运用迭代FFT算法优化平面稀疏阵列

介绍了一种基于迭代FFT算法的优化方法来实现平面稀疏阵列的峰值旁瓣电平优化,给出了详细的优化步骤。在给定的旁瓣约束条件下,利用阵列因子与阵元激励之间存在的傅里叶变换关系,对不同的初始随机阵元激励分别进行迭代循环,可以降低稀疏阵列的旁瓣电平。在迭代过程中,根据稀疏率将阵元激励按幅度大小置1、置0来完成阵列稀疏。仿真实验证明了该方法的高效性和稳健性。     

Low Frequency End Performance of a Symmetrical Configuration Antenna for the Square Kilometre Array (SKA)

The frequency specifications of the Square Kilometre Array (SKA) call for an optimum operation of the antenna elements from 25 down to 100 MHz. The current 12 m diameter US-SKA design is specified from 500 up to 25 GHz, with an upper goal of 35 GHz. At the low frequency end of the band (i.e., 100 MHz), a 12 m reflector antenna is about four wavelengths in diameter. Then, the question is: how well can you do, at this low frequency end of the specified band of operation for the SKA, with a symmetric reflector configuration using an ultra-wide-band prime focus feed? This paper presents the analysis of the antenna performance, in terms of A _eff/T _A, of three symmetric configurations of the 12 m US-SKA antenna design between 100 and 200 MHz.     

上海地震台阵的标定方法

地震台阵标定可以校正视慢度和后方位角，从而进一步校正震源位置，有助于提高地震定位精度及地震类型鉴别研究等。此外，台阵标定也可校正由于台阵接收系统而导致视慢度和后方位角的偏差。     

多点最小二乘匹配的可变权阵阵列松弛算法

本文详细介绍了多点最小二乘匹配的常规算法和由阵列代数表示的阵列松弛算法，并把Ｒａｕｈａｌａ限于等权的情形推广到不等权（变权）的情形，给出了实现阵列松弛的步骤，最后从计算效率，匹配精度对常规算法，等权阵列松弛和不等权阵列松弛进行了比较，分析，揭示了变权阵列松弛法巨大的实用潜力。     

双层套管井中单极子声波测井的响应特征

目前,在深井中采用多层套管实现层间封隔的方法已非常普遍,对多层套管井固井质量评价的需求越来越迫切,目前还未有针对外层套管与地层之间水泥胶结评价的有效手段.本文利用三维有限差分仿真了单极声波测井在双层套管井中的响应特征,探讨了利用套管波幅度和斯通利波频散特征识别外层套管与地层之间环空是否胶结水泥的可行性.数值计算结果显示在两层套管之间胶结水泥时,套管波的幅度或衰减对外层套管和地层之间是否胶结水泥非常敏感,外层环空若充填水泥则全波中的套管波幅度降低明显;在两层套管之间充填泥浆时,全波波形中首先到达的套管波幅度较大,其对外层套管的胶结状况不再敏感,通过对接收的阵列波形做频率-慢度相关分析发现,在外层套管和地层之间胶结水泥后,井孔内接收到的低于10 kHz的外斯通利波慢度明显增大,仿真波形的处理结果与解析计算的斯通利波的频散曲线吻合较好,进一步验证了可尝试利用内层环空激发的外斯通利波判断外层套管与地层之间是否胶结水泥.     

Further evidence for radial velocity anomalies in the lower mantle

Summary Wright andLyons (1981) used a least-squares matching technique (LMM) and an adaptive processing method (ADP) to study the behaviour of slowness and azimuth measurements made on two synthetic interfering wavelets having different arrival vectors and onset times. We have applied these results to the analysis of real array seismograms. Some of the effects generated synthetically are frequently observed on real seismograms of earthquakes recorded at Yellowknife at distances close to 50° and 90°. We have also processed sufficient data to illustrate how the interference phenomenon can be used to confirm the presence of radial velocity anomalies in the lower mantle. NumerousP arrivals from South American earthquakes at distances between 78° and 98° suggest the presence of two radial velocity anomalies at depths close to 2400 and 2730 km below the Caribbean region; these anomalies also appear to vary laterally.Contribution No. 864 from the Earth Physics Branch.     

Teleseismic body waves extracted from ambient noise cross correlation between F-net and ChinArray phase II

The vertical-vertical noise cross-correlation functions (NCFs) between two seismic arrays, the Japan F-net and ChinArray phase II, are calculated using continuous recordings during 2013–2016. After array interferometry to obtain bin stacked NCFs, clear body waves are retrieved at different period bands. Teleseismic direct P waves for distance 15–40 degrees are observed between short period 3–10 ?s while core reflected PcP/ScS waves are more obvious for longer period 30–60s. The signal-to-noise-ratio (SNR) of the short period P waves reaches its highest point with bin widths around 20 ?km while SNRs of PcP and ScS increase slowly with bin width. All those body waves demonstrate clear directivity with strong signals traveling from the east. The time-lapse SNR variations for the PcP and ScS show correlation with the occurrence of major earthquakes, while the P-wave SNR demonstrates seasonal variations with additional contribution from major earthquakes. The present results suggest teleseismic body waves can be retrieved through bin stacking, though further processing is still necessary to obtain finer waveforms such as P wave triplications.     

金银岛岩土台阵原位剪切波速剖面评估

土层的剪切波速是描述土动力学特性的重要参数之一。利用金银岛岩土台阵记录的8次浅源地方震的弱震动数据,使用解卷积的地震干涉测量法识别的剪切波走时,评估了该台阵两个水平方向的原位剪切波速剖面。结果表明:在44.2m深度以上,估计与实测的平均剪切波速剖面基本一致,而在44.2m到103.6m深度范围前者大于后者;本研究估计的平均剪切波速剖面比MEHTA等（2007）估计的平均剪切波速剖面更接近实测结果,在44.2m到103.6m深度范围,本研究估计的平均剪切波速与MEHTA等（2007）估计的平均剪切波速相近,二者均大于实测的平均剪切波速。     

Optimal configurations of wave energy device arrays

In this paper, the influence of the spatial configuration of a wave energy device array upon total power output is investigated. Hydrodynamic interactions are computed using a method capable of producing the linear wave theory solution to arbitrary accuracy. The overall performance of devices with two different power take-off arrangements is maximised at one incident wave frequency and direction by altering the formation of the array. Minimisation of the power is also carried out in a third case in order to demonstrate potential array-related losses. The optimisation is applied using two different approaches in each case: the Parabolic Intersection (PI) method and a Genetic Algorithm (GA). The former is a heuristic technique that has been devised for this study to enable rapid array construction using only simple calculations. The latter is an existing method, applied here with a novel crossover operator. Although considerably more computational effort is required, superior results may be obtained using the GA compared to the PI method. All of the arrays are subsequently analysed under incident waves of different frequency and direction, the resulting behaviour explained in terms of certain geometrical features of the arrangements.     

一种固定选图数的实时幸运成像算法

幸运成像技术是一种从大量短曝光图像中选取少量幸运好图进行配准、叠加的高分辨率图像恢复技术,能够有效减小大气湍流对图像质量的影响,但传统的基于中央处理器(Central Processing Unit,CPU)的幸运成像算法难以实现实时化.利用现场可编程门阵列(Field Programmable Gate Array,...