数字式水声语音通信发射器系统的研制     

程恩  王清池 《海洋科学》2002,26(7):47-49

利用纵振换能器的纵向振动与换能器前盖板的弯曲振动相耦合原理，采用纵振换能器与声反射器配合，研制出一种适应在复杂海洋声信道进行高速率传输，具有低频，宽带，大功率等优点的水声换能器。  相似文献   

用于研究东海天然气水合物的地震资料处理方法   总被引：3，自引：0，他引：3  

刘怀山  周正云 《中国海洋大学学报(自然科学版)》2002,32(3):441-448

通过对东海海域二维地震、单道地震、浅层剖面等资料进行的综合研究表明 :用于研究天然气水合物的地震资料处理应提高速度分析精度和分辨能力 ,进行子波估算 ,压制多次波 ,相对保持振幅 ,DMO,AVO及波阻抗特殊处理等。在地震剖面上天然气水合物主要特征有 :BSR、振幅异常、速度异常、AVO异常等标志特征。据此 ,可对天然气水合物进行识别和预测。东海海域是天然气水合物可能赋存的有利部位 ,其中冲绳海槽是天然气水合物成藏的目标区域。  相似文献   

基于尺度空间的角反射器车载SAR影像坐标定位   总被引：1，自引：0，他引：1  

戴国梦  潘斌  罗天文  魏思奇 《测绘通报》2020,(4):1-5

确定角反射器（CR）在SAR影像中的高精度影像坐标是合成孔径雷达影像（SAR）几何校正、辐射校正和形变检测等研究的基础。本文提出了一种基于尺度空间的角反射器车载SAR影像坐标定位方法。通过对仿真数据和车载SAR影像数据的角反射器进行定位试验，验证了该方法的可行性和稳定性；并与使用地面控制点几何纠正后的角反射器定位结果进行对比，验证了该方法满足子像素级定位精度的需要，且无需地面控制点。  相似文献   

南中国海存在天然气水合物的地球物理证据   总被引：6，自引：0，他引：6  

徐华宁  郑晓东  张光学 《地质科技情报》2006,25(2):60-63

以多道高分辨率地震数据为基础,分析了天然气水合物地震识别的关键技术,即地震成像与地震反演.地震成像结果显示南中国海可能具有含天然气水合物地层的地震反射特征,包括似海底反射(BSR)、振幅空白带、BSR与沉积地层斜交等天然气水合物存在的标志性特征,是南中国海域存在天然气水合物的定性地球物理证据;而地震反演结果则揭示该研究区存在地层速度结构异常,是南中国海存在天然气水合物的定量地球物理证据.  相似文献   

利用InSAR技术获取三峡地区的数字高程模型   总被引：13，自引：8，他引：5  

乔学军  李澍荪  王琪  游新兆  杜瑞林 《大地测量与地球动力学》2003,23(2):122-127

利用先进的合成孔径雷达干涉测量(InSAR)技术，使用38幅1992～2000年间三峡地区的ERS卫星SAR图像，并利用USGS的低精度DEM，得到了该地区的DEM，与GPS高程结果对比的差值为15～128m。干涉结果表明，基线小于200m的串行数据图像对具有较好的相干性；基线大于200m、在晚春和夏季观测的串行数据图像对容易出现失相关，而几乎所有重复轨道的SAR图像对在进行配准时都不相关。为了进一步获得三峡地区较高精度的数字高程模型，在该地区建立了角反射器，为研究和监测三峡地质灾害与地壳运动奠定了良好的基础。  相似文献   

Crustal and Upper-Mantle Seismic Reflectors beneath the Three Gorges Reservoir Region     

邹志辉  周华伟  廖武林 《中国地质大学学报(英文版)》2011,(2)

Seismic studies of the crustal structure beneath the Three Gorges Reservoir(TGR) region in Central China have been limited by the sparse and uneven distribution of seismic stations.To in-crease the station coverage,we made three deployments of a mobile seismologic array in the TGR re-gion during the three summers from 2008 to 2010.Here we present interpretations along a west-east profile through the central TGR region based on new seismic waveform data and a velocity model con-strained by regional earthquak...  相似文献   

A Study of the Fitting Accuracy of the Active Reflector for a Large Spherical Radio Telescope     

Xiao-Qiang Tang  Jin-Song Wang  Qi-Ming Wang Department of Precision Instruments  Tsinghua University  Beijing    National Astronomical Observatories  Chinese Academy of Sciences  Beijing   《中国天文和天体物理学报》2003,3(5):478-490

We propose a spatial three-degree-of-freedom (DOF) parallel mechanism combining two degrees of rotations and one degree of translation to support the active reflector units of a large spherical radio telescope. The kinematics, workspace and accuracy of the mechanism are analyzed. One-dimensional and two-dimensional fitting errors to the working region of active reflector are investigated. Dimensional parameters of the mechanism and active reflector unit are examined with respect to the requirement of fitting accuracy. The result of accuracy analysis shows the effectiveness and feasibility of the proposed mechanism, and gives a design rule to guarantee the highest working frequency required by large radio telescope.  相似文献   

Unique problems associated with seismic analysis of partially gas-saturated unconsolidated sediments   总被引：1，自引：0，他引：1  

M.W. Lee  T.S. Collett 《Marine and Petroleum Geology》2009

Gas hydrate stability conditions restrict the occurrence of gas hydrate to unconsolidated and high water-content sediments at shallow depths. Because of these host sediments properties, seismic and well log data acquired for the detection of free gas and associated gas hydrate-bearing sediments often require nonconventional analysis. For example, a conventional method of identifying free gas using the compressional/shear-wave velocity (V_p/V_s) ratio at the logging frequency will not work, unless the free-gas saturations are more than about 40%. The P-wave velocity dispersion of partially gas-saturated sediments causes a problem in interpreting well log velocities and seismic data. Using the White, J.E. [1975. Computed seismic speeds and attenuation in rocks with partial gas saturation. Geophysics 40, 224–232] model for partially gas-saturated sediments, the difference between well log and seismic velocities can be reconciled. The inclusion of P-wave velocity dispersion in interpreting well log data is, therefore, essential to identify free gas and to tie surface seismic data to synthetic seismograms.  相似文献   

Structural analysis of FAST reflector supporting system     

Y.F. Luo  C.G. Deng  G.Q. Li  Y.M. He 《Astrophysics and Space Science》2001,278(1-2):231-236

According to the deformation and movement requirements of the FAST reflector, a multi-purpose analysis, including the load-bearing behavior, deformation, construction costs of the reflector supporting structure and its model, is presented in this paper. The advantages and disadvantages of steel and aluminum alloy structures are also discussed and compared through detailed design calculations under load-bearing capacity and normal working conditions. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

Two dimensional fluid flow models at two gas hydrate sites offshore southwestern Taiwan     

《Journal of Asian Earth Sciences》2014

Fluid migration patterns are important for understanding gas hydrate and hydrocarbon systems. However, conducting experiments on or below the seafloor is difficult because crustal fluid flow rates are usually very slow, so long term observations are needed. Temperature can be used as a good tracer for studying fluid flows. Temperatures derived from bottom-simulating reflectors (BSRs) might help to understand fluid migration patterns in shallow marine sediments. In this study, we studied 2D fluid flow patterns in two potential gas hydrate provinces offshore southwestern Taiwan: the Yung-An Ridge in the active margin and Formosa Ridge in the passive margin. We used 2D bathymetry, average seafloor temperatures and regional geothermal gradients measured by thermal probes, as constraints to construct 2D theoretical conductive temperature fields using finite element methods. We then compared the BSR-based temperature with the theoretical conductive temperature field. The results show a temperature discrepancy attributed to advective heat transfer due to fluid migration. For the Yung-An Ridge, the BSR-based temperatures are about 2 °C higher than the model: Especially in (1) near a fault zone, (2) under the eastern flank where there are strong seismic reflectors in a pseudo-3D seismic dataset, and (3) near a fissure zone. For the Formosa Ridge, our results showed a distinct decrease in temperatures around the southern peak of the ridge, where an active gas plume was found. BSR-based temperatures predict on average 2 °C lower than the model. At these two sites, the shallow temperature fields are strongly affected by 2D bathymetry. However, new insights regarding fluid flow patterns can be obtained using this model approach.  相似文献