RTKLIB 软件静态精密单点定位精度测试与分析     

张建龙  徐爱功  张兆南  吴探诗  李国明 《全球定位系统》2014,(1):37-41

介绍了精密单点定位的基本原理及常用组合量,利用日本东京海洋大学研发的开源软件RTKLIB进行静态精密单点定位数据处理,采用事后、快速、超快速三种星历及钟差产品对某IGS站单天观测值进行解算,并将处理结果和准确值对比。结果表明事后和快速产品单天解收敛曲线基本一致,最终收敛值 X、Y 、Z三个方向偏差在4 cm左右,完全满足一般精度要求的工程需要;采用超快速产品Y 方向上偏差较大,表明超快速产品对该软件的定位精度有一定的影响。  相似文献   

专用底质类型符号系统逻辑体系的设计研究     

温朝江  崔高嵩  卞鸿巍  王沫 《海洋测绘》2013,33(1):53-56

根据我国航海保障和海洋沉积学研究需要,分析了航海图和海洋底质专题图上底质类型符号系统逻辑体系的特点及参考价值,提出了专用底质类型符号系统的设计原则及设计方案。  相似文献   

基于POI数据的城市建筑功能分类方法研究     

曹元晖  刘纪平  王勇  王良杰  吴文周  苏奋振 《地球信息科学学报》2020,22(6):1339-1348

对建筑物进行建模与分析是智慧城市建设的重要任务之一。将城市中数量庞大的建筑物按功能分类,辅助认知城市内部空间结构,对政府部门开展人口估计,土地管理,城市规划等工作具有重要意义。本文以蕴含丰富语义信息的兴趣点（POI, Point of Interest ）作为主要信息源,针对POI分布稀疏导致大量建筑物无法识别出功能的问题,改进了传统的城市功能区定量识别方法。该方法为建筑物内部及周边一定区域范围内的POI赋予反距离权重,通过计算不同类型POI的加权频数密度比例来识别建筑物功能类型。文中以北京市西四环中路附近5000多栋建筑物为例进行实验验证,实现了将目标区域内的建筑物按功能类型划分为居住、商业、公服和3种混合类型,识别率达93.04%,与人工判别的结果对比得出总体分类精度达91.18%。该方法采用易于获取的互联网POI数据,可以实现大范围建筑物功能类型的快速自动化识别,丰富了城市建筑模型语义属性,扩展了POI数据的应用范围。  相似文献   

GPS在易门1∶5万水系沉积物测量质量监控中应用   总被引：1，自引：0，他引：1  

常旭坤 《云南地质》2010,29(4):461-462,428

GPS的单点绝对定位及航迹功能应用到水系沉积物地球化学测量野外施工质量监控,能有效避免人为因素导致点位失真、采样随机性大等问题,提高野外定点精度,并可及时了解野外进度及采样点的到位情况。  相似文献   

湘黔桂交界区贵州省从江县黎家坡南华系剖面新观察——一条良好的南华大冰期沉积记录剖面   总被引：1，自引：0，他引：1  

卢定彪  肖加飞  林树基  刘爱民  牟世勇  陈仁  易成兴  王兴理 《地质通报》2010,29(8):1143-1151

从江县黎家坡南华系剖面位于黔桂交界处,交通尚便,是一条地层发育良好、厚度巨大、沉积连续、层序完整、顶底界线清楚的剖面。内部岩石地层单位由下至上依次为:长安组、富禄组和黎家坡组,其划分标志清楚,易于识别和掌握,并可进行区域对比。在剖面上,南华系与下伏青白口系下江群隆里组和上覆震旦系陡山沱组均为整合接触。该剖面较完整而连续地记录了该区南华大冰期(包括长安冰期、富禄间冰期和南沱冰期)的沉积演化史,是研究雪球事件的良好场所之一。  相似文献   

MORPHOLOGY AND GROWTH PATTERNS OF THE USRI RIVER POINT BARS, BIHAR, INDIA     

《国际泥沙研究》2000,(4)

1 INTRODUCTIONThe exact mechanism of accumulation of sediments in point bars is not clearly known. Many scientistsinvestigated the problem. In the river Klaralven, Sundborg (1956) observed the development of sometransverse bars in the initial stage of the point bar formation. These transverse bars tend to becomelongitudinal as they extend close to the stream bed. Martvall and Nilsson (1972) investigated the problemof point bar formation experimentally in a laboratory flume. The flume st…  相似文献   

Truncated geoid and gravity inversion for one point-mass anomaly   总被引：1，自引：0，他引：1  

P. Vajda  P. Vaníček 《Journal of Geodesy》1999,73(2):58-66

The truncated geoid, defined by the truncated Stokes' integral transform, an integral convolution of gravity anomalies with the Stokes' function on a spherical cap, is often used as a mathematical tool in geoid computations via Stokes' integral to overcome computational difficulties, particularly the need to integrate over the entire boundary spheroid. The objective of this paper is to demonstrate that the truncated geoid does, besides having mathematical applications, have physical interpretation, and thus may be used in gravity inversion. A very simple model of one point-mass anomaly is chosen and a method for inverting its synthetic gravity field with the use of the truncated geoid is presented. The method of inverting the synthetic field generated by one point-mass anomaly has become fundamental for the authors' inversion studies for sets of point-mass anomalies, which are published in a separate paper. More general applications are currently under investigation. Since an inversion technique for physically meaningful mass distributions based on the truncated geoid has not yet been developed, this work is not related to any of the existing gravity inversion techniques. The inversion for one point mass is based on the onset of the so-called dimple event, which occurs in the sequence of surfaces (or profiles) of the first derivative of the truncated geoid with respect to the truncation parameter (radius of the integration cap), its only free parameter. Computing the truncated geoid at various values of the truncation parameter may be understood as spatial filtering of surface gravity data, a type of weighted spherical windowing method. Studying the change of the truncated geoid represented by its first derivative may be understood as a data enhancement method. The instant of the dimple onset is practically independent of the mass of the point anomaly and linearly dependent on its depth. Received: 26 September 1996 /Accepted: 28 September 1998  相似文献   

数字地图符号的形状描述与识别   总被引：11，自引：0，他引：11  

黄文骞 《测绘学报》1999,28(3):233-238

采用地图自动化替代既费时又费力的传统手工数字化,是当代地图制图学的一项重要研究内容,而数字地图符号的描述与识别则是实现这一目标的关键技术。为此,本文利用带搜索控制准则的新边界跟踪算法改进了传统的边界跟踪算法,提出了用傅立叶系数描述符号,给出了如何由链码计算傅立叶系数,并对计算公式作了进一步改进,以及由傅立叶系数提取形状特征不变量,最后,对符号识别进行实验验证,并做了相应的分析讨论。  相似文献   

高铁地震震源子波时间函数及验证          下载免费PDF全文

张固澜  何承杰  李勇  段景  王婷一  詹熠宗  杜皓  罗帆 《地球物理学报》2019,62(6):2344-2354

基于纵横波产生机理并结合高铁列车及铁轨结构,本文给出了高铁列车产生地震纵波及横波震源(点源及等效源)子波的时间函数;通过实际高铁地震数据及合成高铁地震数据分析,验证了高铁地震震源子波时间函数的合理性;在高铁列车匀速、加速及减速运行情况下,利用高铁地震点源子波合成记录分析了高铁地震震源子波的频谱特征,为实际高铁地震数据处理解释奠定了良好的基础.  相似文献   

Target-oriented imaging using extended image volumes: a low-rank factorization approach     

Rajiv Kumar  Marie Graff  Ivan Vasconcelos  Felix J. Herrmann 《Geophysical Prospecting》2019,67(5):1312-1328

Imaging in geological challenging environments has led to new developments, including the idea of generating reflection responses by means of interferometric redatuming at a given target datum in the subsurface, when the target datum lies beneath a complex overburden. One way to perform this redatuming is via conventional model-based wave-equation techniques. But those techniques can be computationally expensive for large-scale seismic problems since the number of wave-equation solves is equal to two times the number of sources involved during seismic data acquisition. Also conventional shot-profile techniques require lots of memory to save full subsurface extended image volumes. Therefore, we can only form subsurface image volumes in either horizontal or vertical directions. To exploit the information hidden in full subsurface extended image volumes, we now present a randomized singular value decomposition-based approach built upon the matrix probing scheme, which takes advantage of the algebraic structure of the extended imaging system. This low-rank representation enables us to overcome both the computational cost associated with the number of wave-equation solutions and memory usage due to explicit storage of full subsurface extended image volumes employed by conventional migration methods. Experimental results on complex geological models demonstrate the efficacy of the proposed methodology and allow practical reflection-based extended imaging for large-scale five-dimensional seismic data.  相似文献