论三角测量单位权方差的先验估计与后验估计

三角洲量单位权方差的先验估值一般用经典菲列罗公式计算。实践中，经常出现三角测量单位权方差的先验估值不等于后验估值的情形．本文根据条件平差的原理，证明了单位权方基的先验估值是有偏估计，经典菲列罗公式是后验估计公式的特殊形式，并推导出了广义菲列罗公式。     

Modeling and sensitivity analysis of navigation parameter errors for airborne synthetic aperture radar stereo geolocation

For the high-resolution airborne synthetic aperture radar (SAR) stereo geolocation application, the final geolocation accuracy is influenced by various error parameter sources. In this paper, an airborne SAR stereo geolocation parameter error model, involving the parameter errors derived from the navigation system on the flight platform, has been put forward. Moreover, a kind of near-direct method for modeling and sensitivity analysis of navigation parameter errors is also given. This method directly uses the ground reference to calculate the covariance matrix relationship between the parameter errors and the eventual geolocation errors for ground target points. In addition, utilizing true flight track parameters’ errors, this paper gave a verification of the method and a corresponding sensitivity analysis for airborne SAR stereo geolocation model and proved its efficiency.     

移动智能终端在贵州省耕地质量地球化学调查的实践应用

基于移动互联网、大数据发展的时代背景,本文提出了移动智能终端辅助耕地质量地球化学调查工作新模式,并应用到贵州省耕地质量地球化学调查实际采样工作中,改变了传统的工作方式,极大地提高了采样工作效率,改善了野外工作设备的便携性和室内外沟通性,加快了贵州省耕地质量地球化学调查评价项目的工作进度,为其他省开展相关工作起到示范作用。     

尼泊尔Ms 8.1级地震活动构造及次生地质灾害研究

2015年尼泊尔Mw 7.8大地震诱发了大量的山体滑坡,对尼泊尔境内与周边地区造成了严重的影响。选取离震中较近的辛杜帕尔乔克地区作为研究区,基于L波段ALOS-2和C波段Sentinel-1A两种合成孔径雷达数据,采用堆叠合成孔径雷达干涉测量（interferometric synthetic aperture radar,InSAR）技术开展震后滑坡的探测与识别,结合光学影像圈定出滑坡隐患点14处。在此基础上,联合升降轨数据和多维小基线集（multidimensional small baseline subset,MSBAS)-InSAR技术获取了典型滑坡的二维时间序列形变特征,结果表明,该典型滑坡的主要形变发生在水平东西向,最大形变速率为-69 mm/a。同时,通过对该典型滑坡时间序列中的趋势项与周期项形变信号进行分析,发现地震对于滑坡运动具有明显的加速作用,且降雨量的增加使得滑坡位移在每年的8月-11月呈现出周期性变化,可为震后滑坡监测研究提供参考。

     

基于SEID模型的单频PPP双频解算方法研究

提出了利用区域内的双频观测值建立区域SEID模型,利用单频观测值反演得到双频观测值,进而组成双频无电离层组合观测值,实现了单频PPP双频解算。算例结果表明,本文提出的新方法大大缩短了定位收敛时间,显著地提高了单频PPP的定位精度。     

利用GPS观测资料分析山西地堑系现今地壳构造活动特征

基于中国地壳运动观测网络1999～2007年的GPS复测资料,建立起整体无净旋转基准,分析了山西地堑系内部地壳运动的细节特征,并利用图形单元法分析了其应变场的分布特征,深入剖析了地壳变形的动力学机制,得出山西地堑系现今构造应变场以NW-SE向拉张应变为主,与区域现代震源机制解及长期构造变形背景相一致;临汾、大同盆地是地堑内剪切应变高值区,现今地壳活动强烈。解释了地堑系内形变异常区的成因,由此揭示出连接临汾与太原盆地的构造隆起带两端的现今地壳活动十分强烈,并同时兼有拉张破裂趋势这一重要的构造事件。     

三维地理信息系统相关技术研究

对已经成为地理信息领域研究热点的三维地理信息系统进行了较为深入地探讨。基于空间认知方法学理论，结合面积对象的思想，提出了一种新的三维地理信息系统数据结构。该数据结构符合人的一般思维，可以方便清晰地存储和管理空间数据，并且有利于三维空间对象的空间分析与显示。针对三维地理信息系统空间分析的基础环节－－三维空间点定位与查询，提出了化三维查询为二维＋一维查询，该方法可以提高三维空间查询的速度。     

Seismic intensity investigation of the 2001 M =6.0 Yajiang-Kangding earthquake and discussion on its background of seismogenic structures

An M=6.0 earthquake occurred on February 23, 2001 in the western Sichuan Province, China. The macro seismic epicenter situated in the high mountain-narrow valley region between Yajiang and Kangding counties. According to field investigation in the region, the intensity of epicentral area reached VIII and the areas with intensity VIII, VII and VI are 180 km², 1 472 km² and 3 998 km², respectively. The isoseismals are generally in elliptic shape with major axis trending near N-S direction. The earthquake destroyed many buildings and produced some phenomena of ground failure and mountainous disasters in the area with intensity VIII. This event may be resulted from long-term activities of the Litang fault and Yunongxi fault, two main faults in the western Sichuan. The movements between the main faults made the crust stress adjusted and concentrated, and finally the earthquake on a secondary fault in the block released a quite large energy.     

Linkage of liquid conductivity of glacier ice with its alkalinity over the north Qinghai-Xizang (Tibet) Plateau

Liquid conductivity (EC) measurement was conducted for the samples collected from several snow pits and ice cores over the Qinghai-Xizang (Tibet) Plateau, with their time range covering seasonal, decadal and centennial scales. Unlike the previous attention mostly focused on the acidity (H⁺) responding to the solid conductance (ECM) of glacial ice, we introduce the alkalinity (OH⁻) of snow and ice to show how it responds to EC. Strong linear relationship was established between EC and OH⁻ for these snow pits and ice cores. Positive correlation is also established between EC and major cations (Ca²⁺, Mg²⁺, Na⁺ and K⁺). Since the cations are known as the proxies for the intensity of mineral dust influx onto glaciers of the northern Qinghai-Xizang Plateau, we believe that EC could be used as an indicator for the history of dust input in deep ice core study. In fact, records in Guliya ice core since the Little Ice Age (LIA) indicate that dust load in glacier may depend on the combination of temperature and humidity. “Cold-dry” combination favors the dust arising, and results in higher EC and OH⁻ values, while “warm-wet” combination prevents dust form and EC and OH⁻ values are lower. In the past century, with the atmospheric warming and precipitation increasing over the northern plateau, which means an atmospheric condition of dust decreasing, both EC and OH⁻ displayed rapid decline.     

崇明地震台FGE磁通门磁力仪D分量基线值的确定

基线值是考察记录仪运行是否稳定可靠的一个重要指标。本文以记录仪的D分量为例,通过认真仔细地分析与探索,使用数据处理的方法,解决了崇明台FGE磁通门磁力仪基线值不稳定的问题。这对基线值的确定和日常的数据处理都具有一定的指导意义。