海南国际旅游岛数字地理空间框架建设与应用

数字城市和数字省区相互之间既有明确的层次关系,同时共性中又有着个性。本文首先简单介绍海南国际旅游岛数字地理空间框架建设的总体架构,重点阐述框架建设项目的主要建设情况以及推广应用情况。     

杭州市城市地下管线共享平台建设与实践

总结了杭州市城市地下管线共享平台建设取得的进展和创新点,并尝试探索未来杭州城市地下管线信息化发展需要解决的关键问题,强调城市地下管线信息共享与服务将是未来杭州市城市地下管线信息化工作的两大主题。     

省级水利地理信息服务平台架构研究

面向专业应用的地理信息公共服务平台建设,是近年来地理信息服务的重点内容之一。本文以江苏省水利地理信息服务平台建设为例,系统探讨了专业型地理信息服务平台建设的主要设计思路、架构选型和服务接口设计等关键内容。研究期望为各类专业型地理信息公共服务平台建设提供借鉴。     

数字城市地理空间框架成果在智慧城市建设中的应用研究——以黑龙江省数字城市建设为例

从测绘地理信息视角出发,通过对数字城市地理空间框架建设成果的总结与分析,结合智慧城市建设的相关内容,以时空信息云平台为载体,对数字城市地理空间框架建设成果在智慧城市中的应用进行了研究.     

基于微信公众平台的智慧旅游系统的开发与实现

主要介绍了五大连池风景区微信公众账号的建设模式,微信公众账号作为景区的宣传推广工具,为游客提供智能化的自助导览服务,解决游客旅行前、中、后所需,实现智慧旅游移动端应用,集旅游推广营销与游客旅行服务构建一体化移动端产品。微信公众账号还将以二维码的形式,在"天地图·五大连池"门户网站、景区入口以及各大商场、酒店醒目位置展示,作为打通线上线下的必要环节,以提升游客访问量,形成智慧旅游O2O闭环。     

渭北台塬县级城市空间扩张的分形研究

基于RS与GIS技术,采用分形理论对渭北台塬县级城市空间扩张特征进行分析。结果表明:1990—2010年台塬区县级城市加速扩张,总面积扩大了2.86倍,年均增长率达8.7%。1990,2000,2010年县级城市空间形态分维值均值分别为1.08,1.09,1.21,变异系数分别为3.06,3.09,3.93,城市空间形态总体简单但渐趋复杂且不断分化。异速生长模型标度因子b值均小于1,人均城市空间较为合理但远未达到最优状态。1990—2000年城市以填充型扩张为主,2000—2010年以外延型扩张为主,用地集约性呈下降趋势。空间上,铜川塬、宝鸡塬扩张较快,人地关系较差;咸阳塬扩张最快,人地关系一般;渭南塬扩张相对较慢,人地关系较优。总体上,亟待加强城市规划以构建节约型城市空间增长模式。     

川北早寒武世碳酸盐岩台缘斜坡沉积特征及变形构造形成机制探讨

基于对川北米仓山西部旺苍县鼓城乡唐家河下寒武统仙女洞组露头剖面的观察与镜下分析发现,仙女洞组下段由生物碎屑泥晶灰岩(L)、粉砂质泥岩(M)、似瘤状砾屑灰岩(L')、角砾灰岩(R)、藻凝块灰岩(A)和含生屑钙质砂岩(S)组合而成,其以角砾灰岩、似瘤状砾屑灰岩和藻凝块灰岩为特征,且发育异地岩块和滑塌变形构造。进一步分析认为:L-M岩石组合为正常的斜坡环境低能沉积;L'-R岩石组合中的角砾灰岩为上斜坡生物灰泥丘崩坍滑动至下部而形成的,似瘤状砾屑灰岩可能是由于L-M岩石组合快速沉积导致沉积物失稳滑动变形、上斜坡生物灰泥丘崩落角砾致使的差异压实和滑动、以及后期物质成分差异引起的压溶作用等共同作用的结果,从而使灰质层发生破碎并被泥质包围形成断续的砾屑状,甚至轻微的位移,进而形成条带特征不明显的杂乱变形构造;微生物岩(Mb)组合为上斜坡的灰泥丘沉积;S-M岩石组合为斜坡上部的浊流沉积。根据上述分析结果建立米仓山西部仙女洞组碳酸盐岩台缘斜坡沉积模式,表明仙女洞组沉积早期米仓山西部存在台缘斜坡相沉积。     

ON THE FORMATION AND MAINTENANCE MECHANISMS OF THE COLD WATER MASS OF THE YELLOW SEA

An analytical study is made on the formation of the Cold Water Mass of the Yellow Sea (CWYS) and the relevant thermally driven circulation. The temperature and velocity field, obtained by solving the coupled equations of motion and heat conduction, show that, in summer, the CWYS has a horizontal cyclonic circulation (component) with vertical upwelling in the middle and downwelling at the edges, that the vertical convection (u-w components) occurs only within a thin layer near the thermocline. and that the deeper layer remains almost motionless. This current structure represents well the mechanisms responsible for the maintenance of the thermocline or CWYS during the wanner months. Comparisons between the theoretical and observed temperatures show very good qualitative and quantitative agreements for corresponding seasons.     

Characterization, lateral variability and lateral extent of discontinuity surfaces on a Carbonate Platform (Barremian to Lower Aptian, Oman)

Hiati of various duration in carbonates are commonly expressed as discontinuity surfaces. The understanding of processes that form and affect these surfaces leads to an improved sequence-stratigraphic interpretation, a reliable outcrop correlation, and better models for reservoir compartmentalization. Various intraformational discontinuities were analysed and interpreted in a well-exposed study window, 2·5 km in lateral length and 60 m in height comprising the Barremian-Aptian Qishn Formation (Haushi-Huqf area, central Oman). This study focuses on the lateral extent and morphology of the surfaces, the petrography of the underlying rocks, and the facies changes and geochemical trends across these discontinuities. Furthermore, the lateral variability of discontinuity surfaces was documented. Three genetic types of discontinuities are differentiated: (i) erosion surfaces; (ii) omission surfaces (hard- and firmgrounds); and (iii) composite surfaces with evidence for both subaerial exposure and submarine boring. Field observations, combined with petrographic and geochemical data, suggest that 17 surfaces are laterally extensive for at least 20 km and record relative sea-level fluctuations of regional scale. In contrast, a large number of laterally limited surfaces (<1 km) are related to locally active processes such as waves and current erosion. The lateral variability along extensive surfaces is the result of the depositional environment below the discontinuity, the sea-floor topography, waves and currents and differential erosion. The most pronounced lateral variability is present along six laterally extensive composite surfaces that record terrestrial exposure and subsequent flooding of a tidal flat environment. This variability is caused by spatial variability in the tidal flat environment, meteoric alteration and differential erosion. This study emphasizes the spatial and temporal complexity of processes that form and modify discontinuity surfaces. This variability must be kept in mind when interpretations and correlations are based on one-dimensional sections or cores.     

数字城市地理空间信息公共平台的设计

数字城市建设的目的是实现城市各种信息的数字化共享,地理空间信息是数字城市建设的基础信息,如何实现数字城市地理空间信息的共享是数字城市建设过程中的基本问题.在以往的数字城市建设中,地理信息往往作为城市某些职能部门的"私有"信息,其共享性得不到保证,严重影响了数字城市建设.地理空间信息公共平台的设计目的是实现地理信息共享.阐述的公共平台的系统设计主要分为公共基础空间数据库的建立、地理空间信息共享环境的设计以及地理空间信息公共技术平台设计3个方面的内容.