用于JATC远程时间比对的双频GPS接收机   总被引：1，自引：1，他引：0  

高玉平  漆溢  王正明 《时间频率学报》2006,29(1):6-12

中国科学院国家授时中心为“我国综合原子时（JATC）建立与保持的研究”项目研制的双频多通道GPS时间传递接收机NTSCGPS-2，不仅具有远程时间比对的功能，还增加了我国综合原子时需要的本地钟比对功能和精密定位功能。在不增加其它比对设备的情况下，满足JATC项目对远程时间比对的要求。NTSCGPS-2具有如下性能特点：（1）采用双频观测，可实测电离层时延；（2）远程（西安-上海、西安-澳门）时间比对精度达到2ns；（3）具有本地钟间的比对功能，在正常共视观测的同时，还可进行2个本地钟间的比对；（4）具有精密定位功能，相对定位精度为5cm。  相似文献   

用于双天线干涉实验的数字相关接收机   总被引：1，自引：1，他引：0  

张坚  颜毅华  刘飞  王威 《天文研究与技术》2006,3(2):148-153

介绍了用于双天线干涉实验的数字相关接收机器的构成和信号处理过程。  相似文献   

GNSS接收机与全站仪控制点恢复测量及精度分析     

孙玉强  袁兴明 《测绘与空间地理信息》2021,44(4):132-134,138

主要利用GNSS接收机与全站仪对基坑控制点进行恢复测量,GNSS接收机通过RTK技术在基坑周边重新布设5个控制点,利用全站仪假定方向推算出控制点的坐标,并且分析其相对精度。通过实地观测计算分析,推算出的坐标与基坑中心点位置X方向相差5 mm、Y方向相差4 mm,恢复后的控制点能够对其他特征点进行详细测设。利用高精度的0.5″级全站仪进行点位测量精度对比分析,点位精度在2 mm范围之内,可以得出工程单位所用的仪器可满足精度,能够用于此类工程点位测设工作。  相似文献   

FY2卫星展宽云图接收机设计与实现     

段云飞  熊承伟  王军海  李在海 《气象科技》2013,41(2):207-211

静止气象卫星是监测地表、大气、海洋以及空间环境等相关数据的重要手段,为气象、农业、空间环境等领域提供着大量的科学数据.重点对FY2接收机的实现方法进行了研究,主要内容包括二次变频方法、基于HSP50110/HSP50210的数字解调、差分解码、关键参数设置以及信号指示等.最后以误码率为指标并结合图像接收效果对接收机性能进行直观评估,结果表明,所设计的接收机图像清晰、误码率低,具有一定的实际意义与参考价值.  相似文献   

基于波动方程的检波点二次定位     

黄龙泽 《海洋地质译丛》2011,(2):34-38

在进行浅海过渡带地震资料采集时,需要将电缆和检波器沉放到海底,由于洋流、潮汐等因素的影响会使检波点的实际位置与预设位置不同,从而严重影响了后续的地震资料处理工作,因此需要对检波点进行二次定位。在海底检波点二次定位中,炮点位置已知而检波点位置未知,需要从多个炮点位置正向外推波场,使波场逐步延拓到检波点,以此来获得检波点的位置。具体实现是在海底划分网格应用克希霍夫积分法外推渡场,获得网格点的能量值,能量最高的网格点便是检波点的位置。在划分网格时需要先粗分网格,求得网格点能量值,然后在能量高的网格点区域重新细分网格,通过细分网格点的能量值来确定出检波点位置。在检波点二次定位中利用的主要是直达波的波场信息,在预处理时,需要突出直达波压制干扰波。基于波动方程的检波点二次定位在模拟和实际地震资料处理中都得到了良好的效果,验证了这种方法的可行性。  相似文献   

浅海爆炸声传播损失及简正波分离实验研究     

刘立勇  王婷婷 《热带海洋学报》2011,(3)

文章简要介绍了浅海声传播损失的研究背景和基本理论方法。通过1/3倍频程滤波对浅海爆炸宽带信号的不同频段在浅海的传播损失情况进行了分析,描述了浅海环境对声传播损失的影响;同时在不知道先验信息的条件下,利用垂直阵声压数据成功地进行了简正波分离,并与理想条件下Kraken简正波模型计算出的结果进行了比较分析。  相似文献   

Destruction of the North China Craton: a perspective based on receiver function analysis     

Chuansong He  Shuwen Dong  M. Santosh  Qiusheng Li  Xuanhua Chen 《Geological Journal》2015,50(1):93-103

The North China Craton (NCC), which is composed of the eastern NCC and the western NCC sutured by the Palaeoproterozoic Trans‐North China Orogen, is one of the oldest continental nuclei in the world and the largest cratonic block in China. The eastern NCC is widely known for its significant lithospheric thinning and destruction during the Late Mesozoic. Models on the destruction of the eastern NCC can be principally grouped into two: (1) thermal/mechanical and/or chemical erosion, and (2) lower crustal and (or) lithospheric delamination. The erosion model suggests that the NCC lithospheric thinning resulted from chemical and/or mechanical interactions of lithospheric mantle with melts or hydrous fluids derived from the asthenosphere, whereas the delamination model proposes lithospheric destruction through foundering of eclogitic lower crust together with lithospheric mantle into the underlying convecting mantle. However, those models lack seismic evidence to explain the destruction process. Here, we analyse the crustal structure and upper mantle discontinuity by employing the H–k stacking technique of receiver function as well as the depth domain receiver function. Our results indicate deep mantle upwelling and lower crustal delamination beneath the eastern NCC, and suggest that either or both of these processes contributed to the unique lithospheric thinning and destruction of the eastern NCC. © 2013 The Authors. Geological Journal published by John Wiley & Sons, Ltd.  相似文献   

The crustal structure beneath the northwest fjords, Iceland, from receiver functions and surface waves   总被引：1，自引：0，他引：1  

Z. J. Du  & G. R. Foulger 《Geophysical Journal International》1999,139(2):419-432

Five broad-band seismic stations were operated in the northwest fjords area of Iceland from 1996 to 1998 as part of the Iceland Hotspot project. The structures of the upper 35  km or so beneath these stations were determined by the modelling and joint inversion of receiver functions and regional surface wave phase velocities. More than 40 teleseismic events and a few regional events containing high-quality surface wave trains were used. Although the middle period passband of the seismograms is corrupted by oceanic microseismic noise, which hinders the interpretation of structural details, the inversions reveal the overall features. Many profiles obtained exhibit large velocity gradients in the upper 5  km or so, smaller zero gradients below this, and, at ~23  km depth, a zone 2–4  km thick with higher velocity gradients. The two shallower intervals are fairly consistent with the 'upper' and 'lower' crust, defined by Flovenz (1980 ). The deep zone of enhanced velocity gradient seems to correspond to the sharp reflector first reported by Bjarnason et al . (1993 ) and identified by them as the 'Moho'. However, this type of structure is not ubiquitous beneath the northwest fjords area. The distinctiveness of the three intervals is variable, and in some cases a structure with velocity gradient increasing smoothly with depth is observed. We term these two end-members structures of the first and second types respectively. Structures of the second type correlate with older areas. Substantial variation in fundamental structure is to be expected in Iceland because of the great geological heterogeneity there.  相似文献   

Wavefield decomposition for passive ocean bottom seismological data   总被引：1，自引：0，他引：1  

M. Thorwart  T. Dahm 《Geophysical Journal International》2005,163(2):611-621

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依舒断裂带北段莫霍面特征与泊松比     

李大伟  教智浡  胡宝慧 《地震地磁观测与研究》2021,42(5):76-81

伊舒断裂带北段是黑龙江省地震跟踪监测重点区域之一,具有较强的地震活动性,为主要历史强震发生区域。利用该区域4个固定地震台记录到的远震地震事件资料,采用频率域反褶积方法,提取远震P波接收函数,再利用H—κ叠加方法计算台站下方莫霍面深度和泊松比。结果表明：受太平洋板块俯冲作用的影响,块体间相互挤压,双鸭山地震台下方莫霍面发生了错断,并且一侧莫霍面叠置在另外一侧上方,鹤岗地震台西侧莫霍面上方存在1个速度间断面;区域内泊松比值较高,为0.266—0.277,反映了上地幔铁镁物质上涌到下地壳中。  相似文献