热镀锌原板变速连续退火再结晶动力学

为了探讨热镀锌原板变速连续退火工艺参数与其再结晶的关系,对St01ZStO1Z钢种进行等温再结晶实测TTT图的墓础上,对其变速连续退火再结晶动力学进行了研究,采用差分法计算了连续退火温度场,获得了热镀锌板连续退火连续加热转变再结晶CHT图,并编制了相应的计算机程序,已用于生产实际,提高机组产能或者速度10%.     

喷雾法合成气体水合物的实验研究

为了寻求一种高效的气体水合物生产方式,提出了利用喷雾喷嘴高度分散液相的气体水合物生成装置,在不同的压力与表面活性剂条件下进行了实验．并结合晶体化学方法分析了喷射方式生成气体水合物的机理．验证了这种方式能够克服工业规模下水合物储存气局限性,将促进气体水合物储气应用技术的发展。     

Examination of dynamic recrystallization during compression of AZ31 magnesium

This study aimed to investigate dynamic recrystallization(DRX)behavior during compression of magnesium alloy AZ31. Cylinder samples were cut from the extruded rod and hot rolled sheet AZ31 for compression test.The samples were compressed using a Gleeble 1500D at a temperature of 300℃and a strain rate of 0.01 s-1.Grain orientations and misorientation angles across grain boundaries for the tested samples were obtained by using electron backscatter diffraction(EBSD)technique.The results showed that strong basal texture was observed after 50%compression(ε=0.69)on both the extruded and hot rolled samples,which have different initial textures.It was observed that with increased strain,DRX grains gradually rotated to basal orientation,and grain boundaries with misorientation angle of near 30°was formed in the samples.At the strain of 0.69,a high fraction of high-angle(60°)boundaries was present in the extruded sample,whereas almost no high angle boundaries were observed in the hot rolled sheet sample.     

基于40Cr高温动态力学性能的磨削表面动态再结晶行为

通过分离式霍普金森压杆(SHPB)实验得到了40Cr合金钢在高温高应变率下真应力-真应变曲线,据此确定了材料发生动态再结晶的临界条件.采用解析法和实验法分别求解了磨削强化层的温度场和塑性应变场分布.结果表明,磨削强化层在磨削深度方向具有较大的温度和塑性应变梯度;150μm强化层内会发生奥氏体转变;磨削表面最高温度可达1060℃.在磨削亚表面60μm内会产生剧烈的塑性变形,达到了再结晶的临界条件.较大的磨削深度使磨削强化层塑性应变增大,再结晶现象越充分,微观组织细化程度越高.     

聚丁二炔(Polydiacetylene)单晶中量子成核和热成核相变过程

本文研究聚丁二炔(Polydiacetylene)中的量子成核和热成核相变过程。在从PDB相向PDA相的相变过程中。会出现一个畴壁;相反,在从PDA相向PDB相的相变过程中,会出现一个反畴壁。我们认为,畴壁的形成是一种涨落的结果;利用统计物理的方法,对两种成核过程进行了详细的讨论,发现在ETCD-PD中,主要是热成核相变;而在ETDU-PD中,主要是量子成核相变,与实验事实符合。图5,参13     

双相钢拼焊板温拉伸晶粒尺寸模型的建立与应用

在形变温度为550 ～700℃、应变速率为0.000 1～0.100 0 s-1范围内,对B340/590DP双相钢拼焊板进行温单向拉伸试验和金相分析试验,研究双相钢拼焊板变形条件和晶粒尺寸之间的关系.基于Z参数建立了双相钢拼焊板母材和热影响区的晶粒尺寸数学模型,研究温拉伸条件下双相钢拼焊板晶粒尺寸的变化规律.结果表明:应变速率越低、形变温度越高,双相钢拼焊扳动态再结晶现象越明显,母材和热影响区晶粒尺寸越大;将该模型导入ABAQUS软件,通过试验和仿真结果比较,验证了所建晶粒尺寸模型的准确性,通过此模型可以预测不同变形条件下双相钢拼焊板母材和热影响区的晶粒尺寸.     

Mg-9Gd-4Y-0.6Mn合金在293～723 K时的变形行为及微观组织演变

研究Mg-9Gd-4Y-0.6Mn 合金在应变速率为0.01 s-1、变形温度为293～723 K时的压缩塑性变形行为, 并在光学显微镜下观察合金在不同变形温度下的表面滑移线及孪生变形形貌与内部微观组织. 研究结果表明： 合金流变应力应变曲线在不同温度呈现出不同的形状, 加工硬化、动态回复和动态再结晶在不同的温度各自起到了重要的作用;在523 K以上时非基面滑移已被激活, 形变孪生在296～723 K范围都存在, 在673 K以上出现动态再结晶;动态再结晶晶粒优先在原始晶界和粗大第二相粒子处形核, 同时在723 K还观察到晶界弓出形核和＂孪生＂动态再结晶现象.     

变形温度、变形程度与退火方式对 TC11 钛合金显微组织的影响

文章采用金相跟踪法研究了变形温度、变形程度及随后的退火方式对ＴＣ１１钛合金显微组织的影响。     

40CrNiMo钢的热变形组织变化

利用G leeble 1500热/力学模拟实验机,对40CrN iMo钢进行双道次热模拟单向压缩试验。变形温度分别为710℃、760℃、950℃,变形速率为0.5~30 s-1,变形量为0.05~0.4,道次间停留时间为1~100 s。分析了钢热变形组织特征,结果表明钢在950℃温度变形过程中发生奥氏体动态再结晶,在760℃温度变形过程中,应变奥氏体诱发铁素体析出,而在710℃温度变形过程中,应变奥氏体加速了铁素体析出。     

Fine three-dimensional P-wave velocity structure beneath the capital region and deep environment for the nucleation of strong earthquakes

A detailed 3-D P-wave velocity model of the crust and uppermost mantle under the capitol region is determined with a spatial resolution of 25 km in the horizontal direction and 4-17 km in depth. We used 48750 precise P-wave arrival time data from 2973 events of local crustal earthquakes, controlled seismic explosions and quarry blasts. These events were recorded by 123 seismic stations. The data are analyzed by using a 3-D seismic tomography method. Our tomographic model provides new information on the geological structure and complex seismotectonics of this region. Different patterns of velocity structures show up in the North China Basin, the Taihangshan and the Yanshan Mountainous areas. The velocity images of the upper crust reflect well the surface geological, topographic and lithological features. In the North China Basin, the depression and uplift areas are imaged as slow and fast velocity belts, respectively, which are oriented in NE-SW direction. The trend of velocity anomalies is the same as that of major structure and tectonics. Paleozoic strata and Pre-Cambrian basement rocks outcrop widely in the Taihangshan and Yanshan uplift areas, which exhibit strong and broad high-velocity anomalies in our tomographic images, while the Quaternary intermountain basins show up as small low-velocity anomalies. Most of large earthquakes, such as the 1976 Tangshan earthquake (M 7.8) and the 1679 Sanhe earthquake (M 8.0), generally occurred in high-velocity areas in the upper to middle crust. However, in the lower crust to the uppermost mantle under the source zones of the large earthquakes, low-velocity and high-conductivity anomalies exist, which are considered to be associated with fluids, just like the 1995 Kobe earthquake (M 7.2) and the 2001 Indian Bhuj earthquake (M 7.8). The fluids in the lower crust may cause the weakening of the seismogenic layer in the upper and middle crust and thus contribute to the initiation of the large crustal earthquakes.