电子关联对聚乙炔中双激子湮灭过程的影响

在SSH哈密顿基础上引进弱电子关联,对反式聚乙炔链中双激子的湮灭过程实施了分子动力学模拟.电子关联的引入延缓了链中激子的湮灭过程,关联强度U=0eV时,激子的湮灭时间约在t=84fs,计入四个近邻格点上的弱电子关联作用,湮灭时间明显减慢,约为t>100fs.随着弱关联强度的增加,湮灭时间逐渐延长.计算结果表明,在计算有机材料激子快速响应过程中计入电子关联是十分必要的.     

铁掺杂TiO_2-SBA-15催化剂制备及光催化降解甲基橙研究

采用溶胶-凝胶法,将TiO_2负载到介孔分子筛SBA-15上,再通过FeCl3浸渍的方法,将不同量的铁掺杂到TiO_2-SBA-15上.通过FT-IR、XRD、N2吸附-脱附和TEM等手段对铁掺杂TiO_2-SBA-15催化剂进行表征.结果表明:负载TiO_2后的SBA-15依然为高度有序的二维六方结构,比表面积略有减小,说明SBA-15的孔道结构有利于TiO_2的分散.掺铁后的TiO_2-SBA-15的结构改变不大,且TiO_2晶形仍为锐钛矿型.最后以光催化降解甲基橙探究不同铁掺杂量的TiO_2-SBA-15催化活性.结果表明:铁离子掺杂量为0.035%(质量分数),紫外光照射200min时,甲基橙降解率达最高值98.2%.     

鄂尔多斯盆地西缘克里摩里组古喀斯特洞穴特征及发育控制因素

鄂尔多斯盆地西缘下奥陶统克里摩里组发育的古喀斯特洞穴具有良好的勘探前景,但洞穴预测难度大,勘探风险高,需要准确认识古喀斯特洞穴基本特征与储层发育规律,降低勘探风险。通过岩心观察、薄片鉴定以及录井、测井、地震等手段分析表明,该套喀斯特洞穴主要发育在颗粒灰岩内,横、纵向分布稳定,依据岩石学、录测井及地震响应特征可分为垮塌半充填型和暗河充填型,后者进一步分成角砾充填和泥质充填2种类型。喀斯特洞穴具有加里东期大气淡水顺层溶蚀特征,其发育受到岩性、古地貌及古地质条件的共同控制,台缘礁滩微相颗粒灰岩是优先可溶性基岩,古喀斯特斜披提供了有利的水动力条件,加里东期同生微断裂提供了渗流通道,上奥陶统是否覆盖决定了洞穴类型及充填程度。     

小分子势能面及其量子动力学研究

简要介绍了原子与分子物理研究所,近几年来在小分子势能面、量子散射动力学和弱相互作用聚合物光谱等方面的理论研究.     

New crystal structure of molecular complex 1-piperidine carboxylate-piperidinium-H<Subscript>2</Subscript>O studied by X-ray single crystal diffraction

Piperidine absorbs CO2 and H2O in air to form a molecular complex： piperidium-l-piperidinecarboxylate-H2O. The structure of the complex was characterized by X-ray single crystal diffraction. The crystal structure was determined to be triclinic, space group P1^-with a=0.648 6（8） nm, b=0.809 200） nm, c= 1.357 1（16） nm, a=96.96706）°, β =102.506（15）°,γ=104.202 05）°, Z=2. The complex is stabilized via five hydrogen bonds between the three components, N-O electrostatic interaction and O-O interaction （electron transfer） betweenl-piperidinecarboxylate and H2O. Due to electron transference of carbamate ion, the oxygen atom in water molecule is strongly negatively charged and the O-H bond is considerably shorter than that of the free molecule of water. The formation of the molecular complex is a reversible process and will decompose upon heating. The mechanism of formation and stabilization is further investigated herein.     

PM3级别上的最大重迭对称性分子轨道

本文提出了PM3级别上的最大重迭对称性分子轨道计算方案,采用通常的半经验分子轨道方法PM3级别中完全相同的参数,计算了各种分子的几何参数、电离能等,所得结果与实验值及PM3半经验分子轨道方法计算结果相符,说明该计算方案是可行的。同时,由于提出的计算方案过程简单,更易推广使用到从头算方法难以解决的大分子体系和超分子体系的结构和性质研究。     

试论高等法学专业学生社会主义法治理念的培养

高等法学教育是培养社会主义法律人才的基本方式和重要手段。现阶段,在高等法学教育中加强培养学生“依法治国、执法为民、服务大局、公平正义、党的领导”的社会主义法治理念,对于法治国家的建设以及社会主义法治的实现具有非常重要的理论意义和实践价值。培养高校法学专业学生的社会主义法治理念,可以从课堂教学和实践教学两个方面着手进行,这两方面互为补充,互相促进,缺一不可。     

电性距离矢量预测有机污染物的生物富集因子

以电性距离矢量Mt表征165种非离子性有机物(NOC)的分子结构.利用多元回归方法建立了122种NOC的生物富集因子(lg BCF)与32个Mt的数学模型,其相关系数R为0.976.经逐步回归建立最佳四变量(M15,M17,M36,M91)模型,其R为0.960;并以Jackknife法检验,其LOO交互检验系数(q2)为0.915.这4个Mt参数揭示了影响NOC生物富集因子的主要因素,结果表明该模型具有良好的估算能力与鲁棒性.以111个NOC为训练集的生物富集模型作用于11个NOC的检验集,显示出良好的预测能力.     

The occurrence and significance of C25HBI in Cenozoic saline lacustrine source rocks from the Western Qaidam Basin,NW China

The saline lacustrine deposit of the Oligocene Lower Ganchaigou Formation is the main source rock for the Western Qaidam Basin,NW China.In this study,abundant highly branched isoprenoids with 25 carbon atoms (C25HBI) were detected in the upper section of the Lower Ganchaigou Formation.C25HBI is a biomarker for diatoms,and can provide information regarding biogeochemical processes during production and preservation of sedimentary organic matter.The carbon isotopic values of C25HBI in these source rocks were in the range of-18‰ to-20‰.The relative enrichment in 13C of C25HBI suggests that these isoprenoids were derived from diatom blooms.In this case,the diatoms used HCO3-as an additional carbon source to dissolved CO2 in water column due to their high biological productivity.Conversely,the diatom blooms indicated an abundant nutrient supply to the environment and high primary productivity.Thus,the occurrence of 13C-enriched C25HBI could be an ideal marker for good source rocks.The decreased concentration of CO2(aq) in the water column induced by diatom blooms can result in an enrichment in 13C of organic matter synthesized by primary producers.This may be a possible reason for the occurrence of 13C-enriched organic matter in the Cenozoic source rocks of the Western Qaidam Basin.Previous studies have shown that the high carbon number n-alkanes sourced from diatoms have no carbon preference.Hence,the sources of n-alkanes in regional source rocks are complex,and should be considered when discussing the sources of organic matter in future studies.     

Angular dependent NEXAFS study of the molecular orientation of PTCDA multilayers on Au （111） surface

The molecular orientation of perylene-3,4,9,10-tetracarboxylic acid dianhydride (PTCDA) multilayers adsorbed on Au (111) surface has been investigated using angular dependent O K-edge near edge X-ray absorption fine structure (NEXAFS) spectroscopy. The significant angular dependence of important resonant structures (π* and σ*) reveals that PTCDA molecules adopt an ordered geometry on the substrate surface. The average tilt angle of the PTCDA molecular planes is 27°±10° from the Au (111) surface.