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Time-frequency Analysis on Influence of Low resistive Shielding Layer in the Exploration of Transient Electromagnetic Field

机译:瞬态电磁场探测中低阻屏蔽层影响的时频分析

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The transient electromagnetic method will be influenced by shielding effect of the low-resistivity layer during its execution in the area of low-resistivity overlaid layers. Although the value of observing data, such as the induced electromotive force, is relatively large, the exploring depth is greatly reduced actually. In case of an overlying low-resistivity layer, longer exploring time is required to explore the same depth, which is because as a conductive medium, the ground is dispersive, and the electromagnetic wave transmits faster in high-resistivity bodies but slower in low-resistivity ones. What's worse, the electromagnetic wave will consume more energy in the low-resistivity layers. By adopting the smooth pseudo Wigner-Ville distribution and Gabor expansion, this article expands the attenuation curves of induced electromotive force respectively of the typical two-layer (D- and G-type)geo-electricity models and three-layer (H-, A-, K- and Q-type) geo-electricity models to the two-dimensional time-frequency plane. It is indicated by the study through comparing the analysis on time-frequency energy spectrum with the model that energy of the transient electromagnetic field really aggregates and is consumed in the low-resistivity layers; especially with respect to the A-type geo-electricity model (with earth's surface being the low-resistivity layer) describing the North China type coalfield of our country, energy of the transient electromagnetic field has been depleted when arriving at the bottom interface (interfaces of Ordovician limestone and coal series) of the greatest observing significance due to aggregation and consumption in the low-resistivity layers above the base during the process of its diffusion downwards from the ground surface. Therefore, during the transient electromagnetic exploration in areas of strata in A-type model, influence of the low resistive shielding layer shall be taken into full consideration, and relatively longer observing time window shall be selected to ensure the exploring depth and high-power instruments shall be adopted to increase the signal-noise ratio during construction design.
机译:在低电阻率覆盖层的区域中,瞬变电磁方法将在其执行期间受到低电阻率层的屏蔽效果的影响。尽管诸如感应电动势之类的观测数据的值相对较大,但实际上却大大减小了勘探深度。在上层低电阻率层的情况下,需要更长的探索时间才能探索相同的深度,这是因为作为导电介质,地面是分散的,并且电磁波在高电阻率体中的传输速度较快,而在低电阻率体中的传输速度较慢电阻率的。更糟糕的是,电磁波将在低电阻率层中消耗更多能量。通过采用平滑的伪Wigner-Ville分布和Gabor展开,本文分别扩展了典型的两层(D型和G型)地电模型和三层(H型)地电模型的感应电动势衰减曲线。二维时频平面的A,K和Q型地电模型。通过对时频能量谱的分析与模型的比较,表明该研究表明瞬态电磁场的能量确实在低电阻率层中聚集和消耗。特别是对于描述我国华北型煤田的A型地电模型(地表为低电阻层)而言,到达底部界面(界面)时瞬态电磁场的能量已经耗尽。 (奥陶纪石灰岩和煤系)之所以具有最大的观测意义,是因为在其从地表向下扩散的过程中,基层上方低电阻率层的聚集和消耗。因此,在A型模型的地层区域进行瞬变电磁勘探时,应充分考虑低阻屏蔽层的影响,并选择相对较长的观测时间窗口,以确保勘探深度和大功率仪器在施工设计中应采用增加信噪比的方法。

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