吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1268-1275.doi: 10.13278/j.cnki.jjuese.20210049

• 地球探测与信息技术 • 上一篇    下一篇

Kelvin-Voigt黏弹性介质井孔声场有限差分数值模拟与波形特征

岳崇旺1, 王祝文2   

  1. 1. 长安大学地质工程与测绘学院, 西安 710054;
    2. 吉林大学地球探测科学与技术学院, 长春 130026
  • 收稿日期:2021-02-06 出版日期:2021-07-26 发布日期:2021-08-02
  • 作者简介:岳崇旺(1981-),男,讲师,博士,主要从事测井理论及测井解释方法研究,E-mail:ycw1981@163.com
  • 基金资助:
    国家自然科学基金项目(41874135,41504090)

Numerical Simulation and Waveform Characteristics of Borehole Acoustic Field in Kelvin-Voigt Viscoelastic Medium Well

Yue Chongwang1, Wang Zhuwen2   

  1. 1. College of Geological Engineering & Surveying, Chang'an University, Xi'an 710054, China;
    2. College of GeoExploration Science and Technology, Jilin University, Changchun 130026, China
  • Received:2021-02-06 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the National Natural Science Foundation of China (41874135, 41504090)

摘要: 岩石介质具有黏滞性,黏弹性介质模型相对于弹性介质模型更为接近岩石介质的真实情况。根据Kelvin-Voigt黏弹性单元体模型本构关系,推导了柱坐标系下各向同性黏弹性介质时间域交错网格有限差分方程,进行了黏弹性介质井孔声场的数值模拟。模拟结果表明:品质因子和声源中心频率对黏弹性介质中的井内外声场均有影响:井外声场和井内声场的衰减均随品质因子的增大而减小,井外声波和井内反射波振幅随之增大;井外声场的衰减随声源中心频率的增大而减小,井外声波振幅随之增大,井内声场的衰减随声源中心频率的增大而增大,井内反射波振幅随之减小。

关键词: Kelvin-Voigt模型, 黏弹性介质, 交错网格有限差分, 井孔声场, 波形特征

Abstract: The rock medium has viscous properties, and the viscoelastic medium model is closer to the real situation of the rock medium than the elastic medium model. According to the constitutive relationship of the Kelvin-Voigt viscoelastic element model, the staggered grid finite difference equations of the viscoelastic isotropic medium in the cylindrical coordinate system are derived, and the numerical simulation of acoustic field of the wellbore in viscoelastic medium are completed. The simulation results show that the rock quality factor and the acoustic source center frequency have effects on the acoustic field inside and outside the well in the viscoelastic medium:The attenuation of the acoustic field outside and inside the well decreases with the increase of the quality factor, and the wave amplitude outside the well and the reflected wave amplitude increase accordingly; The attenuation of the acoustic field outside the well decreases with the increase of the source center frequency, and the wave amplitude outside the well increases accordingly; The attenuation of the acoustic field in the well increases with the increase of the source center frequency, and the wave amplitude in the well decreases accordingly.

Key words: Kelvin-Voigt model, viscoelastic medium, staggered grid finite difference, borehole acoustic field, waveform characteristics

中图分类号: 

  • P631.8
[1] 孙成禹.地震波理论与方法[M]. 东营:中国石油大学出版社,2007. Sun Chengyu. Theory and Methods of Seismic Waves[M]. Dongying:China University of Petroleum Publishing House, 2007.
[2] Madja G, Chin R C Y, Followill F E. A Perturbation Theory for Love Waves in Anelastic Media[J]. Geophysical Journal of the Royal Astronomical Society, 1985, 80(1):1-34.
[3] 刘瑞珣,张秉良,张臣. 描述岩石黏弹性固体性质的开尔文模型[J]. 地学前缘,2008,15(3):221-225. Liu Ruixun, Zhang Bingliang, Zhang Chen. The Kelvin Model Describing Rock Materials with Behaviour of a Viscoelastic Solid[J]. Earth Science Frontiers, 2008, 15(3):221-225.
[4] Emmerich H, Korn M. Incorporation of Attenuation into Time-Domain Computations of Seismic Wave Fields[J]. Geophysics, 1987, 52(9):1252-1264.
[5] Robertsson J O A, Blanch J O, Symes W W. Viscoelastic Finite-Difference Modeling[J]. Geophysics, 1994, 59(9):1444-1456.
[6] Robertsson J O A. A Numerical Free-Surface Condition for Elastic/Viscoelastic Finite-Difference Modeling in the Presence of Topography[J]. Geophysics, 1996, 61(6):1921-1934.
[7] Saenger E H, Bohlen T. Finite-Difference Modeling of Viscoelastic and Anisotropic Wave Propagation Using the Rotated Staggered Grid[J]. Geophysics, 2004, 69(2):583-591.
[8] Bai Tong,Tsvankin I. Time-Domain Finite-Difference Modeling for Attenuative Anisotropic Media[J]. Geophysics, 2016, 81(2):c69-c77.
[9] 杜启振,杨慧珠. 线性黏弹性各向异性介质速度频散和衰减特征研究[J]. 物理学报,2002,51(9):2101-2108. Du Qizhen, Yang Huizhu. Velocity Dispersion and Attenuation in Anisotropic Linear Viscoelastic Media[J]. Acta Physica Sinica, 2002, 51(9):2101-2108.
[10] 杜启振. 各向异性黏弹性介质伪谱法波场模拟[J]. 物理学报,2004, 53(12):4428-4434. Du Qizhen. Wavefield Forward Modeling with the Pseudo-Spectral Method in Viscoelastic and Azimuthally Anisotropic Media[J]. Acta Physica Sinica, 2004, 53(12):4428-4434.
[11] 苑春方,彭苏萍,张中杰,等. Kelvin-Voigt均匀黏弹性介质中传播的地震波[J].中国科学:D辑:地球科学, 2005, 35(10):957-962. Yuan Chunfang, Peng Suping, Zhang Zhongjie, et al. Seismic Wave of Propagation in Homogeneous Kelvin-Voigt Viscoelastic Medium[J]. Science in China:Series D:Earth Sciences, 2005, 35(10):957-962.
[12] 孙成禹,印兴耀.三参数常Q黏弹性模型构造方法研究[J]. 地震学报,2007,29(4):348-357. Sun Chengyu, Yin Xingyao. Construction of Constant-Q Viscoelastic Model with Three Parameters[J]. Acta Seismologica Sinica, 2007, 29(4):348-357.
[13] 孙成禹,肖云飞,印兴耀,等. 黏弹介质波动方程有限差分解的稳定性研究[J].地震学报,2010,32(2):147-156. Sun Chengyu, Xiao Yunfei, Yin Xingyao, et al. Study on the Stability of Finite Difference Solution of Visco-Elastic Wave Equations[J].Acta Seismologica Sinica, 2010,32(2):147-156.
[14] 郭智奇. 黏弹各向异性介质波场模拟与储层信息研究[D]. 长春:吉林大学,2008. Guo Zhiqi. Wave Field Modeling in Viscoelastic Anisotropic Media and Reservoir Information Study[D]. Changchun:Jilin University, 2008.
[15] Guo Zhiqi, Liu Xiwu, Fu Wei, et al. Modeling and Anlysis of Azimuthal AVO Responses from a Viscoelastic Anisotropic Reflector[J]. Applied Geophysics, 2015, 12(3):441-452.
[16] 刘财,胡宁,郭志奇,等. 基于分数阶时间导数常Q黏弹本构关系的含黏滞流体双相VTI介质中波场数值模拟[J].地球物理学报,2018,61(6):2446-2458. Liu Cai,Hu Ning, Guo Zhiqi, et al. Numerical Simulation of the Wavefield in a Viscous Fluid-Saturated Two-Phase VTI Medium Based on the Constant-Q Viscoelastic Constitutive Relation with a Fractional Temporal Derivative[J]. Chines Journal of Geophysics, 2018,61(6):2446-2458.
[17] 邵广周,赵凯鹏,吴华. 基于MPI的面波有限差分正演模拟[J].吉林大学学报(地球科学版),2020,50(1):294-303. Shao Guangzhou, Zhao Kaipeng, Wu Hua. Finite Difference Forward Modeling of Surface Waves Based on MPI[J]. Journal of Jilin University (Earth Science Edition), 2020, 50(1):294-303.
[18] 张壹,王赟,王祥春,等. 黏弹性介质地震波吸收衰减研究进展[J].石油物探,2021,60(2):238-250. Zhang Yi, Wang Yun, Wang Xiangchun, et al. Research Progress on the Absorption Attenuation of Seismic Waves in Viscoelastic Media[J]. Geophysical Prospecting for Petroleum, 2021, 60(2):238-250.
[19] Alford R M, Kelly K R, Boore D M. Accuracy of Finite-Difference Modeling of Acoustic Wave Equation[J]. Geophysics, 1974, 39(6):834-842.
[1] 张恩威, 孟庆涛, 唐佰强, 胡菲, 党微.  基于机器学习的TOC测井预测方法:以松辽盆地南部青山口组一段为例[J]. 吉林大学学报(地球科学版), 2026, 56(3): 1062-1075.
[2] 曹志民, 张丽, 郑兵, 韩建. 基于SMOTE平衡数据的极端随机树岩性识别[J]. 吉林大学学报(地球科学版), 2025, 55(4): 1372-1386.
[3] 乔科宇, 邹长春, 彭诚.

基于CIFLog软件的测井旋回地层学分析模块开发与应用 [J]. 吉林大学学报(地球科学版), 2025, 55(2): 686-696.

[4] 曹志民, 丁璐, 韩建, 郝乐川, .

基于集成机器学习的测井曲线大尺度差异超分辨 [J]. 吉林大学学报(地球科学版), 2025, 55(2): 670-685.

[5] 蔺学旻, 肖红琳. 缝洞型储层声波远探测测井响应模拟及应用——以塔河油田碳酸盐岩缝洞型储层为例[J]. 吉林大学学报(地球科学版), 2025, 55(1): 312-327.
[6] 李建光, 孙超, 蔡来星, 屈少波, 童雪瑞, 窦中浩, 姜志海. 煤系岩石电性特征与含水饱和度定量关系实验——以山西宁武榆树坡为例[J]. 吉林大学学报(地球科学版), 2024, 54(5): 1724-1735.
[7] 庞志超, 肖华, 毛晨飞, 陈国军, 梁琬坤, 高明, 张啸. 准噶尔盆地南缘地区含膏质地层岩性特征及测井识别方法[J]. 吉林大学学报(地球科学版), 2024, 54(4): 1419-1431.
[8] 管耀, 王清辉, 冯进, 杨清, 石磊. 基于机器学习的蚀变火成岩测录井综合岩性识别——以南海北部珠江口盆地惠州26-6井区为例#br#[J]. 吉林大学学报(地球科学版), 2024, 54(1): 345-358.
[9] 王婷婷, 孙振轩, 戴金龙, 姜基露, 赵万春.

松辽盆地中央坳陷区储层岩性智能识别方法 [J]. 吉林大学学报(地球科学版), 2023, 53(5): 1611-1622.

[10] 张强, 李家金, 王毛毛, 唐湘飞. 基于改进主成分分析法的测井曲线岩性分层技术[J]. 吉林大学学报(地球科学版), 2022, 52(4): 1369-.
[11] 刘亮, 丁慧, 潘和平, 王磊. 考虑裂缝规模的红河油田延长组油层产能模糊识别方法[J]. 吉林大学学报(地球科学版), 2023, 53(1): 297-306.
[12] 丁磊, 陈殿远, 胡向阳, 张恒荣, 王一. 加速动态时间规整算法在测井曲线相似性度量中的改进及其应用[J]. 吉林大学学报(地球科学版), 2022, 52(6): 2042-2050.
[13] 张丽华, 王敏, 单刚义, 潘保芝, 曹玥. 不同岩性火山岩孔隙度压力敏感性及其影响因素:以长岭断陷火山岩为例[J]. 吉林大学学报(地球科学版), 2022, 52(2): 382-389.
[14] 崔裔曈, 王祝文, 徐方慧, 韩锐羿, 齐兴华. 基于斯通利波及电成像测井数据对火成岩裂缝地层的特征分析[J]. 吉林大学学报(地球科学版), 2022, 52(2): 624-632.
[15] 吴蒙, 秦云虎, 王晓青, 杨柳, 朱士飞, 张震, 毛礼鑫, 张静, 李国璋. 任家庄煤矿煤层煤质测井响应及其预测模型[J]. 吉林大学学报(地球科学版), 2022, 52(2): 633-643.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 初凤友,孙国胜,李晓敏,马维林,赵宏樵. 中太平洋海山富钴结壳生长习性及控制因素[J]. J4, 2005, 35(03): 320 -0325 .
[2] 周丽萍, 申向东, 李学斌, 白忠强. 天然浮石粉水泥土力学性质的试验研究[J]. J4, 2009, 39(3): 492 -497 .
[3] 黄玉龙, 王璞珺, 邵锐. 火山碎屑岩的储层物性--以松辽盆地营城组为例[J]. J4, 2010, 40(2): 227 -236 .
[4] 潘殿琦,张祖培,潘殿彩,陈义民,徐 瑞. 人工冻土纵波波速与温度和含水率的关系[J]. J4, 2006, 36(04): 588 -591 .
[5] 付 哲,周云轩,刘殿伟,刘万崧. 基于特征的面向对象虚拟GIS数据模型设计与原型系统实现[J]. J4, 2006, 36(04): 647 -652 .
[6] 滕吉文, 刘财, 韩立国, 阮小敏, 闫雅芬, 张永谦. 汶川—映秀MS8.0地震的介质破裂与深部物质运移的动力机制[J]. J4, 2009, 39(4): 559 -583 .
[7] 卢进才,李玉宏,魏仙样,魏建设. 鄂尔多斯盆地三叠系延长组长7油层组油页岩沉积环境与资源潜力研究[J]. J4, 2006, 36(6): 928 -0932 .
[8] 黄继国,黄国鑫,聂广正,魏海娟,吕爱民,王雪松. 中温UBF与UASB两相厌氧系统处理垃圾渗滤液的实验研究[J]. J4, 2007, 37(1): 144 -0147 .
[9] 孙才志,刘玉兰,杨 俊. 下辽河平原地下水生态水位与可持续开发调控研究[J]. J4, 2007, 37(2): 249 -254 .
[10] 舒萍,曲延明,王国军,丁日新,艾兴波,纪学雁,唐华风,边伟华,王璞珺. 松辽盆地火山岩储层裂缝地质特征与地球物理识别[J]. J4, 2007, 37(4): 726 -0733 .