Fabrication and Properties of CoSm-Based Multilayer Thin Films

In recent years, SmCo series thin films have been found to be good candidates for fabricating integrated electromagnetic components and ultrahigh density magnetic recording media[1,2]. Up to now,intensive studies of such films have been carried out in order to obtain appropriate microstructure, crystallographic orientation and other properties. Substitution of Cu or Ni for Co in SmCo/Cr series films leads to a decrease of the saturation magnetization, magnetic switching volume, and to an increase of uniaxial anisotropy and coercivity[3-5].Various deposition conditions have also been investigated[6]. The large increase in coercivity for the annealed SmCo/Cr films is due to the growth of crystallitest[7,8]. In this article, we report a study of the deposition process,structure, and magnetic behavior of sputtered Sm (Co,Cu, Ti)/Cr series thin films.     

Growth of Magnetite Nanoparticles under Magnetic Fields

1 Introduction Over the past several years, the preparation and characterization ofnanoscale magnetic materials, especially one-dimensional (1D) nanostructure, have attracted much attention as the nanomaterials would allow investigating the fundamental aspects of magnetic-ordering phenomena in magnetic materials with reduced dimensions and could lead to new potential applications such as data storage technology[1-6].     

测定血小板衍生生长因子活性方法的改进

以BALB／C小鼠胚胎成纤维细胞(BALB／C3T3)作为靶细胞，经20mmol／L醋酸钠平衡后的CM—Sepharose(CMS)吸附过的胎牛血清作为基础培养血清，应用[3-(4，5-dimethylthi—azolyl)-2，5-diphenyhetrazolium bromide，MTT]方法测定血小板源生长因子(platelet—derived growth factor，PDGF)诱导细胞增殖的生物活性，结果表明，该方法具有良好的量效关系，且精确度、重现性均较高。     

机械合金化工艺对Fe-Ni合金显微结构的影响

对机械合金化制备的Fe-Ni粉体利用X射线衍射(XRD)进行分析，得到了不同Ni含量和不同球磨时间Fe-Ni纳米晶的XRD谱．实验表明，w(Ni)=10％和20％时，Ni溶入Fe晶格，分别在球磨20h和50h后形成单一的a(bcc)相；w(Ni)=50％时，其先后经历了γ(fcc)→←a(bcc)正逆转变，在球磨120h后最终形成单一γ(fcc)相．无论是a(bcc)相还是γ(fcc)相．它们的固溶度均比块体Fe-Ni合金显著提高．w(Ni)=35％时，则始终是两相共存．对试样的XRD谱采用3种不同的方法测定了Fe-Ni粉体的晶粒尺寸和显微畸变，发现经球磨20h后，不同Ni含量的粉体均呈纳米结构，并随球磨时间延长，Fe-Ni纳米晶的晶粒尺寸下降而显微畸变上升．     

纳米Ni-Al2O3金属陶瓷粉末热压致密化过程

采用粒径小于100 nm,金属Ni包覆Al2O3得到的纳米Ni-Al2O3化学包覆粉为原料,将Ni含量不同的几种纳米Ni-Al2O3(粒径约为38 nm)金属陶瓷复合粉末首先采取模压成形方式压制成直径为30 mm的圆片,然后放在石墨模具中在热压机上进行热压,研究热压(HP)温度和Ni含量对致密化过程的影响.研究结果表明:当Ni含量为20%和热压温度为1 400℃时,制品密度和显微硬度最高;在1 400℃热压2 h,Al2O3-Ni2O烧结体的相对密度最高,达到99.6%,Al2O3-Ni5的显微硬度HV达到1 690.9kg/mm2;随着Ni含量的增加,制品硬度降低,当Ni含量超过20%时,硬度降低非常显著,Ni含量为50%时HV降至1 316.7 kg/mm2;烧结体中Ni颗粒均匀分布在基体中,且大部分位于三角晶界处,有效地阻止了Al2O3基体晶粒的长大.     

几种石蒜属花卉观赏性状的灰色评价

以灰色关联度对14种石蒜属花卉的观赏性状进行了评价．结果表明石蒜(Lycoris radiata)的加权关联度Ri为最大(0．713 888)，即观赏效果最好，这与实际运用效果相符；其次是安徽石蒜(L．anhuiensis)，Ri=0．708 429；排在第三位的是长筒石蒜(L．longituba)，Ri=0.703032．其他由大到小次序为夏水仙(L.squamigera)、玫瑰石蒜(L．rosea)、陕西石蒜(L．shaanxiensis)、乳白石蒜(L．albiflora)、短蕊石蒜(L．caldwellii)、麦杆黄石蒜(L．straminea)、肉红石蒜(L．incornata)、中国石蒜(L．chinensis)、换锦花(L．sprengeri)、忽地笑(L．aurea)、江苏石蒜(L．houdyshelii)．从灰色关联度分析结果看，花形整齐、奇特(雄蕊长于花被片，花被片强烈皱缩反卷)，花色稀有和秋冬出叶的，灰色关联度大,14种石蒜均适合作地被，但以秋冬出叶、花葶较矮的种更为适宜，如石蒜、玫瑰石蒜、麦杆黄石蒜、江苏石蒜等。     

利用网络、多媒体手段建构高级英语教学模式

着重研究、分析如何利用网络等多媒体手段进行综合英语的课件制作和教学，并通过调查分析说明根据教学实际，在建构主义理论指导下利用网络等多媒体手段进行综合英语教学有利于培养出兼备语言能力和言语能力的人才。     

略论唐朝治桂政策实施的背景

唐朝以前，桂东地区的封建庄园经济。土地私有制已有所发展，而桂西地区大体上仍停留在前封建制阶段，社会经济相当落后，尤其是农业经济与桂东有着相当大的差距。唐朝统治者审时度势，根据当时广西社会发展的变化，调整了其治桂政策，在桂东地区设立正州正县，而在桂西地区则继续沿袭前代的的羁縻政策。     

Detection of the translational oscillations of the Earth''''s solid inner core based on the international superconducting gravimeter observations

Before about 100 years, the layered structures of the Earths body and the existence of the liquid core had been found, then the solid inner core and detailed structures in the interior of the Earth are demonstrated, it proves that the satisfied achievements had been obtained in recogni-tion of the Earths interior structures. In recent years, with the increasing requirements of the basic sciences and space techniques to geodynamics of the Earths interior, the theoretical study and practical de…     

Simple scaling relations in geodynamics： the role of pressure in mantle convection and plume formation

Scaling relations are important in extrapolating laboratory experiments to the Earth‘s mantle. In planetary interiors, compression becomes an important parameter and it is useful to explore scalings that involve volume. I use simple volume scaling relations that allow one to extrapolate laboratory experiments and upper mantle behavior, in a thermodynamically self-consistent way, to predict lower mantle behavior. The relations are similar to the quasi-har-monic approximation. Slabs and plates have characteristic dimensions of hundreds of kilometers and time constants of 100 million years, but the volume scalings predict order of magnitude higher values in the deep mantle. The scaling relations imply that the deep mantle is a sluggish system with ancient features. They imply irreversible chemical stratification and do not favor the plume hypothesis.