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地下核爆炸地震波二次源特征
引用本文:何永锋,赵克常,张献兵,马裕然,王洋.地下核爆炸地震波二次源特征[J].地球物理学报,2012,55(5):1742-1748.
作者姓名:何永锋  赵克常  张献兵  马裕然  王洋
作者单位:1. 装甲兵工程学院基础部, 北京 100072; 2. 北京大学地球与空间科学学院, 北京 100871
摘    要:层裂是地下核爆炸震源物理过程中最重要的非球对称源过程.对其机制的研究,多基于面波资料,本文基于远场体波资料,利用经验格林函数方法,消除路径及接收场地效应,利用地下核爆炸远场地震波P波数据对震源时间函数进行了反演,结果显示明显的双脉冲特征,该二次源特征不随方位角及震中距变化,说明它源自震源本身,其双脉冲特征与层裂机制相符.

关 键 词:地下核爆炸  层裂  经验格林函数  
收稿时间:2011-04-26

The characteristic of the waveform from the second source induced by underground explosion
HE Yong-Feng , ZHAO Ke-Chang , ZHANG Xian-Bing , MA Yu-Ran , WANG Yang.The characteristic of the waveform from the second source induced by underground explosion[J].Chinese Journal of Geophysics,2012,55(5):1742-1748.
Authors:HE Yong-Feng  ZHAO Ke-Chang  ZHANG Xian-Bing  MA Yu-Ran  WANG Yang
Institution:1. Academy of Armored Forces Engineering, Beijing 100072, China; 2. School of Earth and Space Science, Peking University, Beijing 100871, China
Abstract:It was widely accepted that the spall slapdown is the primary contributor to the non-spherical source of underground explosions based on the study of surface waves.In this article,body waves are analyzed to search the mechanism of the non-spherical process of the underground nuclear explosion.The second arrival after the P arrival is obvious and the shape of the two pulses is remarkably consistent in a wide azimuthal range.This indicates that the second arrival is not due to any structural features but is part of the source itself,and can be explained by the spall process.
Keywords:Underground nuclear explosion  Spall  Empirical Green′s function
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