新疆实验次声台阵设计

次声测量与数据是次声各项研究的基础,而次声台阵是现代次声测量的主要形式,为此设计并建立了两个无人值守式实验次声四元台阵。描述了次声台阵的结构,对台站的仪器构成进行了说明,重点对其降噪管和通信系统进行了描述。降噪管为十字玫瑰花瓣型降噪管,给出了其降风噪性能。台站通信系统基于VPN进行架构,实现了数据的实时自动传输和FTP传输功能。实测结果表明实验台阵的噪声主要是由微气压、山背波和台阵附近的随机干扰噪声构成。台阵记录到了大量当量较小的区域地表采矿、采石微差爆破次声信号,也记录到了2013年2月15日俄罗斯陨石大爆炸事件相关的清晰的次声信号。分析结果表明,该次声台阵具有良好的性能,具有一定的推广价值。     

火箭发射的次声信号分析*

在距离发射点20km和230km的两个阵列上,记录了我国一次火箭发射产生的次声波。从信号中识别出点火与声爆事件,观察到火箭在飞行中产生持续的次声波,以及声爆前后明显能量特征上的变化,观测到完整的火箭发射和飞行过程中系列次声波。为了验证采集信号中包含声爆事件,使用Fisher检测估计方位角和视速度,计算结果与火箭飞行轨迹一致,并且声爆信号的预计到达时间和估计方位与实际的时间和方位角相符合。结合火箭速度变化的特征,给出了声爆前低频能量较弱现象的解释和火箭超声速后次声能量特征的变化,揭示了火箭产生次声波的机理,为火箭发射等目标的监测提供有益的借鉴和参考。     

大地震前出现的异常次声波观测研究

研究了一种在大地震前出现的异常次声波,揭示其与地震发生的空间、时间、强度的对应关系.利用CASI-ICM-2011型次声测量传感器在一系列Ms6.0级以上大地震发生前2周以内检测到的一种频率范围0.001 Hz至0.01 Hz的次声波,其特征有:幅值范围50 Pa至200 Pa,持续时间0.5 h至4 h,传播速度10 m/s至30 m/s,震级越高信号越强.通过建立广域次声传感器网络,成功定位了芦山地震前4天出现的异常次声波,以及巴基斯担地震前12天出现的异常次声波.通过对8年时间连续监测数据的分析,研究了这类次声波的出现规律.同时,对其产生机理提出了大地起伏激发次声波的假设,进行了理论论证,并用智利地震测量信号和玉树地震测量信号证明S波可以激发出本地同振的次声波.文中所列举的数个震前异常次声信号的观测结果对于地震预测的信息获取具有参考价值.     

基于一维卷积神经网络的化爆和地震次声分类*

次声事件的分类识别方法应用广泛,传统分类方法在很多方面进行了尝试,但由于次声信号具备非线性的特点,致使分类难度较大,分类精度不高,这对次声事件的分类工作提出了挑战。针对次声事件中的化学爆炸与天然地震信号分类问题,文章构建了一种改进的深度卷积神经网络分类模型用于实现两类次声信号的分类。论文采用"全面禁止核试验条约组织"官网上收集到的化学爆炸和天然地震次声信号进行数据集的构建,使用改进的深度卷积神经网络分别与BP网络和一维LeNet-5网络进行对比分析。实验结果表明,论文的测试识别率能够达到82.72%,较上述算法有优势。     

1998年11月17日狮子座流星雨的次声观测

采用三台ＣＳＨ－１型次声接收器,在北京昌平区布置了一个次声测量三点阵,并观测到１９９８年１１月１７日狮子座流星雨产生的次声波Ｐ－ｔ曲线和波速波向图,借助快速富立叶变换,分析Ｐ－ｔ曲线的波形得到次声的三维动态谱,频谱分析结果表明,（１）各流星产生的次声波大都很短暂,持续时间在１－５分钟内;（２）流星次声波的周期都在４０－４０８秒内,少数在１－４８０秒内;（３）在１１月１７日１９：２１－２０：４１期间     

火山:大自然的烟花

<正>地球深部炽热的岩浆沿通道上升,穿过地球表层薄弱的地方喷出地面,我们把这一过程称为火山喷发。火山喷发出来的熔岩和碎屑流等物质围绕喷口堆积形成的不同形状的山丘就是火山。与我们常见的连绵起伏的山脉不同的是,火山大多呈现出孤     

雷雨次声波的三维动态频谱测量研究

采用三台电容式次声接收器，在北京昌平安装次声三点阵，并测量到2000年7-8月15次强雷阵雨的次声波P-t曲线及其三维动态频谱，频谱分析结果表明：（1）雷阵雨的次声波主要来自雷次声。（2）雷次声的频谱有三大特点：其一是听到雷声越响时，雷次声振幅越强；其二是特强振幅持续时间很长；其三是周期范围时而连续、时布分布在周期较长和较短端，形成谱图上一个个空洞。据此可区别与其它次声波。（3）初步探讨了雷次声的产生机理和传播特点。     

次声方法测定台风方位的试验

海上台风眼中的驻波或大浪可以辐射出次声波,在几千公里远用灵敏的次声传声器可以接收到它。我们在我国沿海地区安装了次声观察站,在有关部门的协作下,记录到大量台风产生的次声波,为了试验次声测定台风信号到达方位的方法,1978年夏季在福州建立了探测台风的次声阵,本文简要叙述试验用次声测试系统和测定方位角的方法及结果。     

基于薄膜动圈式的次声波监测装置设计

基于薄膜动圈式声-电转换原理,利用次声波产生的空气微压波动带动薄膜上线圈受迫振动,引起线圈内磁通量的变化产生感应电动势,将声信号转换成电信号进行采集,设计便携式次声监测装置.在模拟简谐次声环境中的测量结果表明,该装置能够准确地测量出振动频率,并对其幅度进行监测.     

X射线脉冲星导航动态模拟实验系统研制与性能测试

本文设计了一种半实物实验系统,能模拟出航天器在地球轨道及深空飞行时接收脉冲星周期X射线信号的情形.该系统主要由动态信号数据库、X射线模拟源、真空系统和探测系统组成.模拟源可以模拟出任意波形的脉冲轮廓,探测系统的时间分辨率优于2μs,通过分析时间转化模型给出了动态信号生成方法.实验模拟了航天器在近地轨道飞行一周接收Crab脉冲信号,将采集的光子到达时间转换到太阳系质心时后累积脉冲轮廓与标准轮廓相关度为0.9882.     

Infrasonic waves generated from the volcano eruption in Tonga

The Hunga-Tonga-Hunga-Ha'apai volcano in Tonga erupted violently on January 15, 2022. After 8 hours and 39 minutes, an infrasound array in Kunming at a distance of 10151 km away from the volcano recorded a sequence of strong infrasonic waves. The average period of the first four infrasonic waves is 443 s with propagation speed of 321 m/s. The azimuth angle of this event has been estimated by applying the progressive multi-channel correlation(PMCC) method to process the received signals. During continuous monitoring, the infrasonic waves propagating along and opposite to the direction towards the Kunming array around the earth are recorded respectively.     

Infrasonic waves caused by the earthquake on 12 July 1993 in Japan

I.IntroductionTheinfrasonicwavesradiatedbytheseismicwaves1knownasseismicinfrasound,canspreadoutandcanbereceivedbytheinfrasoundmonitoringsystemwhichhavebeendevelopedandarebeingperfecteddaybydayI1-1o].Theseismicwavspropagateinal1directionswithintheearthbodyandradiateseveraltypesofinfrasonicwaves.Oneofthemcalledthelocalinfrasonicwaveisradiatedbyearthsurfaceattheveryinfrasoundstationwhereseismicwavesarepassingthrough;thesecondtypecalledepicentralinfrasonicwavesareradiatedbythestrongmotionoftheear…     

大气中一种低频次声波观测研究

分析大气中存在的一种低频次声波。利用宽频带次声测量传感器阵列组成的广域分布网络,对此种次声波进行了近5年不间断的检测。对所测次声信号的观察统计发现,它与自然事件密切相关。对这种信号波形、频谱、时频图及相关性进行分析进一步发现,该波通常以一组或间歇性多组形式出现,频率主要在0.001~0.02 Hz之间、幅度一般可达50~200 Pa。在2008年3月20日新疆于田地震、2008年5月12日四川汶川地震以及2009年10月29日陕甘川三省交界处的地震前,均检测到了大幅值的低频次声波。本文的分析结论对研究大气次声波的多样性及其与自然现象的关系提供了新的参考,对地震信息探测具有一定的实际意义。      

Joint seismic-infrasonic processing of recordings from a repeating source of atmospheric explosions

A database has been established of seismic and infrasonic recordings from more than 100 well-constrained surface explosions, conducted by the Finnish military to destroy old ammunition. The recorded seismic signals are essentially identical and indicate that the variation in source location and magnitude is negligible. In contrast, the infrasonic arrivals on both seismic and infrasound sensors exhibit significant variation both with regard to the number of detected phases, phase travel times, and phase amplitudes, which would be attributable to atmospheric factors. This data set provides an excellent database for studies in sound propagation, infrasound array detection, and direction estimation.     

Disturbances of the upper atmosphere and ionosphere caused by acoustic-gravity wave sources in the lower atmosphere

The results of observations of acoustic-gravity waves in the troposphere and the ionosphere at middle latitudes during periods of passage of the solar terminator are presented. Tropospheric observations were performed using a lidar. The frequency characteristics of variations of the tropospheric parameters are determined based on observations of the intensity of the scattered lidar signal. The characteristics of variations of the total electron content (TEC) in the atmosphere are determined from data collected by GPS navigation satellites. An analysis of the observational data showed that the spectrum of variations of the atmospheric and ionospheric parameters is indicative of acoustic-gravity waves (AGW) propagating from the lower atmosphere. Modeling studies of the vertical propagation of AGW from the Earth’s surface showed that such waves quickly (within ~15 min) reach altitudes of the upper atmosphere (~300 km). The refraction and dissipation of waves in the upper atmosphere produces perturbations of the background state of the atmosphere and gives rise to the waveguide propagation of infrasonic wave components. The observed manifestations of TEC disturbances caused by AGW propagating from the lower atmosphere can be explained by the diurnal variation of the altitude of the ionosphere and the waveguide propagation of infrasonic waves.     

Method and results of estimating acoustic characteristics of bottom-sediment upper layers in the shelf region using seismic exploration instruments

The potential of seismic exploration instruments for estimating the surface layers of soil in the towing zone of an extended multielement array is investigated. In contrast to the well-known method of common depth point, in which the main estimated parameters are the transit times of waves reflected from deep layers of the sea bottom, two-dimensional spectral analysis is used to measure the longitudinal wavenumbers of the modes forming an infrasonic field in the water layer. The measured longitudinal wavenumbers of modes serve initial data for estimating the acoustic characteristics of the upper layers of bottom sediments directly in the towing zone of pulse emitter and extended multielement array. It is concluded that the use of data on the parameters of upper soil layers in seismic exploration should increase the accuracy of contouring oil and gas condensate fields.     

Responses of the Ionosphere to the Great Sumatra Earthquake and Volcanic Eruption of Pinatubo

A sudden ionospheric disturbance was detected by the Doppler shift sounding equipment at Beijing, about 25 min later after the outbreak of the Sumatra earthquake on 26 December 2004. This ionospheric disturbance appeared less than lOmin after the earthquake was first recorded at Beijing seismological station by the arrival of the seismic Rayleigh wave. The analysis shows that about 18rain is the time necessary for the seismic Rayleigh wave to propagate from the epicentre to Beijing and then about 5-10min for acoustic waves to propagate from the surface of the Beijing area to the altitude of the ionosphere. Also, a report was made as another example to show the ionospheric response of Doppler shift observation at Beijing area during the Mount Pinatubo eruption of 1991. These two examples show clear evidence of the lithosphere-atmosphere-ionosphere coupling. The former case is in the frequency domain of infrasonic waves of the Earth surface oscillation due to the Rayleigh waves caused by the earthquake, while the latter is in the acoustic-gravity wave category directly excited in the atmosphere by the mass and energy eruptions of Mount Pinatubo.