基于MLP和SPSO的机器人行为选择与运动控制方法

针对传统行为选择机制(ASM)不能很好地做出控制决策的问题,提出一种基于多层感知(MLP)前馈神经网络的ASM,并将其应用到移动机器人目标跟踪中。首先,根据具体应用场景预定义多个机器人行为。然后,根据机器人配备的图像和红外传感器获得的目标位置和障碍物信息,通过MLP神经网络从预定义行为中选择出所需执行的行为。另外,为了构造最优的MLP模型,采用一种简化粒子群算法(SPSO)来优化网络权值参数。机器人目标跟踪仿真的结果表明,提出的ASM能够准确选择出合适的行为,实现了控制机器人跟踪目标移动且能够避开各种障碍物。     

Intergranular oxidation of silicon in 20Cr-25Ni niobium-stabilized stainless steel at 1140–1230 K

The kinetics of intergranular oxidation of silicon in a 20Cr-25Ni Nb-stabilized stainless steel are reported, at temperatures in the range 1140–1230 K, in CO₂ at 40 bar pressure. The depth of attack increased parabolically with respect to time, with an activation energy of 335±30 kJ/mol. The mechanism of growth is discussed in terms of classical internal-oxidation theories, and an alternative explanation based on an available-space theory is developed. The internal oxidation rates in a number of different alloys are compared with diffusivities of metals in the base alloy. It is proposed that intergranular oxidation in the 20–25 Nb steel is controlled by the rate of outward diffusion of iron or chromium in the alloy.     

当前网络政治参与中存在的问题与对策

针对我国当前网络政治参与中存在着非法参与行为多、政务信息不公开致使公众政治参与缺乏信息基础、政府对公众网络政治参与的行为与观点缺乏回应等问题,本文提出了采取完善政治参与和网络政治参与的法治化机制,建立健全网络参政相关法规,保障公民网络参政议政权益,规范和打击非法政治参与行为;修改政府信息公开的法律法规,加大政府信息公开力度与规范网络监督机制;建立政府对公民网络政治参与的回应制度,以解决公民网络政治参与的相关问题,推动法治文明.     

基于成因机理及主控因素约束的多尺度裂缝“分级-分期-分组”建模方法——以四川盆地元坝地区上二叠统长兴组生物礁相碳酸盐岩储层为例

油气藏中普遍发育多类、多尺度天然裂缝,其成因具有多期次性,规模具有多级次性,发育受多种地质因素综合控制,这些特点为裂缝的精细三维地质建模带来了很大挑战。以四川盆地元坝地区上二叠统长兴组生物礁相碳酸盐岩储层为例,提出了一种基于成因机理及主控因素约束的多尺度裂缝“分级-分期-分组”三维地质建模方法,认为多尺度裂缝建模应遵循等时约束、层次约束及成因控制等原则,建模过程中应充分开展裂缝地质研究,根据研究区实际建立合理的裂缝级次、期次划分方案,分级、分期开展裂缝三维建模。(1)大尺度裂缝主要采用确定性方法进行建模,中-小尺度裂缝则采用其成因机制和发育主控因素进行约束建模;(2)在裂缝分期、分组描述和参数统计获得关键地质规律认识的基础上,通过地质力学方法分期开展中-小尺度裂缝分布预测,进而采用“分期-分组”的思路进行建模;(3)最终将大尺度裂缝模型和中-小尺度裂缝模型进行融合,得到多尺度裂缝网络模型。元坝地区长兴组储层多尺度裂缝建模实践表明,上述建模方法可有效弥补传统方法在建立中-小尺度裂缝模型精度方面的不足。     

基于深度学习的相对地质时间体估计方法

常规自动解释方法难以正确追踪三维地震数据体中被断层错断的地震反射层位。为此,提出了基于深度学习的相对地质时间体估计方法。首先,针对相对地质时间体估计需求,设计一个由编码器—解码器框架组成的相对地质时间体估计网络;其次,采用结构相似性准则为损失函数,利用生成的准确标注合成训练数据集对相对地质时间体估计网络进行训练,使其具备准确地从地震数据体中估计相对地质时间体的能力;最后,通过提取多个恒定的相对地质时间体等值面实现多个地震反射层位的自动追踪。测试结果表明,该方法不仅在验证数据集上显示出优异性能,而且在实际地震数据体上也获得了较好效果;利用估计的相对地质时间体能够一次性获得多个能够表征地层空间形态的地震反射层位。     

四氢萘催化裂化研究进展

加氢处理油中含有一定量的环烷基单环芳烃,研究四氢萘催化裂化有利于加强对更多环数环烷基单环芳烃催化裂化的认识。综述了四氢萘催化裂化过程的反应机理,认为四氢萘主要遵循单分子裂化机理;从反应活化能、扩散、吸附等动力学角度对四氢萘裂解行为进行了解释;催化剂适宜的孔径和BrØnsted酸强度有利于四氢萘开环;随着反应温度升高、剂/油质量比增大、质量空速减小,四氢萘反应活性增强,同时氢转移反应愈发明显。适宜的催化剂孔径和Brnsted酸强度、反应温度、剂/油质量比以及质量空速有利于四氢萘裂化生成低碳烯烃。     

基岩型富氦气藏形成条件

氦气是一种广泛应用于军工、航天、医疗等高新技术产业的稀缺战略资源,但其在世界分布极其不均,中国是贫氦国家面临着严峻的氦气供给安全问题。在系统总结前人研究成果基础上,结合本次实验分析对比了世界上最成熟的氦气生产气田（美国潘汉德—胡果顿气田）与中国氦气生产潜力较大的东坪气田,探讨两者的成藏要素及富氦机理。结果发现：两者均是以天然气作为载体气的基岩型富氦气藏,储层物性好,均发育以膏岩为主的低渗致密的良好盖层。两者的差异性在于,前者花岗岩形成年代更为古老,尤其是碳酸盐岩地层中富含的花岗岩碎屑,其年龄集中在元古宙,平均比东坪气田花岗岩的形成年代早400 Ma;前者氦气运移模式偏向于单一的饱和地下水脱溶释放,而后者存在“过路”古老花岗岩储层的天然气“萃取”释放。两者对比之下,提出形成年代久远的高U、Th氦源岩、充足的载体气、良好的基岩风化壳储层与致密的盖层,和充足的地下水（边底水）作为媒介参与氦气运移,是形成基岩型富氦气藏的必要条件。     

Oxidation behavior and mechanism of aluminum oxynitride (AlON) at elevated temperatures

The oxidation behavior and mechanism of aluminum oxynitride (AlON) powder exposed to air at elevated temperatures between 800°C and 1300°C was investigated by X-ray diffractometry (XRD), scanning electron microscope (SEM), electron spin resonance (ESR), nuclear magnetic resonance (NMR), and simultaneous thermogravimetry, differential thermal analysis, and mass spectrometry techniques (TG-DTA-MS). The weight of AlON gradually increases to a maximum value at 1150°C and then decreases with further heating. Meanwhile, AlON powder undergoes chemical changes, as evidenced by lattice expansion, and turns eventually into alumina. ESR spectra reveal the occurrence of lone pair electrons in the oxidized products and the intensity of corresponding resonance signal increases before disappearing with the increase in temperature. Combined with the results of NMR and TG-DTA-MS, the measured data suggest that Al-N in [AlO₃N] tetrahedron and [AlO₅N] octahedron are gradually oxidized into Al-O-N group with lone pair electrons, which causes continuous weight gain and lattice expansion. Further oxidation at higher temperatures results in alumina and N₂.     

Experimental investigations of machining characteristics and removal mechanisms of advanced ceramics in high speed deep grinding

Machining characteristics and surface integrity of advanced ceramics, including alumina, alumina–titania, and yttria partially stabilized tetragonal zirconia, were studied under high speed deep grinding conditions. Material removal mechanisms involved in the grinding processes were explored. The material removal in the grinding of alumina and alumina–titania was dominated by grain dislodgement or lateral cracking along grain boundaries. The removal for zirconia was via both local micro fracture and ductile cutting. It was found that under a feed rate of 500 mm/min and for all the wheel speeds used, an increase in the wheel depth of cut (DOC) from 0.1–2 mm slightly improved the ground surface finish, but greatly prolonged the wheel life. This increase did not deepen the subsurface damage layer for the alumina and alumina–titania, but resulted in a slightly deeper damage layer for the zirconia.