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。     

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.     

不同倍性(2×、3×、4×)鸭梨基因组DNA甲基化水平与模式分析

以鸭梨(Pyrus.bretschneideri Rehd.cv.‘Yali')多倍体(2×、3×、4×)为材料,应用甲基化敏感扩增多态性(methylation sensitive amplified polymorphism,MSAP)技术研究不同倍性鸭梨基因组DNA甲基化水平及模式变化.共筛选22对引物,平均每对引物产生约50条带,统计100～500 bp的扩增带,共计954个位点.分析表明:鸭梨2×、3×、4×分别检测到831、886、852个位点,发生甲基化位点分别占15.5%、20.0%、16.8%,其中全甲基化占9.7%、11.9%、9.7%.分析这些位点甲基化模式表明:甲基化模式在三个倍性间类型相同的占所检测位点的69.2%,仅两种倍性相同的为25.4%,各不相同的占5.5%,其中三倍体41.4%甲基化位点发生改变,显示出独特的DNA甲基化特点.     

一维p-Biharmonic方程非零解的存在性

利用一维p-Biharmonic方程在Navier边值条件下特征值问题的相关结果,Leray-Schauder度理论以及标准分支定理讨论了一维p-Biharmonic方程在Navier边值条件下非零解的存在性问题.     

峨眉地幔热柱活动与贵州西部二叠系煤的形成环境研究

晚二叠世乐平期,最为强烈、规模最大的一次峨眉地幔热柱强烈活动在贵州西部形成西北高、东南低的古地理格局.沉积相带由早二叠世的近东西向变为晚二叠世北东向排布.沉积相带由西向东,由陆相渐变为海陆交替相,最后变为海相环境.在贵州西北部的威宁一带形成陆相沉积环境.遵义至安顺一线以西的黔西和黔西南地区,属于海陆交替的陆地边缘相区,...