集中式银证通系统中双向交易的设计与实现

首先介绍银证通基本概念,阐述了集中式银证通系统设计的基本理念、体系结构,然后在此基础上讨论了银证通系统中双向交易的设计和实现,提出了两种解决方案,分析了最初方案的缺点所在,进而提出了改进方案,达到了预期的效果.     

网络安全动态防御体系研究及应用

在分析P2DR2模型的基础上,阐述了发展网络安全动态防御体系的重要性,讨论了其功能需求,提出了改进的IDS分析响应系统模型,并以其为核心构建了网络安全动态防御体系,还讨论了实现的关键技术并给出了应用实例.     

望奎局抓学习全力提升队伍素质

他们一是深入开展了专项学教活动。制定了《望奎县国土资源局学习制度》,对每月的学习内容做了系统安排,不断巩固提高学习成果。二是深入开展了“关注民生、服务发展”活动。制定出台了《活动实施方案》等行风建设方案,有效规范了国土干部的从政行为,促进了工作作风的好转。三是深入开展了“双学促廉”活动。     

杏花春雨

正如雾似烟的细雨清润的杏花有了些许的兴奋,排着队,一片一片地洇红了由近及远的几条山谷。杜鹃很是深情的一声声的鸣叫,令舒展了枝条的杏树陡然收敛了放荡的思绪。该是唱一杯杏花酒的时刻了,就着这细雨、这杏花,和那唱着歌儿已经远去了的杜鹃。北方的春天,虽说少了江南特有的那一份烟的婉约和水的妩媚,却多了北方固有的山的刚毅与河的奔放。被春天反复熏染得或浓、或淡的远山,像极了白石老人笔下的丹青水墨。尤其雨后的山谷,杏树枝条的颜色较先前暗了许多,杏花却愈发明丽粉白。都因了一场春雨,再也寻不到杏花一     

澳大利亚土地登记的现状、特点和启示

介绍了澳大利亚土地登记的背景和现状,归纳了土地权利的基本类型,分析了澳大利亚现行土地登记的内涵以及主要特点,提出了改革我国土地登记模式的框架性构想和建议。     

佳木斯局成功化解一件二十年信访积案

1月22日,佳木斯市华侨公司的职工代表3人来到了市国土局,送来了由市书法家书写的条幅：“依法行政化解纠纷,案结事了和谐稳定”,标志着经历了十多年的信访积案,得到了有效化解,表达了企业职工对市国土局感激之情,赞誉之情。     

Q型聚类分析在枣庄市地下水污染研究中的应用

该文给出了Q型聚类分析的原理和计算方法,并结合清凉泉水源地的污染问题进行了研究。通过长系列的水质监测资料,查明了清凉泉水源地水质动态变化特征,并对特征污染因子进行了聚类分析,基本查明了清凉泉水源地的污染途径,得到了较满意的结果。     

地质摄影家赵洪山《地质摄影》正式出版发行

4月26日,著名地质摄影家赵洪山编著的《地质摄影》一书,由中国文史出版社正式出版发行。《地质摄影》是国内第一部系统介绍地质摄影的著作。此书首次对"地质摄影"给出了定义,并追溯了世界地质摄影的历史,指出了地质摄影的特点,介绍了地质摄影的经验和方法,分析了地质摄影与风光摄影等其他摄影门类的联系和区别,从而形成了系统的地质摄影理论。同时,该书还收录了作者众多精美的地质摄影作品,既展示了国内地质摄     

开发WebGIS的ArcIMS新技术应用分析

本文论述了 Arc IMS的体系结构 ,阐述了 Arc IMS的运行机制 ,着重分析了 Arc XML在这一结构内的作用 ,并介绍了服务器端的逻辑和物理层次、客户端的基本功能 ,从而剖析了 Arc IMS的核心部分。同时从使用的角度 ,介绍了如何管理 Arc IMS服务器 ,并分别论述某功能部件。最后对站点安全这个万维网地理信息系统必须密切关注的问题 ,结合 Arc IMS平台的特点进行了分析 ,并提出一些解决方法。     

下猛药激发活力——宁明县国土资源局作风效能建设的经验

积极、认真开展"转变作风,提高效能"活动,给宁明县国土资源局带来了不少可喜的变化. "今年总的感觉,我们的精神面貌变了,各项工作顺了,内部活力增加了,而活力的增加,又使机关的行政效能得到了提高".     

The flood of the Nenjiang river and the Songhua river in 1998 and the comprehensive management of the river basins

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Modeling the Water-Flushing Properties of the Yangtze Estuary and Adjacent Waters

As a multi-branch estuary system, the Yangtze Estuary presents distinctive characteristics of hydrodynamic processes through co-action among river runoff, tides, wind-waves, and gravitational circulation. To study the pathways of flushing water along all of the estuary's branches and analyze their differences, especially those due to the influence of seawater intrusion and discharge variations, a free surface flow modeling suite TELEMAC-MASCARET involving passive tracers was applied to the Yangtze Estuary and the adjacent waters. The open boundary conditions were provided by the Nao.99 b model(Matsumoto et al., 2000), which was calibrated using observed velocity and salinity data obtained in March 2002. The water age, which was used as the diagnostic tool to study the flushing efficiency of the water body across the estuary, was solved by additional advection-diffusion-reaction equations implemented in the TELEMAC modeling system. The transport properties were investigated under different river discharge scenarios, which represented seasonal impacts; aspects relating to the influence of tide, surface wind stress, and density-induced circulation on age were also investigated. Model results showed that river runoff is one of the dominant factors influencing the spatial distribution of the mean age, while tidal force is another important factor. The horizontal freshwater age distribution demonstrated similarity compared with the salinity distribution; the vertical age distribution resembled the stratification pattern of salinity in all branches where stratification persists. An experimental numerical simulation of tracing saltwater age from the lower reaches of the estuary was conducted, and implicated the connectivity with transport processes of freshwater from upstream. Additionally, a particle tracking algorithm was used to analyze the dynamic characteristics of the four passages. The South Passage and South Channel were found to be significant as main water flow passages, while salinity intrusion in the North Branch was found to cause a return flow that partially joins the South Branch flushing water.     

Freshening of the intermediate water of the South China Sea between the 1960s and the 1980s

Variation in intermediate water salinity in the South China Sea (SCS) between the 1960s and 1980s was studied using historical hydrographic data. The results demonstrate that the water was significantly fresher in the 1980s than in the 1960s, indicating that vertical mixing at intermediate water depth was reduced in the 1980s. This was partially because of the change of the SCS meridional overturning circulation (MOC) connecting local intermediate water with deep water. Data assimilation showed a 0.5Sv (1 Sv=10 6m 3/s) reduction in the strength of the MOC, which is about one third of the mean SCS MOC. Because the SCS MOC is linked to the Pacific Ocean, such an interdecadal variation in the intermediate water SCS may reflect anthropogenic climate change in the world ocean.     

时空对象行为分类与形式化表达

基于行为驱动的传统时空数据模型只关注时空对象的空间运动行为,忽略了行为对时空对象属性、关系等的改变,导致行为对时空对象的驱动机制研究不足。时空行为是全空间信息系统表达的重要特征之一,为此,本文从以下几个方面阐述了时空对象的行为。首先,本文阐述3行为的定义及将行为作为时空本体的元组的必要性。其次,研究了时空对象行为的复杂性、可继承性及在时态上的延续性等特征。再次,根据行为的作用对象,将时空对象的行为分为空间行为、属性行为、关系行为及复合行为4类行为,并给出了上述4类行为的定义与形式化表达方式。最后,分析了时空本体中时空行为的驱动机制。通过时空行为分类及其在时空本体中的形式化表达研究,为基于行为驱动的时空对象构模奠定了理论基础。     

高句丽王朝时期的文化艺术研究

通过高句丽王朝接受中原文化的途径、方式、程度,并结合高句丽王朝较其他少数民族在文化发展上的优势,对高句丽王朝时期的文化艺术发展作综合判断,认为高句丽文化艺术是边疆文化的重要组成部分,对东北亚地区的文化交流和传播做出重要贡献。     

Foraminiferal Changes and Response to the Channel Diversion and Discharge Fluctuation of the Yellow River in the North Yellow Sea During the Past Century

Diversion of the Yellow River is a unique geological event in offshore China, causing changes of the sedimentary environment in eastern China Seas. The last diversion took place in AD 1855, with the estuary diverted from the Yellow Sea into the Bohai Sea. The identification of the river diversion events in the shelf sediments would not only provide the definite ages for the sediments, but also give a clue for better understanding of the sedimentation in that area. In this study, 210 Pb, grain size, geochemical element, and foraminiferal data in core H205 from the north Yellow Sea were systematically investigated. A high-resolution sedimentary record was established, which was coupled with the Yellow River diversion and runoff changes. The results show that the foraminiferal composition and foraminiferal abundance of the sediments from the north Yellow Sea had good response to the Yellow River diversion in 1855. Before the change, shallow water assemblages dominated the foraminifera, and the abundance of each foraminiferal species was very low. After the diversion event, the abundance of most foraminifera increased sharply, with a maximum increase of 16 times, and the assemblage was still dominated by shallow water species. Furthermore, the changes in foraminiferal abundance in the core sediments corresponded well with the discharge fluctuation of the Yellow River since 1855. When the Yellow River began entering the Bohai Sea, the Yellow River water, which is rich in nutrients, along with the coastal currents affected the north Yellow Sea, increased the primary productivity in the north Yellow Sea, which is the main reason for the abrupt increase and fluctuation of foraminiferal abundance in this area. At the meantime, the East Asian winter monsoon could also promote the development of nearshore foraminiferal species by enhancing the coastal currents.     

Formation and evolution of the modem warm current system in the East China Sea and the Yellow Sea since the last deglaciation

To reconstruct the formation and evolution process of the warm current system within the East China Sea (ECS) and the Yellow Sea (YS) since the last deglaciation, the paleoceangraphic records in core DGKS9603, core CSH1 and core YSDPI02, which were retrieved from the mainstream of the Kuroshio Current (KC), the edge of the modem Tsushima Warm Current (TWC) and muddy region under cold waters accreted with the Yellow Sea Warm Current (YSWC) respectively, were synthetically analyzed. The results indicate that the formation and evolution of the modem warm current system in the ECS and the YS has been accompanied by the development of the KC and impulse rising of the sea level since the last deglaciation. The influence of the KC on the Okinawa Trough had enhanced since 16 cal kyr BE and synchronously the modem TWC began to develop with the rising of sea level and finally formed at about 8.5 cal kyr BP. The KC had experienced two weakening process during the Heinrich event 1 and the Younger Drays event from 16 to 8.5 cal kyr BP. The period of 7-6 cal kyr BP was the strongest stage of the KC and the TWC since the last deglaciation. The YSWC has appeared at about 6.4 cal kyr BP. Thus,the warm current system of the ECS and the YS has ultimately formed. The weakness of the KC,indicated by the occurrence of Pulleniatina minimum event (PME) during the period from 5.3 to 2.8 cal kyr BE caused the main stream of the TWC to shift eastward to the Pacific Ocean around about 3 cal kyr BP. The process resulted in the intruding of continent shelf cold water mass with rich nutrients. Synchronously, the strength of the YSWC was relatively weak and the related cold water body was active at the early-mid stage of its appearance against the PME background, which resulted in the quick formation of muddy deposit system in the southeastern YS. The strength of the warm current system in the ECS and the YS has enhanced evidently, and approached to the modern condition gradually since 3 cal kyr BP.     

Changes in the thermal and hydraulic regime within the active layer in the Qinghai-Tibet Plateau

The change trends of air temperature,precipitation and evaporation from 1999 to 2008 shows that the climate in the Qinghai-Tibet Plateau permafrost region had become warmer.The analysis of the systematic active-layer data monitoring network along the Qinghai-Tibet Highway indicated that the active-layer thickness had been increasing and the soil temperature was rising.The soil temperature was rising in winter but not at the end of spring or during the entire summer.With thickening and warming of the active layer,the liquid water content of the active layer had an obvious downward migration and liquid water content in the top horizons decreased,but in the deeper horizons it increased.     

施氏獭蛤幼虫和稚贝发育及行为的研究

进行了施氏獭蛤(Lutraria sieboldii Reeve)的人工育苗、幼虫发育及行为观察实验。结果显示:在施氏獭蛤幼虫发育过程中,壳顶后期幼虫只有鳃丝及足出现,而没有眼点出现,发达的足和鳃丝是幼虫变态的标志;幼虫变态期明显的分为3～5d的爬行期和3～5d的附着期;爬行期幼虫有单条水管形成,附着期幼虫只有一条分叉的足丝,水管为单管型;底栖稚贝期开始形成两条水管,底栖稚贝早期的幼虫不具备潜沙能力,只进行爬行活动,随着水管的快速发育,幼虫逐渐具备潜沙能力,幼虫壳长达2500μm、水管长达6000μm以上时,最终具备和成体一样的完全潜沙能力。     

Formation and evolution of the modern warm current system in the East China Sea and the Yellow Sea since the last deglaciation

To reconstruct the formation and evolution process of the warm current system within the East China Sea (ECS) and the Yellow Sea (YS) since the last deglaciation, the paleoceangraphic records in core DGKS9603, core CSH1 and core YSDP102, which were retrieved from the mainstream of the Kuroshio Current (KC), the edge of the modern Tsushima Warm Current (TWC) and muddy region under cold waters accreted with the Yellow Sea Warm Current (YSWC) respectively, were synthetically analyzed. The results indicate that the formation and evolution of the modern warm current system in the ECS and the YS has been accompanied by the development of the KC and impulse rising of the sea level since the last deglaciation. The influence of the KC on the Okinawa Trough had enhanced since 16 cal kyr BP, and synchronously the modern TWC began to develop with the rising of sea level and finally formed at about 8.5 cal kyr BP. The KC had experienced two weakening process during the Heinrich event 1 and the Younger Drays event from 16 to 8.5 cal kyr BP. The period of 7–6 cal kyr BP was the strongest stage of the KC and the TWC since the last deglaciation. The YSWC has appeared at about 6.4 cal kyr BP. Thus, the warm current system of the ECS and the YS has ultimately formed. The weakness of the KC, indicated by the occurrence of Pulleniatina minimum event (PME) during the period from 5.3 to 2.8 cal kyr BP, caused the main stream of the TWC to shift eastward to the Pacific Ocean around about 3 cal kyr BP. The process resulted in the intruding of continent shelf cold water mass with rich nutrients. Synchronously, the strength of the YSWC was relatively weak and the related cold water body was active at the early-mid stage of its appearance against the PME background, which resulted in the quick formation of muddy deposit system in the southeastern YS. The strength of the warm current system in the ECS and the YS has enhanced evidently, and approached to the modern condition gradually since 3 cal kyr BP. Supported by the National Natural Science Foundation of China (Nos. 90411014 and 40506015), the National major Fundamental Research and Development Project (No. 2007CB815903) and the CAS Pilot Project of the National Knowledge Innovation Program (No. KZCFX3-SW-233)