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61.
62.
陈明娥 《测绘与空间地理信息》2017,(8)
结合龙岗区网格化管理的实际,通过对龙岗区网格数据管理需求的分析,探索龙岗区信息采集终端指挥与管理平台的架构。该移动业务系统的主要功能是:为龙岗区基层网格信息员和网格志愿者、社会公众等提供信息服务,建设龙岗区工作动态实时监控、高效管理的信息指挥平台,以及完成该系统与市区其他业务系统的数据对接。基于此,本文分别从技术、系统架构和系统功能等方面对龙岗区信息采集终端管理与指挥平台系统进行设计和研究。 相似文献
63.
JOHN A. FISHER CARMEN B. E. KRAPF SIMON C. LANG GARY J. NICHOLS TOBIAS H. D. PAYENBERG 《Sedimentology》2008,55(6):1915-1930
Douglas Creek terminal splay, sited on the western shoreline of Lake Eyre North, central Australia, covers a surface area of approximately 4 km2 with a down‐system length of 2·5 km from the distributary channels terminus to the splay fringe. Two distributary channels feed two sediment lobes which have amalgamated to form the terminal splay. Three primary facies associations have been identified sub‐dividing the creek terminus into distributary channel, proximal and distal splay sections. Proximal splay sediments are characterized by erosionally based, relatively thick (> 100 mm), stacked sheets of coarse to medium sand which commonly display trough and planar cross‐bedding, whereas the distal splay is characterized by thin (generally < 50 mm) massive beds of very fine sand, silt and clay. The change in splay sedimentology is interpreted as reflecting the transition from bedload‐dominated deposition to suspended load‐dominated deposition from decelerating sheetfloods as they spread out from the channel onto the dry lake bed. A proximal to distal splay transition zone is also noted where deposits of both facies associations interfinger laterally and vertically. In scale, geometry and facies associations, the Douglas Creek terminal splay is very different to the often cited Neales terminal splay complex located 70 km to the north. It is suggested that these architectural differences reflect variations in discharge volume, input sediment distribution and the degree of vegetation cover. Understanding the variation in terminal splay architecture has very significant implications for the modelling of analogous subsurface petroleum systems, which at present relies on few modern‐day analogues. 相似文献
64.
为了打造帆船之都,促进青岛旅游业和旅游经济的发展,提出了利用休渔期,选择安全性能好的渔船和经过专门培训的渔民搞海上旅游观光、垂钓并发展渔村餐饮业,以解决渔民增收和生活问题,使旅游码头和渔港码头优势互补,共同发展,为青岛旅游业开辟另一条新路。 相似文献
66.
关于端基分析法测定壳低聚糖的相对数均分子质量问题的探讨 总被引:3,自引:0,他引:3
为使端基分析法更具合理性。文中以铁氰化钾为显色剂。以盐酸氨基葡萄糖和N-乙酰基-D-葡萄糖胺为还原糖的标准品,建立了端基分析法测定低聚糖相对数均分子质量的标准曲线。实验结果证明:通过不同浓度的标准溶液绘制的标准曲线,测得壳低聚糖的相对数均分子质量差别比较大。以凝胶色谱法测定的相对数均分子质量为对照,经分析得:以盐酸氨基葡萄糖为标准品建立的标准曲线方程和以N-乙酰基-D-葡萄糖胺为标准品建立的标准曲线方程更为合理。 相似文献
67.
Smart Client既可以运用网络和Web Services存取各种外部系统的资源,又能使用本地计算机的所有资源,充分发挥客户端的运算能力,是一种全新软件模式。Office 2003 System中提供了一个Smart Document的功能。使用以文档为基础的方式扩充智能感知的XML标记功能,和用户交互更容易。微软还提出了一套Information Bridge Framework(IBF),来协助开发人员建立方案来连接Microsoft Office应用程序与Web服务。应用Microsoft的Smart Client,结合Office 2003 System以及.NET技术,构建一种部署成本低、维护容易、构架轻小、健壮的应用系统。 相似文献
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69.
在分析移动环境下进行数据同步操作的基本需求的基础上,就目前受到广泛支持的数据对象同步协议——SyncML进行了语义模型的改进和完善,并在此基础上提出了一套SyncML客户端的设计与实现方案. 相似文献
70.
Stable carbon and oxygen isotope analyses of ungulate grazers from four archaeological sites located in different environs within the Caledon River Valley have provided a relatively well‐dated proxy palaeoenvironmental and palaeoclimatic sequence for the period between 16 000 and 6000 calendar (cal.) yr BP. Within the overall trend towards hot mid‐Holocene temperatures and a summer rainfall pattern, stable carbon isotope results show that there were three periods when growth season temperatures were cool enough for C3 grasses to be present: 16 000–14 000; 10 200–9600, and 8400–8000 cal. yr BP. Similar trends were recorded in stable oxygen isotope values, reflecting shifts in either temperature or available moisture. Although having a similar pattern to that of the lower altitude site, sites situated in foothills and montane portions of the valley consistently maintained lower temperatures until the mid‐Holocene altithermal. At this time growth season temperatures warmed sufficiently for a 100% C4 grassland to expand in altitude from the warmer low lying localities. In relation to present understanding of synoptic and global climatic patterning, these findings suggest that the early to middle Holocene transition was not a gradual warming trend, but rather it was marked by a series of climatic fluctuations. Of particular note is the possible global, rather than regional, occurrence of the 8200 cal. yr BP ‘event’. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献