX—应力最大值

    Figure  7.  Nephogram of maximum principal stress distribution in the well site

    图  8  模型4880~5025 m深度中心轴线上修正前后的最大、最小水平主应力曲线图

    Figure  8.  Maximum and minimum horizontal principal stress curves before and after correction on the center axis of themodel from 4880 m to 5025 m

    表  1  董11井原始测井数据

    Table  1.   Original logging data of the well Dong 11

    层号 顶界深度/m 底界深度/m 层厚/m 纵波时差/(μs/ft) 密度/(g/cm3) 结论
    1 4881.7 4883.1 1.4 62.69 2.46 干层
    2 4896.5 4904.6 8.1 60.48 2.36 含油水层
    3 4948.2 4950.1 1.9 60.22 2.41 干层
    4 4960 4962.1 2.1 60.64 2.22 干层
    5 4969.6 4970.6 1 64.28 2.13 干层
    6 4980.9 4989.3 8.4 61.5 2.37 差油层
    7 4993.2 5011.6 18.4 59.87 2.26 含油水层
    8 5012.5 5019.2 6.7 60.66 2.39 含油水层
    9 5020.9 5027.9 7 61.13 2.39 干层
    下载: 导出CSV

    表  2  董11井地层岩石物理参数及地应力计算结果

    Table  2.   Calculation results of formation rock physical parameters and ground stress of the well Dong 11

    层号 横波时差/(μs/ft) 泊松比 杨氏模量/MPa 静态泊松比 静态杨氏模量/MPa 垂向应力/MPa 水平最大主应力/MPa 水平最小主应力/MPa
    1 123.242209 0.325465 39925.5 0.207738 30865.54 112.2952 134.2244 103.3246
    2 122.771372 0.339779 39013.7 0.211307 30199.91 112.71265 135.7413 104.0711
    3 120.249713 0.332629 41307.1 0.209524 31874.06 113.83045 136.9144 104.782
    4 129.550533 0.359714 33449.4 0.216277 26137.97 114.10415 138.0337 106.2004
    5 142.575909 0.37244 26745.3 0.219449 21243.94 114.3123 137.7953 107.2011
    6 124.423321 0.33835 38104.9 0.210951 29536.48 114.6573 137.7719 105.9069
    7 125.946987 0.354034 35878 0.214861 27910.86 115.0552 139.2071 106.7745
    8 121.915141 0.335491 39938.3 0.210238 30874.87 115.36455 138.7411 106.3589
    9 122.859752 0.335491 39326.5 0.210238 30428.27 115.5612 138.8552 106.5873
    下载: 导出CSV
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  • 收稿日期:  2018-09-14
  • 修回日期:  2019-01-04
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