Data loci in algebraic optimization

We consider parametric optimization problems from an algebraic viewpoint. The idea is to find all of the critical points of an objective function thereby determining a global optimum. For generic parameters (data) in the objective function the number of critical points remains constant. This number is known as the algebraic degree of an optimization problem. In this article, we go further by considering the inverse problem of finding parameters of the objective function so it gives rise to critical points exhibiting a special structure. For example if the critical point is in the singular locus, has some symmetry, or satisfies some other algebraic property. Our main result is a theorem describing such parameters.     

中国银杏种植业良种化进程的思路

阐述良种化的概念和意义;根据我国银杏生产发展的现状,提出中国银杏种植业现阶段良种化的进程是：加快产区良种选育和新发展区良种引种试验,加快良种苗木繁殖体系建设,用良种接穗改造低产劣种株,同时稳步发展良种苗种植;认为银杏在现阶段只宜采用科学的选择育种方式。     

Synthesis and Crystal Structur of (4,4''-H2bipy)[CdBr4]·H2O

The title compound (4,4'-H2bipy)[CdBr4]·H2O 1 has been synthesized via hydrothermal reaction and characterized by X-ray diffraction. The crystal belongs to monoelinic,space group P21/c with a=8.260(3), b=23.926(7), c=9.774(2) (A), β=106.777(9)°,C10H12Br4CdN2O, Mr=608.26, V=1849.4(9)(A)3, Z=4, Dc=2.185 g/cm3, S=1.005, μ(MoKα)=9.814 mm-1, F(000)=1128, R=0.0646 and wR=0.0989. The crystal structure analysis of 1reveals that the title compound features an isolated structure, based on discrete 4,4'-H2bipy moieties and lattice water molecules which are linked by hydrogen bonds together with tetrahedral cadmium atoms terminally coordinated by four bromine atoms.     

云南几次中强地震热红外异常特征对比研究

云南省位于多个地块交界处，构造活动活跃且地震活动频发。利用中国静止气象卫星风云二号系列相当黑体温度TBB数据，应用小波变换和相对傅氏功率谱的时频相对功率谱方法（T-F RPS），提取并分析了云南省2008年至今发生的5.5级以上地震热红外异常信息，且对比分析了特征周期、特征幅值、异常形态、异常演化过程等参数。结果表明：（1）该系列地震热红外异常信息易于用时频相对功率谱方法（T-F RPS）提取识别，且异常特征具有"出现-扩大-减小-消失"的规律；（2）异常特征周期和持续时间也具有一定的规律性；（3）异常沿着断层延展，震中位于异常边缘一侧或者异常区域交汇地带，发震时刻多位于相对功率谱幅值下降阶段；（4）震级与相对功率谱峰值有一定的相关性，震级高，峰值也较高；（5）地震类型与异常面积有一定的相关性，双震型地震异常面积较大。此外，讨论了地震热红外异常与构造活动、气候状况、天气情况和季节等因素的关系。     

综采工作面瓦斯治理分析

分析了综采工作面瓦斯涌出的特征和在各种通风系统下瓦斯涌出情况，提出了改进工作面通风系统和瓦斯抽放两种综采工作面瓦斯治理技术方案。     

从藏书排架谈种次号的确定方法

针对种次号排架存在的弊端，提出了若干改进方法，在一定程度上解决了内容特征基本相同的图书或适宜集中排架的图书不能集中的问题，便于读者在查找图书过程中的挑选与比较。     

造园中山石的运用

借鉴中国古典园林以其得体的山石点缀、构筑造园，及古人在造园用石方面谨慎而注重布局的经验，针对目前新营造的园林中不顾及环境条件，不考虑建筑风貌，随意到处堆叠庞大的假山的状况，提出了合理的山石造园的措施与体会。     

Mg-Ni合金在球磨过程中温度变化的理论及实验研究

通过计算磨球运动的最大速度估算了Mg-Ni粉末在球磨过程中可能达到的最高温度,并采用X-射线衍射仪(XRD)、扫描电子显微镜(SEM)、能谱分析仪研究了样品经400 r/min球磨不同时间后的相结构、形貌及微区成分的变化规律.结果表明:当球磨速度为400r/min时,可使落入两个直径为20mm的碰撞磨球之间、质量为0.033 3 g的粉末温度从298 K升到932 K.利用实验得出的片状金属的质量(0.015～0.025 g)推算出样品在400r/min球磨时的温度变化范围为845.6～1 409.4 K,使镁粉熔化的最小球磨速度为269 r/min,经400r/min球磨15 h后,Mg-Ni样品由成分不均的晶体相组成,球磨35 h后则转变为成分均匀的非晶体.图4,表2,参5.     

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.