浅析城市部件的数字化采集方法

为了提高城市管理水平、实现科学和规范化管理,借鉴"数字城市管理系统"模式的成功案例,根据网格化城市管理系统的要求,实施网格化管理信息化建设工程,进行城市部件的数据采集工作,并将所获取的数据成功地转入数据库。本文根据城市部件数字化采集工作的实际经验和做法,从城市部件的类型及编码、城市部件数据采集方法和精度要求以及城市部件成果数据库的建立三个部分进行了分析和阐述,以供测绘工作者参考。     

模糊聚类的DEM确定耕地坡度方法

针对实际应用的坡度计算中没有考虑DEM高程精度影响这一状况,提出采用模糊聚类法进行坡度分级,给出了具体的精度评定方法,并采用我国南方某地区一个镇的第二次土地调查耕地成果数据进行了分析,与传统的直接计算方法进行了比较。结果表明,两种方法得到的图斑坡度级别基本相同;从总体分类精度与Kappa系数计算来看,两者基本接近,模糊聚类法略微优于直接计算法,而且由于其顾及了DEM高程精度的影响,得到的分级结果可靠性更高。     

数字校园系统构建研究——以西安建筑科技大学为例

在综述数字化校园系统构建发展的基础上,以西安建筑科技大学校园为例,基于组件式地理信息系统二次开发库SuperMap Objects 5.0及Visual Basic 6.0程序开发工具,探讨了在组成"数字建大校园"的体系构架、系统功能、数据组织模型等基础上,最终构建了西安建筑科技大学校园地理信息系统。     

城市规划管理统一信息平台

针对目前规划业务的现状,提出建设规划统一信息平台的必要性,整合已有系统资源,解决纵横两个规划方面的问题,并列出建设统一信息平台必需的技术要素。     

一种基于数字水印的视频多点广播立即源认证模型

基于数字水印和TESLA,提出了一种视频多点广播立即源认证模型,利用查找表的视频水印算法,将视频重要分量的消息认证码、公开密钥和立即认证散列值等嵌入到视频的非重要分量中;从而达到视频数据多点广播的立即源认证,避免了接收方数据包缓存,并给出公开延迟时间间隔d的一种计算方法。     

渭南黄土台塬晚新生代环境与城市建设

根据对W7、W8两钻孔中的孢粉、微体古生物化石和矿物成分分析,结合野外考察及古地磁地层年代资料与标准剖面对比,作者提出本区第四纪地层划分的初步意见并阐述了晚新生代环境.根据W7、W8两孔相当层位的深度变化,推断张性正断层的存在,进而讨论了与城市建设有关的地下水资源和黄土塌陷问题.     

没有围墙的GIS实验室

美国前副总统戈尔认为数字地球可以变成一个“没有围墙的实验室”,那么什么是“没有围墙的实验室”,如何建设 ?本文在对当前数字地球研究成果分析的基础上 ,指出“没有围墙的实验室”的核心就是“没有围墙的 GIS实验室”.     

The influence of seasonal and local weather conditions on rock surface changes on the shore platform at Kaikoura Peninsula, South Island, New Zealand

A traversing micro-erosion meter (TMEM) was used to measure micro-scale surface changes in a 45 cm² area of an intertidal mudstone shore platform on Kaikoura Peninsula, New Zealand, with hourly readings taken over 5 days for two seasons, within 4 h either side of low tide. For all monitoring events, the relative height of a total of 120 co-ordinates were obtained, resulting in 4200 and 4800 measurements for the summer and winter seasons respectively. Within seasons, samples were grouped according to the presence of rain or no rain. Significant changes were found in the micro-topography with variations in temperature and among rain and no rain sample groups. For both seasons, in the absence of rain, there were positive linear relationships between rock surface temperatures and rock surface elevations, and regression analysis explained 42.3% and 46.5% of this variation for the summer (y = 0.098 + 0.004x; p-value = 0.007) and winter (y = 0.007 + 0.012x; p-value < 0.001) seasons respectively. It is suggested that incorporating weather readings alongside measurements of surface change could not only improve extrapolations of shore platform erosion from short-term studies, but also differentiate fluctuations in rock surfaces due to changes in rock surface temperatures from other processes involved in shore platform erosion.     

Estuarine shore platforms in Whanganui Inlet, South Island, New Zealand

Whanganui Inlet is a low mesotidal environment where wave energy at the shoreline is limited due to a small fetch, a narrow entrance and tidal flat accretion to intertidal elevations. Wave energy is therefore only an erosive force at high tide and under storm conditions. Despite this low-energy environment extensive shore platforms occur within the inlet. They are sub-horizontal and range in width from 4.1 to 185.2 m with an average of 44.9 m. All the platforms are formed in sandstone of low resistance (mean N-type Schmidt Hammer rebound value of 17 ± 8) and have their seaward edges buried by intertidal sediment flats. The majority of platforms occur at around MHWN level, corresponding to the elevation of those flats. Where wave energy is highest, opposite the inlet's entrance and at those sites with the largest fetch, platforms develop to 0.5–1.0 m below MSL. A higher platform level is also found at MHWS elevations, however it appears to be relict with active erosion of its seaward edge occurring and therefore is most likely related to a higher mid-Holocene sea level. Apart from the location of the lowest platforms little correspondence is found between platform morphology and wave energy. Platform evolution appears to be intrinsically linked to the intertidal sediment flats which determine the degree of surface saturation of the bedrock and, hence, the number of wetting and drying cycles the platforms may undergo. As the seaward edge is buried platform development is primarily through retreat of the landward cliff. This process can, however, be complicated by the migration of intertidal water channels onto the seaward edge of the platforms or relative sea level fall which may rejuvenate landward retreat of the low-tide cliff.     

西藏南羌塘扎仁地区晚侏罗世索瓦早期岩相古地理特征

通过沉积相分析,本文将南羌塘扎仁地区晚侏罗世索瓦早期划为碳酸盐台地和河口砂坝两种沉积环境,对深化研究区该期岩相古地理研究有意义。