社区:通往农村环境自治的阶梯

农村环境自治是村民自治在环境领域的特殊体现和具体样式,是村民自治的延伸。它关系着我国新型城镇化的进程,关系着农村居民的生活舒适程度。农村环境自治的基本诉求是培育农民的环境自觉和环境意识,走一条社会资本与制度资本相结合的治理道路。而社区凭借其规模小、稳定、同质性高以及拥有共同意识等优势成为农村环境自治的承载主体。社区作为通往农村环境自治的阶梯离不开政府的政治支持、充足的资源配置以及完善的法律保障,非政府环保组织的积极参与也是社区环境治理不可缺少的社会力量。     

基于SRIO的FPGA间数据交互系统设计与应用

基于时分长期演进(time division long term evolution,TD-LTE)射频一致性测试系统中数据交互的分析研究,为了很好地满足现场可编程门阵列(field programmable gate array,FPGA)间的大容量数据交互,设计了一种高速的嵌入式技术串行高速输入输出口(serial rapid IO,SRIO),实现2块FPGA芯片间的互连,保证在TD-LTE系统中上行和下行数据处理的独立性和交互的便捷。基于Xilinx公司的Virtex-6系列XC6VLX475T芯片,给出了SRIO接口的整体性设计方案,经过ModelSim软件仿真,确定适合项目需要的数据交互的格式类型和事务类型,对接口代码进行综合、板级验证、联机调试等,在ChipScope软件上对比分析数据传输的正确性,通过测试模块统计比较发送和接收信号的误比特率,确定了SRIO接口在高速数据传输的稳定性和可靠性,成功验证了SRIO接口在FPGA之间数据的互连互通,并将该方案作为一种新的总线技术应用于TD-LTE射频一致性测试仪系统开发中。     

TiO2-聚苯胺纳米复合薄膜的电沉积制备

为获得形貌均匀、晶形细小的TiO2-聚苯胺纳米复合薄膜,研究沉积条件对复合膜的影响,采用电化学沉积技术进行了复合膜的制备试验.试验确定了膜沉积的优化条件:电位为-1.5 V(VSSCE),pH=1.5～2.0,沉积时间为1 300 s.采用电化学方法、扫描电镜及热分析等测试手段对电沉积复合膜进行了表征.结果表明:循环伏安峰电流越小,对应的沉积膜的沉积质量越好;基底不同,复合膜形貌有着显著差异.扫描电镜观察发现:沉积液中苯胺分子对电沉积反应过程、沉积物粒度及形貌有很大的影响,苯胺小分子的添加有利于得到晶形更为细小的TiO2-聚苯胺纳米复合薄膜.     

一种验证软件演化过程行为的代数推导方法

针对现有软件过程验证主要以结构验证和性质验证为主,缺乏行为验证的不足,提出了一种验证软件演化过程行为的代数方法.该方法使用通信进程代数ACP对软件演化过程元模型EPMM进行扩展,提出软件演化过程元模型代数EPMM-A.针对EPMM建模产生的软件演化过程模型,一方面使用EPMM-A形式定义软件演化过程模型的行为规约,另一方面在其公理系统的支持下,基于等式推导验证软件演化过程模型的行为与行为规约是否一致,使行为验证方式从模型推导(非形式化)变为代数推导(形式化).为了说明代数推导的正确性,证明了软件演化过程元模型代数的公理系统具有可靠性.     

医院导向系统的研究与改进

针对医院现有的导向系统所存在的缺陷,设计了一种新型的智能化医院导向系统,旨在解决患者就诊无法及时并准确找到相应科室医生就诊的问题。文中通过分析医院导向系统的特点和不足,提出了新的设计方案,并利用智能算法与数据挖掘技术使系统更优化。     

Capping stack - An industry in the making

This paper gives an overview of recent development of the marine well containment system (MWCS) after BP Macondo subsea well blowout occurred on April 20,2010 in the Gulf of Mexico. Capping stack,a hard-ware utilized to contain blowout well at or near the wellhead is the center piece of MWCS. Accessibility to the dedicated capping stacks is gradually becoming a pre-requirement to obtain the permit for offshore drilling/workover, and the industry for manufacturing,maintenance,transportation and operation of the capping stack is in the making.     

对《信号检测与估计》课程设置的构想

《信号检测与估计》是通信、电子工程等有关学科中本科生培养的一门专业技术课程。目前,在该课程的设置中存在明显的理论和实践相脱节的问题,使学生在学习后不能将课程的基本理论运用到具体实践中。文中针对该问题展开讨论,并提出了课程设置改革的构想。     

High-pressure polymorph of TiO2-II from the Xiuyan crater of China

Abundant TiO2-II, a high-pressure polymorph of titanium dioxide, was found in the gneiss fragments of impact-produced breccias from the Xiuyan crater. Rutile in the gneiss was severely fragmented and fine-grained clasts less than 2 ~tm in size had been transformed to TiO2-II. Irregular thin layered TiO2-II is also observed in coarse-grained ruffle fragments, where the TiO2-II layers distributes along fractures and cracks in rutile, About 30 percent of rutile in the gneiss had been transformed to TiO2-II. Fine grains of TiO2-II display light bluish grey to light yellow brown in plane-polarized reflected light. Crystallographic investigation shows that TiO2-II has an orthorhombic structure with space group Pbcn. The cell parameters are a=4.543（1）/~, b=5.491（9）/~ and c=4.895（2） ,~. Its empirical formula calculated on the basis of two oxygen atoms can be written as （Tio.985Feo.oosNbo.oor- Si0.003Zr0.0Ol）l.0O302, or simply formula TiO2. According to the shock effects of quartz and feldspars, the peak shock pressure and post-shock temperature in the TiO2-II-bearing gneiss are estimated to be between 35 and 43 GPa and 300-900~C, respectively. The finding of TiO2-II in the shock-metamorphosed gneiss provides another mineral physics evidence for shock origin of the Xiuyan crater.     

Analysis of deep-layer and bottom circulations in the South China Sea based on eight quasi-global ocean model outputs

This study is a preliminary analysis of the South China Sea (SCS) deep circulations using eight quasi-global high-resolution ocean model outputs. The goal is to assess models’ ability to simulate these deep circulations. The analysis reveals that models’ deep temperatures are colder than the observations in the World Ocean Atlas, while most models’ deep salinity values are higher than the observations, indicating models’ deep water is generally colder and saltier than the reality. Moreover, there are long-term trends in both temperature and salinity simulations. The Luzon Strait transport below 1500 m is 0.36 Sv when averaged for all models, smaller compared with the observation, which is about 2.5 Sv. Four assimilated models and one unassimilated (OCCAM) display that the Luzon deep-layer overflow reaches its minimum in spring and its maximum in winter. The vertically integrated streamfunctions below 2400 m from these models show a deep cyclonic circulation in the SCS on a large scale, but the pattern is different from the diagnostic streamfunction from the U.S Navy Generalized Digital Environment Model (GDEM-Version 3.0, GDEMv3). The meridional overturning structure above 1000 m is similar in all models, but the spatial distribution and intensity below 1500 m are quite different from model to model. Moreover, the meridional overturning below 2400 m in these models is weaker than that of the GDEMv3, which indicates a deep vertical mixing process in these models is biased weak. Based on the above evaluation, this paper discusses the impacts of T/S initial value, topography, and mixing scheme on the SCS deep circulations, which may provide a reference for future model improvement.