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A method for monitoring a high-resistivity reservoir rock formation

机译:一种监测高电阻率储层岩层的方法

摘要

A method for monitoring a high-resistivity reservoir rock formation ( 2 ) below one or more less resistive formations ( 3 ). The method includes transmitting an electromagnetic signal (S) propagating from near a seafloor or land surface ( 1 ) by means of an electromagnetic transmitter ( 5 ) powered by a voltage signal generator (G). The electromagnetic signal (S) propagates from the seafloor ( 1 ) and is guided along a conductive string ( 7 ) to the high-resistive formation ( 2 ), and propagates as a guided-wave electromagnetic signal (S 2 ) at a relatively higher speed (V 2 ) inside the high-resistivity formation ( 2 ) than a propagation speed (V 3 ) in the less resistive formations ( 3 ). The guided-wave electromagnetic signal (S 2 ) gives rise to an upward refracting electromagnetic signal (R 3 ) having the relatively lower propagation speed (V 3 ) in the less resistive formations ( 3 ) and having an exit angle nearer to the normal (N) to the interface between the high-resistivity formation ( 2 ) and the lower-resistivity formation ( 3 ), and gives rise to a steeply rising refraction wave front (F 3 ). The refracted electromagnetic wave front (F 3 ) includes refracted electromagnetic signals (R 3 ) detected along an array of sensor antennas ( 6 a, 6 b, 6 c, . . . , 6 k, . . . , 6 n) positioned along the seafloor. The array having a direction away from the transmitter ( 5 ).
机译:一种监测一个或多个电阻率较低的地层(3)以下的高电阻率储层岩层(2)的方法。该方法包括借助于由电压信号发生器(G)供电的电磁发射器(5)发射从海底或陆地表面(1)附近传播的电磁信号(S)。电磁信号(S)从海底(1)传播,并沿着导电线(7)被引导至高阻构造(2),并作为导波电磁信号(S 2)在相对较高的位置传播。高电阻率地层(2)内的传播速度(V 3)高于低电阻率地层(3)内的传播速度(V 3)。导波电磁信号(S 2)产生一个向上折射的电磁信号(R 3),在电阻较小的地层(3)中具有相对较低的传播速度(V 3),并且出射角更接近法线( N)到达高电阻率地层(2)和低电阻率地层(3)之间的界面,并引起陡峭上升的折射波阵面(F 3)。折射电磁波阵面(F 3)包括沿着沿其定位的传感器天线(6a,6b,6c,...,6 k,...,6 n)阵列检测到的折射电磁信号(R 3)。海底。阵列具有远离发射器(5)的方向。

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