鄂尔多斯盆地塔巴庙区块下石盒子组砂岩储层含气性预测

针对鄂尔多斯盆地塔巴庙区块下石盒子组砂岩储层预测的重点和难点,结合其地质、地球物理特征,采用地震属性提取技术、地震测井联合反演技术、可视化解释技术等,初步建立了一套适合该区地质特征的三维储层预测的技术方法.查明了下石盒子组目的层段储集体的空间展布特征,预测了目的层段含气性特征.在此基础上,对研究区进行了评价,划分了有利储层发育带及有利含气储集带.对本区的天然气勘探开发起了重要指导作用.      

Quantitative comparison of river inflows to a rapidly expanding lake in central Tibetan Plateau

The recent rapid expansion of inland lakes on the Tibetan Plateau (TP) are a good indicator of the consequences of climate change. Quantifying the hydrological cycle of the lake basin is fundamentally important to understand the causes of lake growth. However, the hydrological processes of the TP interior are very complex and difficult to investigate because of the lack of observations. This is especially true for estimating the lake changes when run‐off inflows are affected by small lakes located in the flow routes within drainage areas. We used an integrated hydrological model, in combination with glacier melt and lake retention models, to analyse the run‐off inflows to Lake Siling Co, the largest endorheic lake in Tibet. It includes four subdrainage basins: Zhajiazangbu, Zhagenzangbu, Alizangbu, and Boquzangbu. Lake Siling Co was characterized by considerable increases during warm season from 1981 to 2012, due to the increased run‐off from Zhajiazangbu accounting for about 51–62% of the total run‐off inflows. Moreover, the dramatic increases exhibited during cold seasons were related to the increased retention water released from the small lakes within Zhagenzangbu and Alizangbu. Of the studied subdrainage basins, Boquzangbu contributed the least during both warm and cold seasons. On average, the annual amount of evaporation from lakes within the drainage area was about 2 times greater than that of glacier melt run‐off. Our results suggest that the retention effects of lakes on river inflows should receive more attention, because understanding these effects is potentially crucial to improved understanding of lake variations in the TP.     

室内位置服务智慧化应用研究

针对人们室内活动增多对室内位置智能化服务需求迫切的问题,该文简要阐述了主要的室内定位技术,搭建了室内位置服务云平台,并研发了终端大众位置服务软件.在云计算平台和Android平台分别提供了地图浏览与查询、定位导航、信息交互、用户管理等服务.通过蓝牙校正行人航迹推算的混合室内定位,开展了位置联动、位置感知、位置搜索等智能化位置应用研究.提供了位置信息智慧化服务模式,支撑了大众位置服务中所需的找到走失的人、找回车位、寻找和访问店铺等工作,将为推进室内定位技术应用、扩宽智慧化位置服务领域形成有益参考.     

GPS反射信号用于海冰识别与海面测高

针对全球定位系统反射信号干涉测量(GPS-IR)反演海面参数技术模型简单且应用单一的问题,该文提出引入表征信号振幅变化的阻尼系数来修正粗糙面对反射信号的影响,以非线性最小二乘算法对修正模型的参数进行识别.实验表明:在海冰识别上,阻尼系数的变化可清晰反映测站附近海冰状态的变化,证明了岸基GPS-IR识别海冰的可行性;在海面测高上,反演值与验潮站的实测值的相关系数达到0.98以上,相比经典频谱分析理论,均方根误差和平均绝对误差降低了约50％.     

基于SRTM控制的高分遥感影像区域网平差方法

针对异轨高分辨率卫星影像基高比小、重叠区域弱交会现象,本文提出SRTM(Shuttle Radar Topography Mission)控制的高分遥感影像区域网平差方法.该方法以高程值为相邻影像连接点的高程控制,进行光束法区域网平差,进行影像RPC(Rational Polynomial Coefficient)参数精化,避免弱交会情况下高程误差放大现象,降低同名点的相对偏移.采用高分一号四景进行实验,结果表明:通过引入高程控制的光束法区域网平差,改善纠正后影像连接区域错开现象,影像平面相对定位精度提高到一个像素以内,满足相邻影像的拼接需求.     

不同IGS精密产品对PPP收敛速度影响分析

精密单点定位(PPP)是一种新型定位技术并广泛应用,如卫星的精密轨道确定、高精度导航服务、大地测量与航空摄影测量、地震预测、空间大气探测等领域.与RTK技术相比,目前精密单点定位存在一定的瓶颈,其收敛速度较慢,对精密单点定位的市场应用和市场推广均产生了不利影响,因此分析精密单点定位收敛速度的影响因素变得十分重要.IGS各家的分析中心具备卫星的精密轨道确定和精密钟差的解算能力,能够给用户提供免费的服务产品,其中部分分析中心还提供了不同采样间隔的精密产品.本文详细分析了不同分析中心以及不同采样间隔的精密产品对PPP收敛速度的影响,并得出了一些结论.