基于SOA的地球系统科学数据共享平台架构设计与实现

为了能够有效整合集成分散、异构的地球系统科学数据资源,为用户提供“一站式”的数据共享服务,需要一种分布式的数据共享平台.本文首先分析了分布式地球系统科学数据共享平台对互操作的需求,然后设计了基于SOA(Service-Oriented Architecture)的分布式地球系统科学数据共享平台的总体架构.该平台由物理上分布、逻辑上统一的总中心、认证中心和分中心共同构成,采用Web Services技术将数据共享核心业务封装成一系列的Web服务:数据中心信息同步服务、元数据推送与管理服务、多源异构数据访问服务等.通过Web服务这种松散的耦合机制,不仅能够很好地实现数据中心之间的互操作,而且具有良好的开放可扩展性,可快速纳入新的异构系统作为分布式数据共享平台的节点,其数据共享核心服务,也可以方便地集成到其他应用系统中,为它们提供数据共享的功能.最后介绍了Web服务实现与部署的方法.分布式的地球系统科学数据共享平台已经应用到国家科技基础条件平台建设项目:地球系统科学数据共享网中.截止到2007年底,通过共享平台成功整合了10.23TB的分散数据资源,为3万多用户提供17TB的数据服务.     

多源异构数据整合应用研究

针对多源数据库之间的异构差异及互操作应用,分析和研究了异构数据集成体系结构、模式映射、模式冲突及解决办法、查询处理、数据集成及数据管理等相关问题,提出了中间件体系结构的异构多源数据库整合系统解决方法,模式映射方案采用GAV,系统采用JAVA语言设计,使用JBoss4.2设计,算法采用类JAVA语法描述,模式以及模式集成信息采用XML描述.以实际用例测试,成功解决了模式冲突的消解、全局查询的分解和数据集成处理等问题,系统运行效果良好,具有实际应用价值.     

移动GIS的体系结构与关键技术

阐述了移动GIS的概念,提出了一个由表示层、逻辑层和数据层所构成的分布式体系结构,介绍了移动接入技术、移动访问技术、移动定位技术、嵌入式技术和语音技术等关键技术。     

地震行业骨干网“一网双平面”架构

通过对地震行业现有骨干网络架构的优缺点进行分析,阐述"一网双平面"骨干网架构在地震行业骨干网的通信质量、可靠性、资源有效利用等优势,从建设成本、组网策略、业务分流、网络与信息安全等方面提供建议,为地震行业骨干网进一步优化、实现承载业务系统的安全高效运行提供参考。     

基于B/S架构的区域前兆数据库信息服务与运行管理平台的设计与实现

区域前兆台网的大量数据存于数据库中。为便捷地查询测项信息、台站工作日志和观测日志、台站基础信息,并减少区域台网中心工作人员工作量,提高工作效率,我们建立了基于B/S架构的前兆数据信息服务与管理平台。该平台很好地解决了上述问题,并在江苏省地震监测中心、预报研究中心、各省属地震台和市县地震部门广泛使用。     

Stratigraphic record in the transition from basin floor to continental slope sedimentation in the ancient passive-margin Windermere turbidite system

Well-exposed, vertically dipping, glacially polished outcrops of the Neoproterozoic Windermere Supergroup in the southern Canadian Cordillera include basin-floor deposits of the Upper Kaza Group overlain by slope channel complexes of the Isaac Formation. Within the 2·5 km thick Kaza and Isaac succession is an up to 360 m thick interval composed of diverse deep-water stratal elements including scour and interscour deposits, distributary channels, fine-grained turbidites, terminal splays, mass-transport deposits, erosional and levéed channels and avulsion splays, which collectively were formed during the development of an ancient passive-margin channel-lobe system. The proportion and vertical and lateral arrangement of stratal elements reveal three distinct complexes. The lower complex, consisting mostly of distributary channels and small and large scours, is interpreted to represent the detachment of lobes from an upflow levéed channel, wherein a well-developed channel-lobe transition zone was formed by efficient, siliciclastic flows during a period of sustained transport bypass and limited deposition coincident with the onset of falling relative sea level. The middle, comparatively thicker and more sandstone-rich complex, comprises distributary channel fills, fine-grained turbidites and lesser terminal splays that are interspersed with small scours, capped by a slope levéed channel filled with coarser-grained siliciclastic sediment. The abundance of basin-floor elements suggests negligible separation between the levéed channel and lobe, and therefore a poorly-developed channel-lobe transition zone, resulting from inefficient, siliciclastic-rich depositional flows that became dominant during lowstand and/or ensuing transgression. The stratal makeup of the upper complex resembles the lower detached complex, suggesting a return to efficient flows, and an abrupt change to mixed carbonate–siliciclastic sediments associated with highstand conditions. Accordingly, the stratigraphic architecture and stacking pattern of the Kaza–Isaac interval, which relate to the formation of multiple channel-lobe transition zones, were controlled by temporal changes in sediment supply and flow characteristics during the long-term progradation of the Laurentian continental margin.     

Architecture of a distal pre-vegetation braidplain: Cambrian middle member of the Wood Canyon Formation,southern Marble Mountains,California, USA

Architectural element analysis and detailed mapping of a 300 m along-strike exposure of the middle member Wood Canyon Formation, southern Marble Mountains, California, USA, provides new evidence for extensive braided–fluvial channel-belt deposits with adjacent overbank environments. Three-dimensional models constructed using ‘Structure from Motion’ techniques, combined with field-based observations, allowed interpretation of outcrop-scale trends, barforms, channel fills and fine-scale features. The ca 80 m thick member is divisible into five distinct units, including units M1 to M3 that form the bulk of the stratigraphy. Units are defined by stacking patterns of three facies associations (Facies Association 1 to Facies Association 3), each representing the product of a subenvironment within the fluvial system. In Facies Association 1, stacked cosets, interpreted as low-relief fluvial bars and channel fills, preserve vertical-accretion and downstream-accretion elements under unimodal north-north-west palaeoflow, with minor lateral accretion near bar edges. Deposits of Facies Association 2 to Facies Association 3, linked to overbank environments, are found only in unit M2, in the middle 27 m of the middle member. Floodplains, represented by Facies Association 2, include crumbly red-orange intervals of fine to medium-grained sandstone and thinner sets of cross-bedding than Facies Association 1, interbedded with thicker cross-stratification indicative of overbank splay or overland flow aggradation from adjacent channel belts during flood stage. Possible aeolian beds of Facies Association 3 preserve broad festooned trough cross-strata that average 23 cm in thickness; their small size, medium-grained sandstone and iron oxide cement suggest a high water table. The diverse assemblage of interpreted subenvironments, paired with bedform and facies patterns, implies a perennial fluvial system that gradually built large sand bars as the channel belt migrated and avulsed across an unconfined braided–fluvial reach, leaving the overbank area on its flanks subject to weathering and aeolian transport. Despite the occurrence of strata deposited in low-energy and ponded settings, and a marine influence proposed for nearby sections of middle member, no ichnofossils were encountered.     

The sedimentology of an ephemeral fluvial–aeolian succession

Ephemeral fluvial systems are commonly associated with arid to semi-arid climates. Although their complex sedimentology and depositional settings have been described in much detail, depositional models depicting detailed lateral and vertical relationships, and interactions with coeval depositional environments, are lacking compared to well-recognized meandering and braided fluvial systems. This study critically evaluates the applicability of current models for ephemeral fluvial systems to an ancient arid fluvial example of the Lower Jurassic Kayenta Formation of the Colorado Plateau, USA. The study employs detailed sedimentary logging, palaeocurrent analysis and photogrammetric panels across the regional extent of the Kayenta. A generic model that accounts for the detailed sedimentology of a sandy arid ephemeral fluvial system (drawing upon both ancient and geomorphological studies) is developed, along with analysis of the spatial and temporal interactions with the aeolian setting. Results show that the ephemeral system is dominated by laterally and vertically amalgamated, poorly channelized to sheet-like elements, with abundant upper flow regime flat beds and high sediment load structures formed between periods of lower flow regime conditions. Through interaction with a coeval aeolian system, most of the fluvial deposits are dominated by sand-grade sediment, unlike many modern ephemeral fluvial systems that contain a high proportion of conglomeratic and/or finer grained mudstone and siltstone deposits. During dominantly fluvial deposition, high width to thickness ratios are observed for channelized and sheet-like elements. However, with increasing aridity, the aeolian environment becomes dominant and fluvial deposition is restricted to interdune corridors, resulting in lower width to thickness ratio channels dominated by flash-flood and debris-flow facies. The data presented here, coupled with modern examples of ephemeral systems and flood regimes, suggest that ephemeral flow produces and preserves distinctive sedimentological traits that can not only be recognized in outcrops, but also within core.     

高光谱矿物填图技术与应用研究

回顾和总结了"九五"以来,中国国土资源航空物探遥感中心在高光谱矿物识别和矿物填图领域所取得的成果,包括主要岩矿光谱特征与影响因素分析;矿物的种类识别、丰度反演和成分识别;中—热红外多/高光谱的数据处理和矿物识别;高光谱矿物识别的地质应用模式、矿物填图的工作方法和技术流程、矿物填图的技术体系;矿物填图在区域地质找矿、矿区勘查和成矿与找矿模型、植物地球化学探测、矿山环境监测以及月球和行星探测等方面的应用示范。最后,提出了高光谱矿物填图近期的研究方向。     

网络环境下的虚拟古典建筑场景建模

在研究我国古典风格建筑特点和对比分析现有建模软件的优缺点的基础上,选择3DStudioMax建立场景模型,并通过VRML编程进行场景驱动,嵌入网页发布。