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41.
 绝大部分的亚硝酸盐和氰化物属于钙钛矿型结构,但有部分化合物为“反”钙钛矿型结构,充填空洞A位的阳离子的拓扑体积为0。阴离子团NO2-和CN-的拓扑体积都近乎常数,分别为41.73Å3和40.03Å3,标准方差σn-1=1.516和σn-1=1.25。由此,进一步证明了原来的一套离子拓扑体积数值的普适性。“反”钙钛矿型结构中A位阳离子的平均半径rA>1.00Å时,三价阳离子会产生扩容效应,其扩容系数大约是其本身拓扑体积的2倍;正钙钛矿型结构中,当A位是由半径较大的Cs+充填时,Cs+也会产生扩容效应,其扩容系数约为24Å3。氰化物中结晶水分子的拓扑体积近乎常数,为24Å3或0。  相似文献   
42.
空间信息网格是网格技术在地理信息服务领域中的具体应用。从网格技术的发展趋势和地理信息服务的需求来看,构建空间信息网格势在必行。本文分析了空间信息网格技术的特点和网格服务体系结构,对当前发展空间信息网格技术的重要任务进行了简要阐述。  相似文献   
43.
This paper presents a study on the modeling of fuzzy topological relations between uncertain objects in Geographic Information Systems (GIS). Based on the recently developed concept of computational fuzzy topological space, topological relations between simple fuzzy spatial objects are modeled. The fuzzy spatial objects here cover simple fuzzy region, simple fuzzy line segment and fuzzy point. To compute the topological relations between the simple spatial objects, intersection concepts and integration methods are applied and a computational 9-intersection model are proposed and developed. There are different types of intersection, and we have proposed different integration methods for computation in different cases. For example, surface integration method is applied to the case of the fuzzy region-to-fuzzy region relation, while the line integration method is used in the case of fuzzy line segment-to-fuzzy line segment relation. Moreover, this study has discovered that there are (a) sixteen topological relations between simple fuzzy region to line segment; (b) forty-six topological relations between simple fuzzy line segments; (c) three topological relations between simple fuzzy region to fuzzy point; and (d) three topological relations between simple fuzzy line segment to fuzzy point.  相似文献   
44.
薄伟伟 《北京测绘》2006,(1):25-27,39
介绍了Agent技术应用于分布式GIS中的优势,提出了基于目标的Multi-Agent系统体系结构的建立过程,最后通过实验验证了该体系结构的可行性。  相似文献   
45.
46.
邹伟  王燕妮  杨萌 《江苏地质》2013,37(4):606-610
在分析现有三维矢量拓扑关系的基础上,提出了三维矢量数据结构的要素拓扑模型(Feature Topological Mod—el,FTM)。FTM三维拓扑模型比传统三维模型的优势有3点:(1)直接引入三角形对象,更加有利于表示任意形状的三维体数据。(2)简化基本拓扑关系的定义,使用相对简单的三角形和边的拓扑关系,表达相对复杂的实体和曲线的拓扑关系;使用带拓扑关系的边的集合表示三维曲线,既表达了曲线对象,又不影响基本拓扑关系的维护。(3)使用实体之间的包含模型,解决环(洞)的拓扑关系。同时,使用FTM对三维离散三角形数据进行拓扑化处理,对其中存在的拓扑错误提出具体的解决方案。该拓扑模型成功应用于自主研发的三维勘查软件“探矿者”中。  相似文献   
47.
无线传感器通常用于环境监测,如气候变化、水质和监控灾害管理等。目前,灾害管理是一项十分关键和紧迫的工作,在海啸预警和预测系统方面尤为突出。本文在研制区域水文态势地理信息服务系统(RHSGISS)的基础上,为减缓灾害,研究出了海啸早期预警系统的一种本体式表达。该系统由地震监测台站、海底压力记录仪(BPR)和验潮仪等组成,其主要功用是解释复杂的多维数据。该数据由各种传感器、系统间的互操作性以及处理异构数据等生成。目前的核心问题在于将获取自海啸早期预警系统多个组件的异构数据进行融合以及提供基于Web网络的数据服务。面向特定陆表监测与应急响应任务,本文通过使用开放地理空间联盟(OGC)确定的传感器网络赋能实现(SWE)框架,构建了基于"北斗"卫星导航系统的GPNT服务体系,能为所有接入空天地一体化对地感测网环境下的用户共享互操作性和可伸缩性提供便利。本体因其功能上可以提供明确含义的信息,而成为了解决信息异质性问题的手段。本文在传感器网络数据与数据语义方面提出了一种面向服务的架构(SOA)模型,目的是要提供使用本体和Jena规范来表示更有意义的早期海啸预警系统信息。  相似文献   
48.
《The Cartographic journal》2013,50(3):225-231
Abstract

This paper is about different worlds, and how we try to unite them. One of these worlds is the world of National Atlases: collections of complex, high-quality maps presenting a nation to the geographically interested. The second is the world of National Spatial Infrastructures: highly organized, standardized and institutionalized large collections of spatial data and services. In the paper, we describe the two worlds and their fundamental differences and we present the theoretical framework in which these worlds could be united. We introduce a test bed we are using to try out the theoretical framework in a real-life use case. In the architecture of that test bed, we introduce a National Atlas Services layer and describe how we have created an Atlas Map Viewer component, using the Open Web Platform. We conclude by commenting on the results thus far and taking a look into future developments.  相似文献   
49.
Security has recently become a major concern in distributed geo-infrastructures for spatial data provision. Thus, a lightweight approach for securing distributed low-power environments such as geo-sensor networks is needed. The first part of this article presents a survey of current security mechanisms for authentication and authorisation. Based on this survey, a lightweight and scalable token-based security infrastructure was developed, which is tailored for use in distributed geo-web service infrastructures. The developed security framework comprises dedicated components for authentication, rule-based authorisation and optimised storage and administration of access rules. For validation purposes, a prototypical implementation of the approach has been created.  相似文献   
50.
Seafloor images of coarse‐grained submarine channel–levée systems commonly reveal complex braid‐plain patterns of low‐amplitude bedforms and zones of apparent bypass; however, mechanisms of channel evolution and the resultant channel‐fill architecture are poorly understood. At Playa Esqueleto the lateral relationships between various elements of a deep‐marine slope channel system are well‐exposed. Specifically, the transition from gravel‐dominated axial thalwegs to laterally persistent marginal sandstones and isolated gravel‐filled scours is revealed. Marginal sandstones pass into a monotonous thin‐bedded succession which built to form relatively low‐relief levées bounding the channel belt; in turn, the levées onlap the canyon walls. Three orders of confinement were important during the evolution of the channel system: (i) first‐order confinement was provided by the erosional canyon which confined the entire system; (ii) confined levées built of turbidite sandstones and mudstones formed the second‐order confinement, and it is demonstrated that these built from overspill at thalweg margins; and (iii) third‐order confinement describes the erosional confinement of coarse‐grained thalwegs and scours. Finer‐grained sediment was transported in suspension and largely was unaffected by topography at the scale of individual thalwegs. Facies and clast analyses of conglomerate overlying channel‐marginal scours reveal that they were deposited by composite gravity flows, which were non‐cohesive, grain‐dominant debris flows with more fluidal cores. These flows were capable of basal erosion but were strongly depositional; frictional freezing at flow margins built gravel levées, while the core maintained a more fluidal transport regime. The resultant architecture consists of matrix‐rich, poorly sorted levées bounding better‐sorted, traction‐dominated cores. The planform geometry is interpreted to have consisted of a low‐sinuosity gravel braid‐plain built by accretion around mid‐channel and bank‐attached bars. This part of the system may be analogous to fluvial systems; however, the finer‐grained sediment load formed thick suspension clouds, probably several orders of magnitude thicker than the relief of braid‐plain topography and therefore controlled by the levées and canyon wall confinement.  相似文献   
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