Magnetic characteristics and their paleoclimatic significance of Fengzhou loess in the Qinling Mountains of China

The Fengzhou loess section is very typical in the Qinling Mountains. The section, about 82 m thick and underlain by the Neogene red clay, consists of 33 layers of loess and 33 layers of paleosol. The section covers Brunnes normal polarity zone and Matuyama reversed polarity zone, and the B/M boundary is located in the middle of L₈. Matuyama reversed polarity zone records Jaramillo, Olduvai and Reunion normal polarity subchrons. The boundary between Matuyama reversed polarity zone and Gauss normal polarity zone (M/Ga) appears in the lithological boundary between loess and the Neogene red clay. Loess accumulation in Fengzhou started before 2.48 Ma. The magnetic susceptibility curve indicates 33 cold-dry and humid-warm cycles of paleoclimatic variation in the Qinling Mountains during the last 2.48 Ma. The above climatic fluctuation may be well compared with that of the oxygen isotopic records from deep-sea deposits.     

死区电流极性检测的一种新方法

针对逆变器死区期间电流过零点检测不准确会影响死区补偿效果的问题,比较了几种常规检测方法,分析了这些方法存在的不足,根据电流极性检测原理并结合反馈电流补偿法,提出了一种新的检测方法,设计了具体的逻辑电路并仿真仿真结果表明该方法能准确检测出死区期间电流极性,从而验证了该方法的有效性,为下一步实现可靠的死区补偿提供了有力的判据     

铝合金变极性TIG焊熔池与阴极清理区视觉检测系统

基于铝合金变极性钨极惰性气体（TIG）焊接光谱分析,选择合适的滤波片和减光片,建立了在线检测铝合金变极性TIG焊熔池与阴极清理区的视觉检测系统,获得了清晰的熔池和阴极清理区图像,并且观察到了不同反极性比时熔池和阴极清洁区的变化,焊后对比结果表明,与通过视觉系统检测到的图像一致.此外,还得出了反极性比对阴极清理宽度和焊缝宽度的影响规律曲线,为优化焊接生产工艺提供了依据.     

渗硼层过渡区组织的研究

研究了纯铁、碳钢及低合金钢的渗硼层与基休之间形成的过渡区的组织和性能。低、中碳钢渗硼层过渡区的晶粒异常粗大，而纯铁及高碳钢的渗硼层过渡区组织无异常粗大现象。中碳钢的过渡区在紧靠硼化物层的窄小区域内有富碳现象，但整个过渡区并不富碳。渗硼过渡区的异常粗大组织主要是由于过渡区中的硼与ＡｌＮ作用后形成ＢＮ，使ＡｌＮ的阻碍奥氏体晶粒长大作用减弱而造成的。高碳钢渗硼层前沿的羽毛状组织中包含有 Ｆｅｓ（Ｃ．Ｂ）及 ＦｅＢ这两个相。     

钻杆内过渡带特性参数测试

过渡带长度Ｌ和曲率半径Ｒ是评定钻杆内过渡带质量的重要特性参数。怎样描述过渡带曲线，如何检测Ｒ和Ｌ，一直是钻杆质量检测中难以解决的问题。本文提出以最佳抉合圆分段拟合过渡带曲线的方法，并相应研制成ＴＺ－１型过渡带检测仪，其测量精度≤２％。     

界面过渡区微力学性质对高周疲劳性能的影响

为了解界面过渡区性质对混凝土高周疲劳性能的影响,采用纳米压痕技术测试了矿渣取代水泥的质量分数分别为0%、30%、50%、80%的混凝土中实际界面过渡区及邻近区域的压痕硬度分布,并测试相应配合比混凝土在不同应力水平下的抗弯疲劳寿命.试验结果显示:随矿渣取代水泥质量分数的增加,基体与界面过渡区之间压痕硬度的差异减少;当应力水平低于0.85时,混凝土的疲劳寿命对数值随基体压痕硬度与界面过渡区压痕硬度的比值的降低而增大;基体与界面过渡区间压痕硬度差异的减少,相对提高界面过渡区抑制疲劳损伤的能力,从而改善混凝土高周疲劳性能.     

基于暂态电流极性比较原理的多线路集成保护研究

提出了电力系统集成保护的方案,描述了一种基于暂态电流极性比较原理的多出线集成保护系统.当故障发生后,对母线所有出线的暂态电流模量的模极大值进行极性比较就可以判别故障发生的相对位置.理论分析和仿真结果表明,利用单侧母线各出线的暂态电流信号的模量进行小波变换后的模极大值极性来判别故障的相对位置是切实可行的.     

丹霞盆地红层时代的初探——古地磁研究的新证据

该文叙述了丹霞盆地红层的古地磁学研究工作的全部过程。通过对岩石剩余磁性的测量及数据分析,揭示了丹霞红层下部存在着一个长间距的正极性带,这可以跟地磁极性年表中的“白垩纪静磁带”相对比;上部则以反极性为主。结合同位素年龄测量资料,对照地磁极性年表,对丹霞盆地红层的时代归属得出以下认识:丹霞红层下部长坝组最老地层的时代为早白垩世早期,上部丹霞群最年轻地层为晚白垩世中期。     

硬岩矿深部开采过渡区厚度优选与数值分析

针对某铁矿进入深部开采过程中采场出现的地压问题,优化并选取了合理的采场参数.考虑到矿体中存在软弱夹层,会对过渡区的稳定性造成影响,通过极限平衡法,决定采用8.5,10及12 m厚度的过渡区以备选用,运用大型数值分析软件FLAC 3D进行三维数值模拟,对其稳定性进行对比分析.结果表明,随着厚度的增加,过渡区中应力集中现象越来越小,在开挖过程中,顶板位移也随着厚度的增加而减小,仅12 m厚过渡区的塑性区没有贯通.所以留设12 m过渡区可保证采场的稳定,满足过渡期间安全生产的要求,为矿山的安全平稳过渡生产提供依据.     

Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite

The distribution of water in the Earth's interior reflects the way in which the Earth has evolved, and has an important influence on its material properties. Minerals in the transition zone of the Earth's mantle (from approximately 410 to approximately 660 km depth) have large water solubility, and hence it is thought that the transition zone might act as a water reservoir. When the water content of the transition zone exceeds a critical value, upwelling flow might result in partial melting at approximately 410 km, which would affect the distribution of certain elements in the Earth. However, the amount of water in the transition zone has remained unknown. Here we determined the effects of water and temperature on the electrical conductivity of the minerals wadsleyite and ringwoodite to infer the water content of the transition zone. We find that the electrical conductivity of these minerals depends strongly on water content but only weakly on temperature. By comparing these results with geophysically inferred conductivity, we infer that the water content in the mantle transition zone varies regionally, but that its value in the Pacific is estimated to be approximately 0.1-0.2 wt%. These values significantly exceed the estimated critical water content in the upper mantle, suggesting that partial melting may indeed occur at approximately 410 km depth, at least in this region.