数字城市规划系统关键技术分析

分析了数字城市规划系统的业务需求，介绍了其基础数据更新、工作流、无纸化办公、历史空间信息管理等主要关键技术，并对其进行了讨论。     

数字地籍测绘实施中的技术问题

数字地籍测绘是目前土地管理部门的首选方案,需要制定街坊划分、界址线设定、工作底图与采集草图一体化作业、数据文件管理、街坊线、图斑的绘制等技术措施。     

A coupled,dynamical and chemical model for the prestellar core L1544: Comparison of modeled and observed C<Superscript>18</Superscript>O,HCO<Superscript>+</Superscript>, and CS emission spectra

We consider radiative transfer in C¹⁸O, HCO⁺, and CS molecular lines in a spherically symmetrical, coupled, dynamical and chemical model of a prestellar core whose evolution is determined by ambipolar diffusion. Theoretical and observed line profiles are compared for the well-studied core L1544, which may be a collapsing protostellar cloud. We study the relationship between the line shapes and model parameters. The structure of the envelope and kinematic parameters of the cloud are the most important factors determining the shape of the lines. Varying the input model parameters for the radiative transfer—the kinetic temperature and microturbulent velocity—within the limits imposed by observations does not result in any substantial variations of the line profiles. The comparison between the model and observed spectra indicates that L1544 displays a flattened structure, and is viewed at an oblique angle. A two-dimensional model is needed to reproduce this structure.     

Caledonian Low-Temperature Granulite-Facies Metamorphism in the West Kunlun Orogenic Belt—SHRIMP Chronological Evidence from Zircon

The West Kunlun orogenic belt is located at the conjunction of the paleo-Asian tectonic system and the Tethys tectonic system. Petrological and mineralogical studies of the Early Cambrian metamorphic surface crust in this region have shown that in case the metamorphism reached low-temperature granulate facies, the typical mineral assemblage is biotite-garnet-silimanite-K feldspar-plagioclase-quartz. The peak metamorphic temperatures are within the range of 720–740°C and the pressure is 0.6 GPa ±. Three types of metamorphic zircon have been detected in the metamorphic rocks: the complex inclusion-bearing type ; the early relic zircon inclusion-bearing type; and the inclusion-free type. SHRIMP age determination of these three types of metamorphic zircon have revealed that these zircons were formed principally during 400–460 Ma, indicating that pre-Cambrian metamorphic surface crust rocks underwent low-temperature granulite facies metamorphism during the Caledonian. In combination with the geological characteristics of this region, it is considered that when the oceanic basin was closed, there occurred intense intracontinental subduction (type A), bringing part of the Early Cambrian metamorphic basement in this region downwards to the lower crust. Meanwhile, there were accompanied with tectonic deformation at deep levels and medium- to high-grade metamorphism. This study provided important chronological and mineralogical evidence for the exploration of the evolutionary mechanism and process of the West Kunlun Early Paleozoic. Part of the results from the research project “ Research on the West Kunlun pre-Cambrian tectonic events” under the program “ Research on the important geological problems of China’ s pre-Cambrian” (No. 200113900070) sponsored by the China National Geological Surveying Bureau.     

Confirmation of an Early Cretaceous age for the Qihulin Formation in eastern Heilongjiang Province, China: constraints from a new discovery of radiolarians

The coal-bearing, alternating marine and non-marine Longzhaogou Group in eastern Heilongjiang, northeastern China, has long been considered as Jurassic, or mainly Jurassic, in age. However, recent studies have demonstrated that the ammonites and dinoflagellate cysts are of Early Cretaceous age. This has now been confirmed by new radiolarian evidence. The radiolarian fauna recovered from the upper Qihulin Formation of the Longzhaogou Group consists of nine poorly preserved species referable to nine genera. Novixitus is a Cretaceous genus, and the specimens of Archaeodictyomitra sp. and Xitus sp. recovered resemble A. vulgaris Pessagno and X. spicularius (Aliev), respectively.     

Development of Geological Data Warehouse

Data warehouse (DW), a new technology invented in 1990s, is more useful for integrating and analyzing massive data than traditional database. Its application in geology field can be divided into 3 phrases: 1992-1996, commercial data warehouse (CDW) appeared; 1996-1999, geological data warehouse (GDW) appeared and the geologists or geographers realized the importance of DW and began the studies on it, but the practical DW still followed the framework of DB; 2000 to present, geological data warehouse grows, and the theory of geo-spatial data warehouse (GSDW) has been developed but the research in geological area is still deficient except that in geography. Although some developments of GDW have been made, its core still follows the CDW-organizing data by time and brings about 3 problems: difficult to integrate the geological data, for the data feature more space than time; hard to store the massive data in fifferent levels due to the same reason; hardly support the spatial analysis if the data are organized by time as CDW does. So the GDW should be redesigned by organizing data by scale in order to store mass data in different levels and synthesize the data in different granularities, and choosing space control points to replace the former time control points so as to integrate different types of data by the method of storing one type data as one layer and then to superpose the layers. In addition, data cube, a wide used technology in CDW, will be no use in GDW, for the causality among the geological data is not so obvious as commercial data, as the data are the mixed result of many complex rules, and their analysis needs the special geological methods and software; on the other hand, data cube for mass and complex geo-data will devour too much store space to be practical. On this point, the main purpose of GDW may be fit for data integration unlike CDW for data analysis.     

三江源生态环境监测研究

青海省生态环境监测系统主要由遍布全省各典型生态系统区的生态环境监测站网、卫星遥感信息接收处理系统，信息收集、处理、模拟、评价系统，综合信息服务与反馈等部分组成。建立环境监测系统的目的是对青海省的生态环境进行系统监测和评估，及时为各级政府、有关部门和公众提供准确、全面的生态环境监测信息，为生态环境保护和建设提供科学依据。青海省生态环境监测系统于2003年5月1日开始业务运行，目前尚处于起步阶段。     

干旱对运城冬小麦的影响

0引言运城市地处φN34°35'至φN35°49'之间,属暖温带大陆性季风气候。基本气候特征是冬季气候干燥雨雪少,春季干旱风沙多,夏季炎热阵雨多,秋季凉爽有连阴。年降水量从东南往西北递减,山地多于丘陵,丘陵多于盆地。主要农作物以冬小麦为主,冬小麦的播种面积占耕地面积的60%以上,居所有农作物之首。影响本地冬小麦产量的主要气象灾害则是干旱。1降水量的时空分布运城市历年平均降水量为472mm至596.7mm,降水的时空分布为东南地区多于西北地区,山地、丘陵地带多于河滩地,其中垣曲、永济、平陆相对多为550mm以上;绛县、盐湖、芮城、闻喜、万荣…     

CT诊断新生儿缺氧缺血性脑病的临床价值

目的 探讨CT诊断新生儿缺氧缺血性脑病（HIE）与临床症状的关系。方法 CT轴位扫描46例新生儿，观察脑实质密度及脑脊液腔系统的变化。结果 HIE以脑白质密度减低为主力（100%），可伴有蛛网膜下腔出血，CT诊断正确率97.6%。结论 CT诊断HIE较有优势，但应密切结合临床。早期正确诊断该病，对新生儿预后较为有利。     

正电子断层扫描仪与PET图像重建概述

概述了PET（Positron emission tomography，正电子断层扫描仪）及其图像重建的基本原理、方法与临床使用，介绍了常用的图像重建FBP（滤波反投影，Filtered Back-Projection)算法和OSEM（有序子集最大似然法，Ordered Subset Expectation Maximization)算法，描述了如何通过PET的临床协议中的参数选择以得到满意的重建效果。此外，对PET的准三维重建也做了一些简介。