浅水多波束测深仪高分辨率波束形成方法研究

常规波束形成技术以其稳健性好、计算量低等特点得到广泛应用,但其空间分辨率受阵元个数限制,不能突破瑞利限。因此,常规波束形成技术应用于高精度浅水多波束测深仪时,存在空间分辨率不足和旁瓣干扰等问题。对比研究了最小方差无失真(MVDR)及多重信号分类(MUSIC)波束形成在浅水多波束测深仪中的应用,给出了浅水多波束测深仪的常规波束形成、MVDR和MUSIC处理方法,并结合能量法和相位法两种底检测测深算法,处理了iBeam8120浅水多波束测深仪外场数据,验证了本文方法的性能。     

SeaBeam全海深多波束测深系统及应用

为更好地发挥SeaBeam深水多波束系统在深远海海洋调查中获取高精度地形地貌数据的作用、方便广大调查和研究人员使用,本文以SeaBeam3012多波束为例,较系统地分析介绍了其测量技术原理.开展了该系统的硬件组成、设备功能和技术特点等方面的介绍,从声学和信号处理等角度对其Swept Beam技术进行分析,并以"向阳红0...     

一种基于正交投影的波束形成算法

提出了一种基于正交投影的波束形成算法.首先由MVDR算法确定初始权向量;其次根据该权向量与其它用户波达角方向的关系,建立干扰信号的导向矢量矩阵;然后通过正交投影原理,将期望信号的导向矢量投影到干扰信号的零空间上,从而求得最优权值.仿真结果证明了该算法的有效性.     

浅层地震探测的可控震源信号设计

在工程与环境物探中,浅层地震探测是一种常用的高分辨率物探方法,但是这种方法使用的炸药震源和枪击震源破坏力大,对人和建筑物都有危害,因而被禁止在人口稠密的地区使用．因此,无公害的电磁驱动可控震源技术得到了发展和应用．利用扫描信号压缩技术,小能量弹性波Chirp信号可持续向地下发送,不损害地面和建筑物,对人群也没有影响,是一种较理想的城市浅层地震震源．本文介绍了电磁驱动可控震源的信号设计方法,并简要介绍了具有波束定向能力的相控震源的设计思想．     

GPS接收中的自适应盲波束形成算法

给出了一种用于对抗干扰的GPS接收盲自适应波束形成算法。该方法基于一种新的解扩器和一阶恒模算法。优点是在形成波束对准期望信号并消除干扰时,不需要直接给出这些信号的DOA（信号来向）信息。计算机仿真结果给出了对抗干扰的性能。     

一种基于FFT波束形成的BDI算法分析研究

多波束条带测深你是进行海底地形测绘的主要设备，该设备的信号处理部分所要完成的主要任务就是精确测量深点目标回波的DOA（Direction of Arrival）和TOA（Time of Arrival）。研究了基于FFT波束形成技术的BDI（Bearing Diviation Indicator）算法，算法可完成对海底回波信号的时间和方向的联合估计。通过计算机仿真工作和海试数据的处理，得出结论：FFT波束形成技术可以有效地提高波束形成的数目：BDI可以精确地海底回波信号进行回波时延估计和方向估计，尤其是BDI算法可以提高镜向海底区域的边缘波束的测量精度。     

Wave extraction with portable high-frequency surface wave radar OSMAR-S

High frequency surface wave radar (HFSWR) has now gained more and more attention in real-time monitoring of sea surface states such as current, waves and wind. Normally a small-aperture antenna array is preferred to a large-aperture one due to the easiness and low cost to set up. However, the large beam-width and the corresponding incorrect division of the first- and second-order Doppler spectral regions often lead to big errors in wave height and period estimations. Therefore, for the HFSWR with a compact cross-loop/monopole antenna (CMA), a new algorithm involving improved beam-forming (BF) and spectral division techniques is proposed. On one hand, the cross-spectrum of the output sequence by the conventional beam-forming (CBF) with all the three elements and the output with only the two loops is used in place of the CMA output self-spectrum to achieve a decreased beam-width; on the other hand, the better null seeking process is included to improve the division accuracy of the first- and second-order regions. The algorithm is used to reprocess the data collected by the portable HFSWR OSMAR-S during the Sailing Competition of the 16th Asian Games held in Shanwei in November 2010, and the improvements of both the correlation coefficients and root-mean-square (RMS) errors between the wave height and period estimations and in situ buoy measurements are obvious. The algorithm has greatly enhanced the capabilities of OSMAR-S in wave measurements.     

一种基于扩频码滤波的盲波束形成算法

通过研究分析传统的应用于CDMA系统的自适应波束形成带给系统的复杂度,采用先把接收信号与本地扩频码相乘解扩后再进行基于扩频码滤波的波束形成技术,并基于最大化信干噪比准则,提出一种计算复杂度小、在不同通信环境下性能良好的综合方案.仿真结果证实了算法的有效性.     

The use of teleseismic P-wave complexity for seismic event screening – results determined from GRF and GERESS array data

Seismic data recorded at the broad-band teleseismic GRF array and theshort-period regional GERESS array, which is a designated IMS primarystation, are analyzed to determine the effectiveness of teleseismic P-wave complexity for the purpose of seismic event screening within theframework of Comprehensive Nuclear-Test-Ban Treaty verification. For theGRF array, seismic waveform data from nearly 200 nuclear explosions havebeen recorded since its installation in the late 1970's, which were studiedalong with several thousand earthquakes from the last few years.Additionally, we investigated teleseismic P wave complexity for a similarnumber of earthquakes recorded at GERESS. However, owing to itsoperation starting in 1991, only a limited number of nuclear explosionseismograms are available for study.For nuclear explosions, complexity does not exceed levels of 0.3 except fora number of events from the Nevada Test Site recorded only at the GRFarray and located at a large distance where PcP may interfere with the initialP wavelet. Since all events with complexity at GRF larger than 0.3 areexclusively located on Pahute Mesa within the Nevada Test Site,near-source geology or topography must play a dominant role for theseincreased complexity values, while PcP may not contribute significantly tothe high-frequency energy measured by the complexity parameter.Although many earthquakes show complexities below this level, for morethan 25% of the earthquakes investigated the complexities determined arelarger than 0.7, thus showing distinctly larger values than nuclearexplosions. Therefore, this percentage may be screened as earthquakes fromall seismic events detected. As currently only about half of the eventsdetected by the global IMS network are screened out based on focal depthand the m _b :M _s criterion, teleseismic P-wavecomplexity may contribute significantly to the task of seismic eventscreening.