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Application of the Wavelet Packet Method in Discrimination Between Nuclear Explosion and Earthquake

机译:小波包方法在核爆炸与地震识别中的应用

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摘要

Although the CTBT (Comprehensive Nuclear Test-Ban Treaty) was passed in 1996, it is still necessary to develop new and highly efficient methods (Wu Zhongliang, Chen Yuntai, et al.,1993; Xu Shaoxie, et al. 1994; Richard L. Garwin, 1994) to monitor possible events. Many discrimination criteria (Xu Shaoxie, et al., 1994; Institute of Geophysics, Chinese Academy of Sciences, 1976; Richard L. Garwin, 1994) have been put forward since the 1950s. The results show that each of the existing criteria has its own limitation, but the seismological method is an important and efficient method in the discrimination between nuclear explosion and earthquake. Especially in recent years, because of the little and little equivalent as well as the increasing hiding steps used in the test, a number of more efficient seismological methods have been worked out. In this paper, a new discrimination method, the Wavelet Packet Component Ratio (WPCR) method, is put forward. This method makes full use of the difference in variation with time between the spectra of nuclear explosions and earthquakes. Its discrimination efficiency is rather high.
机译:尽管《全面禁止核试验条约》(CTBT)于1996年通过,但仍然有必要开发新的高效方法(吴忠良,陈云泰等,1993;徐绍Sha等,1994; Richard L (加尔文,1994年)来监视可能发生的事件。自1950年代以来,已经提出了许多判别标准(徐绍et等,1994;中国科学院地球物理研究所,1976;理查德·加温,1994)。结果表明,现有的每个标准都有其局限性,但地震学方法是区分核爆炸和地震的一种重要而有效的方法。特别是近年来,由于测试中使用的等效项越来越少,并且隐藏步骤越来越多,因此已经设计出了许多更有效的地震方法。提出了一种新的判别方法,即小波包分量比(WPCR)方法。该方法充分利用了核爆炸和地震频谱之间随时间变化的差异。其判别效率很高。

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