5Gb/s单片集成GaAs MSM/PHEMT 850nm光接收机前端

采用0.5μm GaAs PHEMT工艺研制出了一种单片集成850nm光接收机前端,它包括金属-半导体-金属(MSM)光探测器和分布放大器.探测器光敏面积为50μm×50μm,电容为0.17pF,4V偏压下的暗电流小于17nA.分布放大器-3dB带宽接近20GHz,跨阻增益约46dBΩ;在50MHz～16GHz范围内,输入、输出电压驻波比均小于2;噪声系数在3.03～6.5 dB之间.光接收机前端在输入2.5和5Gb/s非归零伪随机二进制序列调制的光信号下,得到较为清晰的输出眼图.     

MATLAB中频谱分析单元的建模与应用

在许多应用场合中，常常需要对采集到的波形进行频谱分析，本文首先对MATLAB中的频谱分析模块进行了研究与分析，然后利用该软件构造了一种使用方便、功能较强具方便二次开发的频谱分忻模块。通过对两个例了进行的频谱分析，验证了该频谱分析模块是有效的。     

基于光谱复原的高光谱高空间遥感数据融合研究

文章提出了基于图像光谱复原的空间域遥感数据融合模型(SFSR),不仅大大提高了融合后各波段图像空间分辨率,而且保持融合后多光谱或成像光谱图像数据光谱特性不变.这对融合后遥感数据多光谱特性分析和基于光谱波形特征的计算机自动分类都是至关重要的.     

一种基于调制m序列的直接序列扩频信号调制方法

为提高直接序列扩频通信系统的频谱利用率,该文提出在m序列周期等于信息比特位宽整数倍情况下的直接序列扩频信号——调制m序列的信号调制与解调方法(m-DSSS).首先结合调制m序列相关性数值仿真结果验证m-DSSS信号捕获可行性,然后根据信息比特的排列组合情况,设计一种基于多通道的m-DSSS信号调制和解调方法,并对m-D...     

一种用C语言实现的工业流程图形压缩方法

针对过程控制的特点,提出了一种工业流程图形的压缩方法。该方法节省了大量图形文件的存储空间,在工控机上调用时,易于实现过程参数的定时采集和控制。     

Ge_xSi_1-x/Si异质结构的近红外吸收光谱测量

测量分析了采用 RRH/VLP—CVD 方法外延生长的 Ge_xSi_(1-x)/Si 异质结构中 Ge_xSi_(1-x)合金薄层的近红外吸收光谱。由谱线计算出 Ge_(0.15)Si_(0.85)与 Ge_(0.45)Si(0.55)合金层的带隙分别为1.02eV 和O.88eV,与相同组分的体合金一致。结果表明用红外吸收光谱测量研究异质结构薄层材料的能带结构及带隙是一种准确、简便的方法。     

DS／FH／TH混合扩频系统抗干扰性能的计算机模拟

在扩频通信中,抗干扰性能是评价扩频通信体制优劣的重要指标。本文研究DS/FH/TH混合扩频系统的抗干扰性能,建立了系统模型及计算机模拟方案,通过计算机模拟获得了在连续波、脉冲波多音干扰、部分带宽干扰、脉冲噪声干扰情况下的系统误码率曲线,具有一定的实用价值。     

EFFECT OF MICRITE CONTENT ON CALCITE CEMENTATION IN AN UPPER JURASSIC CARBONATE RESERVOIR,EASTERN SAUDI ARABIA

Cementation is a primary factor reducing the porosity of carbonate rocks. It is a challenge to accurately model cementation for reservoir quality prediction because cementation is often a syndepositional process. In addition, cementation requires fluid flow to transport chemical species for precipitation within the pore spaces in a sediment. The development of fully‐coupled depositional‐hydrogeochemical models for cementation prediction is desirable, but the parameters which control the extent of cementation need to be identified and evaluated. This study uses petrographic data from 583 carbonate samples from 15 wells in an Upper Jurassic (Kimmeridgian) reservoir at a giant oilfield in eastern Saudi Arabia to investigate the controlling effects of micrite content on cementation in carbonate rocks. The results indicate that the amount of cement decreases with increasing micrite content in the carbonate rocks analysed. In addition, a modified Houseknecht method has been developed to assess the relative fractions of porosity reduction in carbonate sediments due to compaction and cementation. The method highlights variations in depositional porosity for different rock textures and distinguishes microporosity from interparticle porosity. In the studied samples, the total porosity loss due to compaction and cementation is generally less than 45%, and samples lose more porosity due to compaction than cementation. The relative importance of compaction and cementation in reducing porosity is different for different rock textures: wackestones and mudstones lose porosity mostly as a result of compaction, while grainstones, mud‐lean packstones and packstones lose porosity due to both compaction and cementation.     

Crystal structure of poly(tetrafluoroethylene) homo- and copolymers in the high pressure phase

X-ray diffraction measurements are reported for 27°C, pressures to 5.2 GPa and concentrations of CF₃ units to 0.049 CF₃/CF₂. These show both orthorhombic and monoclinic structures to exist under high hydrostatic pressure. It is proposed that shear stresses generated at elastic inhomogeneities in the sample lead to the monoclinic phase. Energy calculations are consistent with this concept. They also indicate that conformational and rotational disorders raise the entropy of the high pressure phase III. Perfluoromethyl branches increase the volume/CF₂ of phase III more than that of the low pressure phase I. At high CF₃ concentrations and pressures, both phases become metrically hexagonal. The volume of transition becomes zero at a concentration near 0.05 CF₃/CF₂ and no transition is observed to a pressure of 5.2 GPa. There appears to be a critical point near 27°C, a CF₃ concentration of 0.05 and a pressure of 3.5 to 5 GPa.     

液—固磁场流态化模型及普遍化相图

本文考察了磁场流态化的基本特征,并结合实验分析了均匀磁场中液-固流态化模型参数的变化规律,对Ma 和 Kwauk 提出的指数模型作了补充,使之与经典流态化加以统一,并在此基础上获得了磁场流态化的普遍化关系图。完善后的模型可根据经典流态化的基础数据直接预示磁场作用下流态化的一些特征,模型计算结果与水-钢丸系统的实验数据吻合较好。