一种新的有源换流晶闸管电流源PWM变频器

普通晶闸管电流源变频器(CSI)由于六拍换流存在着较大的谐波，且脉宽调制式(PWM)电流源逆变器一般需要具有反向电压关断能力的门极关断电路，这就限制了它的应用．该文提出一种采用一个门极可关断开关和六个晶闸管的新的PWM电流源逆变器，此电路通过有源换流来实现传统的晶闸管CSI的脉宽调制．文章阐述了这种变流装置的调制技术并给出仿真实验结果．该电路适合于高性能和大功率的应用场合．     

中断实验的设计及外部中断源扩展的实现

针对授课过程中学生对中断优先权以及中断屏蔽等概念不理解的情况设计了一款简单实用的由8031组成的中断实验系统．通过该实验，可以直观地看到中断、中断优先权、中断屏蔽、外中断源扩展的过程，使学生较容易地理解掌握单片机控制系统中中断的处理方法，提高了实验效果．     

我国植物源农药的研究进展

简述了我国植物源农药的资源研究现状，植物源杀虫剂、杀线虫剂、杀菌剂和抗病毒剂的研究进展及植物源农药今后的研究方向。     

一种电流求和型的低功耗Bandgap电压基准源

为满足标准P阱CMOS工艺要求 ,设计了一种新的电流求和型Bandgap电压基准电路 ,实现了相对于地的稳定电压输出 ,并且能提供多电压基准输出 .电路采用 0 6μmUMCP阱CMOS工艺验证 ,HSPICE模拟结果表明 :电路输出基准电压为 80 0mV ;在 - 40～ 85℃的温度变化范围内 ,电路温度系数仅为 1 4× 1 0 -6/℃ ;电源电压为 3 5V时 ,电路功耗低 ,消耗电流仅为 1 5 μA .该电路不需改变现有工艺 ,输出灵活 ,有望在多基准电压的低功耗系统中获得较广泛的应用     

原子吸收光谱法在我国海洋环境样品分析中的应用

综述原子吸收光谱法在海洋环境样品分析中的应用，通过参考近50篇相关文献，主要介绍了原子吸收光谱法在河口海区沉积物、海洋生物、海水和海洋大气等方面的具体应用。基本上反映了原子吸收光谱法在环境化学分析领域的最新应用，并阐明了独到的见解．因而具有一定的参考价值．     

Ethernet—PON QoS实现方案

以Ethernet为基础的无源光网络(Ethernet—PON)是未来实现带宽、多业务综合接入的重要技术手段，如何提供服务质量(QoS)保证是EPON接入的核心技术之一。首先分别介绍EPON技术和轮询算法、业务分级，然后对基于轮询算法和业务分级的动态带宽分配进行探讨，并对解决Ethernet-PON的QoS问题进行分析研究。     

Quaternary high-resolution opal record and its paleoproductivity implication at ODP Site 1143,southern South China Sea

The correlation of opal content and MAR with oxygen isotopic records of benthonic foraminifera at Site 1143, southern South China Sea indicates that,since about 900 ka,the increasing opal content and MAR during the interglacial periods is inferred to reflect the bigher surface productivity ,for the intensified summer monsoon during the interglacial periods would result in the enhanced upwelling and nutrient supply,Time-sequence spectral analyses of oxygen isotopic record ,opal content and MAR at intervals of 0-900 ka reveal that the changes of surface productivity were dominantly forced by the variations of the earth orbital cycles.     

Cryptomelane（KxMn8-xO16）： Natural active octahedral molecular sieve（OMS-2）

The Xiangtan manganese deposit (XTM) used to be considered a supergene oxide manganese ore in South China. We reported a new identification of the naturally outcropping cryptomelane by examining the physical, chemical and structural features of the XTM supergene oxide manganese ore. The MnO2 content was over 90%, K2O more than 3%, and water from 2.2%-3.1% which is similar to one in zeolite. The cell parameters of the cryptomelane were given as a0 = 0.9974 nm, b0 = 0.2863 nm, c0 = 0.9693 nm and β= 91.47°. There was a larger pseduotetragonal tunnel in the natural cryptomelane that was formed by [MnO6] octahedral double chains with aperture of 0.462×0.466 nm2, filled with K cations resulting in some Mn3+ substituting for Mn4+ to balance the negative charges of structure. The finding is important not only for prospecting manganese resources in South China, but also in application of octahedral molecular sieve of natural cryptomelane as that developed in the tetragonal molecular sieve of natural zeolite o     

东营凹陷沙三段-沙二下亚段T-R层序特征及成因

将东营凹陷古近系沙三段沙二下亚段划分为 3个三级层序 ,即沙三下层序 (SSⅠ )、沙三中层序 (SSⅡ )和沙三上沙二下层序 (SSⅢ )。SSⅠ和SSⅡ层序由湖进体系域和湖退体系域组成T R旋回 ,其特征是代表层序边界的不整合分布局限 ,湖进体系域厚度小 ,主要为细粒沉积物 ,退积式叠加 ;湖退体系域较厚 ,由进积式叠加的砂岩、砾岩和泥岩组成。T R层序的形成主要是由于层序形成早期的构造沉降和气候起主导作用 ,其基底快速沉降 ,湖水供应充分 ,湖平面快速上升。在层序形成晚期 ,沉积物供给和气候起主导作用 ,沉积物供给多 ,快速向前推进 ,湖平面下降。构造沉降和沉积物供给因素对层序控制作用的转换促使其形成层序和体系域的边界。T R层序与三分层序之间的转换是由于层序形成的不同阶段的主控因素不同而引起的     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.