太赫兹时域光谱技术在危险品检测方面的应用

太赫兹波(terahertz, THz, T-ray)是指频率介于0.1～10 THz之间的电磁辐射,在电磁波谱上位于微波和远红外线之间。大多数爆炸物、毒品在此波段有特征吸收。与在公共安全领域检测武器、爆炸物、毒品等危险品的传统方法相比,太赫兹辐射能量低,不会产生电离辐射,也不会引起安全担忧。而且,太赫兹波对于衣物等大多数包装材料有很强的穿透力,对物质的检测可以做到高灵敏、无损伤和远距离,因此在反恐、毒品、安全检测等方面具有显著潜在优势。文章介绍了国内外太赫兹时域光谱技术(terahertz time domain spectroscopy, THz-TDS)在爆炸物及毒品检测方面的研究最新进展;详细讨论了黑索金(RDX)的研究现状,并初步探讨了影响实验结果的几种因素。     

利用HITRAN资料研究黑碳和沙尘气溶胶粒子的光学特性

在IDL程序语言中实现Mie理论的数值算法,利用HITRAN资料提供的气溶胶粒子复折射指数,计算分析了沙尘、黑炭2种气溶胶粒子在不同半径（1μm,2.5μm和10μm）时,对波长为400nm和860nm光的散射效率以及散射相函数矩阵元素。结果表明：黑炭与沙尘有明显的光学性质差别,沙尘粒子不仅散射效率大于黑碳,而且后向散射比黑碳粒子强。 2种粒子对400 nm和860 nm太阳光的偏振也不同,可以利用此特性鉴别这2种气溶胶。     

非结构子网格压力方法

纯拉氏流体力学计算失败的根源是砂漏运动和虚假涡旋,运用子网格拉氏质量与其相关的子网格密度得到子网格压力,子网格压力产生的扰动隅角力能消除这些虚假运动,以便消除困扰拉氏流体力学算法的网格畸变带来的数值计算困难.将包括子网格压力的相容流体算法推广到非结构网格,研制包括非结构子网格压力的相容流体程序,对Saltzman活塞问题进行数值模拟,从数值结果分析可知,非结构子网格压力方法能抑制虚假涡旋,消除砂漏畸变.     

磁化铁氧体覆盖二维导体目标FDTD分析的移位算子方法

采用移位算子方法把时域有限差分法推广应用于二维磁各向异性色散介质—磁化铁氧体中.证明了电磁波横向入射二维轴向磁化铁氧体目标情形下,电磁波可按目标的轴向分解为横电波(TE波)和横磁波(TM波),且TE波的散射特性与铁氧体介质无关,而TM波的散射特性与介质电磁参量密切相关,同时对其物理原因进行了分析.通过采用移位算子方法处理磁化铁氧体频域本构关系,得到该情形下目标电磁散射的移位算子时域有限差的迭代计算公式,同时解决了电磁波在各向异性和频率色散介质中传播的问题.计算了轴向磁化铁氧体涂敷VonKarman型导体柱的TM波双站雷达散射截面,分析了铁氧体参量对目标双站雷达散射截面的影响.结果表明:恰当地选择铁氧体参量能有效地减少目标的雷达散射截面,本文时谐因子取exp〔jωt〕.     

理解全球化：基于“经济−社会−政治”体系共生演化视角的分析

20世纪80年代以来,一波超级全球化席卷全球。当今世界进入了百年未有之大变局,全球化陷入困境。应当如何理解当前的全球化困境？百年未有之大变局究竟变在何处？为此,可以从经济学、政治学、社会学与国际关系的综合视角,构建“经济−社会−政治”为一体的、动态演化的框架,以理解当今世界全球化的深层次矛盾。近一波全球化过程中全球经济力量与收入分配格局发生了变化,出现了发达经济体的经济停滞和新兴经济体的赶超,也导致了社会各阶层和不同社会群体的收入和财富差距发生巨变。全球化中全球经济基础的变化,即全球化中的全球经济力量格局变迁与收入分配恶化将对各国的经济和社会基础产生重大影响,进而影响上层建筑：国家的主导思想和意识形态。一个国家在国际关系和经济政策领域主导思想的演变,势必影响其对外战略和政策选择,进而影响本国的经济走向乃至全球化的历史进程。     

毛细管电泳非接触电导法测定4种中枢神经系统用药

运用毛细管电泳非接触式电导检测方法对4种中枢神经系统用药-盐酸阿扑吗啡、氢溴酸加兰他敏、富马酸喹硫平、氯氮平的分离进行了研究。考察了电泳介质的种类、浓度、分离电压、进样时间对分离效果的影响,在10 mmol/L三羟基氨基甲烷(Tris)-8 mmol/L柠檬酸(Cit)-20%甲醇的运行缓冲液中,激发电压为60V,激发频率为600kHz,4种药物在15 min内得到了分离。4种药物的线性范围分别为0.97～15.6 mg/L;0.97～15.6 mg/L;0.48～15.6 mg/L和0.97～250 mg/L,检测限为0.32,0.32,0.16和0.32 mg/L。     

The Intrusion of the Meissen Pluton (Elbe Valley-Zone): Evidence from Geochemical and Isotopic Data

Abstract

Geochemical and mineralogical investigations of plutonic rocks from the Meiβen massif indicate different magmatic evolution trends of the Freital sequence as well as for the central part of the complex Constant ε-Nd_T-345 values of ?1.5 of the Freital sequence and major/trace element data point to a fractional crystallization process. Based on ε-Nd values, ¹⁴⁷Sm/¹⁴⁴Nd ratios as well as on geochemical data affinities to alkali basalts cannot be excluded.

Analogous conclusions have been drawn regarding mineral chemical data [10] and cathodoluminescence spectra of apatite [13]. Assimilation of old continental crust, reflected by relics of apatite and zircon, may be the reason that the ε-Nd values plot at the lower end of the “mantle array”. The pyroxene-monzodiorite from Gröba belongs to the same source environment as the Freital sequence (Nd-characteristics).

The geological evolution of the central part of the studied plutonic complex is completely different to the Freital sequence: most of the intrusions show signatures of open system fractionation processes. The ε-Nd_T-345 value of ?1.46 of the Leuben monzonite indicates a narrow relation to the Freital sequence, whereas the ε-Nd_T-345 value of +2.27 of the Spitzgrund monzonite either reflects the derivation of another basic material then the Freital-type or the participation of other mixing component(s) from geologically young crust.

Fabric and mineral chemical investigations of the porphyry-like granite GII point to a mixing process of basic xenocrysts, resembling the corresponding minerals of the Freital sequence, and granite melts [10]. Large amounts of old zircon cores [11] indicate the inheritance of continental crust components by the Hauptgranit. Isotopic investigations on various granitic samples (GII, Hauptgranit and Riesensteingranit) reflect an increasing trend towards the crustal source(s) of their parental melts. The ε-Nd_T-345 values are ?3.75, ?4.16 and ?6.13, respectively.

Chemical parameters and the ε-Nd_T value of the Riesensteingranit agree with data of granites from the Saxonian Granulite Massif (see e.g. Wand et al. [8]; von Quadt, 1992). Thus, it may be possible that both granite types derived from similar sources.     

Lewis acid-base adducts of zwitterionic alkali metal methanides and silanides with BH3

The synthesis, structures and spectroscopic properties of M(MeOCH₂CH₂OMe₂Si)₃CBH₃ (M-1-BH₃) and M(MeOCH₂CH₂OMe₂Si)₃SiBH₃ (M-2-BH₃) (M?=?Li, Na, K) derived from reactions of BH₃ with the alkali metal zwitterions [M(MeOCH₂CH₂OMe₂Si)₃C] (M-1) and [M(MeOCH₂CH₂OMe₂Si)₃Si] (M-2) (M?=?Li, Na, K), resp., are reported. X-ray analysis and DFT calculations reveal discrete zwitterionic structures with the octahedral alkali metal cations rigidly locked and charge separated from the BH₃ units via pendant donors groups. Solution experiments with the hydride acceptors B(C₆F₅)₃ and [Ph₃C]₂[B₁₂C₁₂] indicate that Na-1-BH₃ can donate hydrides to form cations of formula [Na(MeOCH₂CH₂OMe₂Si)₃CBH₂]⁺.     

Geochemical investigation of alluvial sediments: validation of ICP-OES determination of heavy metals. A case study from the Utrata River Valley (central Poland)

The development and validation of a reliable analytical procedure for the determination of selected metals (Cd, Cr, Cu, Pb, Zn and Mn) in sediments accumulated in the Utrata River (Poland) is described. The aqua regia extraction followed by inductively coupled plasma optical emission spectrometry (ICP-OES) was used for this purpose. The optimized analytical procedure was validated, and adequate quality control actions were implemented in order to provide reliable data. The precision under’ within-laboratory’ reproducibility conditions was estimated from duplicate analysis. Certified reference material (CRM) was used in order to evaluate the accuracy of the results regarding the sewage sludge amended soil CRM 143R. The detection limits for all elements of interest were well-below their content in the investigated sediment samples. The obtained reliable data could be used for assessment of the relationship between human economic activity in the past and the geochemical features of the sediments.     

Oxidation stability of various Ti-alloys

Since titanium metal first became a commercial reality in 1950, corrosion resistance has been an important consideration in its selection as an engineering structural material. Titanium has gained acceptance in many media where its corrosion resistance and engineering properties have provided the corrosion and design engineer with a reliable and economic material. Titanium, like any other metal, is subject to corrosion in environments of air, oxygen, moisture, and so on. In this work, high-temperature stability of Ti and various Ti-alloys (by ASTM standard) was investigated. The best results showed that for Ti-Gr.5 alloy, the oxidation at 800 °C was 3.39% and at 900 °C 8.35%. For the comparison, commercial pure Ti-alloys Ti-Gr.2 and Ti-Gr.37 containing Al were used, whereas the oxidation resistance was much worse.