一种识别结构主要失效模式的有效算法

发展了线性互补规划法中的Ｌｅｍｋｅ算法,并与可靠性分析中的分支－约界法相接合,提出一种识别结构主要失效模式的算法,它既不用进行结构重分析,也不用通过判别结构的刚度矩阵Ｋ的奇异性来识别主要失效模式,而是应用一种新的简易结构失效判别准则,最后通过数值算例说明了方法的实用性。     

热电联产热力系统参数与结构方案同步综合

将复杂非线性蒸汽动力系统参数优化扩展到热电联产流程结构和蒸汽参数的联合优化,提出的混合整数非线性规划（ＭＩＮＬＰ）模型包含非凸非线性费用目标函数、复杂非线性过程约束及多方案选择的组合优化０－１变量逻辑约束．应用算例表明,所采用的模型和改进的遗传算法解决热力系统组合方案优化问题是可行的．     

4-Hydroxy-2-quinolones 131. Bromination of 3-allyl-4-hydroxy-2-oxo-1,2-dihydroquinoline

The bromination of 3-allyl-4-hydroxy-2-oxo-1,2-dihydroquinoline by molecular bromine is accompanied by the closure of a five membered furan ring and gives the corresponding 2-bromomethyl-3,9-dihydro-2H-furo[2,3-b]quinolin-4-one. __________ Translated from Khimiya Geterotsiklicheskikh Soedinenii, No. 11, pp. 1677–1686, November, 2007.     

Controlled Rate Thermal Analysis of Hydrated Borates

Quasi-isothermal-isobaric analysis was applied as a main method for investigation of thermal decomposition of borates. The structural mechanism of the dehydration and dehydroxylation of selected borates is considered. It has been found that they consist of two independent stages: formation of gaseous water molecules localized into the structural framework and their release. The internal pressure of gaseous water molecules is the factor influencing the course of these processes. The strengths of the chemical bonds of the components and the freedom of their displacement also determine thermal stability of hydrated borates. This revised version was published online in July 2006 with corrections to the Cover Date.     

Finite-size scaling study of a first-order temperature-driven symmetry-breaking structural phase transition

We present a study of finite-size effects in a model exhibiting a first-order temperature-driven symmetry-breaking structural phase transition in theL × cylindrical geometry in theL limit. Exact studies demonstrate the applicability of our scaling ansatz even in the one-dimensional limit, making this model ideal for studying finite-size effects. The scaling ansatz, similar to the previously developed ansatz for field-driven transitions, demonstrates that latent heat is crucial in driving these transitions. This ansatz is supported by a 2×2 phenomenological transfer matrix based upon the symmetries of the system; this produces an analytic free energy which has the scaling form. Order parameter probability distributions show that the high- and low-temperature phases coexist only in a small finite-size-affected regime near the bulk transition temperature; this regime vanishes exponentially fast asL diverges.     

Variation of physicochemical properties in the aggregates of structual isomers

The regions of variation of density, enthalpy of formation, and detonation velocity of all of the formally possible structual isomers were determined for several molecular formulas of C,H,N,O-containing explosives. The histograms of the distribution of the structual isomers over these parameters were constructed.Translated fromIzvestiya Akademii Nauk. Seriya Khimicheskaya, No. 5, pp. 859–862, May, 1995.The authors are grateful to Mrs. I. D. Solodukhina for the design of the graphical material.The work was carried out with the financial support of the Russian Foundation for Basic Research (Project No. 94-03-09323).     

深过冷Cu-20Wt%Pb亚偏晶合金的凝固行为

采用熔融玻璃净化和循环过热相结合的方法，使Cu-20wt％Pb亚偏晶合金获得了208K的深过冷，在宽过冷范围内研究了Cu-Pb亚偏晶合金的组织演化规律。结果表明，过冷合金熔体初生相为α(Cu)，在0～146K的过冷度范围内，均有两次再辉现象；在183～208K的过冷范围内，只出现一次再辉。当△T≤98K时，合金凝固组织为粗大枝晶α 枝晶间Pb相；当116K△≤T≤146K时，凝固组织已无明显的枝晶形貌，组织由细密α基体 细小的Pb颗粒组成；当△T≥183K时，凝固组织与中等过冷度下的组织相似，只是Pb相更细小，分布更均匀。当△T≥133K时试样出现裂纹。     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6～1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.     

基于晶粒尺寸的结构钢热变形流变应力数学模型

从晶粒尺寸角度出发，提出晶粒形变度的概念，建立了一个用以描述金属材料热变形行为的数学模型，具有精度高、简单直观、受分界点影响小且计算曲线连续等优点．该模型具有一定微观物理基础，既能描述动态再结晶前的强化阶段，又能描述动态再结晶后软化阶段的热变形流变应力，对两种结构钢的热变形流变应力进行了计算，并与试验值及其他模型的计算结果进行了比较．     

20CrMnTi结构钢热变形行为及其数学模型

利用Gleeble-1500热模拟实验机研究了20CrMnTi结构钢在温度为1223～1243K，变形速率为0．01～5s^-1条件下的热变形行为．通过奥氏体再结晶动力学回归计算了20CrMnTi的形变激活能，以及峰值应力与变形温度、应变速率之间的关系；提出采用加工硬化率-应变(θ-ε)图可以准确地判断该钢发生动态软化的类型，并可以确定动态再结晶开始和结束以及最大软化率时所对应的应变．给出了反映该钢动态再结晶进行过程的动态再结晶状态图，以及动态再结晶开始时间和完全再结晶时间与形变温度的关系图，并回归出了20CrMnTi钢的再结晶动力学方程．