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作 者:张文伟[1,2,3] 真齐辉 底青云 ZHANG WenWei;ZHEN QiHui;DI QingYun(Key Laboratory of Shale Gas and Geoengineering,CAS,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China;Institutions of Earth Science,Chinese Academy of Sciences,Beijing 100029,China;University of Chinese Academy of Sciences,Beijing 100049,China)
机构地区:[1]中国科学院地质与地球物理研究所中国科学院页岩气与地质工程重点实验室,北京100029 [2]中国科学院地球科学研究院,北京100029 [3]中国科学院大学,北京100049
出 处:《地球物理学报》2018年第10期4171-4181,共11页Chinese Journal of Geophysics
基 金:国家重大科研装备研制项目"深部资源探测核心装备研发"(ZDYZ2012-1)-05子项目"多通道大功率电法勘探仪"项目与智能导钻系统集成与试验(XDA14050100)联合资助
摘 要:视电阻率在电磁法勘探中起重要作用,可以作为初步解释结果,多通道瞬变电磁法通过大地脉冲响应的峰值时刻定义视电阻率.鉴于传统方法计算峰值时刻视电阻率需要恢复完整大地脉冲响应,本文通过研究大地脉冲响应及其频谱特征,提出一种新的频率域比值法.利用参考谱及其与一般谱的伸缩因子计算一般谱的峰值时刻,进而得到视电阻率.该方法只需大地脉冲响应单个频点幅度谱,从而不用估计整个大地脉冲响应.实际计算时,可以用大地脉冲响应多个频点幅度谱得到平均视电阻率.模拟数据与实测数据结果表明,在一维介质中,频率域比值法可以得到合理的视电阻率.Apparent resistivity has played a significant role in electromagnetic exploration and is able to be used for preliminary interpretation.Multi-channels transient electromagnetic method defines the apparent resistivity using the peak time of earth impulse response.However,traditional method evaluating peak-time apparent resistivity need to recover the entitle earth impulse response.In this paper,a new frequency-domain ratio method is proposed by studying characteristics of both the impulse response and its spectrum.Apparent resistivity is obtained by calculating the peak time of the general spectrum using reference spectrum and scaling factor between the reference spectrum and the general one.Only single-point spectrum is needed to get the peak time,instead of estimating the entitle earth impulse response.In practical,multiple-points spectrum can be exploited to obtain the averaged apparent resistivity.The results from synthetic and field data show that frequency-domain ratio method gives reasonable apparent resistivity in one dimensional media.
关 键 词:多通道瞬变电磁法 频率域比值法 大地脉冲响应 峰值时刻 视电阻率
分 类 号:P631[天文地球—地质矿产勘探]
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