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1.
研究液体中声吸收对三种具有不同波形的脉冲光声信号的影响,把吸声介质视为一个线性、时空不变的低通滤波器,得到了考虑声吸收后光声脉冲的幅值和波形随传播距离变化的表达式。  相似文献   

2.
在不同的条件下,脉冲激光在液体中激发的光声脉冲波的波阵面可近似为平面,柱面或球面.具有不同波阵面的声脉冲在液体中传播时,其前沿上升时间随传播距离的变化规律不同,因此,液体非线性参量和声脉冲上升时间改变量之间的关系也不同。本文讨论了平面、柱面和球面的波阵面的光声脉冲波的上升时间和传播距离的关系,并给出了相应的B/A的表达式.  相似文献   

3.
当高强度周期性调制的光束或脉冲激光柬入射到介质中时,通过光与物质的相互作用,部分光能转变为声能,从而在介质中形成声波,这一效应称为光声效应。在光声效应的基础上发展起来的光声光谱技术,已广泛用于物质结构的研究。  相似文献   

4.
袁长迎  炎正馨  蒙瑰  李智慧  尚丽平 《海洋学报》2010,32(10):6908-6913
采用恒流驱动耦合机械斩波技术在激光光声光谱装置上系统测量了5%—100%宽浓度范围甲烷气体的共振光声信号,发现在高浓度区共振光声信号呈现异常的饱和特征.基于气体吸收和光声光谱原理定量分析了光声信号饱和的主要原因及影响因素,研究表明,气体样本对入射光强吸收而导致的声源与本征共振模式的耦合系数改变是异常饱和的主要原因,并导出判定光声信号饱和深度的准则以用于判定高浓度气体饱和深度.  相似文献   

5.
本文研究了水下光击穿时所激发的声脉冲在低频段的频谱、频谱曲线在60kHz附近有一个明显的峰,给出了一个频谱的表达式,它与实验结果吻合较好。  相似文献   

6.
海洋声层析是1979年美国科学家W.Munk等人提出的,通过测量传播时间等声传播信号有关参量反演声波所穿越的海洋特征,得到大面积海域中的海洋动力学状态及其变化的估计。声层析方法自提出以来受到各国的重视。在最初的20 a间,以全球测温计划(ATOC)为代表的一系列验证实验推动了声层析的理论研究、设备研制和应用。步入21世纪后,声层析与海洋动力学的数据同化、利用滑翔机等设备的移动声层析以及沿海声层析得到重视,并进行了相关的理论与实验研究。纳入成像旗下的声层析希尔伯特方法、有效低功耗的分布式传感网络声层析,以及被动声层析,或将成为声层析未来研究的重要方向。  相似文献   

7.
当高强度周期性调制的光束或脉冲激光束入射到介质中时,通过光与物质的相互作用,部分光能转变为声能,从而在介质中形成声波,这一效应称为光声效应。在光声效应的基础上发展起来的光声光谱技术,已广泛用于物质结构的研究。 近十年来,人们对非密封的大范围介质空间中激光激发声波的现象进行了研究,特别是激光在液体中激发声波的现象引起了人们极大的兴趣。它有可能导致一种新的水下声源——激光声源。与传统的水下声源相比,激光声源有许多优点,例如,可以比较容  相似文献   

8.
孙伟峰  李美成  赵连城 《海洋学报》2010,32(10):7291-7297
基于密度泛函理论的第一性原理方法,系统研究了Ga和Sb纳米线的电子能带结构和声子结构以及电子-声子耦合(EPC)作用.通过对声子的完整Brillouin区分析来研究纳米线的结构稳定性.结果表明,所考察的纳米线显示出不稳定性,不稳定声子波矢远离Brillouin区中心.与通常的Peierls变形机理相比,不稳定的横向声子模会导致一种无开口带隙的相变.Sb比Ga纳米线的EPC要强很多,并且横向变形导致的锯齿形结构使纳米线中的电子-声子相互作用增加了几个数量级.  相似文献   

9.
介绍了一种猎雷声呐脉冲信号被动定位的测向方法。反猎水雷采用被动声自导方式,利用猎雷声呐发射的窄带脉冲信号,采用自适应 notch 滤波器估计信号的包络、频率、相位差。采用时延差粗测与相位差精测相结合的方法实现时延估计。此方法不仅对 CW 脉冲信号可测向、测距,还可适用于调频、跳频信号。 该方法已通过仿真及实测数据验证有效。  相似文献   

10.
浅海海底声参数是影响声场传播的重要参量。文中根据信号的相位特性对反演稳定性的影响进行了数值模拟;并于2002年8月在黄海海区进行了海底声参数反演实验。利用垂直入射脉冲和海底回波数据进行海底声参数反演,由于海底回波信号随穿透深度增加而导致回波信号的信噪比降低,为了有效地增加海底声阻抗反演深度,提出平滑分段抽取冲激响应,重建声阻抗剖面的方法。结合Hamilton经验公式,分离海底声速、密度,反演结果与海底采样样本分析值、经验值吻合较好。  相似文献   

11.
国外对加州海狮水下声进行了不少研究,但尚未取得一致结论。我们对北京动物园中的加州海狮(Zalophus californianus) “东东”和“玲玲”的水下声信号进行了测试和分析。发现它们在水下发出许多种声信号。在缓慢的自由游泳状态发出幅度较低、没有明显规律的脉冲,而当快游接近池壁或跳出水面之前和入水之时,则发出上升时间短、幅度很大的脉冲列。“东东”三岁半,好动,发声极多,其脉冲声信号较易测到。  相似文献   

12.
The propagation attenuation of sound wave in liquid with the surficial sediment of ocean is discussed. Considering suspended particles in the shape of nonspheroid. we have improved the theory on sound attenuation and compared the theoretical values with the measured ones. The results indicate that the theory modified is in stricter accordance with the actual situation.  相似文献   

13.
The results of experiments on the physical modeling of long-range infrasonic propagation in the atmosphere are given. Such modeling is based on the possible coincidence between the forms of the vertical profiles of the effective sound speed stratification in the atmospheric boundary layer (between 0 and 600 m for the case under consideration) and in the atmosphere as a whole (from the land surface up to thermospheric heights (about 150 km)). The source of acoustic pulses was an oscillator of detonation type. Owing to the detonation of a gas mixture of air (or oxygen) and propane, this generator was capable of producing short, powerful (the maximum acoustic pressure was on the order of 30 to 60 Pa at a distance of 50 to 100 m from the oscillator), and sufficiently stable acoustic pulses with a spectral maximum at frequencies of 40 to 60 Hz and a pulsing period of 20 to 30 s. The sites of acoustic-signal recording were located at different distances (up to 6.5 km) from the source and in different azimuthal directions. The temperature and wind stratifications were monitored in real time during the experiments with an acoustic locator—a sodar—and a temperature profiler. The data on the physical modeling of long-range sound propagation in the atmosphere are analyzed to verify the physical and mathematical models of predicting acoustic fields in the inhomogeneous moving atmosphere on the basis of the parabolic equation and the method of normal waves. A satisfactory agreement between calculated and experimental data is obtained. One more task was to compare the theoretical relations between variations in the azimuths and angles of tilting of sound rays about the horizon and the parameters of anisotropic turbulence in the lower troposphere and stratosphere with the experimental data. A theoretical interpretation of the experimental results is proposed on the basis of the theory of anisotropic turbulence in the atmosphere. The theoretical and experimental results are compared, and a satisfactory agreement between these results is noted.  相似文献   

14.
利用混响时间及其频率特性实测值,通过分析计算,在一些建筑条件限制下,采用恰当地声学处理措施,调整了混响时间及其频率特性,提出一种简便有效的方法。  相似文献   

15.
This paper uses acoustical method to obtain the sound speed structure information of the deep sea sediment. The time-frequency characteristics of the explosive sound signals in the deep sea are analysed by using the narrow-band filters, and the bottom-reflecting path and bottom-refracting path are separated in time domain. Based on the two kinds of selected bottom models the travel-time difference between the two paths mentioned above is calculated according to the ray theory, and simple analytical formulae are obtained. The bottom model, which is more suitable for the experimental area, is identified by comparing the theoretical with experimental travel-time differences versus range.  相似文献   

16.
A three-dimensional thermo-mechanical coupled finite element model is built up to simulate the phenomena of dynamical contact and frictional heating of crack faces when the plate containing the crack is excited by high-intensity ultrasonic pulses. In the finite element model, the high-power ultrasonic transducer is modeled by using a piezoelectric thermal-analogy method, and the dynamical interaction between both crack faces is modeled using a contact-impact theory. In the simulations, the frictional heating taking place at the crack faces is quantitatively calculated by using finite element thermal-structural coupling analysis, especially, the influences of acoustic chaos to plate vibration and crack heating are calculated and analysed in detail. Meanwhile, the related ultrasonic infrared images are also obtained experimentally, and the theoretical simulation results are in agreement with that of the experiments. The results show that, by using the theoretical method, a good simulation of dynamic interaction and friction heating process of the crack faces under non-chaotic or chaotic sound excitation can be obtained.  相似文献   

17.
为了解水下强噪声对大黄鱼的影响,结合行为学方法开展了3个年龄的大黄鱼声刺激实验.结果发现:3个年龄的大黄鱼在水中声压约10Pa时均能对声波发生条件反应,但是,它们的声波敏感频率和直接致死的声压阈值差异较大;1个月幼苗和8个月小鱼的声波敏感频率分别为800Hz和600Hz,直接致死的声压阈值约为40Pa和4kPa.13个月大鱼的声波敏感频率也在600Hz,但当声压达到4kPa时,鱼群受惊吓明显,且未能直接致死.另外,这些曾经暴露在强声波中的各年龄段的大黄鱼在随后48h里较多出现相继死亡的现象.表明这些长时间暴露在水下噪声中的大黄鱼可能会因累积效应引起行为模式改变和间接致死等慢性危害.  相似文献   

18.
Experimental results of the seismic profiling with bottom penetration up to 1000 m based on broadband signals and conducted in the Caspian Sea sites are presented. Use has been made of synchronized sequences of probing pulses with linear frequency modulation at a frequency deviation of 50 to100 Hz. The pulses were emitted by a towed sound source of an original design (acoustic power up to 300 W, frequency ranged from 100 to 1000 Hz) and received by a standard digital seismic streamer. The processing of the signals involved the matched filtering of the individual pulses and the trajectory accumulation of a long sequence of pulses lengthwise the horizontal-homogeneous reflecting layers of the bottom structure. The adaptive stacking procedure taking into account the linear inclinations of the individual layers allowed us to enlarge the stacking interval by up to 100 pulses and to increase the effective depth and the spatial resolution of the seismic profiling, which gave us a total increase of more than 30 dB in the S/N ratio. In our view, the seismic profiling using low-power (about 100 W) and broadband (up to several hundred Hz) coherent sound sources represents a promising technology for decreasing the hazardous impact on aquatic ecosystems. The approach developed is an alternative to the conventional technology of marine seismic prospecting based on powerful pulse sources of the shock type (air guns, sparkers) in the low frequency range (less than ~200 Hz).  相似文献   

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