基于反函数原理的可控源大地电磁法全场域视电阻率定义

    Definition of full-field apparent resistivity of controlled source magnetotellurics based on inverse function principle

    • 摘要: 在电磁探测中,数据采集范围逐步扩大,为了避免非远区的电阻率畸变,基于反函数原理,给出了适合可控源电磁法全场域视电阻率的定义方法。该方法可以利用单分量进行广域视电阻计算,同样也可以利用多个分量进行广域视电阻计算。分别利用电场分量、磁场分量以及电场与磁场的比值计算均匀半空间与层状模型的全场域视电阻率,结果表明基于反函数原理的可控源大地电磁视电阻率定义方法能实现不受空间制约的频域视电阻率定义,可更好地反映地下介质电阻率的分布。

       

      Abstract: With the development of the wide-field electromagnetic method, the scope of data collection has been gradually expanded. To avoid the none-far-field resistivity distortion, this paper proposes a definition method suitable for the full-field apparent resistivity of the controlled-source electromagnetic method based on the inverse function principle. With this method, the full-field apparent resistivity can be calculated using a single component or multiple components. The full-field apparent resistivity of a homogeneous half-space model and a layered model was calculated using individual components of electric and magnetic fields and their ratios. The results show that the definition method proposed in this paper can achieve the definition of frequency-domain apparent resistivity that is not limited by space and thus can better reflect the resistivity distribution of underground media.

       

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