云南红宝石矿床中镁砂川闪石的发现及其意义

镁砂川闪石是１９８４年在日本发现的 新矿物，在世界上产地很少。本文对其物理性质、化学成分、Ｘ射线粉晶衍射和红外吸收光谱等方面进行了研究。     

山东金伯利岩中的钛钡铬石—钛钾铬石系列

山东金伯利岩中的副矿物钛钡铬石、钛钾铬石在我国属首次发现,它们是锶钛铁矿族一个类质同象系列的大阳离子分别以Ba和K为主的两种新矿物。本文通过化学成分、穆斯堡尔谱、反射光谱、X射线粉晶衍射等分析研究,为这两种矿物提供了有意义的矿物学资料。     

中国地震台网、全球地震台网地震目录数据库和震相数据库

地震目录和震相数据在地震学研究中具有重要意义，本文介绍了中国地震台网、全球地震台网地震目录数据库和震相数据库的内容和查询使用方法。     

STREAM-SUBSURFACE EXCHANGE, SUSPENDED SEDIMENT TRANSPORT, AND THE COUPLED TRANSPORT OF COLLOIDS AND CONTAMINANTS IN SEDIMENT BEDS

1 INTRODUCTION Alluvial streams generally have permeable bed sediments that can admit significant pore water flows. Steady flow of surface water over bed roughness features such as sand waves or pools and riffles can then drive water flow into and out of the shallow subsurface. This is often termed hyporheic exchange, and the subsurface region where mixing between stream and ground waters occurs is the hyporheic zone (Hynes, 1983). The hyporheic zone has been shown to be a critical com…     

海上设施精密定位研究

介绍了海上设施精密定位的原理和方法,分析了其误差来源和适用范围,以南海某平台的实例实现了海上设施精密定位.     

大连城市空间意象分析

近年来,城市空间意象研究开始在我国城市地理学界逐渐兴起。通过问卷调查、图片辨认和认知地图调查对大连市微观空间情景和宏观空间结构意象进行研究,在国内首次将因子分析方法应用于微观空间情景的意象偏好分析,并运用均值比较检验及方差分析研究了年龄、性别、学历等属性对个人辨认照片数目及意象范围的影响。研究结果表明：大连市总体可意象程度较高;微观空间情景的意象受其功能、区位、使用者、自然环境以及建筑本体的影响;宏观空间结构意象是以道路为主要支撑,以居住区与商业区为背景,人口集散地与特色建筑点缀其中的立体框架结构;意象区域是以中部为主轴向东西两个方向辐射,并且主要集中在市中心、商业区及风景旅游区;由于受到年龄、性别、学历的影响,个人的意象范围大小存在一定的差异。在此研究基础上,对大连市旅游规划及城市规划提出了相应的建议。     

IRIS DMC的数据服务

介绍了IRISDMC的数据来源、数据服务内容和数据请求工具,这对于较好地使用其数据资源及做好中国的地震数据服务工作有一定的意义。     

海上距离元胞自动机分析法

针对障碍存在情况下距离变换研究较少的问题,提出了一种基于元胞自动机的绕障欧氏距离变换方法。以南海为例,基于海陆分布数据和目标点数据,以最短绕障路径长度为元胞状态,设计了包含距离算子的元胞状态转换规则。通过元胞自动机模拟距离扩散计算过程,得到绕障距离变换结果,并分析了绕障效果和精度。结果表明:本文方法动态直观地展示了绕障距离变换过程,能够自动计算绕过障碍的最短距离;具有更新机制,能够根据邻域的变化修正状态值;为绕障距离变换问题提供了一种近似的解决途径,错误率低于3.96%,可应用于航线设计、海上救助等领域。     

第二次世界大战后英国乡村景观研究的脉络走向及启示

英国是全球乡村景观建设和发展的典范。从地理学、生态学及规划学等综合的视角出发,首先从社会背景上分析二战后英国乡村景观的演变轨迹;其次从学术背景梳理英国乡村景观的研究历程,并从学科角度提炼不同阶段的研究重点及研究特征;最后从研究趋势方面讨论学者们最新的研究议题。在梳理和总结英国乡村景观研究的基础上,提出对中国乡村景观研究的启示和借鉴。     

Organic biomarkers in the twilight zone—Time series and settling velocity sediment traps during MedFlux

The transfer of material through the twilight zone of the ocean is controlled by sinking particles that contain organic matter (OM) and mineral ballast. During the MedFlux field program in the northwestern Mediterranean Sea in 2003, sinking particulate matter was collected in time series (TS) and settling velocity (SV) traps and analyzed for amino acids, lipids, and pigments (along with ballast minerals) [Lee, C., Armstrong, R.A., Wakeham, S.G., Peterson, M.L., Miquel, J.C., Cochran, J.K., Fowler, S.W., Hirschberg, D., Beck, A. Xue, J., 2009b. Particulate matter fluxes in time series and settling velocity sediment traps in the northwestern Mediterranean Sea. Deep-Sea Research II, this volume [doi:10.1016/j.dsr2.2008.12.003]]. The goal was to identify how organic chemical compositions of sinking particles varied as a function of their in-situ settling velocity. The TS record was used to define the biogeochemical character and temporal pattern in flux during the period of SV trap deployment. Temporal variations in organic and mineral compositions are consistent with particle biogeochemistry being driven by the seasonal succession of phytoplankton. Spring diatom bloom conditions led to a high flux of rapidly sinking aggregates and zooplankton fecal matter; summer oligotrophy followed and was characterized by a higher proportion of slowly sinking phytoplankton cells. Bacterial degradation is particularly important during the low-flux summer period. Settling velocity traps show that a large proportion of particulate organic matter sinks at 200–500 m d⁻¹. Organic compositions of this fast-sinking material mirrors that of fecal pellets and aggregated material that sinks as the spring bloom terminates. More-slowly sinking OM bears a stronger signature of bacterial degradation than do the faster-sinking particles. The observation that compositions of SV-sorted fractions are different implies that the particle field is compositionally heterogeneous over a range of settling velocities. Thus physical and biological exchange between fast-sinking and slow-sinking particles as they pass down the water column must be incomplete.