图的控制圈的一个下界

引进控制圈的定义,同时讨论了一类2-连通图的控制圈的一个下界,若G是2-连通的非 Hamilton图,含有控制圈C,令R=V(G)-V(C),如果存在v∈V(C),使dR(V)≧2,则G包含的控制圈的长至少为2σ-2.     

小康住宅电气设想

针对小康住宅电气设计中线路截面、需要系数、配电型式、保护方式、电视、电话、保安对讲等作了初步探讨。     

轴流压缩系统振动模型分支的进一步研究

用微分方程定理论和分支理论的方法，讨论了轴流压缩系统的振动模型，证明了周期解和Ｈｏｍｏｃｌｉｎｉｃ轨道的存在性。分析了当某些参数变化的动力学行，结果为预测压缩系统振动的增长和衰减提供了重要参数设计。     

6V150柴油机热力循环的热力学分析

研究6V150柴油机有效能量利用情况,采用了发动机性能仿真软件与热力学分析相结合的方法.使用仿真软件BOOST建立了柴油机的仿真模型,并用实验所得数据和发动机的基本特性定义仿真模型的初始值,得出热力学分析所需要的数据;对柴油机的各个组成部分抽象为控制体进行热力学第一定律、第二定律计算,得出柴油机工作过程的损失分布规律,进而从热力学第二定律的角度提出改善柴油机能量利用的方向.     

2016年中国肿瘤防治热点回眸

 2016年是中国肿瘤防治重要的一年。回顾了中国2016年在肿瘤预防领域采取的环境治理、防治肥胖、大病医保及健康体检等措施,简述了在治疗肺癌、白血病、乳腺癌、消化道癌和鼻咽癌等方面取得的重要进展,盘点了新药研发、免疫治疗和转化医学研究平台建设等方面取得的成绩,分析了中国肿瘤防治的发展前景。     

冻融循环下纳米黏土改性滨海水泥土的微观结构

为探究冻融循环下纳米黏土对滨海水泥土微观结构的改性效果,通过扫描电子显微镜微观测试对土体微观结构变化规律进行分析,探讨了土体的微观结构定量化参数与宏观力学特征的关联性.以纳米滨海水泥土为对象,利用扫描电子显微镜和Image Pro Plus软件获取土体在0、1、5、7、9、11次的冻融循环下的微观结构特征和量化参数.结果表明:①在未冻融的环境下,纳米黏土改善滨海水泥土微观结构效果明显,孔隙明显减小.②在冻融环境下,纳米黏土在冻融循环初期对滨海水泥土微观结构的改性效果好,表现在冻融循环0～5次内孔隙面积平均减少14.3％,而冻融循环7～11次时仅平均减少4.3％的孔隙面积.通过概率密度函数的分布可知纳米黏土抑制了滨海水泥土超大孔隙的发育.③纳米滨海水泥土的压缩系数对颗粒面积变化比较敏感,颗粒的数量、不均匀系数等微观结构参数对压缩系数的影响较小.     

Global structures of the DE3 tide

The Hough mode decomposition (HMD) is used to investigate the global structures of the eastward propagating diurnal tide of zonal wavenumber 3 (DE3). The tide is delineated by using the SABER/ TIMED temperatures collected during 2002―2006. The HMD analysis results show that the DE3 tide is primarily dominated by two leading propagating Hough modes, i.e., (-3, 3) and (-3, 4) modes; the in-fluences .of the other Hough modes including trapped modes can be neglected. Based upon the HMD analysis results, this paper first reported the maximum of the tidal activity in the MLT region. The re-sults show that the DE3 tide exhibits annual unimodal distribution with the maximal amplitude occur-ring at 110 km in late summer (around July each year). Moreover, characteristic 2-year period variation is observed in the (-3, 3) Hough mode. And this type of inter-annual variation is further reflected in the tidal amplitude at 110 km height. For example, corresponding to the 2-year variation of the (-3, 3) mode, the DE3 tidal amplitude exhibits two substantially enhanced activities with maximal amplitude exceed-ing 12 K in 2002 and 2004, respectively. Moreover, current investigation results indicate that the influ-ence of the second propagating Hough mode, (-3, 4) mode, is important, in particular at the height un-der 100 km, where the DE3 amplitudes exhibit antisymmetric distribution with respect to the equator. The (-3, 4) mode exhibits bimodal distribution over a yearly course, which dominates the DE3 tide in the lower mesosphere. For example, two maximal DE3 activities were observed in late-winter-to-early- spring and late-autumn-to-early-winter, respectively. The first maximum is seen in the south of the equator, and the second maximum is in the north of it.     

均衡二部图中含指定顶点独立6-圈的个数

给出了均衡二部图具有含指定顶点的k个独立圈,其中恰好含s个4-圈和k-s个6-圈的最小度条件。     

The study of metal cycles in China

A model of Fe-flow in the life cycle of steel product was put forward and analyzed. Three important resource and environmental indicators for Fe-flow analysis, that is, steel scrap index, iron ore index and iron loss index were derived from this model. Illustrative examples, demonstrating the influence of the variation of steel output on steel scrap index and iron ore index, were given. Case studies for estimating the values of steel scrap index of Japan, China and USA in the period of 1988-1997 were carried out. It was clarified that the main reason of severe deficiency in steel scraps for China’s steel industry was its continued rapid growth. The study of iron, copper, zinc and lead cycle in China was carried out successfully according to this model.     

冻融循环条件下灰岩力学性能试验研究

为研究灰岩在不同冻融循环条件下岩石物理力学性能变化情况,利用快速冻融机和2 000 KN三轴压缩试验机对不同冻融次数下灰岩进行单轴压缩试验,得到冻融灰岩应力-应变关系曲线。结果表明：随着冻融次数的增加,抗压强度、弹性模量、泊松比均逐渐降低,且降低程度服从指数衰减模型,20次冻融之前,岩样应力-应变曲线塑性阶段不明显,随着冻融次数的继续增加,塑性特征逐渐明显,岩样脆性逐渐降低;试验得到不同冻融次数下饱水岩样波速均大于干燥状态下的波速,且随冻融次数的增大呈指数形式降低;最后,基于波速建立以岩石动弹模为损伤变量的冻融损伤方程,拟合结果显示损伤随冻融次数的增加而增大,但增长速率逐渐减少。