基于Fe基非晶薄带的宽线性GMI传感器

基于Fe76Si7.6B9.5p5C1.9非晶合金薄带的巨磁阻抗特性,研制了一种新型磁敏传感器.介绍了Fe76Si7.6B9.5P5C1.9非晶合金薄带的GMI特性及磁敏传感器的电路原理,并对磁敏传感器进行了性能测试.实验结果表明:该传感器的重复性好,迟滞误差小,线性范围广,并且在弱磁场作用下仍然可以保持良好的线性度,灵敏度为3.49mV/(A·m-1).     

低频脉冲磁场处理Fe73.5Cu1Nb3Si13.5B9非晶合金的磁致伸缩

用低频脉冲磁场处理Fe73.5Cu1Nb3Si13.5B9非晶合金试样,用透射电镜分析处理后样品的结构,用自制磁致伸缩测量仪测定处理前后样品的磁致伸缩系数。结果表明,低频脉冲磁场处理后的非晶合金Fe73.5Cu1Nb3Si13.5B9发生了纳米晶化,处理后非晶合金的磁致伸缩系数比原始样品减小很多,使非晶合金的软磁性能得到改善。     

Co_(66)Fe_4Mo_2Si_(16)B_(12)结构与磁性能的研究

采用铁芯测试仪测得合金样品的初始磁导率随温度的变化曲线,定出居里温度;用磁化强度小角旋转法测量非晶及晶化合金条带的饱和磁致伸缩系数λs;研究了不同温度退火后Co66Fe4Mo2Si16B12合金的磁性.结果表明:Co66Fe4Mo2Si16B12合金经退火后非晶相和剩余非晶相的居里温度随退火温度升高而提高;Co66Fe4Mo2Si16B12合金经高于500℃退火后磁性能变坏,是饱和磁致伸缩系数变大所致.     

非晶合金Fe73.5Cu1Nb3Si13.5B9磁致伸缩系数的测量

采用自制磁致伸缩测量系统,测量了非晶合金Fe73.5Cu1Nb3Si13.5B9的磁致伸缩系数.此测量系统的优点是性能稳定,精确度高(其灵敏度可达0.3×10-7),并且可以连续测量,直至得到饱和磁致伸缩系数λs和磁致伸缩曲线.     

基于非晶丝GMI效应的微磁探测器

非晶丝具有优良的软磁和近零磁滞特性,为设计出灵敏度高、输出线性范围宽的微磁探测器,通过分析非晶丝巨磁阻抗(Giant Magneto Impedance,GMI)效应影响因素和存在的问题,设计了特殊结构的磁敏感元件,解决了带负反馈电路传感器电路复杂和双线圈绕制困难的问题。同时设计了高频脉冲电流发生器、信号预处理电路和数字信号处理模块,共同构成微磁探测器。对传感器和探测器分别进行了实验。结果证明:该传感器在±3Oe磁场范围内具有良好的线性,传感器磁场灵敏度可达65mV/Oe,并具有良好的温度稳定性;探测器的磁场分辨率为50μOe,能够灵敏探测微小铁磁物体。     

CoFeBSiNb非晶合金带材纵向驱动巨磁阻抗效应研究

采用单辊快淬法制备了具有强非晶形成能力的Co63Fe4B22Si5,6Nb5非晶合金带材。利用HP4294A阻抗分析仪测量了经不同温度退火的Co基非晶合金带材在纵向驱动模式下的巨磁阻抗效应（GMI）．实验结果表明：材料经去应力退火后,其软磁性能得到了有效的改善,其中经580℃退火1h的Co基非晶薄带在475kHz电流驱动下的GMI比值可高达2400％,其灵敏度达114％／（A·m^-1）．     

热处理过程中Co基非晶丝的层间耦合作用对GMI效应的影响

用氢氟酸去掉Co69.20Fe4.16Si12.35B10.77Cr3.42Mo0.1非晶玻璃包裹丝的玻璃层,获得了高纯度的Co基非晶丝,再对非晶细丝在空气或氢气保护中进行了退火处理,研究了退火过程中退火温度和退火时间对Co基非晶丝巨磁阻抗效应(GMI)的影响.研究发现,随着退火温度升高和退火时间加长,Co基非晶丝巨磁阻抗表现出非单调且非对称的变化,灵敏度随着退火温度的升高和退火时间的加长表现为先增大后减小的行为.在退火温度为673K,退火时间为9h的条件下,磁阻抗的灵敏度最高,可达227%.分析指出氧化层和纳米晶芯层的耦合相互作用可能是Co基非晶丝软磁性能得到改善的主要原因.     

具有气敏涂层的GMF静态磁机耦合模型及实验研究

为实现超磁致伸缩薄膜(GMF)在微气体传感器领域的应用,需要研究其在气敏涂层条件下的磁致伸缩特性.以几何非线性弹性理论为基础,将磁致伸缩效应等效为GMF上体积力作用下的变形效应,建立了具有气敏涂层的悬臂梁式结构双层GMF低磁场下静态磁机耦合模型,解析了GMF悬臂梁末端的磁场与位移的数学关联.通过对双层薄膜TbDyFe/PI/SmFe和TbDyFe/Cu/SmFe进行试验,验证了磁场与位移数学关联的正确性.结果表明,曲线模型有较好的预测性,具有气敏涂层的GMF表现出更好的磁致伸缩效应.     

轻稀土Pr基立方Laves相超磁致伸缩材料的超高压合成及其磁弹性能研究

通过超高压退火方法,成功获得了轻稀土Pr基立方Laves相Pr(Fe_1-xGa_x)_2.35(x=0,0.06,0.12,0.17)超磁致伸缩合金材料,系统研究了其微结构、磁性转变以及磁致伸缩性能。实验结果表明,高压退火是合成轻稀土Pr基立方Laves磁致伸缩相结构的有效手段;适度的Fe过量可以在磁致伸缩相中引入软磁α-Fe相。热重分析表明随着Ga含量的增加,Pr(Fe_1-xGa_x)_2.35合金的居里温度呈现单调降低趋势。微量Ga掺杂(x=0.06)和α-Fe相的引入可以有效改善样品的软磁性能,使轻稀土Pr基立方Laves相合金在保持较大磁致伸缩响应的前提下,降低其磁弹响应滞后。本工作可为价格便宜、磁弹相应优异的轻稀土Pr基超磁致伸缩材料的开发提供实验和理论指导。     

基于纵向激励的铁基非晶带弱磁传感器研究

为研制高性能的弱磁传感器,通过纵向激励方式,使得铁基非晶带Fe78Si9B13具有高巨磁阻抗(GM I)效应。在传感器电路设计中,RC反相振荡电路与开关管构成脉冲信号发生电路;峰值检波电路、无源低通滤波电路与AD620差分运算电路构成信号调理电路;由双运放组成的V/I转换电路作为负反馈电路。对基于GM I效应的弱磁传感器的输出进行了试验标定与数据分析。测试结果表明:在磁场-210μT至210μT范围内,灵敏度为5.7 mV/μT、线性度为0.87%,重复性为0.63%,迟滞误差为±0.36%,达到了实际的弱磁场测试要求。     

Markedness and its Interpretation in Language Use

Language markedness is a common phenomenon in languages, and is reflected from hearing, vision and sense, i.e. the variation in the three aspects such as phonology, morphology and semantics. This paper focuses on the interpretation of markedness in language use following the three perspectives, i.e. pragmatic interpretation, psychological interpretation and cognitive interpretation, with an aim to define the function of markedness.     

Characterization of Ordovician carbonate reservoirs, southeastern Saskatchewan, Canada

The discovery of the prolific Ordovician Red River reservoirs in 1995 in southeastern Saskatchewan was the catalyst for extensive exploration activity which resulted in the discovery of more than 15 new Red River pools. The best yields of Red River production to date have been from dolomite reservoirs. Understanding the processes of dolomitization is, therefore, crucial for the prediction of the connectivity, spatial distribution and heterogeneity of dolomite reservoirs.The Red River reservoirs in the Midale area consist of 3～4 thin dolomitized zones, with a total thickness of about 20 m, which occur at the top of the Yeoman Formation. Two types of replacement dolomite were recognized in the Red River reservoir: dolomitized burrow infills and dolomitized host matrix. The spatial distribution of dolomite suggests that burrowing organisms played an important role in facilitating the fluid flow in the backfilled sediments. This resulted in penecontemporaneous dolomitization of burrow infills by normal seawater. The dolomite in the host matrix is interpreted as having occurred at shallow burial by evaporitic seawater during precipitation of Lake Almar anhydrite that immediately overlies the Yeoman Formation. However, the low δ18O values of dolomited burrow infills (-5.9‰～ -7.8‰, PDB) and matrix dolomites (-6.6‰～ -8.1‰, avg. -7.4‰ PDB) compared to the estimated values for the late Ordovician marine dolomite could be attributed to modification and alteration of dolomite at higher temperatures during deeper burial, which could also be responsible for its 87Sr/86Sr ratios (0.7084～0.7088) that are higher than suggested for the late Ordovician seawaters (0.7078～0.7080). The trace amounts of saddle dolomite cement in the Red River carbonates are probably related to "cannibalization" of earlier replacement dolomite during the chemical compaction.     

低渗透非均质砂岩油藏启动压力梯度研究

理论推导与室内实验相结合,建立了低渗透非均质砂岩油藏启动压力梯度确定方法。首先借助油藏流场与电场相似的原理,推导了非均质砂岩油藏启动压力梯度计算公式。其次基于稳定流实验方法,建立了非均质砂岩油藏启动压力梯度测试方法。结果表明:低渗透非均质砂岩油藏的启动压力梯度确定遵循两个等效原则。平面非均质油藏的启动压力梯度等于各级渗透率段的启动压力梯度关于长度的加权平均;纵向非均质油藏的启动压力梯度等于各渗透率层的启动压力梯度关于渗透率与渗流面积乘积的加权平均。研究成果可用于有效指导低渗透非均质砂岩油藏的合理井距确定,促进该类油藏的高效开发。     

On Tragic Consciousness In The Works By Ernest Hemingway

As an American modern novelist who were famous in the literary world, Hemingway was not a person who always followed the trend but a sharp observer. At the same time, he was a tragedy maestro, he paid great attention on existence, fate and end-result. The dramatis personae's tragedy of his works was an extreme limit by all means tragedy on the meaning of fearless challenge that failed. The beauty of tragedy was not produced on the destruction of life, but now this kind of value was in the impact activity. They performed for the reader about the tragedy on challenging for the limit and the death.     

A computer generator for randomly layered structures

AcomputergeneratorforrandomlylayeredstructuresYUJia shun1,2,HEZhen hua2(1.TheInstituteofGeologicalandNuclearSciences,NewZealand;2.StateKeyLaboratoryofOilandGasReservoirGeologyandExploitation,ChengduUniversityofTechnology,China)Abstract:Analgorithmisintrod…     

An Index mechanism for multi-scale view in spatial databases

There are numerous geometric objects stored in the spatial databases. An importance function in a spatial database is that users can browse the geometric objects as a map efficiently. Thus the spatial database should display the geometric objects users concern about swiftly onto the display window. This process includes two operations:retrieve data from database and then draw them onto screen. Accordingly, to improve the efficiency, we should try to reduce time of both retrieving object and displaying them. The former can be achieved with the aid of spatial index such as R-tree, the latter require to simplify the objects. Simplification means that objects are shown with sufficient but not with unnecessary detail which depend on the scale of browse. So the major problem is how to retrieve data at different detail level efficiently. This paper introduces the implementation of a multi-scale index in the spatial database SISP (Spatial Information Shared Platform) which is generalized from R-tree. The difference between the generalization and the R-tree lies on two facets: One is that every node and geometric object in the generalization is assigned with a importance value which denote the importance of them, and every vertex in the objects are assigned with a importance value,too. The importance value can be use to decide which data should be retrieve from disk in a query. The other difference is that geometric objects in the generalization are divided into one or more sub-blocks, and vertexes are total ordered by their importance value. With the help of the generalized R-tree, one can easily retrieve data at different detail levels.Some experiments are performed on real-life data to evaluate the performance of solutions that separately use normal spatial index and multi-scale spatial index. The results show that the solution using multi-scale index in SISP is satisfying.     

Achieving Unusual States of Matter Under High Pressure

正The periodicity of the elements and the non-reactivity of the inner-shell electrons are two related principles of chemistry,rooted in the atomic shell structure.Within compounds,Group I elements,for example,invariably assume the+1 oxidation state,and their chemical properties differ completely from those of the p-block elements.These general rules govern our understanding of chemical structures and reactions.Using first principles calcula-     

Exchange-Correlation and Electronic Excitation Energies from Pairing Matrix Fluctuations

We have developed an adiabatic connection to formulate the ground-state exchange-correlation energy in terms of pairing matrix linear fluctuations.This formulation of the exchange-correlation energy opens a new channel for density functional approximations based on the many-body perturbation theory.We illustrate the potential of such approaches with an approximation based on the particle-particle Random Phase Approximation(pp-RPA).This re-     

Density Functional Theory for the Response of Periodic Systems to Electric Fields Based on the Vector Potential Approach

正The electronic and nuclear(structural/vibrational)response of 1D-3D nanoscale systems to electric fields gives rise to a host of optical,mechanical,spectral,etc.properties that are of high theoretical and applied interest.Due to the computational difficulty of treating such large systems it is convenient to model them as infinite and periodic(at least,in first approximation).The fundamental theoretical/computational problem in doing so is that     

On the Thermodynamic Limit for Responses to Static Electromagnetic Fields

For molecular systems,the quantum-mechanical treatment of their responses to static electromagnetic fields usually employs a scalar-potential treatment of the electric field and a vector-potential treatment of the magnetic field.Although the potential for each field separately is associated with the choice of an(unphysical)origin,the precise choice of the origin for the electrostatic field has little consequences for the results.This is different for the