Fe—Mo合金的时效析出行为

用 X 射线、电子衍射及透射电镜观察等方法研究了 Fe-27Mo 及 Fe-16Mo 合金的时效析出行为.结果发现,在873～1453K 时效时.时效初期,两种合金中均有一种新的过渡相——R 相析出.随时效进行,过渡相 R 将向平衡相μ(1213～1453K)或 Laves(873～1213K)转度.过渡相 R 为菱形点阵,点阵常数α=0.8977nm,α=74.4°,其 Mo 含量为48%,呈棒状或块状形态析出.时效初期由于过渡相 R 的析出引起合金硬化.     

大跨径斜拉拱桥结构受力的敏感性分析

斜拉拱桥是一种多变量结构体系,各设计参数影响结构受力且参数的不同取值对结构的安全性影响存在较大差异。湘潭市湘江四大桥主桥(120 400 120)m斜拉钢管混凝土飞燕式拱桥的参数敏感性分析结果表明,主拱轴线偏差、钢管内混凝土的收缩徐变等对结构的影响较大。     

脑血管病和颅内肿瘤患者CSF-CK-BB实验与临床研究

采用层析荧光改良法对84例脑血管病（CVD）和颅内肿瘤（ICT）患者脑脊液（CSF）中脑型肌酸激酶同功酶（Brain Type Creatine Kinase Isoenzyme,CK-BB）活性作了测定。结果表明,在CVD急性期和ICT患者的CSF-CK-BB活性均有明显升高,且以出血性卒中（HCVD）的升高最为显著,其次为ICT,而缺血性卒中（ICVD）的升高则相对较低;同时CSF-CK-BB活性升高与CVD和ICT患者脑损伤的程度、范围和预后相关,而与ICT的病理性质及瘤腔内坏死范围无关。     

加筋板的双重非线性分析

本文综合工程实际的需要,对船体加筋板结构进行了双重非线性有限元分析。采用Prandtl-Reuss流动理论,具体导出了加筋板在双重非线性状态下理想弹-塑性和强化材料的单元刚度矩阵;用增量切线刚度法-迭代法相结合的混合解法来提高求解精度;对单剛、等效节点力的计算,均采用Gauss积分法和进行分层精度判别来节约机时和内存。     

DJ_2型交流传动客运电力机车用JD121异步牵引电动机

介绍了为 DJ2 型交流传动客运电力机车研制的 JD12 1异步牵引电动机 ,着重叙述了电机设计的前期分析过程 ,给出了电机的基本参数 ,对电机的结构特点和基本特性作了简要说明     

对《起重机设计规范》疲劳强度设计方法的修正

本文通过对《起重机设计规范》中构件静强度及疲劳强度设计方法的分析，结合概率设计理论，归纳了起重机金属结构构件静强度概率设计方法，基于设计规范中的疲劳强度数据，提出了一种简便，可行的强度概率设计方法，使设计规范中的内容得到补充和修正。     

船用控制装置的结构电磁兼容设计

本文通过对船用控制装置中电磁干扰传播途径、各类屏蔽机理的分析,提出了船用控制装置结构设计中解决电磁兼容问题的几种有效方法.     

船体与组合推进器水动力相互干扰特征的模型试验及推力减额特性的评估分析

以船体、导管和前置定子及转子组成的系统的推力减额特性为研究对象,基于因子分析理论,提出了该三因子系统的水动力相互干扰分析模型,导出了诸因子之间相互影响的求解公式,并采用分解试验方法实现了所有效应的准确测定.分析研究了系统推力减额的两种不同处理方式,建立了相应的评价指标体系.通过对两个特定方案的评估分析,推荐采用k2和t2作为系统推力减额性能优劣的综合评价指标,并建议采取以减小RrlH和RrlSD为主要方向的优化策略.     

Carbonate chemistry dynamics and carbon dioxide fluxes across the atmosphere–ice–water interfaces in the Arctic Ocean: Pacific sector of the Arctic

Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO₂) concentration and other non-CO₂ radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO₂ concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO₂. The Arctic Ocean's role in determining regional CO₂ balance has been ignored, because of its small size (only  4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO₂ exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO₂ because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO₂; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO₂ sink that also must be included in any Arctic regional CO₂ budget. Both the direction and amount of CO₂ transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO₂ accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO₂ decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO₂ sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO₂ ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO₂ range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources.     

HX_D3B型交流传动电力机车转向架

介绍了HXD3B型交流传动9600kW、6轴货运电力机车转向架的主要技术及结构特点,总结了其构架、一系悬挂装置、轮对、二系悬挂装置、基础制动装置、驱动装置、电动机悬挂装置、牵引装置和附属装置等主要部件的结构设计和技术特点。