韩波博士简介

<正>韩波,男,1983年8月生,安徽颍上人。2007年毕业于华东师范大学电子系,获工学学士学位。2012年毕业于华东师范大学电子系(硕博连读),获工学博士学位,2012年至今在阜阳师范学院计算机与信息工程学院从事教学科研工作,2014年东南大学毫米波国家重点实验室客座研究。韩波博士主要从事微波毫米波片上元件建模与设计研究。内容主要涉及:异质结三极管     

大尺寸单晶金刚石同质连接技术

介绍了制备人造单晶金刚石的技术途径及发展现状,重点讨论并对比了几种化学气相沉积法(CVD)金刚石制备技术的优缺点,详细阐述了基于微波等离子体CVD (MPCVD)法的同质连接技术——一种突破晶体尺寸限制,实现大尺寸单晶金刚石的有效途径。通过该技术实现了英寸级单晶金刚石晶片的制备,并针对横向生长、界面质量及演化、三维结构连接控制等核心科学技术问题进行了分析和讨论,展望了其在尖端应用领域的发展前景。     

井下WPT技术机理研究

为解决井下无线传感器电池容量受限的问题,根据井下无线传感器带壮分布的特点,提出了井下无线运动充电的思想.构建充电系统模型,讨论了充电信道建模、接收微带天线设计、多天线协作三个方面的技术路线.本文在研究井下微波输能传输特性的基础上,探讨在低功率密度下,多天线协作的移动无线充电技术在井下运动式充电特性,使用这个技术对无线传感器节点充电,解决井下无线传感器网络能量补充问题,突破现有节点单纯依靠电池供电的局限.     

光与光基技术推动人类文明与进步

2015年是光和光基技术国际年,简称2015国际光年.联合国之所以做出这一决议,是基于光和光基技术对世界人民的生活以及全球社会多层面未来发展的重要性.希望通过各种宣传提高人们对于光科学技术的认识并加强这方面的教育,这对于世界各国应对可持续发展、能源、社区保健和提高生活质量的挑战至关重要.     

基于专利的难溶性含钾岩石生产钾肥技术分析

难溶性含钾岩石的开发和利用对提高我国钾肥产能，保障粮食生产安全有重要意义。该文围绕难溶性含钾岩石生产钾肥技术，通过专利数据库和专利分析系统，统计了本行业相关的专利数据，并对其进行了各种指标的分析，从而揭示了该技术领域中一些非常有价值的情报信息，为科研立项、课题选择、产品攻关、建立知识产权预警制度等提供一定参考。     

Hybrid SVM／HMM Method for Face Recognition

A face recognition system based on Support Vector Machine(SVM) and Hidden Markov Model (HMM) has been proposed. The powerful discriminative ability of SVM is combined with the temporal modeling ability of HMM. The output of SVM is moderated to be probability output, which replaces the Mixture of Gauss (MOG) in HMM. Wavelet transformation is used to extract observation vector, which reduces the data dimension and improves the robustness.The hybrid system is compared with pure HMM face recognition method based on ORL face database and Yale face database. Experiments results show that the hybrid method has better performance.     

Comparison of Drought-Resistance about Three Wild Rocky-Grasses

In this experiment, using the methods of drought-stress in the pot and PEG simulative drought-stress, three native rocky-slope grasses Pogonatherum panideum（Lam.） Hack, Erioophorum comosum nees and Cynodon dactylon cultivated in the pots were selected as materials to study their drought-resistance by analyzing the indexes such as the leaf area index, the drying roots accumulation, the holding water ability of leaf, the relative conductance of leaf, the soluble protein, chlorophyll. At the same time, by comparing with membership function value of each index, the order of each grass drought-resistance was decided. The results showed that the drought-resistance of Erioophorum comosum nees was stronger than Cynodon dactylon and drought-resistance of Cynodon dactylon was stronger than Pogonatherum panideum （Lam.） Hack. The purpose of the experimental results was to find theoretical foundations for selecting and cultivating native protecting-slope vegetations to adapt to rocky slopes.     

Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

反应气压对生长金刚石膜的影响

实验以CH3CH2OH和H2 为气源,用微波等离子体CVD法沉积金刚石膜,并用金相显微镜(×400)观察其沉积效果,X射线衍射仪表征其成膜质量,最后分析反应气压对金刚石膜的影响.