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Continuous TDEM for monitoring shale hydraulic fracturing

机译:连续TDEM监测页岩水力压裂

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摘要

Monitoring and delineating the spatial distribution of shale fracturing is fundamentally important to shale gas production.Standard monitoring methods,such as time-lapse seismic,cross-well seismic and micro-seismic methods,are expensive,timeconsuming,and do not show the changes in the formation with time.The resistivities of hydraulic fracturing fluid and reservoir rocks were measured.The results suggest that the injection fluid and consequently the injected reservoir are characterized by very low resistivity and high chargeability.This allows using of the controlled-source electromagnetic method (CSEM) to monitor shale gas hydraulic fracturing.Based on the geoelectrical model which was proposed according to the well-log and seismic data in the test area the change rule of the reacted electrical field was studied to account for the change of shale resistivity,and then the normalized residual resistivity method for time lapse processing was given.The time-domain electromagnetic method (TDEM) was used to continuously monitor the shale gas fracturing at the Fulin shale gas field in southern China.A high-power transmitter and multi-channel transient electromagnetic receiver array were adopted.9 h time series of Ex component of 224 sites which were laid out on the surface and over three fracturing stages of a horizontal well at 2800 m depth was recorded.After data processing and calculation of the normalized resistivity residuals,the changes in the Ex signal were determined and a dynamic 3D image of the change in resistivity was constructed.This allows modeling the spatial distribution of the fracturing fluid.The model results suggest that TDEM is promising for monitoring hydraulic fracturing of shale.
机译:监测和描述页岩压裂的空间分布对页岩气的生产至关重要。标准监测方法,如时移地震法,井间地震法和微地震法,既昂贵又费时,并且没有显示出变化。测量了水力压裂液和储层岩石的电阻率,结果表明注入流体以及注入的储层具有极低的电阻率和较高的荷电率,这允许使用控制源电磁法( CSEM)来监测页岩气的水力压裂。根据测试区域的测井和地震数据提出的地电模型,研究了反应电场的变化规律,以解决页岩电阻率的变化,并然后给出了归一化残余电阻率法用于时移处理的方法。时域电磁法( (TDEM)连续监测中国南部富林页岩气田的页岩气压裂,采用大功率发射器和多通道瞬变电磁接收器阵列。在224个站点的Ex分量的9 h时间序列记录并记录了水平井在2800 m深度的三个压裂阶段的数据。经过数据处理和归一化电阻率残差的计算后,确定了Ex信号的变化,并获得了电阻率变化的动态3D图像该模型结果表明TDEM在监测页岩的水力压裂方面很有前途。

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  • 来源
    《应用地球物理(英文版)》 |2018年第1期|26-34|共9页
  • 作者单位

    Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China;

    Jianghan Division, Petroleum Geophysics Engineering Company, SINOPEC, Wuhan 430040, China;

    Geophysical Prospecting Company, CCDC, Chengdu, 610213, China;

    Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China;

    Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China;

    Hubei Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China;

    Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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