用场发射涨落法研究原子在金属单晶面上的表面扩散

本文介绍了用场发射涨落法研究吸附原子(或分子)在金属单晶面上表面迁移的原理、实验装置和方法以及所取得的新的研究结果。这些研究结果包括:吸附的气体(H_2,O_2,CO等)在W(110)面上的表面扩散;吸附的气体(H_2)在Ni(100)面上的表面扩散;在较高温度时钨台阶表面上钨原子的表面自扩散和热租糙化过程的研究等。     

四方晶系下钕离子的基态分裂

采用点电荷晶场模型,通过模拟四方晶系化合物NdCuAs2和Nd2Ge2In的磁化率倒数-温度曲线,得到了Nd3+的各级分裂能和相应波函数,并分析了晶场效应对化合物磁性质的影响.结果表明,Kramers离子Nd3+的十重简并基态4I9/2在晶场效应的作用下分裂为5个双态,计算结果与实验吻合得较好.     

一种基于FPGA快速进位链的时间数字转换电路

设计了一种基于FPGA快速进位链的时间-数字转换电路.该电路采用延迟内插技术,引入双链结构消除建立/保持时间对寄存器阵列输出结果的影响,并采用半周期平均延迟测试法,在Xilinx Virtex-4芯片上实测获得了59.19ps的分辨率.该电路采用使能控制模块将寄存器阵列输出结果的锁定时间控制在一个时钟周期内.使用FPGA Editor软件对该电路中单级延迟宏单元进行配置,并利用用户约束文件替代传统的手工布局布线,使得电路具有可移植性.此外,利用该电路对实测芯片中的CLB组合开关参数进行了测试,结果满足数据手册中提供的参数值的范围.     

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。     

Effective College English Vocabulary Teaching

There are over two million modern English words, thus English becomes a language with the largest vocabulary in the world. Moreover, English vocabulary is constantly being renewed and enlarged with the development of the society and advancement of science and technology. So vocabulary development becomes language learners’ top priority. Unfortunately, learning English words by rote can’t guarantee that students will have a large vocabulary, let alone enable students to make practical use of the words they h...     

基于FPGA的IP仿真验证平台

IP（集成电路知识产权芯核）的仿真和硬件验证是IP开发中不可缺少的环节．文中基于FPGA（现场可编程门阵列）开发了一个IP仿真验证平台,并使用PCI（外部设备互连）总线来测试IP．用户只要将自已设计的IP插入所开发的仿真验证平台,就可以方便地对IP进行测试．文中还对所设计的平台进行了软件仿真,以验证其功能,并在载有Xilinx Spartan-3 600E FPGA的PCI插卡上进行上板调试．结果表明,所建立的基于FPGA的IP仿真验证平台可以对IP进行有效的仿真和验证,并具有良好的稳定性和实用价值．     

Re-situating fieldwork and re-narrating disciplinary history in global mega-geomorphology

In 1985, more than thirty geomorphologists, planetary scientists, and remote sensing specialists gathered at a conference center in Oracle, Arizona, to discuss an emerging area of research that they called “mega-geomorphology.” Building on a conference of the same name held in London in 1981, they argued that new techniques of remote sensing and insights emerging from the study of extraterrestrial planets had created opportunities for geomorphology to broaden its spatial and temporal scope. This new approach was, however, neither unproblematic nor uncontested. In the discussions around mega-geomorphology that took place in the mid-1980s, the perceived conflict between the use of remote-sensing techniques to observe phenomena on vast spatial scales, on one hand, and the disciplinary centrality of fieldwork and field experience to geomorphology, on the other, was a recurrent theme. In response, mega-geomorphologists attempted to re-situate fieldwork and re-narrate disciplinary histories in such a way as to make remote sensing and planetary science not only compatible with geomorphological traditions but also means of revitalizing them. Only partially successful, these attempts reveal that the process of adopting a planetary perspective in geomorphology, as in other earth sciences, was neither straightforward nor inevitable. They also show how the field and fieldwork could remain central to geomorphology while also being extensively revised in light of new technical possibilities and theoretical frameworks.     

东坪基岩气藏气水相对渗透率的确定方法

东坪基岩气藏储层岩性差异大,非均质性强.孔缝发育区岩石松散,无法钻取完整的岩芯,而致密带几乎不渗透,无法通过驱替实验获取相对渗透率曲线,这成为困扰气藏动态分析和开发指标计算的难题.基于水驱气藏物质平衡原理,建立了不依赖水侵量的储层含水饱和度计算方法,避免了水侵量计算方法中的不确定因素,提高了含水饱和度计算的准确性.建立...     

神木气田低渗致密储层特征与水平井开发评价

鄂尔多斯盆地东部神木气田是长庆气区目前增储上产的重要组成部分,系统研究其储层特征、空间叠置结构及水平井开发适用性对气田科学开发具有重要意义。实验分析表明,神木气田山西、太原组储层岩石类型主要为岩屑石英砂岩、岩屑砂岩及石英砂岩,孔隙类型以溶蚀孔、晶间孔及粒间孔为主,储层孔隙度分布于2.0%~10.0%,平均为6.6%,渗透率分布于0.10~1.00 mD,平均为0.83 mD,整体属低孔、致密砂岩储层。测试分析表明,孔隙度5.0%、渗透率0.10 mD、含气饱和度45%为有效储层物性下限标准。基于密井网解剖,将有效砂体空间结构类型划分为多层孤立分散型、垂向多期叠加型、侧向多期叠置型等3种。研究表明,神木气田不适合开展大规模水平井开发,可在有限地区进行局部式水平井部署。     

苏里格气田盒_8段沉积相及砂体展布特征

苏里格气田盒8段是重要含气层位。本次研究充分利用钻井岩心、录井和测井资料,对该地区沉积相和砂体展布进行分析。研究认为该段从盆地北部由北向南依次发育辫状河沉积相和毯式浅水辫状河三角洲相,辫状河沉积相包括河道亚相和洪泛沉积两种亚相,毯式浅水辫状河三角洲相包括三角洲平原亚相、三角洲前缘亚相、前三角洲亚相。对盒8段砂体展布进行研究表明,在平面上顺物源方向呈现出条带状的分布特征,厚度变化差异较大,但平面上分布较为连续。