C/S模式WebGIS架构技术     

王占昌  刘春娥  包存义  张雪亭 《西北地质》2005,38(1):100-107

针对客户端／服务器(C／S)模式下三层体系构建原理以及地学空间数据库网络发布(WebGIS)特点,以MapGuide空间数据库引擎为核心,分析了嵌入式WebGIS功能接口和事件响应机理。提出了空间数据库与关系型数据库两大引擎之间实现互动链接的有效技术措施,从而弥补了MapGuide Viewer。插件赖以支持的MWF格式在专业属性数据操作方面的先天性不足。以青海地调院局域网建设实例为基础,详细阐述了C／S模式下青海省基础地学数据库网络框架建设的实现途径。该技术的成功运用,无疑拓宽了青海省地学数字化成果的共享应用渠道,提高了成果的再利用价值。  相似文献   

CO<Subscript>2</Subscript> Air–Sea Exchange due to Calcium Carbonate and Organic Matter Storage,and its Implications for the Global Carbon Cycle     

Abraham?LermanEmail author  Fred?T.?Mackenzie 《Aquatic Geochemistry》2005,11(4):345-390

Release of CO₂ from surface ocean water owing to precipitation of CaCO₃ and the imbalance between biological production of organic matter and its respiration, and their net removal from surface water to sedimentary storage was studied by means of a quotient θ = (CO₂ flux to the atmosphere)/(CaCO₃ precipitated). θ depends not only on water temperature and atmospheric CO₂ concentration but also on the CaCO₃ and organic carbon masses formed. In CO₂ generation by CaCO₃ precipitation, θ varies from a fraction of 0.44 to 0.79, increasing with decreasing temperature (25 to 5°C), increasing atmospheric CO₂ concentration (195–375 ppmv), and increasing CaCO₃ precipitated mass (up to 45% of the initial DIC concentration in surface water). Primary production and net storage of organic carbon counteracts the CO₂ production by carbonate precipitation and it results in lower CO₂ emissions from the surface layer. When atmospheric CO₂ increases due to the ocean-to-atmosphere flux rather than remaining constant, the amount of CO₂ transferred is a non-linear function of the surface layer thickness because of the back-pressure of the rising atmospheric CO₂. For a surface ocean layer approximated by a 50-m-thick euphotic zone that receives input of inorganic and organic carbon from land, the calculated CO₂ flux to the atmosphere is a function of the CaCO₃ and C_org net storage rates. In general, the carbonate storage rate has been greater than that of organic carbon. The CO₂ flux near the Last Glacial Maximum is 17 to 7×10¹² mol/yr (0.2–0.08 Gt C/yr), reflecting the range of organic carbon storage rates in sediments, and for pre-industrial time it is 38–42×10¹² mol/yr (0.46–0.50 Gt C/yr). Within the imbalanced global carbon cycle, our estimates indicate that prior to anthropogenic emissions of CO₂ to the atmosphere the land organic reservoir was gaining carbon and the surface ocean was losing carbon, calcium, and total alkalinity owing to the CaCO₃ storage and consequent emission of CO₂. These results are in agreement with the conclusions of a number of other investigators. As the CO₂ uptake in mineral weathering is a major flux in the global carbon cycle, the CO₂ weathering pathway that originates in the CO₂ produced by remineralization of soil humus rather than by direct uptake from the atmosphere may reduce the relatively large imbalances of the atmosphere and land organic reservoir at 10²–10⁴-year time scales.  相似文献   

The evolution characteristics of positive and negative earthquakes before strong quakes in Kanto area and the Hyugo earthquake in Japan     

王裕仓  宋治平  细野耕司  陈学中  尹祥础 《地震学报(英文版)》1998,11(1):35-42

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Last Glacial snowlines in the Tibetan Plateau: an argument against an extensive coalescing icesheet     

Z.-D Feng 《GeoJournal》1998,44(4):355-362

Two opposing theories are circulating with regard to the extent of the Last Glacial ice cover in the Tibetan Plateau. One says that only less than 20% of plateau was covered with ice, and another insists that the plateau be completely covered with an extensive coalescing icesheet. The extent of the ice cover is thought to be significant in shaping global climatic systems, and a further discussion on this issue may help to understand the earth's surface feedback mechanisms to the global climates. This paper focuses on the Last Glacial snowline reconstruction and uses the reconstructed snowline to argue against the existence of an extensive coalescing icesheet. The reconstructed Last Glacial snowlines suggest that the snowlines dropped 500–700 m in the western and northern marginal mountains and about 1000 m in the southern and eastern marginal mountains of the Tibetan Plateau. However, the magnitude of the snowline dropping decreases dramatically towards the interior of the plateau, from 300–400 m in those mountains adjacent to the marginal mountains to about 100 m in the driest area in the interior. This means that the snowlines were too high and associated glaciers were too limited to extend to the vast intermountainous basins. To be blamed are weakened summer monsoons and lowered condensation elevations, both of which were probably responsible for not bringing in an adequate amount of precipitation into the interior for developing an extensive coalescing icesheet. The relatively high radiation in these relatively low latitudes could be a major negative force to prevent the snow and ice from forming a coalescing icesheet. In contrast, the enhanced plateau blockade to the monsoons may have helped to significantly lower the snowlines and expand the glaciers in the outer slopes of the southern and eastern marginal mountains. The westerlies may have greatly helped those glaciers in the western and northern marginal mountains. This revised version was published online in July 2006 with corrections to the Cover Date.  相似文献   

北祁连加里东期俯冲-增生楔结构及动力学   总被引：28，自引：1，他引：27       下载免费PDF全文

张建新 《地质科学》1998,33(3):290-299

北祁连加里东朝俯冲-增生楔可分为浅部和深部两个单元。浅部单元主要由蛇绿岩、蛇绿混杂岩及深海复理石所组成,极浅变质或没有变质。深部单元主要由HP/LT蓝片岩、透镜状的蛇纹岩、变辉长岩及绿片岩(主要为退变质产物)所组成。普遍遭受HP/LT变质作用和绿片岩相的退变质作用。两个单元同时形成于不同的构造层次,具有类似的原岩特征。在加里东期,俯冲-增生楔共经历4期变形作用(D₁,D₂,D₃,D₄)和3期变质作用(M₁,M₂,M₃).从D₁→D₄反映了俯冲-增生楔从俯冲作用→深部构造板底垫托作用→折返(构造顶蚀)→剥蚀的动力学演化过程。  相似文献   

亚南极冰川雪冰内MSA的季节变化(英)     

HAN Jian-Kang  XIE Zi-Chu 《冰川冻土》1998,(4)

Methanesulphonate was investigated as a potential contributor to the sulphur budget based on the analysis on Antarctic snow/ice from Coffins Ice Cap, King George Island (62°10' S, 58°50,W). The anion was found to be present at a mean concentration of 0. 17 μeq. L-1 with a maximum of 0.73 μeq. L-1. A distinct seasonal variation exists in the top 10 m of the core, equivalent to more than two years of deposition. Dating resulted from δ18O profile suggests that the principal peaks of methanesulphonate are associated with snow deposited in autumn and secondary peaks in spring. The seasonal patterns of methanesulphonate in the subantarctic snow displays a phase difference from that observed in marine air from low and middle latitudes.  相似文献   

陕西段家坡黄土剖面中布容／松山古地磁界线附近铱异常的发现及其启示   总被引：3，自引：0，他引：3  

马配学  侯泉林 《地质学报》1998,72(2):173-177

利用高灵敏度放射化学中子活化分析方法,对我国陕西段家坡黄土剖面早－中更新统（约０．７３Ｍａ）沉积界线附近铱和其它元素的丰度进行了测定。结果表明,在布容／松山（Ｂ／Ｍ）古地磁界线附近铱的含量明显增大,最大值为４６．３ｐｇ／ｇ。相对于整个剖面的平均背景值（约１５ｐｇ／ｇ）大约富集了３倍。用地壳元素钪进行标准化之后,铱异常十分明显,而其它元素在界线附近则没有变化。黄土剖面上铱异常的赋存层位与西南太平洋钻  相似文献   

中国数字地震台网数据管理中心日常工作软件的升级和应用     

邹立晔  郭燕平 《地震地磁观测与研究》1998,19(3):60-69

文中阐述了中国数字地震台网数据管理中心（ＣＤＳＮ ＤＭＣ）日常工作软件的升级和升级后新软件的主要功能,并结合新软件的主要命令及运行实例,对升级后软件的实际应用作了简要叙述。  相似文献   

采样过程和模数转换对记录的影响及“真实地面运动”获取——地震学上用的数字信号处理的基本原理和实例(讲座3)     

陈祥熊  江燕 《地震地磁观测与研究》1998,(2)

通过采样过程和模数转换对记录影响的分析,讨论了数字地震仪记录的动态范围,以及如何使用谱分析方法去除仪器对最终记录的影响,以便获取“真实地面运动”的近似。  相似文献   

Y11B航空物探(电/磁)综合站西北找水初步成果   总被引：1，自引：1，他引：0  

孟庆敏 《物探与化探》1998,22(4):241-246

1997年9月23日～10月8日,在甘肃省安西—敦煌地区用Y11B航空物探(电/磁)综合站和GPS导航定位进行了地下水勘查试生产工作。用均匀大地模型,结合已知的水文地质资料,初步圈定了淡水区、过渡类型水区、咸水区和苦水区及泉水湖。所推断的水质和土壤含盐量与大的水文地质单元和1:20万水文地质普查报告都吻合得很好,且细节更为清楚。对差异较大的地方做了分析和解释。  相似文献