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Review paper: Instrumentation for marine magnetotelluric and controlled source electromagnetic sounding

机译:评论文章:船用大地电磁和受控源电磁测深仪

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We review and describe the electromagnetic transmitters and receivers used to carry out magnetotelluric and controlled source soundings in the marine environment. Academic studies using marine electromagnetic methods started in the 1970s but during the last decade these methods have been used extensively by the offshore hydrocarbon exploration industry. The principal sensors (magnetometers and non-polarizing electrodes) are similar to those used on land but magnetotelluric field strengths are not only much smaller on the deep sea-floor but also fall off more rapidly with increasing frequency. As a result, magnetotelluric signals approach the noise floor of electric field and induction coil sensors (0.1 nV/m and 0.1 pT) at around 1 Hz in typical continental shelf environments. Fluxgate magnetometers have higher noise than induction coils at periods shorter than 500 s but can still be used to collect sea-floor magnetotelluric data down to 40-100 s. Controlled source transmitters using electric dipoles can be towed continuously through the seawater or on the sea-bed, achieving output currents of 1000 A or more, limited by the conductivity of seawater and the power that can be transmitted down the cables used to tow the devices behind a ship. The maximum source-receiver separation achieved in controlled source soundings depends on both the transmitter dipole moment and on the receiver noise floor and is typically around 10 km in continental shelf exploration environments. The position of both receivers and transmitters needs to be navigated using either long baseline or short baseline acoustic ranging, while sea-floor receivers need additional measurements of orientations from compasses and tiltmeters. All equipment has to be packaged to accommodate the high pressure (up to 40 MPa) and corrosive properties of seawater. Usually receiver instruments are self-contained, battery powered and have highly accurate clocks for timekeeping, even when towed on the sea-floor or in the water column behind a transmitter.
机译:我们回顾并描述了用于在海洋环境中进行大地电磁和受控源探测的电磁发射器和接收器。使用海洋电磁方法的学术研究始于1970年代,但在最近十年中,这些方法已被海上油气勘探行业广泛使用。主要传感器(磁力计和非极化电极)与陆地上使用的传感器相似,但是大地电磁场强度不仅在深海底小得多,而且随着频率的增加而下降得更快。结果,在典型的大陆架环境中,大地电磁信号以大约1 Hz的频率接近电场和感应线圈传感器的本底噪声(0.1 nV / m和0.1 pT)。 Fluxgate磁力计在小于500 s的时间内比感应线圈具有更高的噪声,但仍可用于收集40-100 s的海底大地电磁数据。使用电偶极子的受控源发射器可以在海水中或在海床上连续拖曳,实现1000 A或更高的输出电流,这受海水的电导率和可以通过拖曳设备的电缆传输的功率的限制在船后面。在受控的源探测中,最大的源-接收器间隔取决于发射器偶极矩和接收器本底噪声,在大陆架勘探环境中通常约为10 km。接收器和发射器的位置都需要使用长基线或短基线声学测距进行导航,而海底接收器则需要使用罗盘和倾角仪对方位进行额外的测量。必须包装所有设备以适应高压(最高40 MPa)和海水的腐蚀性。通常,接收器仪器是独立的,由电池供电的,并且具有高度精确的时钟以进行计时,即使拖曳在发射器后面的海底或水柱中也是如此。

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