水压致裂试验过程中的地电效应研究

陈宝华, 史磷华, 骆永妙

陈宝华, 史磷华, 骆永妙. 1989: 水压致裂试验过程中的地电效应研究. 地震学报, 11(3): 309-318.
引用本文: 陈宝华, 史磷华, 骆永妙. 1989: 水压致裂试验过程中的地电效应研究. 地震学报, 11(3): 309-318.
Chen Baohua, Shi Linhua, Luo Yongmiaocom sh advance. 1989: A STUDY OF THE GEOELECTRIC EFFECT ON THE PROCESS OF HYDRAULIC FRACTURING EXPERIMENTS. Acta Seismologica Sinica, 11(3): 309-318.
Citation: Chen Baohua, Shi Linhua, Luo Yongmiaocom sh advance. 1989: A STUDY OF THE GEOELECTRIC EFFECT ON THE PROCESS OF HYDRAULIC FRACTURING EXPERIMENTS. Acta Seismologica Sinica, 11(3): 309-318.

水压致裂试验过程中的地电效应研究

A STUDY OF THE GEOELECTRIC EFFECT ON THE PROCESS OF HYDRAULIC FRACTURING EXPERIMENTS

  • 摘要: 本文总结了在水压致裂试验现场多台电法仪器测量和记录到的加压过程中的地电效应,并得到一些能反映岩石破裂情况的有意义的结果:(1)随着压力增加,电阻率明显上升.当压力超过岩石临界应力的一半以后,电阻率即很快地下降,卸压后又逐步回升,其变化椭圆的长轴方向与岩石破裂面的延伸方向是一致的;(2)以压力孔为中心的自然电位及ZK2,ZK14孔的井下电位都伴随着加压过程而变化,强烈反映了过滤电场与孔隙水压力的相关性.
    Abstract: In the paper,the geoelectric effects associated with the pressurization measured and recorded by electric instruments in sites of hydraulic fracturing experiments are summarized,and some significant results corresponding to rock failure are also obtained as follows:(1)With the increase of pressure,the resistivity rises distinctly. Affer the pressure has exceeded a half of rock critical stress,the resistivity drops rapidly; and during the release stress,the resistivity gradually rises again.(2)The self-potential centered on the pressure hole and the electric potential in the wells ZK2 and ZK14 change with the pressurization,all reflect strongly the correlation between the percolated electric field and the pore pressure gradient.
  • [1] Brace, W.F. and Orang, A.S., 19G8. Electrical risistivity changes in saturated rocks during fracture and frictional sliding. J. Geopl:ys. Res., 73, 1433——1445.

    [2] Лархомеко, Э.И., 1965, Электрицеские Свойства Горных Пород..Иаука,No.3,104——107.

    [3] 张天中、华正兴、涂明发,1985. 1.2千巴围压下岩徉破裂和摩擦滑动过程中电阻率变化.地震学报,7, 428——432.

    [4] 赵玉休、钱复业、杨体成、刘建毅,1983.原地电阻率变化的实验.地震学报,5, 217——324.

    [5] 林纪曾、粱国昭、赵毅、谢明富,1980.东南沿海地区的震源机制与构造应力场.地震学报,2,245——257.

    [6] 中南矿冶学院物探教研室,1980.金属矿电法勘探,182——191.冶金工业出版社.

    [7] 孙正江、王华俊,1984.地电概论,23——32.地震出版社.

    [1] Brace, W.F. and Orang, A.S., 19G8. Electrical risistivity changes in saturated rocks during fracture and frictional sliding. J. Geopl:ys. Res., 73, 1433——1445.

    [2] Лархомеко, Э.И., 1965, Электрицеские Свойства Горных Пород..Иаука,No.3,104——107.

    [3] 张天中、华正兴、涂明发,1985. 1.2千巴围压下岩徉破裂和摩擦滑动过程中电阻率变化.地震学报,7, 428——432.

    [4] 赵玉休、钱复业、杨体成、刘建毅,1983.原地电阻率变化的实验.地震学报,5, 217——324.

    [5] 林纪曾、粱国昭、赵毅、谢明富,1980.东南沿海地区的震源机制与构造应力场.地震学报,2,245——257.

    [6] 中南矿冶学院物探教研室,1980.金属矿电法勘探,182——191.冶金工业出版社.

    [7] 孙正江、王华俊,1984.地电概论,23——32.地震出版社.

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  • 发布日期:  2011-09-01

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