核爆次声背景噪声信号特征分析
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摘要
核爆炸次声监测技术是《全面禁止核试验条约》规定的监测技术手段之一,主要用来监测大气层中的核爆炸。根据核爆次声监测对背景噪声信号影响的关注,重点介绍了地震、火山喷发、闪电、大风等非核爆次声信号的特征,了解这些特征对于开展核爆次声监测有益。
Infrasound monitoring is one of the four monitoring technologies stipulated in " The Comprehensive Nuclear-Test-Ban Treaty".According to the interest in the understanding of background noise during nuclear explosion infrasound monitoring,the discussion is concentrated on the infrasound caused by earthquake,volcanic eruption,lightning,gale and so on.It's very important to understand these characteristics for developing nuclear explosion infrasound monitoring.
Infrasound monitoring is one of the four monitoring technologies stipulated in " The Comprehensive Nuclear-Test-Ban Treaty".According to the interest in the understanding of background noise during nuclear explosion infrasound monitoring,the discussion is concentrated on the infrasound caused by earthquake,volcanic eruption,lightning,gale and so on.It's very important to understand these characteristics for developing nuclear explosion infrasound monitoring.
引文
[1]Alexis Le Pichon.Infrasound Monitoring for Atmos-pheric Studies[M].USA:Springer:220-223.
[2]林琳,杨亦春.大气中一种低频次声波观测研究[J].声学学报,2010,35(2):200-207.
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[5]Cook RK.Infrasound radiated during the MontanaEarthquake of 1959 August 18[J].Geophys J R astrSoc,1971,26:191-198.
[6]Mutschlecner JP,Whitaker RW.Infrasound fromearthquakes[J].Geophys Res,2005,110(D1):doi:10.1029/2004JD005067.
[7]王晓航.四川地震波形分析[C].2011年北京第一届次声学会议,2011.
[8]Campus P.Eruptions detected with the global infra-sonic array network of the International MonitoringSystem[C].Japan,18 November,2007.
[9]Campus P.Monitoring volcanic eruptions with theIMS infrasound network[R].Inframatics 15:6–12.
[10]Richard Wunderman,Lee Siebert,James Luhr,et al.A global perspective on volcanoes and eruptions[R].Smithsonian Institution,2004.
[11]John W Ewert,Christopher G Newhall.Status andchallenges of volcano monitoring worldwide[R].U.S.Geological Surver,2004.
[12]John J Lyons,Gregory P Waite,William I Rose.Pat-terns in open vent,strombolian behavior at fuego vol-cano,guatemala,2005—2007[J].Bulletin of Volcan-ology,2009,72(1):1-15.
[13]刘俊民,唐伟,王晓明,等.次声信号产生机理与特性分析[J].环境工程,2010,28(4):92-96.
[14]苏昉,田维.4-8级大风的次声波三维动态频谱测量研究[J].石油大学学报:自然科学版,2002,26(1):108-111.
[15]Jelle Assink,Laslo Evers,Iwan Holleman,et al.Characterization of infrasound from lightning[R].Royal Netherlands Meteorological Institute,2008.
[2]林琳,杨亦春.大气中一种低频次声波观测研究[J].声学学报,2010,35(2):200-207.
[3]刘正彦等.台湾次声波系统[C].2011年北京第一届次声学会议,2011.
[4]Grover FH,Marshall PD.Ground to air coupledwaves from a distant earthquake[J].Nature,1968220(5168):686-687.
[5]Cook RK.Infrasound radiated during the MontanaEarthquake of 1959 August 18[J].Geophys J R astrSoc,1971,26:191-198.
[6]Mutschlecner JP,Whitaker RW.Infrasound fromearthquakes[J].Geophys Res,2005,110(D1):doi:10.1029/2004JD005067.
[7]王晓航.四川地震波形分析[C].2011年北京第一届次声学会议,2011.
[8]Campus P.Eruptions detected with the global infra-sonic array network of the International MonitoringSystem[C].Japan,18 November,2007.
[9]Campus P.Monitoring volcanic eruptions with theIMS infrasound network[R].Inframatics 15:6–12.
[10]Richard Wunderman,Lee Siebert,James Luhr,et al.A global perspective on volcanoes and eruptions[R].Smithsonian Institution,2004.
[11]John W Ewert,Christopher G Newhall.Status andchallenges of volcano monitoring worldwide[R].U.S.Geological Surver,2004.
[12]John J Lyons,Gregory P Waite,William I Rose.Pat-terns in open vent,strombolian behavior at fuego vol-cano,guatemala,2005—2007[J].Bulletin of Volcan-ology,2009,72(1):1-15.
[13]刘俊民,唐伟,王晓明,等.次声信号产生机理与特性分析[J].环境工程,2010,28(4):92-96.
[14]苏昉,田维.4-8级大风的次声波三维动态频谱测量研究[J].石油大学学报:自然科学版,2002,26(1):108-111.
[15]Jelle Assink,Laslo Evers,Iwan Holleman,et al.Characterization of infrasound from lightning[R].Royal Netherlands Meteorological Institute,2008.
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