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地震数据采集系统频谱均衡滤波理论研究
引用本文:袁子龙,宁静,李婷婷.地震数据采集系统频谱均衡滤波理论研究[J].吉林大学学报(地球科学版),2007,37(4):828-832.
作者姓名:袁子龙  宁静  李婷婷
作者单位:大庆石油学院,地球科学学院,黑龙江,大庆,163318;大庆石油学院,地球科学学院,黑龙江,大庆,163318;大庆石油学院,地球科学学院,黑龙江,大庆,163318
基金项目:黑龙江省自然基金项目(E0317),黑龙江省科技攻关项目(GZ05A102)
摘    要:建立视等厚层状吸收介质模型,计算地层吸收衰减特性,以此为依据给出了频谱均衡滤波器的数学模型和设计框图。选择主频为200 Hz的雷克子波,理论计算原始地震反射波的特征参数(主振幅、主频率、频带宽度)。利用所设计的频谱均衡滤波器对原始地震反射进行滤波,能够有效补偿地层的吸收衰减,地震反射波的特征参数得到明显改善。时间从0.5~3.0 s,主振幅增强了20.55~30.40 dB,主频率提高了104~74 Hz,频带被拓宽了205~186 Hz,分辨率提高到2.9~13.9 m(分辨率提高了56%~67%)。

关 键 词:地层吸收  地震反射波  分辨率  主振幅  主频率  频带宽度  均衡滤波  高频提升
文章编号:1671-5888(2007)04-0828-05
修稿时间:2006-09-13

Study on the Theory of Spectrum Equilibrating Filter in Seismic Data Acquisition System
YUAN Zi-long,NING Jing,LI Ting-ting.Study on the Theory of Spectrum Equilibrating Filter in Seismic Data Acquisition System[J].Journal of Jilin Unviersity:Earth Science Edition,2007,37(4):828-832.
Authors:YUAN Zi-long  NING Jing  LI Ting-ting
Institution:Collegeof Earth Sciences,Daqing Petroleum Institute,Daqing,Heilongjiang 163318,China
Abstract:A set of uniform thickness models of layered absorption media were established.The absorption and attenuation character of stratum were calculated as well.Based on these results the mathematic model and spectrum equilibrating filter(SEF) frame were designed.Ricker wavelet whose predominant frequency is 200Hz was chosen as the exciting wave,and the character parameters(predominant amplitude,predominant frequency and frequency bandwidth) of its reflected wave were calculated.Filtered by SEF the strata's absorption and attenuation was compensated and the parameters of reflected wave could be improved as well.When time range changed from 0.5s to 3.0s,the predominant amplitude,predominant frequency and frequency band increased 20.55-30.40 dB,104-74 Hz and 205-186 Hz,respectively,and the resolution increased to 2.9-13.9 m(increasing 56%-67%).
Keywords:strata's absorption  seismic reflected wave  resolution  predominant amplitude  predominant frequency  frequency bandwidth  equilibrating filter  high frequency increasing
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