基于对象存储的集群文件系统CFSlight设计与实现

在线存储以及数据密集型应用的发展,对信息存储性能的要求越来越高,分布式存储系统是应对数据存储需求的重要研究方向.基于对象存储技术和Linux操作系统平台设计与实现的集群文件系统CFSlight,能够有效提高存储系统的可扩展性、I/O性能、可用性等技术指标,具有很好的发展前景.     

一种解决噪声主动控制中时滞问题的思路

对噪声主动控制进行了探讨，提出一种利用计算机存储概念和寻址技术，从计算机数据处理系统入手解决时滞问题的思路，并给出了结构图。     

负载BaCeO3/γ-Al2O3催化剂的储氮和抗硫特性

用XRD、FT-IR等手段研究了钙钛矿型BaCeO3系列样品的晶相和氮氧化物吸收物种,并测定了它们的储氮量(NSC). 结果表明:加入贵金属反而使NSC降低. 而对于负载的BaCeO3/γ-Al2O3样品,加入贵金属后,NSC值提高了3倍以上,其顺序为Pt>Rh>Pt-Rh. 结果还表明,BaCeO3和Pt/BaCeO3样品在φ(SO2)<0.006 %时,仍具有较高的NSC值,而Pt/BaCeO3/γ-Al2O3样品不但具有很高的储氮能力而且具有更好的抗硫性能.     

高速数字存储示波器的超前滞后电路设计

数字存储示波器的核心是时基电路，超前／滞后控制电路是时基电路的核心。其设计是数字存储示波器的关键。用可编程语言FPGA实现设计了用前置计数器和后置计数器控制触发点前后的采集样点数和数据的方案。     

基于TDI的网络安全存储系统研究与实现

提出了传输层网络安全存储系统的体系结构和实现方法 ,将用户管理、访问控制、数据加密和审计日志等安全措施集中到普通网络存储系统中 ,并重点对系统中基于TDI的过滤驱动程序原理和实现进行了分析 .该系统为提高目前网络存储系统的安全性提供了一种方便安全、管理集中、高效可靠的解决方案     

井冈山自然保护区甜槠群落物种多样性分析

以甜槠群落6个样地调查资料为基础,对该群落的区系组成和不同样地、不同层次的物种多样性进行了分析,结果表明:(1)甜槠群落中有维管植物59科85属116种(含变种);属的地理成分以热带成分占优势,温带成分占有一定的比例。(2)乔木层、灌木层和草本层的各项物种多样性指标在群落各样地间均有一定的差异;在群落垂直结构中,灌木层的多样性指数最大,乔木层次之,草本层最小。     

C－isotope composition and significance of the Sinian on the Tarim plate

102 samples of limestones,mudrocks shales and tillites from the Sinian in Kuluketage have been analyzed ,Four formations in the Sinian belong to glacial deposits in which the differences in δ^13C are distinct (-14.7‰- 4.2‰),Distinctly negative δ^13C excursions for three times support the viwe of three glacial deposits in this area suggested by previous authors,except for the durations of them ,δ^13C values are generally positive in the Beiyixi Formation of lower part of the Lower Sinian ,representing probably the rock records of a continental rift related to break-up of the Rodinian supercontinent,There are three times of distinct excursions of δ^13C curve in all strata,The first one is from positive values at the bottom to about -5‰ at the top of the Beiyixi Formation ,The second one,from 0‰-3‰ in the Arletonggou Formation of upper part of the Lower Sinian to -3.4‰---14.4‰ in the Teruiaiken Formation.The third one,from positive values in the Zhamoketi Formation of lower part of the Upper Sinian to negative values in glacial varves at the top of the Hankeerqiaoke Formation.     

Inorganic chemical composition and source signature of PM2.5 in Beijing during ACE-Asia period

Aerosol samples for PM2.5 were collected in Beijing for 38 consecutive days from March to April 2001 using an IMPROVE Sampler. Concentrations of 20 elements in PM2.5 were determined using a PIXE method. Results show that the average mineral dust concentration of PM2.5 was 14.6 Ilg/m3 during the observation period. On the sand-dust event days of March 21 and April 10, dust PM2.5 mass concentrations were 62.4 and 54.1 μg/m^3, respectively.These demonstrate that fine particle pollution by dust event in Beijing was very severe. The enrichment factors of S and Cu reached minimums on the dusty days and were high on the non-dusty days. It is considered that enrichment factors of elements in PM2.5, which are associated with human activities, can probably provide an effective method to distinguish local sources from external sources of dust. Factor analysis on the chemical composition in PM2.5 shows that sources of crustal matters, anthropogenic emission, and oil combustion contributed to PM2.5 levels in air in the springtime of 2001 in Beijing.     

Isotopic evolution of the terminal Neoproterozoic and early Cambrian carbon cycle on the northern Yangtze Platform, South China

Profound geotectonic, climatic and biological changes occur during the terminal Neoproterozoic and its transition into the early Cambrian. These are reflected in temporal variations of the chemical and isotopic composition of seawater. We are studying a sequence of sedimentary rocks at the Shatan section, northern Yangtze Platform, Sichuan Province of China. This succession comprises, in ascending stratigraphic order, predominantly calcareous sediments of the Sinian upper Dengying Formation and black shales of the lower Cambrian Guojiaba Formation (time equivalent of Niutitang Fm.). Paleoenvironmental setting represents shallow-water shelf deposits. The objective of our study is to provide temporal records for the isotopic compositions of organic and carbonate carbon throughout this time interval. Organic carbon isotope values display a range between -35.8‰ and -30.1‰ with clear stratigraphic variations. Carbonate carbon isotope data vary between -3.5‰ and +0.5‰. These secular variations are interpreted to reflect perturbations of the global carbon cycle, specifically changes in the fractional burial of organic carbon. However, local conditions have further affected the isotopic signals.     

Structural and Chemical Diversity of TI-Based Cuprate Superconductors

The first TI一based euprate supereonduetor,TI一Ba-Cu一(),was diseovered by 2.2.Sheng and A.M.Hermann仁1〕. TI beeomes supereondueting at 2.38 K.NumerousTI eompounds and alloys are supereondueting.TIMo6Ses has the highest transition temperature of1 2.2 K among all non一euprate Tl eontaining alloyand eompound supereonduetors.Before thediseovery of the euprate supereonduetors,some TIeontaining oxide supereonduetors were found,among whieh TI。.3W()3 has the highest transitiontemPerature,2.14 K. Sinee the diseovery of TI euPratesuPereonduetors,two distinet families have beenidentified.Soon after the diseovery of TI一Ba一Cu-(),supereonduetivity was eonfirmed in TI一Ba一Ca-Cu一()samples.The ehemieal eompositions anderystal struetures of those eompounds were workedout as T12BaZCu()6,T12BaZCaCuZ()。,andT12BaZCaZCu3OI。[2〕.This 15 the first family of TIeuPrate supereonduetors,whieh features two TIatoms in eaeh ehemieal formula.