系统误差下基于双重模糊拓扑的编队航迹精细关联算法

为解决系统误差下编队内各目标航迹精细关联的难题,基于编队目标航迹的特点,利用模糊拓扑的思想,提出了一种系统误差下基于双重模糊拓扑的编队航迹精细关联算法.算法首先基于循环阈值模型对各传感器获得的航迹进行编队识别,然后利用编队中心航迹代替编队整体,深入分析系统误差对编队中心航迹的影响,建立第一重模糊拓扑模型,完成编队航迹的预互联和普通目标航迹的对准关联,最后基于预关联编队内目标航迹之间或与航迹关联对之间的拓扑关系建立第二重模糊拓扑模型,实现编队内目标航迹的精细关联.经仿真数据验证,与基于目标不变信息量的模糊航迹对准关联算法、基于航迹迭代的航迹对准关联算法和修正的加权法相比,该算法综合性能明显优越,能很好满足工程上对系统误差下编队内目标航迹精细关联的需求.      

盐津--珙县地区五峰组--龙马溪组页岩气富集成藏条件

利用野外观察及实验数据资料,对盐津-珙县地区五峰组-龙马溪组页岩气形成条件进行分析,并探讨其富集成藏的主控因素.研究结果表明盐津-珙县地区五峰组-龙马溪组下部黑色页岩是深水陆棚沉积产物,该区页岩气“甜点段”五峰组—段—四段和龙马溪组一段—五段发育完整,有机碳质量分数在2.7%~6.0%之间,主要为中高-高有机碳含量,富有机质黑色页岩厚度分布在30~50 m.在高含气层位,纳米级有机质孔和黄铁矿晶间孔大量发育,平均孔隙度为2.28%~3.48%,为吸附气和游离气提供良好的储集空间.研究区内构造强度较弱,通天断层少,具有良好的顶底板条件,压力系数平均大于1.0,因而保存条件良好.分析表明,高有机碳含量、纳米级孔隙发育、高脆性矿物含量、高压力系数是盐津-珙县地区页岩气富集成藏的主控因素.     

Formation mechanism of the graphite-rich protective layer in blast furnace hearths

A long campaign life of blast furnaces is heavily linked to the existence of a protective layer in their hearths. In this work, we conducted dissection studies and investigated damage in blast furnace hearths to estimate the formation mechanism of the protective layer. The results illustrate that a significant amount of graphite phase was trapped within the hearth protective layer. Furthermore, on the basis of the thermodynamic and kinetic calculations of the graphite precipitation process, a precipitation potential index related to the formation of the graphite-rich protective layer was proposed to characterize the formation ability of this layer. We determined that, under normal operating conditions, the precipitation of graphite phase from hot metal was thermodynamically possible. Among elements that exist in hot metal, C, Si, and P favor graphite precipitation, whereas Mn and Cr inhibit this process. Moreover, at the same hot-face temperature, an increase of carbon concentration in hot metal can shorten the precipitation time. Finally, the results suggest that measures such as reducing the hot-face temperature and increasing the degree of carbon saturation in hot metal are critically important to improve the precipitation potential index.     

Kinetics and formation mechanisms of intragranular ferrite in V-N microalloyed 600 MPa high strength rebar steel

To systematically investigate the kinetics and formation mechanisms of intragranular ferrite (IGF), isothermal heat treatment in the temperature range of 450℃ to 600℃ with holding for 30 s to 300 s, analysis of the corresponding microstructures, and observation of the precipitated particles were conducted in V-N microalloyed 600 MPa high strength rebar steel. The potency of V(C,N) for IGF nucleation was also analyzed statistically. The results show that the dominant microstructure transforms from bainite (B) and acicular ferrite (AF) to grain boundary ferrite (GBF), intragranular polygonal ferrite (IPF), and pearlite (P) as the isothermal temperature increases from 450℃ to 600℃. When the holding time at 600℃ is extended from 30 s to 60 s, 120 s, and 300 s, the GBF content ranges from 6.0vol% to 6.5vol% and the IPF content increases from 0.5vol% to 2.8vol%, 13.1vol%, and 13.5vol%, respectively, because the ferrite transformation preferentially occurs at the grain boundaries and then occurs at the austenite grains. Notably, V(C,N) particles are the most effective nucleation site for the formation of IPF, accounting for 51% of the said formation.     

双河油田VII油组油层的灰色关联评价

本文将双河油田Ⅶ油组油层视为-个灰色系统,以各油层的评价参数构造-个标准的最佳油层。由灰色关联分析方法计算各油层与最佳油层间的关联度,根据关联度的大小对各油层进行分类评价。评价结果与实际情况吻合甚好。     

基团电负性研究(Ⅹ Ⅳ)——基团电负性与某些碳氢化合物的标准生成热

通过分析基团电负性与ΔΔ_fH~0(RG/CH_3G)之间的关系,提出了一个计算碳氢化合物标准生成热的简单方法: Δ_fH~0(RG)=Δ_fH~0(CH_3G)+(1.18n~(1/2)-0.98)X_G-21.31n+19.90式中,Δ_f(RG)和Δ_fH~0(CH_3G)为烃(RG和CH_3G)的标准生成热;X_0为基团G的电负性;G=Me,i-Pr,t-Bu,CH=CH_2,CH=CHMe(E,Z),C≡CH和Ph;n为直链烷基R中的碳原子个数,34个可比较值的平均偏差为1.05kJ/mol。     

颗粒运移的计算机模拟

本文在用网络模型描述多孔介质的基础上,用Monte-Carlo法研究了颗粒在网络模型中运移沉积的机理以及颗粒浓度和颗粒尺寸分布对多孔介质渗透率损害的影响。本文应用的方法不仅限于颗粒运移、沉积机理的研究,而且还适合于其他领域的研究。     

分子天文学的发展与展望

介绍分子天文学及其在天文研究中的重要作用;综述近年来在分子云大尺度分布、分子云与恒星形成、拱星包层和恒星演化晚期、天体脉泽等方面的主要成果和进展;讨论了分子天体化学发展的情况及其重要意义;并提出对今后的发展趋势及主要研究课题的展望。     

东风山前寒武纪含铁建造金矿床的同位素地球化学特征

东风山金矿体赋存在含铁层之下的东风山群角岩层中。赋矿层位中富含磁黄铁矿、黄铁矿、锰铝榴石和锰铁闪石。通过对该矿床的硫、氧、碳和铅同位素研究,表明硫化物中的硫和地层铅主要来自深源,其次地层中的含硫有机物被生物分解形成的硫也产生一定影响。东风山群形成于早元古代。东风山金矿属高温热接触变质的同生床。     

铝阳极极化特性研究

分别测量了在阻挡型和多孔型电解质溶液中,铝阳极的恒电压和恒电流极化曲线.根据铝阳极极化曲线的特点,讨论铝在阳极氧化过程中有关阻挡层的形成、部分溶解,以及转化为多孔层等过程与极化电压和电流的关系.提出了在低极化电压或电流下,孔胚按“慢少成孔”机理在高极化电压或电流下按“快多成孔”机理的观点.