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Artificial Source Near-Zone Frequency Domain Electromagnetic Sounding Method

机译:人工源近区频域电磁探测方法

摘要

#$%^&*AU2020100504A420200514.pdf#####Abstract The invention discloses an artificial source near-zone frequency domain electromagnetic sounding method, comprising the following steps of: S1, setting a transmitting source and a receiving system, and observing a total vertical magnetic-field component of an artificial source; S2, calculating a primary vertical component generated by the transmitting source at an observation point; S3, calculating a pure induction electric field generated by the earth at the observation point based on the total vertical magnetic-field component and the primary vertical component generated by the transmitting source; and S4, calculating the resistivity and depth information of the earth based on the pure induction electric field generated by the earth. According to the characteristic that a primary field and an induction field in the vertical magnetic-field component are easy to separate, the invention provides a method for sounding a formation electrical structure by utilizing the pure induction field, and the method is a novel artificial source frequency domain electromagnetic observation and data processing technology, which can significantly shorten a transmitter-receiver distance of artificial source frequency sounding and improve the resolution of the formation electrical structure.1/5 S1, setting a transmitting source and a receiving system, and observing a total vertical magnetic-field component of an artificial source. S2,, calculating a primLoary veBrtical -compon-ent generated by the transmiLttiLng sourc-e at an observation poi-nt. 53, tdi-=latingam uktianelectric field genenated by the emrth at the abservatin maint bsed n the total vertical mEsnetic-field cr- net md the Primerr vertical crminet grated by the tr -i tting source. 54, calculating the resistivity and depth information of the earth based on the pure induction electric field generated by the earth. Fig. 1
机译:#$%^&* AU2020100504A420200514.pdf #####抽象本发明公开了一种人工源近区频域电磁测深方法,包括以下步骤:S1,设置发送源和接收系统,并观察人造源的总垂直磁场分量; S2,计算发射源在观测时产生的主要垂直分量点; S3,计算地球在观测点产生的纯感应电场基于总垂直磁场分量和初级垂直分量由发射源产生;和S4,计算电阻率和深度信息基于地球产生的纯感应电场的地球。根据垂直磁场分量中的主场和感应场的特性易于分离,本发明提供了一种探测地层电气结构的方法利用纯感应场,该方法是一种新型的人工源频域电磁观测和数据处理技术,可以大大缩短人工源频率探测的收发距离,提高了信号的分辨率。形成电气结构。1/5S1,设置发送源和接收系统,以及观察磁场的总垂直磁场分量人工来源。S2,计算由...生成的primLoary veBrical-分量。在观察点传输信号。53,tdi- = latingam英国埃姆特电场产生的电场abservatin维护在垂直垂直总磁场中由排放源磨碎的Primerr立式生奶油。54,计算电阻率和深度信息地球是基于由地球。图。1

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