GOCE卫星径向重力梯度一阶、二阶径向偏导数标准差的近似解析公式     

徐天河  贺凯飞 《测绘学报》2011,40(4)

基于Kaula准则,推导卫星重力梯度径向分量Tzz一阶、二阶径向偏导数T.zz、Tzz标准差的近似解析表达式,给出GOCE卫星.Tzz、Tzz标准差的近似估计值,由此分析Tzz延拓处理中可忽略的延拓误差最大高度。解析公式表明：T.zz、Tzz标准差的计算公式可近似表示成若干伽玛函数线性组合的开方,GOCE卫星.Tzz、Tzz标准差近似解析估值分别为1.269×10^-15s^-2m^-1和1.109×10^-20s^-2m^-2,由此若得到满足1 mE的精度要求,可忽略的延拓误差最大高度对于T.zz应小于0.8km,而对于Tzz应小于13.4km,延拓中重力场模型阶次应不低于200。最后基于模拟的GOCE卫星轨道,利用严格公式计算出的T.zz、Tzz标准差,验证近似解析表达式估算结果的正确性,解析结果与严格公式计算结果的相对误差小于2%。  相似文献   

室内全景三维控制场设计与建立     

梅文胜  徐芳  陈潇 《测绘信息与工程》2011,36(6):39-42,45

探讨了全景三维控制场中标志的设计与布设、三维基准网观测与平差、标志点的观测与计算等,给出了球形标志观测精度的评价方法,对其实际观测精度进行了统计与分析,控制场可满足全景检校及试验研究的需要。  相似文献   

参数优化的建筑物多边形化简研究     

安晓亚  孙群  肖强  严薇 《测绘科学》2011,36(5):146-147,171

本文针对建筑物多边形化简当前存在的问题,将参数优化的方法引入化简的全过程,在渐进式图形化简的基础上,通过把建筑物多边形的几何特征、结构特征和化简所遵循的一系列约束规则参数化、变量化表示,建立了建筑物多边形化简的数学模型,通过对模型的求解,来达到化简建筑物多边形的目的。成果已经应用于数字地图的生产,实践证明该算法的化简效果好,普适性较高,符合应用需求。  相似文献   

基于RS与GIS的雅安市土地利用景观格局变化分析研究   总被引：1，自引：0，他引：1  

田维渊  曾世斌  杨武年  罗光兵  张俊峰 《测绘与空间地理信息》2011,34(2):95-97,100

以TM遥感影像等为数据源,借助RS与GIS技术,选择了能反映研究区景观空间格局的景观指数,分析研究了雅安市2000年至2007间的景观空间格局动态变化.从两期景观指数对比得出:林地是研究区景观基质类型,研究期内景观异质性升高,破碎度增大.  相似文献   

Strymon and Strymonikos Gulf basins (Northern Greece): Implications on their formation and evolution from faulting     

Markos D. Tranos 《Journal of Geodynamics》2011

In Central and Eastern Macedonia of Northern Greece large NW–SE trending basins filled up mainly with terrestrial sediments developed during the Neogene over the Alpine basement rocks. Among them, the Strymon basin was established along the NNW–SSE trending Strouma/Strymon Lineament which formed over the tectonic boundary of the Serbomacedonian and Rhodope massifs, both representing the hinterland of the Hellenic orogen. The present study suggests that the Strymon basin was not formed as a syn-detachment basin over the Strymon Valley Detachment Fault, considered to have caused exhumation of the Rhodope massif metamorphic complex. Instead, transpressional s.l. tectonics dominated the region in the Late Oligocene-Early Miocene and it progressively changed into a wrench tectonics under which the Strymon basin has been initiated in the Middle Miocene. The basin continued to develop further under a short-lived NW–SE extension in the Middle-Late Miocene. The whole deformation is attributed to the late-stage collisional processes between the Apulia and Eurasia plates. The prevalent NE–SW extension has been constrained later on in the Late Miocene and Pliocene times activating both low-angle and high-angle NW–SE trending faults and causing the regional tilting towards the SW of the mountain fault blocks (i.e., mountain chains). From Quaternary onwards, the Strymon basin has been separated from the Strymonikos Gulf basin due to an N–S extension that mainly activates E–W striking normal faults.  相似文献   

A two-grid method for coupled free flow with porous media flow     

Prince ChidyagwaiBéatrice Rivière 《Advances in water resources》2011,34(9):1113-1123

This paper presents a two-grid method for solving systems of partial differential equations modelling incompressible free flow coupled with porous media flow. This work considers both the coupled Stokes and Darcy as well as the coupled Navier-Stokes and Darcy problems. The numerical schemes proposed are based on combinations of the continuous finite element method and the discontinuous Galerkin method. Numerical errors and convergence rates for solutions obtained from the two-grid method are presented. CPU times for the two-grid algorithm are shown to be significantly less than those obtained by solving the fully coupled problem.  相似文献   

An adaptive time integration scheme for blast loading on a saturated soil mass     

R. Al-Khoury  J. Weerheijm  K. Dingerdis  L.J. Sluys 《Computers and Geotechnics》2011

This paper presents a time integration scheme capable of simulating blast loading of relatively high frequency on porous media, using coarse meshes. The scheme is based on the partition of unity finite element method. The discontinuity is imposed on the velocity field, while the displacement field is kept continuous. The velocity discontinuity is postulated to occur in the time domain. The developed time integration scheme is unconditionally stable and has controllable numerical dissipation in the high frequency range. An important feature of the time scheme is that it allows for controlling the numerical damping in a consistent way. The time scheme has been implemented in combination with Biot’s theory of wave propagation in saturated porous media. Numerical examples have demonstrated that the proposed time scheme is, in addition to being accurate and stable, highly effective for coarse meshes. This makes the developed scheme suitable for large scale finite element analysis.  相似文献   

航磁数据在大兴安岭激流河地区地质填图中的应用     

张庆洲  王振民  李泊洋 《化工矿产地质》2011,33(3):177-180

利用航磁资料对激流河地区进行岩性地质解译,对比1:25万地质调查结果,发现在原来的三叠纪二长花岗岩分布区有一个隐伏的火山机构,该火山机构呈椭圆形、南北走向,面积约60～ 70km2,具有放射状构造.这项解译成果丰富了该地区的地质内容,为进一步的基础地质研究和找矿工作提供了有利信息.  相似文献   

南天山满大勒克蛇绿岩铬铁矿矿物学特征及其意义   总被引：1，自引：0，他引：1       下载免费PDF全文

张炜斌  张东阳  张招崇  黄河  赵莉 《岩石矿物学杂志》2011,30(2):243-258

满大勒克蛇绿岩属于南天山晚古生代蛇绿岩带,主要由蛇纹石化橄榄岩、玄武岩和含放射虫硅质岩组成。其中蛇纹岩富含铬铁矿,并具有豆荚状特征。显微镜观察和电子探针分析表明,铬铁矿具有明显的环带结构,从核部到边部呈现出由铬尖晶石到铬铁矿到磁铁矿的变化特征,元素组成上具有由富Al和Cr、贫Fe到贫Al和Cr、富Fe的变化趋势。利用铬铁矿(铬尖晶石)核部矿物的化学成分,得出铬尖晶石的结晶温度为1359～1394℃,平均1379℃;压力为2.76～3.00GPa,平均2.87GPa;相对于FMQ缓冲剂的地幔氧逸度为FMQ-1.50～FMQ-2.92log单位,平均值为FMQ-2.14log单位;地幔熔融程度F为16.7%～18.0%。结合已有研究成果,推测满大勒克蛇绿岩的基底橄榄岩单元源区为石榴石二辉橄榄岩,形成于亏损的软流圈地幔,对应的大地构造位置为弧前盆地。研究区铬尖晶石的环带特征显示其经历了温度由高到低、氧逸度由低到高的演变,反映了满大勒克蛇绿岩套的橄榄岩单元经历了高温高压的地幔环境(低氧逸度),之后随构造变动被推覆到地壳,定位之后又经历了区域变质作用的演化过程(高氧逸度)。  相似文献   

Comparison of Two Sample Preparation Methods for X‐Ray Fluorescence Spectrometry in the Determination of Ni and Cr     

Surendra P. Verma  Rosalinda González‐Ramírez  Rodolfo Rodríguez‐Ríos 《Geostandards and Geoanalytical Research》2011,35(2):183-192

Pressed powder pellets and fused beads or glass disks are routinely used in X‐ray fluorescence spectrometry for the determination of major and trace elements, respectively, in geological materials. In order to evaluate the performance of these two sample preparation methods, we determined Ni and Cr concentrations of fourteen RMs from Japan, France and South Africa, and eighty‐five igneous and three sedimentary rock samples from Mexico in both powder pellets and glass beads. We also computed new values of statistical parameters for RMs from an outlier‐based multiple‐test method and compared them with the literature mean and confidence limit values. The results showed that the multiple‐test method provided more reliable central tendency and dispersion parameters for RMs than those obtained previously from the two or three standard deviation method, or from robust methods. The powder pellet and fused bead sample preparation methods provided consistent results for Ni and Cr at concentration levels > 50 μg g^?1 in this application; for lower concentration levels, however, these methods showed somewhat greater differences. For quantitative comparisons, both ordinary and weighted least‐squares linear regression models were used to show that the two sample preparation methods provided generally unbiased results.  相似文献