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垂向叠加震源冲击波激发地震波的能量分析
引用本文:宋玉龙,吕公河,王新红,徐德惠,房师欣.垂向叠加震源冲击波激发地震波的能量分析[J].石油地球物理勘探,2004,39(4):371-374.
作者姓名:宋玉龙  吕公河  王新红  徐德惠  房师欣
作者单位:1. 胜利石油管理局物探公司; 2. 山东机器集团有限公司
摘    要:本文根据有关爆破理论,分析了球形装药爆炸时冲击波转换成地震波的能量关系,对多级小药量垂向延迟震源地震波能量叠加的原理进行了研究,认为两级垂向延迟时间取决于两级球形装药的距离,而且在确定此距离时要同时考虑一级球形装药爆炸所形成的粉碎区直径和炸药的殉爆距离。在合理控制两级或多级球形装药起爆时间条件下,能提高地震波的下传能量,同时减少地表的振动。根据这项理论分析结果,进行了垂向延迟叠加震源试验。试验结果表明,垂向延迟叠加震源可在保证一定信噪比的前提下,提高地震波的频率,是高精度地震勘探较理想的激发震源。

关 键 词:震源  地震勘探  冲击波  地震波  能量  
收稿时间:2003-05-08

Analysis of seismic energy produced by shock wave of vertical stack source.
Song Yu-long,L&#,Gong-he,Wang Xin-honXu De-hui,Fang Shi-xin.Analysis of seismic energy produced by shock wave of vertical stack source.[J].Oil Geophysical Prospecting,2004,39(4):371-374.
Authors:Song Yu-long  L&#  Gong-he  Wang Xin-honXu De-hui  Fang Shi-xin
Affiliation:Seismic Prospecting Institute, Geophysical Prospecting Company, Niuzhuang Town, Dongying City , Shandong Province, 257014, China
Abstract:According to explosive theory,the paper analyzed the relation of energy transformed from shock wave into seismic wave when explosion by spherical charge,studied the principle of seismic energy stacked by using multilevel small charge sized and vertically delayed sources,which suggested that two level vertically delayed time depends on the interval of two level spherical charges and it must consider the radius of broken zone formed by explosion of one level spherical charge and the explosion save distance.Under the condition of reasonable controlling on time of ignition of two level or multilevel spherical charge,the downgoing energy of seismic wave can be improved and the vibration of surface can be reduced.The experiment of vertically delayed stack source has been implemented by using the results of the theoretical analysis.The results showed that the vertically delayed stack source can increase the frequency of seismic wave in a precondition of ensuring a certain S/N ratio,that is ideal explosive source for high precision seismic exploration.
Keywords:source  seismic exploration  shock wave  seismic wave  energy
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