基于电源电流和输出电压的模拟电路故障模型研究

基于模拟电路电源电流和输出电压的协同分析,研究了复数域的故障建模方法,提出了一种2D故障模型的数学表达式,该模型为复平面上的一簇圆轨迹。为了扩大故障轨迹之间的距离,在相同测量精度和元件容差条件下提高故障检测率和隔离率,进一步提出了3D复数空间的优化故障模型。两种故障模型都极大简化了测点选择算法和模拟故障状态仿真的复杂度,理论上对模拟电路单故障的覆盖率为100%。基于滤波器电路的实验仿真结果验证了两种故障模型的有效性。     

隔离式协议转换器在压变并行温补系统上的研发与应用

文章提出隔离式协议转换器在压力变送器并行温压补偿系统上的研发与应用,其目的是替换现存以HART总线[1]为基础的并行温压补偿系统的补偿电路,进而简化了补偿电路,提高了主站与工位采集板之间的通讯速率,使系统的维护和维修简单,以及令PCI总线驱动控制PIO数字I/O电路[2]完全的独立出来,只用于温压补偿中气路的切换选择控制;隔离式协议转换器是一款自主研发、自拟协议的独立模块,经压力变送器生产企业的应用与验证,该研发成果能够较好地解决现在温压补偿系统存在的问题,同时易移植于其它温压补偿系统上,并满足压力变送器生产客户的需求。     

多芯Bi2223／Ag带材30K温区的临界电流密度和交流损耗

本文研究了３０Ｋ温区和工频下８１芯Ｂｉ２２２３／Ａｇ带材的临界电流特性和没背场下的交流损耗，临界电流是用ＳＱＵＩＤ磁化法和标准四引法测量；交流损耗理在样品通以正弦电流情况下采用电测法进行测量，结果发现交流损耗随背场的增加而增大，同时与频率的关系是非线性的，并且偏离基于Ｂｅａｎ模型所预言的结果；表明３０Ｋ温区多芯带材Ａｇ基中的涡流损耗的芯间的耦合损耗不可忽略。     

边界条件对磁性Ising系统相图的影响

本文应用Ｍｏｎｔｅｃａｒｌｏ方法求得不同边界条件下铁磁平方点阵Ｉｓｉｎｇ模型的相图，利用有限尺寸的标度理论，得到其相应的相变温度，并同周期性边界条件下的结果作了比较，同时用ＭｏｎｔｅＣａｒｌｏ方法观察了不同边界条件下的动力学过程     

金属颗粒薄膜巨磁电阻效应的影响因素

研究金属颗粒薄膜的颗粒尺寸、磁性组分等对巨磁电阻效应的影响.在自由电子模型和自旋相关散射理论的基础上，计算了金属颗粒膜体系的电子平均散射势.在计算过程中将自旋相关项与宏观量相联系，得到了巨磁电阻效应与磁性成分比例、颗粒尺寸的关系.磁电阻效应的模拟曲线表明，增加磁性成分比例和减小磁性颗粒尺寸可增强颗粒膜的巨磁电阻效应. 关键词：     

加强型Bi-2212超导股线有限元拉伸性能分析

为探究加强型Bi-2212超导股线的力学性能以及不锈钢包带对超导股线力学性能的影响,运用Ansys软件建立加强型Bi-2212超导股线的三维模型,采用有限元分析方法,对其机械结构进行仿真,模拟高温高压热处理后轴向受拉形变量和应力应变分布情况。仿真结果显示,在同样施加100 N拉力的情况下,与超导原线（Bi-2212超导线）相比,密绕Ni₈₀Cr₂₀包带后的加强型Bi-2212超导股线轴向受拉形变程度减小,约10%;应力应变均降低,约30%。采用Ni₈₀Cr₂₀作为外包带制成的加强型Bi-2212超导股线力学性能显著,是未来超导线发展方向之一。     

基于液面旋转平移法的绝对检验技术研究

绝对检验作为一种光学元件高精度检测方法,其中的两平晶绝对检验无法精确测量平移过程中的倾斜误差,导致恢复的面形中二次项出现偏差.液面在位置变化前后能够保持水平,在旋转平移过程中不会产生倾斜误差.推导了平移过程中倾斜误差和恢复面形中离焦项的关系,并通过仿真分析加以验证,当不存在倾斜误差时,残差面PV值小于1nm.在300m...     

High Temperature Melting Curve of Basaltic Glass by Laser Flash Heating

Basalt is an igneous rock originating from the cooling and solidification of magma and covers approximately 70% of Earth’s surface. Basaltic glass melting in the deep Earth is a fundamental subject of research for understanding geophysics, geochemistry, and geodynamic processes. In this study, we design a laser flash heating system using two-dimensional, four-color multi-wavelength imaging radiometry to measure the basaltic glass melting temperature under high pressure conditions in diamond anvi...     

New experimental measurement of natSe(n, γ) cross section between 1 eV to 1 keV at the CSNS Back-n facility

The ⁷⁴Se is one of 35 p-nuclei, and ⁸²Se is a r-process only nucleus, and their (n, γ) cross sections are vital input parameters for nuclear astrophysics reaction network calculations. The neutron capture cross section in the resonance range of isotopes and even natural selenium samples has not been measured. Prompt γ-rays originating from neutron-induced capture events were detected by four C₆D₆ liquid scintillator detectors at the Back-n facility of China Spallation Neutron Source (CSNS). The pulse height weighting technique (PHWT) was used to analyze the data in the 1 eV to 100 keV region. The deduced neutron capture cross section was compared with ENDF/B-VIII.0, JEFF-3.2, and JENDL-4.0, and some differences were found. Resonance parameters were extracted by the R-matrix code SAMMY in the 1 eV-1 keV region. All the cross sections of ^natSe and resonance parameters are given in the datasets. The datasets are openly available at http://www.doi.org/10.11922/sciencedb.j00113.00019.     

Evolution of electrical conductivity and semiconductor to metal transition of iron oxides at extreme conditions

Iron oxides are widely found as ores in Earth's crust and are also important constituents of its interiors. Their polymorphism, composition changes, and electronic structures play essential roles in controlling the structure and geodynamic properties of the solid Earth. While all-natural occurring iron oxides are semiconductors or insulators at ambient pressure, they start to metalize under pressure. Here in this work, we review the electronic conductivity and metallization of iron oxides under high-pressure conditions found in Earth's lower mantle. We summarize that the metallization of iron oxides is generally controlled by the pressure-induced bandgap closure near the Fermi level. After metallization, they possess much higher electrical and thermal conductivity, which will facilitate the thermal convection, support a more stable and thicker D^$primeprime$ layer, and formulate Earth's magnetic field, all of which will constrain the large-scale dynamos of the mantle and core.