浅谈电能表的研制

在简述电能表专用芯片CS5463芯片性能的基础上,介绍了由89C55及CS5463构成的电能表的硬件和软件.     

抽象半线性发展方程正解的存在性

利用线性算子半群理论和抽象锥上的不动点定理 ,在合适的条件下建立了偏序Banach空间中半线性发展方程全局正解的存在性结果     

企业铁路运输调度指挥管理系统研究与设计

随着信息技术快速发展,越来越多的企业意识到了信息化建设的重要性,加大在了信息化上的投资,一系列主流的IT技术也应用到企业信息化建设中。本文结合企业铁路调度指挥系统的设计与实现,提出有关企业运输调度指挥信息化的设计思路和建议。     

SCP-2基因的表达调控研究进展

固醇转运蛋白(SCP-2)是广泛存在于脊椎动物和无脊椎动物中的非特异性脂转运蛋白.任何影响固醇转运蛋白基因表达的因素都会影响甾类激素的合成,进而影响生物体的发育.目前对该基因的转录调控研究较少,主要集中在哺乳动物.环境、激素、转录因子等对SCP-2基因的表达调控均有影响,对SCP-2基因作为害虫防治靶标的可能性进行了初步的探讨.C/EBP蛋白作为调控Sl SCPx基因表达的转录因子,可以调控Sl SCPx基因的表达.推测了C/EBP蛋白成为新的害虫防治的靶标的可能.     

基于STC89C54RD的RFID读卡器的设计与应用

提出并实现了一种基于STC89C54RD的RFID读卡器的设计方案,能运用在新能源电动汽车的交流充电桩上实现启动、停止控制和查询、扣费等功能.通过对应用了本设计的交流充电桩的功能测试,系统实现了预定的功能,并具有控制灵活、工作稳定、使用方便、适应环境能力强等特点.     

基于IFCM-GRA的空间多维热误差温度测点优化

热误差是精密、超精密加工中主要的误差源之一,热误差温度测点优化是热误差补偿的关键问题.在机床空间多维布置的大量温度测点之间存在多重相关性,从众多测点中选取特征点的优劣程度,将直接影响到热误差补偿效果.通过对温度测点间多重相关性及温度与热误差关系的综合分析,采用改进的模糊C-均值(IFCM)聚类算法对温度测点进行聚类,以减小类与类之间温度测点的相关性,且避免FCM算法对初始聚类中心敏感易局部收敛的缺点.对温度测点按灰色关联分析(GRA)中的灰色综合关联度进行排序,从变化量和变化率的角度综合反映温度与热误差的关系.采用IFCM-GRA对温度测点进行优化,提高了热误差模型的鲁棒性及准确性,使温度测点数量大幅度减少.在某型号精密卧式加工中心上进行实验,温度测点从17个减少到4个.在不同转速下,利用多元线性回归对优化出的温度测点与热误差建立模型,所建立模型均能很好地预测热误差变化情况,经对预测模型分析,轴向热误差由几十微米减小到5μm以内.     

上海鳞毛蕨属植物分布新记录

报道了上海分布新记录的四种鳞毛蕨属植物,即假红盖鳞毛蕨、桃花岛鳞毛蕨、轴鳞鳞毛蕨和高鳞毛蕨,并附有新记录种的特征照片;对新记录种及其近缘种的分类特征进行了描述,对新记录种的地理分布进行了补充.凭证标本保存于中国科学院南京地质古生物研究所标本馆(NPA).     

面向对象的三维对流扩散问题有限元程序设计

根据三维对流扩散问题的有限元分析,采用面向对象的程序设计语言C ,建立向量类、矩阵类、单元类、结点类、材料类和有限元方法类等,实现三维对流扩散问题的有限元分析程序开发,对相关的对流扩散问题进行数值模拟.结果表明与用结构化语言开发的传统有限元程序相比,程序更易重用、维护、扩充,并且可以融入用C 编制的大型通用有限元科学和工程计算软件.     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.