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1.
用海洋GPS进行水下运动载体的三维定位   总被引:3,自引:1,他引:3  
用单个装载超短基线的海洋GPS进行水下运动载体的三维定位,和三个智能型浮标进行水下运动载体的三维定位相比,定位精度相当,隐蔽性更好,造价更低,更具实用价值。本文对单个装载超短基线的海洋GPS进行水下运动载体三维定位的原理和精度进行了较为详细的讨论,并得到了一些有益的结论,以供同行参考。  相似文献   

2.
分别采用GAMIT和GrafNav两种不同的软件对南海区域不同时间、不同地点所测得的GPS精密单点定位数据进行了解算,并对同一数据的解算结果进行了精度分析。研究结果表明:这两种方法解算所得结果互差达到厘米级,说明GrafNav满足GPS精密单点定位数据解算要求,具有一定的应用参考价值。  相似文献   

3.
在剖析"Jupiter"GPS接收机工作原理及其硬软件接口的基础上,实现接收机与计算机的实时通讯,为以浮标为搭载,中、远程海洋长基线精密潮位监测定位打下基础.该接收机软件实现原DOS环境下接收信号的GPS接收机,直接在Windows下实时显示、存储和处理数据.该软件不但适用于"Jupiter"接收机,通过配置串口参数,可以用于任意遵循NMEA0183协议的接收机,扩展性强.  相似文献   

4.
结合海上科研工程实践,对GPS精密单点定位模型及数据处理方法进行研究,并采取陆上静动态定位和海上动态定位试验进行了精密单点定位精度统计和分析。结果表明:在超出常规差分定位基线长度限制的广阔海域,采用精密单点定位技术可实现亚米级实时动态定位,为海上高精度实时动态定位应用提供了技术依据。  相似文献   

5.
对中国沿海RBN-DGPS系统升级意见的商榷   总被引:1,自引:1,他引:0  
刘基余 《海洋测绘》2008,28(5):9-12
依据GPS现代化的新近发展,论述了用包括4个民用测距码的三个GPS导航定位信号,船舰只需用一台GPS信号接收机就可以实现精度为±3.66m的在航三维定位测量;同时阐述了用中国的CNSS系统、俄罗斯的GLONAASS系统和欧盟的Galileo系统的三个民用导航定位信号作定位测量,能够用其无电离层效应影响的站星距离,解算出精度为±1m左右的三维位置;而不必要花巨资去升级“中国沿海RBN—DGPS系统”。  相似文献   

6.
GPS卫星定位技术,是开展海洋综合测绘的一种高效手段;如何在海洋测绘中充分发挥GPS技术精确快速定位的特长,是值得我们认真研究的重大课题。为此,本文较详细地论述了以下几个问题。1.根据边长和动静定位需要,选购适宜的GPS信号接收机;2.从海洋国土整体着眼,精心设计GPS海洋定位网的全网结构;为便于评定GPS数据质量,宜采用闭合环路式结构;3.正视SA技术对实时定位精度的损失,运用求差法削弱SA技术的影响。  相似文献   

7.
GPS精密单点定位精度分析   总被引:11,自引:0,他引:11  
首先介绍了精密单点定位技术,然后详细分析了这种技术的精度,最后基于这种技术,对现在运行的无线电指向标/差分GPS台站,提出了改进建议。  相似文献   

8.
概述了GPS eTrex工作原理、性能特点,详细介绍在莱州湾海域的采样过程中GPS eTrex的导航定位情况,对定位精度与定住所用的时间进行了分析比较,证明手持GPS技术提高了海上作业的工作效率。  相似文献   

9.
GPS/GLONASS信号的同机接收问题   总被引:1,自引:0,他引:1  
本文综述了GPS/GLONASS卫星及其导航定位信号的异同点,讨论了GPS/GLONASS集成接收机的研制难点。  相似文献   

10.
一种简易的潜标辅助寻标定位系统   总被引:1,自引:0,他引:1  
介绍一种自主研发的、结合GPS定位和水声测距于一体的潜标自动搜寻定位系统。系统由安装于搜索船只上的全球定位系统GPS接收机、水声释放器甲板单元、综合信号接收处理单元(由计算机组成),以及集成于潜标系统水声释放器上的水声应答系统组成。利用GPS定位原理,将GPS测得的定位信息,与水声测距技术相结合,实现潜标系统的空间定位,为潜标系统的可靠回收提供技术保障。  相似文献   

11.
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.  相似文献   

12.
海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明:土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。  相似文献   

13.
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.  相似文献   

14.
The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.  相似文献   

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17.
《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,  相似文献   

18.
19.
A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria ( 〉 99% ), but also between polar marine bacteria and bacteria from other aquatic environments ( ≥ 98.8% ), including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.  相似文献   

20.
Sediment properties, such as water content and density, have been used to estimate the dry and wet weights, as well as the volume of sediment recovered and discharged, during benthic impact experiments conducted in the Pacific and Indian Oceans. The estimates show that the weights of dry (355-1332 t) and wet sediment (1651-4888 t) recovered during the experiments, are not only a function of the total duration and distance covered during the experiment, but also depend on water content and density of the sediment. Estimation of dry sediment and its volumetric ratio in the discharge, are key parameters for calculating the discharged volume. The estimated volume of wet sediment recovered (1427-4049 m 3 ) as well as discharged (2693-6951 m 3 ) during the experiments, provide important inputs to evaluate the sediment resettlement and migration. Using these estimates, the average depth of excavation on the seafloor, can also been calculated. However, the stages of sediment recovery and discharge are expressed differently in some of the experiments. In order to standardize these, different stages have been identified, and definitions of certain terms have been suggested, for use in the future. The methods of calculating different properties, as well as weight and volume of discharged sediment are described in the paper for use in other applications concerning deep-sea discharges.  相似文献   

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