煤矿瓦斯抽放井一次成井工艺及技术效果

煤矿瓦斯抽放井要求垂直精度高、井径大,通常采用常规钻探工艺时,需进行3-4次扩孔才能达到最终孔径,施工时间较长,钻进效率较低。此次在端氏煤矿施工的大口径瓦斯抽放井,采用了的一次成井钻进技术及工艺方法,钻进口径达到φ660mm,选用了江汉735型和715型系列镶齿牙轮钻头,采用塔式加重钻具控制并保证了钻井的重直度,采用密度较大的化学泥浆和保持大泵量排渣,避免了井底牙轮钻头的重复破碎,确保了钻进效果。与传统的扩孔工艺相比,缩短了施工周期,成井质量高,提高了钻进效率,降低了钻进成本。     

省级应急管理地理信息平台及实现技术研究——以重庆市为例

加强应急管理、有效应对突发事件是国家的一项重要工作,以地理空间信息技术为核心的应急管理地理信息平台建设,已成为目前国内省级应急平台建设的主要模式。本研究建立了应急联动一张图和地理信息应急服务总线,对省级应急资源多源、异构、动态、多时相信息整合技术难题进行探索,实现了地理信息服务与全市各级应急系统的业务融合。目前,研究成果已融入重庆市应急信息资源共享体系,在多个部门的应急业务系统中得到有效的集成应用,为形成全市应急资源全方面共享格局发挥了重要作用。     

基于开源平台构建WebGIS应用系统

本文介绍了开源GIS平台Geoserver及开源客户端OpenLayers,在此基础之上架构了一个三层B/S结构的WebGlS的应用系统,分析了各层的基本功能;对WebGIS系统的GIS服务器配置、空间数据库创建、客户端实现过程中涉及的部分关键技术及解决方法进行了详细的阐述.实验结果表明,基于开源GIS平台可以开发低成...     

数据中心应用集成开发平台标准体系

为了满足空间信息系统快速构建及智能化服务的需要,针对空间信息系统快速构建及智能化服务的特点,全面分析了现有的地理信息标准和信息技术标准,确定数据中心应用集成开发平台标准体系的来源与定位及其设计原则,提出了标准间关系合理、层次结构分明的服务于空间信息系统的快速构建及智能化服务的数据中心应用集成开发平台标准体系。     

数字苏州公共服务平台的构建

结合苏州市地理信息系统平台建设实际情况,分别从建设目标、技术设计,系统开发、共享模式和应用推广等方面总结了数字苏州市公共服务平台建设的思路与经验,同时也提出了当前推广地理信息系统应用集成开发的创新思想.     

福建省地理信息公共服务平台数据应用服务模式探讨

介绍了福建省地理信息公共服务平台数据构成和应用服务,探讨了针对不同用户类型、不同网络环境下的平台数据共享应用服务模式,实现横纵向部门间数据服务的互联互通,为政府、企业和社会公众提供地理信息基础支撑。     

地理信息服务的思考与探究

从地理信息服务的内涵、发展和社会需求等几个方面对地理信息服务进行综合分析,从而提出了加强地理信息服务的几点建议.     

省级地理信息公共服务平台数据体系初步设计

数据体系是地理信息公共服务平台建设的一个重要内容。主要对公共服务平台需求、数据构成及建设等内容进行了描述,为省级地理信息公共服务平台的建设提供参考。     

Block removal and step backwearing as erosion processes on rock shore platforms: a preliminary case study of the chalk shore platforms of south‐east England

Shore platforms frequently exhibit steps or risers facing seaward, landwards or obliquely across‐shore. A combination of soft copy photogrammetry, ortho‐rectification, geo referencing and field measurement of step height are linked in a GIS environment to measure step retreat on chalk shore platforms at sample sites in the south of England over two periods, 1973–2001, 2001–2007. The methods used allow for the identification, delineation and measurement of historic change at high spatial resolution. The results suggest that while erosion of chalk shore platforms by step backwearing is highly variable, it appears to be of similar magnitude to surface downwearing of the same platforms measured by micro‐erosion meters (MEMs) and laser scanning, in a range equivalent to 0·0006 – 0·0050 m y^?1 of surface downwearing. This equates to annual chalk volume loss from the platforms, by the two erosion processes combined, of between 0·0012 m³ m^?2 and 0·0100 m³ m^?2. Results from the more recent years' data suggests that step retreat has variability in both space and time which does not relate solely to climatic variability. The results must be viewed with caution until much larger numbers of measurements have been made of both downwearing and step erosion at higher spatial and temporal resolution. Copyright © 2010 John Wiley & Sons, Ltd.     

Integrated biostratigraphy and carbon isotope stratigraphy of the Lower Cretaceous (Barremian to Albian) Adriatic-Dinaridic carbonate platform deposits in Istria, Croatia

The Adriatic-Dinaridic carbonate platform (ADCP) was one of the largest and relatively well preserved Mesozoic platforms in the Mediterranean region (central Tethys). The peninsula Istria, in the northwestern part of the ADCP, is built up predominantly of shallow-water carbonates of the Middle Jurassic (Dogger) to Eocene age and, to a lesser extent, of Paleogene clastic deposits (flysch and calcareous breccia). This study focuses on a Lower Cretaceous (Barremian to Albian) succession of strata at five localities in western Istria. Stratigraphic determinations are based on identification of nine microfossil assemblages (benthic foraminifera and calcareous algae Dasycladales) and on using their taxa as index fossils. The age of strata with these microfossil assemblages, however, is questionable. Most of the age uncertainties are associated with a regional emersion, which occurred on the ADCP during the Aptian or close to the Aptian-Albian transition. It is unclear what portions of the Upper Aptian and/or Lower Albian are missing along this unconformity. A stable isotope study was conducted on homogenous micritic matrix samples in an attempt to resolve some of these uncertainties. Variations in carbon isotope compositions proved useful for stratigraphic correlation between the examined successions of strata, for improving their age determination, and for relating them to other coeval successions that span an important time interval of major oceanographic changes and carbon-cycle perturbations associated with the Early Aptian oceanic anoxic event (OAE 1a).