外汇汇率时间序列静态属性的抽取

为了能够使用现有的数据挖掘技术(例如粗糙集)对外汇汇率时间序列进行数据挖掘,必须从外汇汇率时间序列数据中抽取决定时间序列行为发展趋势的静态属性.针对外汇汇率时间序列的特殊性,给出了时间序列静态属性抽取技术的几个关键步骤,完成了从外汇汇率时间序列中抽取出静态属性,最后利用这些静态属性组成的数据库,实现了对外汇汇率时间序列比较准确的预测.     

引航员与船长间信息交流方式研究

引航员与船长之间在引航过程中的信息交流是至关重要的,它是达到安全引航的必要手段之一。以前,引航员上驾驶台后利用短暂的车、舵命令来了解船舶性能,与船长交流很少。事实上,他们之间各怀特长,引而不发,这给应急状态时的协同操作带来安全隐患。为使引航工作的安全更有保障,目前上海港引航管理站推出《船长/引航员信息交流卡》突出强调了信息交流在引航工作中的重要性。     

地下工程注浆技术研究新进展

注浆是土木、水利和矿山等工程建设中重要的防渗和加固技术。文章基于国内外注浆技术研究文献,总结了水泥等颗粒性浆液的“渗滤效应”及“黏度时空变异性”等理论研究成果,论述了非水反应高聚物、CW环氧树脂和微生物菌液等注浆新材料的应用现状及发展前景,介绍了细观力学数值模拟研究的突破性进展,可为地下工程注浆技术发展提供借鉴和启发作用。     

酚醛树脂复合材料在轨道交通车辆上的应用

介绍了酚醛树脂复合材料试制的主要原材料、主要设备及仪器、试制流程及测试标准。详细阐述了酚醛树脂复合材料的氧指数、燃烧性能、机械性能、低密度等性能。分析了热压时间、热压温度及生产工艺对酚醛树脂复合材料性能的影响。试验证明,酚醛树脂产品的性能较为优良:热压时间控制在1.1~1.4 h时,复合材料的表面性能良好;热压温度为80~100℃时,可以得到表面质量细腻均匀的复合材料;适当调整生产工艺,可以提高酚醛树脂的产品质量、降低生产成本。     

基于DDE技术实现Matlab与InTouch通讯研究

为了实现Matlab与InTouch之间直接通讯,分别介绍了Matlab软件和InTouch软件所提供的DDE接口,并在Matlab环境下,编写了基于DDE技术的M文件和S函数,这两种方法首次实现了Matlab和In-Touch之间的直接通讯。并解决了利用第三方软件进行接口编程的难题。通过实例证明了这种方法具有编程简单,实现方便等优点,并且支持多输入多输出模型的数据交换。     

SETBOC协议分析及其再改进方案

基于单向身份认证技术的安全电子交易协议SETBOC(Secure E lectron ic Transation Based onOne-way Certification)具有效率高,易实现的优点,分析了SETBOC改进方案的优点和不足。在保留原协议及其改进协议优点的基础上,提出再改进方案,使SETBOC协议满足非数字商品交易的原子性。再改进后的协议保证了商家与顾客的交易更加公平。     

基于软件无线电的船用VDES调制解调的研究

船舶数据交换量的增加导致现有的船用自动识别系统(AIS)87B/88B VHF通信信道堵塞严重,数据的完整性传输受到现实的考验.为解决严峻的通信信道压力,甚高频数据交换系统(VDES)应运而生.文章基于软件无线电(SDR)技术,搭建基于Gnuradio软件及2块HackRFOne硬件的软件无线电开发平台,进行16位正交...     

Dynamics of inorganic nutrient species in the Bohai seawaters

Within the frame of a Sino-German Joint Research Program, two cruises of “R/V Dong Fang Hong 2” were carried out in September–October 1998 and April–May 1999, respectively, to understand the dynamics of nutrients in the Bohai. Nutrient species (NO₃⁻, NO₂⁻, NH₄⁺, PO₄³⁻ and SiO₃²⁻) are determined colorimetrically on board for five anchor and 30 grid stations. In situ incubation experiments are performed to determine planktonic nutrient uptake and benthic exchange flux. Nutrient concentrations display short-term variability and seasonal change in the Bohai, with higher levels in shallow coastal waters than in the Central Bohai. The influence of riverine discharge on nutrient levels can be seen from salinity isopleths, nutrient distribution and species ratios. Near-bottom (nb) waters have similar nutrient concentrations as to the surface waters in the Central Bohai, whereas stratification takes place in the Bohai Strait and North Yellow Sea. In situ incubation experiments provide evidence that the uptake ratio (i.e. N, P) by phytoplankton is proportional to the ratios among nutrient species in ambient waters. Based on the data of this study and previously publications, a preliminary estimate of nutrient budgets via riverine input and atmospheric deposition is established. The results indicate that atmospheric deposition gains importance over rivers in delivering nutrients into the Bohai and sustain the new production, following recent decrease in riverine inflow caused by drought periods in North China and damming practices. A historical review of nutrient data indicates that concentrations of nitrogen increase and phosphorus and silica decrease in the Central Bohai over last 40 years. This potentially has an important influence on the health of ecosystem in Bohai (e.g. food web and community structure), though further study is needed to examine the scenario in more detail.     

Application of new parameterizations of gas transfer velocity and their impact on regional and global marine CO2 budgets

One of the dominant sources of uncertainty in the calculation of air–sea flux of carbon dioxide on a global scale originates from the various parameterizations of the gas transfer velocity, k, that are in use. Whilst it is undisputed that most of these parameterizations have shortcomings and neglect processes which influence air–sea gas exchange and do not scale with wind speed alone, there is no general agreement about their relative accuracy.The most widely used parameterizations are based on non-linear functions of wind speed and, to a lesser extent, on sea surface temperature and salinity. Processes such as surface film damping and whitecapping are known to have an effect on air–sea exchange. More recently published parameterizations use friction velocity, sea surface roughness, and significant wave height. These new parameters can account to some extent for processes such as film damping and whitecapping and could potentially explain the spread of wind-speed based transfer velocities published in the literature.We combine some of the principles of two recently published k parameterizations [Glover, D.M., Frew, N.M., McCue, S.J. and Bock, E.J., 2002. A multiyear time series of global gas transfer velocity from the TOPEX dual frequency, normalized radar backscatter algorithm. In: Donelan, M.A., Drennan, W.M., Saltzman, E.S., and Wanninkhof, R. (Eds.), Gas Transfer at Water Surfaces, Geophys. Monograph 127. AGU,Washington, DC, 325–331; Woolf, D.K., 2005. Parameterization of gas transfer velocities and sea-state dependent wave breaking. Tellus, 57B: 87–94] to calculate k as the sum of a linear function of total mean square slope of the sea surface and a wave breaking parameter. This separates contributions from direct and bubble-mediated gas transfer as suggested by Woolf [Woolf, D.K., 2005. Parameterization of gas transfer velocities and sea-state dependent wave breaking. Tellus, 57B: 87–94] and allows us to quantify contributions from these two processes independently.We then apply our parameterization to a monthly TOPEX altimeter gridded 1.5° × 1.5° data set and compare our results to transfer velocities calculated using the popular wind-based k parameterizations by Wanninkhof [Wanninkhof, R., 1992. Relationship between wind speed and gas exchange over the ocean. J. Geophys. Res., 97: 7373–7382.] and Wanninkhof and McGillis [Wanninkhof, R. and McGillis, W., 1999. A cubic relationship between air−sea CO2 exchange and wind speed. Geophys. Res. Lett., 26(13): 1889–1892]. We show that despite good agreement of the globally averaged transfer velocities, global and regional fluxes differ by up to 100%. These discrepancies are a result of different spatio-temporal distributions of the processes involved in the parameterizations of k, indicating the importance of wave field parameters and a need for further validation.     

钦州湾湾口填海对茅尾海水交换能力的影响

以溶解态的保守物质作为示踪剂,建立茅尾海水交换平面二维数学模型,采用开边界污染物浓度梯度与内侧一致假定考虑了边界污染物回归,计算分析了钦州湾湾口两侧大范围填海工程对茅尾海纳潮量和水体半交换周期的影响情况。研究表明：龙门海峡通道顺畅是维持茅尾海纳潮量的关键因素,湾口宽度保持9.4 km以上茅尾海内纳潮量和水体半交换周期基本不受湾口填海工程影响。