{"title":"地基瞬变电磁法中磁感应数据的一维全波形反演","authors":"Jianhui Li, Xingchun Wang, Xiangyun Hu, Hongzhu Cai, Qingquan Zhi, Shi Chen","doi":"10.1093/jge/gxad025","DOIUrl":null,"url":null,"abstract":"\n The full waveform effects refer to the total effects of turn-on, steady, and turn-off durations for a transmitting-current waveform as well as its repetition number in transient electromagnetic (TEM) methods. In this study, the full waveform effects are investigated using both forward-modelling and inversion methods considering typical background noise. The forward-modelling results of homogeneous half-space models show that the magnetic induction, bz, is less affected by the background noise but more affected by the full waveform effects than the time derivative of magnetic induction ∂bz/∂t. Therefore, this study focuses on investigating the full waveform effects on bz. The inversion results for synthetic and field examples show that the inversion algorithm without considering the full waveform effects leads to over-estimated resistivities in deeper parts of the recovered models compared to the true model. Therefore, it is crucial to consider the full waveform effects when processing TEM data. Furthermore, a standard deviation factor (STDF) is estimated for model parameters of the inversion. The results show that the STDF increases as the layer depth increases for 1D layered models. This indicates that the inverted parameters are well resolved for shallower layers and moderately to poorly resolved for deeper layers.","PeriodicalId":54820,"journal":{"name":"Journal of Geophysics and Engineering","volume":" ","pages":""},"PeriodicalIF":1.6000,"publicationDate":"2023-04-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"One-dimensional full-waveform inversion for magnetic induction data in ground-based transient electromagnetic methods\",\"authors\":\"Jianhui Li, Xingchun Wang, Xiangyun Hu, Hongzhu Cai, Qingquan Zhi, Shi Chen\",\"doi\":\"10.1093/jge/gxad025\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\\n The full waveform effects refer to the total effects of turn-on, steady, and turn-off durations for a transmitting-current waveform as well as its repetition number in transient electromagnetic (TEM) methods. In this study, the full waveform effects are investigated using both forward-modelling and inversion methods considering typical background noise. The forward-modelling results of homogeneous half-space models show that the magnetic induction, bz, is less affected by the background noise but more affected by the full waveform effects than the time derivative of magnetic induction ∂bz/∂t. Therefore, this study focuses on investigating the full waveform effects on bz. The inversion results for synthetic and field examples show that the inversion algorithm without considering the full waveform effects leads to over-estimated resistivities in deeper parts of the recovered models compared to the true model. Therefore, it is crucial to consider the full waveform effects when processing TEM data. Furthermore, a standard deviation factor (STDF) is estimated for model parameters of the inversion. The results show that the STDF increases as the layer depth increases for 1D layered models. This indicates that the inverted parameters are well resolved for shallower layers and moderately to poorly resolved for deeper layers.\",\"PeriodicalId\":54820,\"journal\":{\"name\":\"Journal of Geophysics and Engineering\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":1.6000,\"publicationDate\":\"2023-04-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysics and Engineering\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1093/jge/gxad025\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysics and Engineering","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1093/jge/gxad025","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
One-dimensional full-waveform inversion for magnetic induction data in ground-based transient electromagnetic methods
The full waveform effects refer to the total effects of turn-on, steady, and turn-off durations for a transmitting-current waveform as well as its repetition number in transient electromagnetic (TEM) methods. In this study, the full waveform effects are investigated using both forward-modelling and inversion methods considering typical background noise. The forward-modelling results of homogeneous half-space models show that the magnetic induction, bz, is less affected by the background noise but more affected by the full waveform effects than the time derivative of magnetic induction ∂bz/∂t. Therefore, this study focuses on investigating the full waveform effects on bz. The inversion results for synthetic and field examples show that the inversion algorithm without considering the full waveform effects leads to over-estimated resistivities in deeper parts of the recovered models compared to the true model. Therefore, it is crucial to consider the full waveform effects when processing TEM data. Furthermore, a standard deviation factor (STDF) is estimated for model parameters of the inversion. The results show that the STDF increases as the layer depth increases for 1D layered models. This indicates that the inverted parameters are well resolved for shallower layers and moderately to poorly resolved for deeper layers.
期刊介绍:
Journal of Geophysics and Engineering aims to promote research and developments in geophysics and related areas of engineering. It has a predominantly applied science and engineering focus, but solicits and accepts high-quality contributions in all earth-physics disciplines, including geodynamics, natural and controlled-source seismology, oil, gas and mineral exploration, petrophysics and reservoir geophysics. The journal covers those aspects of engineering that are closely related to geophysics, or on the targets and problems that geophysics addresses. Typically, this is engineering focused on the subsurface, particularly petroleum engineering, rock mechanics, geophysical software engineering, drilling technology, remote sensing, instrumentation and sensor design.