铁磁-反铁磁双层系统低温内能

应用线性自旋波的理论导出铁磁－反铁磁双层系统的Ｈｅｉｓｅｎｂｅｒｇ模型哈密顿量,采用矩阵格林函数运动方程技术得到自旋波的色散关系,利用数值计算的方法得到铁磁－反铁磁双层的低温内能。     

铁磁材料的磁路图解法计算

用试探法计算无分支不均匀恒定磁通磁路的反面问题的计算相当繁琐。本文推导找出一种快捷准确求磁通的方法——图解法。     

电子荷质比测量实验的Matlab仿真

运用Matlab实现了对电子荷质比e/m测量过程的仿真,着重对电子在磁场中的运动轨迹以及磁聚焦现象进行可视化仿真,从而可用于提高本实验项目的教学效果。     

自制孔内摄像系统在钻孔施工中的应用

孔内摄像系统可以直接实时观察钻孔内部影像,能达到地质、测井、钻探无法做到的效果,在地质分析、钻探事故处理中起着非常重要的作用。本文从孔内摄像系统工作原理、工作流程、所用材料,制作过程、操作方法以及在实际施工中的应用加以叙述。     

磁控形状记忆合金伸缩作动器设计及参数分析

该文基于磁控形状记忆合金（MSMA）材料自主设计了一种磁控形状记忆合金伸缩作动器,并阐述其原理。通过建立有限元模型,并对MSMA相对空气导磁率、导磁片的相对导磁率及电流等参数进行了分析。研究表明：当MSMA相对空气导磁率为30、电流大小为3 A时,MSMA棒中心线磁场的均匀性较好;而导磁片的相对导磁率对其均匀性影响较小。设计出了一种新型磁控形状记忆合金伸缩作动器,达到了从理论上充分掌握MSMA棒轴向磁场强度及均匀性,并间接地保证了磁控形状记忆合金伸缩作动器具有较优的控制力。     

Tb~(3+)-GMFX-AR体系的共振瑞利散射光谱特性及吉米沙星的测定

建立了一种新的检测吉米沙星的方法.在p H 5.5 HAc-Na Ac缓冲溶液中,吉米沙星(GMFX)作为配体与铽(Ⅲ)与形成配位阳离子,配位阳离子进一步与茜素红(AR)的阴离子反应形成1∶2∶1(Tb3+∶GMFX∶AR)三元离子缔合物,此时将出现新的共振瑞利散射(RRS)光谱,此RRS光谱分别在370 nm与590 nm波长形成两个散射峰.研究发现,370 nm时,在0.005~4.00μg·m L-1吉米沙星浓度范围内此体系的散射强度(ΔI)与吉米沙星浓度线性相关,该体系对吉米沙星的检出限(3σ)为14.5 ng·m L-1.该法简单、快速、重现度高,选择性好,在吉米沙星检测中具有应用价值.     

Magnetic characteristics and its environmental implications of core YSJD-86GC sediments from the southern South China Sea

Sediments of core YSJD-86GC （referred to as 86GC） collected from the southern South China Sea were selected for environmental magnetic studies. Combined with the published chronological framework, sediment magnetic properties were revealed for the study area since the MIS3 stage. The rock magnetic results indicate that low-coercivity magnetite is the main magnetic mineral within the sediments. Also, a certain amounts of hematite are present. The King plot and Day plot, which reflect the magnetic particle size, show that fine-grained pseudo-sin- gle-domain phase magnetic particles dominate the magnetic minerals in the sediments. Comparison of magnetic parameters and geochemical indicators show that magnetic properties of core 86GC sediments reflect a terrigenous input. Simultaneously, magnetic characteristics of the stud- ied sediment are influenced by the quantity of terrigenous sediment input, oxidation-reduction conditions of the provenance area, and the transportation environment and distance. Sea level fluctuation caused by global climate change was the main factor for variation in concentration of magnetic minerals and magnetic particle size of thestudied core sediments. Thus, variation of sediment magnetic properties in the study area can be used as an indirect indicator of sea level fluctuation.     

Observation of directional change of core field inside flux ropes within one reconnection diffusion region in the Earth’s magnetotail

Two consecutive magnetic flux ropes, separated by less than 30 s （△t 〈 30 s）, are observed within one magnetic reconnection diffusion region without strong guide field in the Earth＇s magnetotail by Cluster multispacecraft. The flux ropes are characterized by bipolar signatures of the south-north magnetic field component Bz accompanied with strong core magnetic field By, intense current J and density depletions inside of them. In spite of the small but non-trivial global scale negative guide field （-By）, there exists a directional change of the core fields of two flux ropes, i.e., -By for the first one, and ＋By for the second one. The directions of the core fields are the same as the ambient cross-tail magnetic field component （By） just outside of flux ropes. Therefore, we suggest that the core field of flux ropes is formed by compression of the local preexisting By and that the directional change of core field is due to the change of local preexisting By. Such a change in ambient By might be caused by some microscale physics.     

磁力偶合器在高压条件下的应用

文中介绍了磁力偶合器的工作原理和计算公式,特别强调了在高压液流条件下设计磁力偶合器应注意的一些问题,作者运用文中叙述的原理和公式,设计制造了几台高压条件下工作的磁力泵,工作性能良好稳定。     

关于地球同步卫星的双星系统

为了提高应用效率,在同一“定点”附近定位两颗地球同步卫星,形成一个双重系统,在该系统中两颗卫星的运动规律与单层情况有何区别,它们之间的相互距离如何变化,本文将对这些问题进行仔细讨论,并给出相应的结论。