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    宋本钦, 李培军, 秦其明, 侯贵廷. 超低频电磁探测信号能量的计算及其地质应用[J]. 中国地质, 2008, 35(6): 1315-1321.
    引用本文: 宋本钦, 李培军, 秦其明, 侯贵廷. 超低频电磁探测信号能量的计算及其地质应用[J]. 中国地质, 2008, 35(6): 1315-1321.
    SONG Ben-qin, LI Pei-jun, QIN Qi-ming, HOU Gui-ting. The calculation of ultra-low electromagnetic signal energy and its geological applications[J]. GEOLOGY IN CHINA, 2008, 35(6): 1315-1321.
    Citation: SONG Ben-qin, LI Pei-jun, QIN Qi-ming, HOU Gui-ting. The calculation of ultra-low electromagnetic signal energy and its geological applications[J]. GEOLOGY IN CHINA, 2008, 35(6): 1315-1321.

    超低频电磁探测信号能量的计算及其地质应用

    The calculation of ultra-low electromagnetic signal energy and its geological applications

    • 摘要: 提要:被动式超低频电磁探测技术是一种有效的探测地下地质体和资源的手段,但采用现有的处理方法得到的探测曲线较容易受到各种噪声的干扰,影响了对所获得的探测曲线的解释。笔者将信号能量引入到超低频电磁探测信号的处理中。首先根据信号能量计算原理,计算不同深度的超低频探测信号的能量值,获取能量曲线。同时,根据具体应用目的,分析其曲线特征,并将信号能量曲线与现有的信号曲线,如最大值曲线、最小值曲线等进行对比分析。结果表明,与现有方法相比,笔者所提出的信号能量曲线方法能更准确地反映地下岩层特征,有利于曲线的地质解译。

       

      Abstract: Abstract:Passive ultra-low electromagnetic (ULEM) detection technique is one of the effective means for detection of subsurface and deep geological bodies and resources. However, the curves of ULEM detection obtained using the existing processing methods is sensitive to the noises, which could hamper the correct interpretation of resulting detection signal curves. In this paper, the signal energy was introduced to the processing of the detection signal. Firstly, according to the calculating principle of the signal energy, the energy value of the ultra-low electromagnetic signal for each sampling depth was calculated, and the energy curve was then generated. The obtained energy curve was analyzed and compared with the existing detection curves, such as the maximum and minimum of the magnitude, for some specific applications. The experimental results showed that compared with existing methods, the proposed signal energy method can more accurately reflect the characteristics of the rocks. The proposed method could facilitate the geological interpretation of the resulting curves.

       

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