DC-AC型非接触电能传输系统变换器设计

提出了适用于DC-AC型非接触电能传输(CPT)系统的新型电路拓扑,并采用不对称DC-AC变换器实现了该新型拓扑。该拓扑简化了DC-AC型CPT系统的电路结构,简化了和系统的控制方式,减少了次级回路电能变换的损耗,提高了整体系统的效率和功率密度。介绍了采用该变换器的电路拓扑和控制策略,对采用该变换器后的CPT系统进行了建模,并在此基础上对系统进行仿真研究,给出了实验结果,对分析和仿真结果进行了验证。     

喷雾干燥-碳热还原法制备介孔球形LiFePO4/C正极材料

以聚乙二醇(PEG)为辅助模板剂和碳源,以廉价的三价铁为铁源,采用喷雾干燥-碳热还原法制备了LiFePO4/C正极材料,并对该材料的微观结构及PEG添加量、焙烧温度等对材料结构和性能的影响进行了表征和研究.结果表明:制得的LiFePO4/C材料呈介孔结构,具有漂亮的差级球状形貌、高的比表面积和容量、优异的循环性;PEG...     

微纳传动系统的BP神经网络非线性控制

对微纳传动系统的动态特性进行了分析,将微纳定位平台简化成等效弹簧质量阻尼模型,应用拉格朗日方法,建立了定位平台的动力学模型。结合压电陶瓷驱动器(PZT)的电容特性,推导了微纳传动系统的总传递函数。利用BP神经网络的自学习、自适应及非线性逼近功能,对该微纳传动系统的PID参数进行在线自整定。结合PID控制简单、实现容易与鲁棒性强的优点,设计了BP神经网络PID(BPNN-PID)控制器,与传统PID控制相比,实现了更高的控制精度和更短的稳态时间,满足了微纳传动系统高精度与快速响应的要求。     

蜂蜜中多种有机磷农药残留的液相色谱串联质谱检测

针对敌百虫、敌敌畏和蝇毒磷为常用的防治蜜蜂天敌或虫害的有机磷农药杀虫剂,易在蜂蜜中产生残留,建立了蜂蜜中敌百虫、敌敌畏和蝇毒磷残留的液相色谱串联质谱(LC-MS/MS)同时测定方法。蜂蜜样品经乙酸乙酯提取、浓缩,用甲醇溶解残渣,液相色谱(LC)分离,电喷雾(ESI)-MS/MS多反应监测(MRM)模式检测,外标基体曲线定量。3种有机磷农药在20～500μg/L范围内线性响应良好,相关系数均大于0.994;获得的检出限均为0.1μg/kg,定量限均为4μg/kg。在加标浓度为10～40μg/kg范围内,平均回收率为78.5%～96.8%,相对标准偏差为9.1%～13.1%。     

干线协调交叉口多相公交信号优先控制策略

针对干线协调交叉口多个相位有公交车到达的情况,为降低公交车延误,建立了以不破坏协调绿波带为前提的多相位公交优先控制策略.在该策略中,提出了“就近原则”以解决多个相位的公交优先申请冲突,对公交优先级别进行排序,并建立了多相位公交优先控制流程;考虑最高优先级别公交车的不同相位属性,采用绿灯延长和绿灯提前起亮两种优先方式,分...     

SOC设计中多bits数据跨时钟域的解决方法

在SOC(System On Chip)设计中,随着数字系统复杂性的提高,系统芯片中集成了越来越多的模块,这些模块通常工作在不同的时钟频率下.各控制器或者模块之间进行数据访问时,需要在将多bits数据同步到不同的时钟下.从跨时钟域时异步信号带来的亚稳态问题及其造成的影响,提出了包括握手信号和FIFO等针对不同的异步信号传输进行不同的跨时钟设计.     

基于QIM的数字图像水印技术研究

笔者提出了一种在DCT域里利用量化索引调制嵌入水印和数字签名的算法.从原始图像中提取一定的特征作为其唯一表征图像的数字签名.在DCT域中,根据数字签名和水印信息进行正负调制,实现水印的嵌入,同时也嵌入丁表征图像的数字签名.在确保了视觉质量和嵌入容量的前提下,得到了良好的水印性能,并且在鲁棒性上经受住了一系列常见的攻击,同时实现了抗拷贝攻击的目的.     

Learning from nature: Fabrication of colloidal PCs with controllable wettability

Colloidal photonic crystals (PCs) with desired wettabilities are of particular importance in various applications. Inspired by biological PCs, such as those of butterfly wings and peacock feathers, which all have evolved to have specific wettability, Professor Song Yanlin and his group in the Laboratory of New Materials, Institute of Chemistry, Chinese Academy of Sciences developed unique approaches to engineer colloidal PCs with desired wettability, based on the well-designed building blocks of latex particles. The range of wettability of these col- loidal PC films could be tailored from superhydrophobicity to superhydrophilicity and even superoleophobicity, by varying the surface     

Optimization of flue gas turbulent heat transfer with condensation in a tube

Conservation equations for sensible and latent entransy are established for flue gas turbulent heat transfer with condensation in a tube, and the entransy dissipation expression is deduced. The field synergy equation is obtained on the basis of the extremum entransy dissipation principle for flue gas turbulent heat transfer with condensation. The optimal velocity field is numerically obtained by solving the field synergy equation. The results show that the optimal velocity field contains multiple longitudinal vortices near the tube surface. These improve the synergy not only between the velocity and temperature fields but also between the velocity and vapor concentration fields. Therefore, the turbulent heat and mass transfers are significantly enhanced.     

Molybdenum isotopic composition as a tracer for low-medium temperature hydrothermal ore-forming systems: A case study on the Dajiangping pyrite deposit,western Guangdong Province,China

Little is known about the range or controls on the molybdenum isotopic composition of low-medium temperature hydrothermal ore-forming systems. We present molybdenum isotope data from 12 hydrothermal syndepositional silicalite and carbonaceous slate samples from the Dajiangping pyrite deposit in western Guangdong Province, South China. The δ ^97/95 Mo values from Orebody III range from −0.02‰ to 0.29‰, with an average of 0.18‰. In contrast, the composition values from Orebody IV display a larger variation from −0.70‰ to 0.62‰. However, the five samples from the main ore bed all show strong negative values. This indicates that the significant variation in molybdenum isotopic composition supports different hydrothermal ore-forming metallogenesis and a metallogenic environment between the two orebodies. Orebody III is likely to have been deposited from submarine exhalative hydrothermal fluids under a relatively strong reducing environment and Orebody IV may have also been influenced by hydrothermal superimposition in a more oxidized disequilibrium condition. In addition, the δ ^97/95 Mo values of Orebody IV are clearly negative, together with the values increasing stratigraphically upward in the ore beds, suggesting that the metallogenic environment of Orebody IV is different from the open oceanic systems. There might be dynamic fractionation in this restricted environment. Therefore, the molybdenum isotope can be used as an effective tracer for the ore-forming fluid and metallogenic environment.