Study on the REM Model for Group Decision Making

IntroductionAsocialchoicefunctionisamappingwhichassignsanonemptysubsetofthepotentialfeasiblesubsettoeachorderedpairconsistentofapotentialfeasiblesubsetofalternativesandascheduleorprofileofvoters'preferences.Consideranopinionaggregationprobleminwhichagroupofexpertsgivetheirscoresthatexpresstheirpreferencestoasetofalternativesanddesiretocombinetheirscoresintoasingleaggregationpreferenceoverthealternativeset.Theunderlyingideahereisthattheconsensusofnumerousexpertsresultsinasuperiorpreferenceonthe…     

季冻区隧道冻胀力影响因素交互性及敏感性正交试验分析

为探究影响季冻区隧道衬砌冻胀力各个因素的交互性及敏感性,依托承担冬奥会人员转运工作的延崇高速主线翠云山隧道,通过建立ANSYS数值模型,对冻胀率、冻融圈厚度、衬砌弹性模量等冻胀力影响因素进行了正交试验。研究结果表明：(1)考虑各个因素对冻胀力的影响时可只考虑其主效应。(2)融圈厚度、冻胀率、衬砌弹性模量、冻结围岩弹性模量以及未冻结围岩弹性模量均对冻胀力的影响较为显著;各因素敏感性排序为：冻结围岩弹性模量>冻胀率>未冻结围岩弹性模量>冻融圈厚度>衬砌弹性模量。(3)相比于原始参数,实验最优参数各部位冻胀力均有所减小且降幅均超过30%,最小降幅发生在拱顶为34.20%,并据此提出了控制冻胀力的措施,为河北地区季冻区隧道建设提供指导。     

影响林木种子贮藏的因素

为了每年提供造林新需的具有生活力的种子及长期保存种质资源,贮藏种子是必要的手段。种子寿命具有遗传性,且因树种而异。种子的贮藏特性可以分成5类:正常型、亚正常型、温带顽拗型、热带顽拗型和中间型。种子含水量和贮藏温度是影响种子贮藏是否成功的两个最重要因素。但因树种及其贮藏特性不同,种子含水量和贮藏温度的最适值也不同。为了保持正常型和亚正常型种子的生活力,这类种子必须密封贮藏;但对顽拗型种子,因其需要保持种子的代谢活性及要进行有氧呼吸,则需要气体交换。     

三轴压缩与干湿循环作用下灰岩的力学试验研究

南京地铁6号线万寿村站至燕尧路站区间深部主要为灰岩,盾构隧洞贯通后,深部岩体对隧洞维护起至关重要的作用,为了对该地铁深部稳定性提供理论指导,利用MTS815试验机对灰岩在经历干湿循环后进行了常规三轴压缩试验,研究了灰岩在不同次数干湿循环作用下和不同围压下的力学特性,结果表明:(1)受干湿循环作用前后试件的应力—应变曲线...     

Effects of Cr and Mo elements on the microstructures and compressive properties of the in situ (TiC_xN_y–TiB_2)/Ni cermets

In-situ(TiC_xN_y–TiB_2)/Ni cermets with 70 wt%TiC_xN_y–TiB_2 were successfully fabricated by combustion synthesis and hot pressing sintering in Ni-Ti-B_4C-BN powder systems.The microstructures,density,compressive properties,and hardness of the TiC_xN_y–TiB_2/Ni cermets with the addition of 0–8 wt%Cr/Mo to the Ni-Ti-B_4C-BN powder systems were compared and analysed.The results showed that the ceramic particles distributed uniformly in the cermets,and the size of the ceramic particles reduced with the Cr/Mo addition.Both Cr and Mo addition can improve the hardness,compressive properties,and fracture strains of the cermets.The hardness,compressive strength,and fracture strain of the(TiC_xN_y–TiB_2)/(Ni+Cr)cermets increased from 1561 HV,2.94 GPa,and 2.9%to 1864 HV,3.65 GPa,and 3.4%,respectively when the Cr content increased to 5 wt%.The hardness and compressive strength of the(TiC_xN_y–TiB_2)/(Ni+Mo)cermets increased from 1561 HV and 2.94 GPa to 1902 HV and 3.43 GPa,respectively when the Mo content increased to 8 wt%.The cermets with Cr had better compressive properties than the cermets with Mo.     

用小波变换和奇异指数表征蔡氏混沌信号键带

计算了蔡氏电路混沌信号的离散二进小波变换及奇异指数，结果发现，当尺度2∧5上的小波变换结果的模大于某一阈值时，其所对应的信号段就是键带，在混沌信号的键带处，奇异指数限大的正值，而在非键带处，奇异指数取负值或小的正值。     

Research on catalysis of sodium-metallochlorophylls in Ni/MH battery

The effects of sodium-metallochlorophylls including sodium-iron chlorophyllin, sodium-copper chlorophyllin and sodium-magnesium chlorophyllin on performance of Ni/MH battery were investigated. The results show that sodium-iron chlorophyllin can effectively activate the gases produced during charge in Ni/MH battery, therefore reducing the reduction potential of oxygen and the oxidation potential of hydrogen, and the increased speed of inner pressure of battery is decreased significantly. With the aid of DMol3 software, the activation process of oxygen and hydrogen by sodiummetallochlorophylls was simulated and analyzed. It was found that the catalysis behavior is in agreement with the experimental results, and the activation process also gets a reasonable explanation from the calculated results.     

基于无速度传感器的直接转矩控制系统优化

针对传统异步电机直接转矩控制系统在低速运行状态下存在磁链轨迹发生波动、转矩脉动大的问题,提出一种新型异步电机直接转矩控制策略。采用滑模控制和空间矢量脉宽调制技术(SVPWM: Space Voltage Pwlse-Width Modulation), 引入滑模控制器, 以提高系统对参数变化和外界干扰的鲁棒性。利用空间电压矢量脉宽调制技术产生系统所需要的任意期望空间电压矢量, 使磁链轨迹更趋近于圆形, 即降低了转矩和磁链脉动,又增强了系统的鲁棒性。同时引入无速度传感器技术, 以提高系统工程应用性。通过在Matlab/ Simulink软件仿真结果表明, 新型直接转矩控制系统改善了磁链轨迹波动并有效地降低了转矩脉动, 使转速估计具有较高精度。     

Silicon in the Earth's core

Small isotopic differences between the silicate minerals in planets may have developed as a result of processes associated with core formation, or from evaporative losses during accretion as the planets were built up. Basalts from the Earth and the Moon do indeed appear to have iron isotopic compositions that are slightly heavy relative to those from Mars, Vesta and primitive undifferentiated meteorites (chondrites). Explanations for these differences have included evaporation during the 'giant impact' that created the Moon (when a Mars-sized body collided with the young Earth). However, lithium and magnesium, lighter elements with comparable volatility, reveal no such differences, rendering evaporation unlikely as an explanation. Here we show that the silicon isotopic compositions of basaltic rocks from the Earth and the Moon are also distinctly heavy. A likely cause is that silicon is one of the light elements in the Earth's core. We show that both the direction and magnitude of the silicon isotopic effect are in accord with current theory based on the stiffness of bonding in metal and silicate. The similar isotopic composition of the bulk silicate Earth and the Moon is consistent with the recent proposal that there was large-scale isotopic equilibration during the giant impact. We conclude that Si was already incorporated as a light element in the Earth's core before the Moon formed.