吴如山, 徐韶辉. 1979: 数字全息成象在钻孔电波勘探中的应用. 地震学报, 1(2): 197-213.
引用本文: 吴如山, 徐韶辉. 1979: 数字全息成象在钻孔电波勘探中的应用. 地震学报, 1(2): 197-213.
Wu Ru-shan, Xu Shao-hui hr. 1979: DIGITAL HOLOGRAPHY APPLIED TO BOREHOLE ELECTROMAGNETIC WAVE EXPLORATION. Acta Seismologica Sinica, 1(2): 197-213.
Citation: Wu Ru-shan, Xu Shao-hui hr. 1979: DIGITAL HOLOGRAPHY APPLIED TO BOREHOLE ELECTROMAGNETIC WAVE EXPLORATION. Acta Seismologica Sinica, 1(2): 197-213.

数字全息成象在钻孔电波勘探中的应用

DIGITAL HOLOGRAPHY APPLIED TO BOREHOLE ELECTROMAGNETIC WAVE EXPLORATION

  • 摘要: 在简述了全息成象的一般原理, 并讨论了全息成象应用于钻孔电波勘探的物理基础之后, 着重介绍了多重全息图的概念及其合成成象技术.指明了对钻孔电波勘探的多次定点观测曲线和多次同步观测曲线, 可利用多重全息图及合成成象技术进行联合处理, 以提高分辨力和成象质量.并证明这相当于接收天线阵和发射天线阵依次聚焦在每一成象点上的双聚焦扫描成象的过程.文中对双孔透射法和单孔反射法都进行了讨论, 并给出了相应的计算公式;然后讨论了资料处理中的几个问题, 如发射点象的干扰及其消除、透射全息的屏蔽区问题、水平同步成象时的双象问题等, 并同时介绍了用衍射点模型进行计算机模拟的结果。最后给出了对水槽模型试验资料的处理结果和野外资料的试算结果.

     

    Abstract: After a brief description on the prineiples of holography and a discussion on the physical fundamentals relating to the application of holography to borehole electromagnetic wave exploration, the conleept of multiple-hologram and the associated teelmique for its synthetic imaging are presented. It is demonstrated that for bore-hole electromagnetic wave exploration the (curves from various fixed-point and synchronously moving measurements can be processed jointly, using the multiple-hologram synthetic imaging technique, to improve the resolution and image quality. It is also proved that this process of synthetic imaging of the multiple-hologram is equivalent in principle to the imaging process of dual-focussed scanning, in which, both the receiving and the tramsmitting antenna arrays are foeussed sequentially on each imaging point. The two-hole penetration method and the single-hole reflection method have been discussed and the relevant formulas for calculation given. Problems encountered in data processing, such as the interferences caused by source point images as well as their elimination, the problem of screened regions in penetra-tion holography and the problem of double images occurring in samelevel synchronously moving measurements, in which the transmitting and the receiving points are at the same level, are diseussed, supported by the results of computer simulations using the diffraction point model. Finally some results of data processing for water tank experiments and a few tentative calcelations of field data are shown.

     

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