Synthesis and Structure of a Dinuclear Copper（Ⅱ）- ditetrazolate Involving in situ Ligand Synthesis

The hydrothermal reaction of 1,2-dicyanobenzene with NaN3 in the presence of CuCl2, 2,2′-bipyridine and H2O affords a novel dinuclear copper(II)-ditetrazolate, [Cu(bpy)- (pdtz)]2 (Hpdtz = 5,5′-1,2-phenylene-ditetrazole, bpy = 2,2′-bipyridine). The pdtz ligand is generated in situ through Sharpless 2 3 cycloaddition reaction. Its crystal structure was deter- mined by single-crystal X-ray diffraction method. The crystal crystallizes in the monoclinic system, space group P21/n with a = 8.2096(16), b = 18.580(4), c = 11.838(2) , β = 103.12(3)o, V = 1758.5(6) 3, Z = 2, Mr = 863.83, Dc = 1.631 g/cm3, F(000) = 876 and μ = 1.272 mm-1. In this novel dinuclear structure, the pdtz ligand adopts a peculiar μ2-η1,η2 coordination mode.     

新疆阿克提什坎金矿床稀土元素地球化学研究

研究了新疆阿尔泰特地区阿克提什坎金矿床的稀土元素及矿区二长花岗岩平衡的热液中稀土元素的组成特征及配分模型，并应用Grang等位线方法讨论了热液蚀变作用过程中稀土元素的行为。研究表明，在热液蚀变作用过程中，稀土元素保持惰性，成矿热液与岩浆热液关系不大，成矿物质主要来源于围岩。     

低温热液条件下有机质富集金机理的实验研究

本文在低温(40—200℃)热液条件下,对不同成熟度的有机质与含金溶液[AuCl_4~-,Au(HS)_2~-]之间的相互作用进行了实验研究。研究观察到在低温热液体系中有机质直接参与了从含金溶液中将游离的金离子固定下来的作用。有机质从溶液中富集金可认为有两种不同性质的作用:第一种是在早期沉积成岩作用阶段(T<120°)时,有机质与含金热液主要发生凝聚作用,使溶液中的金由离子状态从无机相转化到有机相中;第二种是在变生或变质作用阶段(T>120℃)时,有机质与含金热液主要发生氧化还原沉淀作用,还原作用的结果导致元素金的沉淀,同时有机质被氧化、分解。     

单轴压缩条件下溶蚀礁灰岩细观变形破坏特征研究

礁灰岩的溶蚀对海洋工程和岛礁工程的稳定性有明显的影响.孔隙型溶蚀是礁灰岩常见的溶蚀方式.本文通过构建随机溶蚀孔洞的离散元模型,模拟孔洞型溶蚀礁灰岩的细观变形破坏特征,分析其变形破坏规律与裂隙演化特征.结果 表明,基于随机聚类算法构建的溶蚀礁灰岩离散元模型能够很好地模拟孔洞型溶蚀作用,且其变形破坏特征具有明显的规律;随着...     

Stable Electron Field Emission from CeO2 Nanowires by Hydrothermal Method

CeO2 nanowires are successful synthesized by hydrothermal method and their field emission （FE） properties are investigated. The turn-on electric field is 5.8 V/μm at an emitter-anode spacing of 700μm. The FE current is stable and the current fluctuations are less than 3% over 5 h. All the plotted Fowler-Nordheim curves yield straight lines, which are in agreement with the Fowler-Nordheim theory. The relationship between the field enhancement factor β and the emitter-anode spacing d follows a universal equation. Our results imply that the CeO2 nanowires are promising materials for fabricating FE cathodes.     

溶蚀岩体三维随机洞体数学模型的设计

溶蚀岩体是地质体中一种特定的岩体 ,它在水流等自然因素作用下 ,生成了许多溶蚀洞体 ,本文首先对作为其载体的三维地质体进行数学描述和显示 ,然后对如何确定椭球洞体形状和大小、复杂洞体的生成、三维随机洞体的数学模型以及确定性洞体的数学描述和计算机显示进行了详尽的阐述。本文提出的溶蚀岩体三维随机洞体的数学模型为溶蚀岩体的溶蚀率和渗透特性的研究提供了可视化手段 ,能够有力地指导溶蚀岩体三维随机洞体的计算机显示的编程实践     

塔里木盆地奥陶系碳酸盐岩热液蚀变类型及蚀变流体的分带特征

已探明塔里木盆地下古生界碳酸盐岩地层储量巨大。对塔里木盆地西北部柯坪-巴楚-阿图什一带的4块区域开展了系统的野外和重点观测工作,包括蓬莱坝剖面、柯坪水泥厂剖面、托普郎剖面等。本研究通过考察塔里木盆地奥陶系碳酸盐岩热液溶蚀及相关现象。从野外产状、伴生关系以及矿物岩石学特征角度解剖奥陶系地层中热液矿物组合的地质特征。研究表明,该区域存在富镁流体、富氟流体和富硫流体3种流体,分别来源于封存卤水、火成活动和TSR热液。不同性质流体蚀变具有相似的分带性。     

Hydrothermal Synthesis and Crystal Structure of a Novel Binuclear Cd（ Ⅱ ） Coordination Polymer Based on 1,2-Benzenedicarboxylate and Imidazole

The hydrothermal reaction of Cd（OAc）2.H2O with 1,2-benzenedicarboxylate （1,2-BDC）, imidazole and H2O resulted in the formation of a binuclear polymeric Cd（ Ⅱ ） complex {[Cd2（1,2-BDC）2（Im）4].（H2O）}n which was then characterized by elemental analyses and single-crystal X-ray diffraction analysis. The crystal is of monoclinic system, space group P21/c with a = 14.6455（3）, b = 9.3530（2）, c = 23.7838（5）A, β= 106.6290（10）°, Cl12H104CdgN32O36, Mr = 3373.47, V = 3121.64（11）A^3, Dc = 1.795 g/cm^3, F（000） = 1672,μ= 1.428 cm^-1 and Z = 1. The final R = 0.0316 and wR = 0.0687 for 5045 reflections with I 〉 2σ（I）. In the title complex, the two Cd（ Ⅱ） ions are in different coordination environments with distorted octahedral and pengonal bipyramidal geometries, respectively. Two Cd polyhedra are linked together through one μ2-η^1：η^1 and one μ2-η^1：η^1 carboxylate groups from different 1,2-BDC ligands, giving rise to a binuclear Cd（ Ⅱ ） cluster, and such clusters are connected by bridged 1,2-BDC ligands to form a 2-D structure along the c axis. The inter- and intermolecular hydrogen bonds further connect the 2-D structures into a 3-D supramolecular network.     

Synthesis, Characterization, and Properties of Supported Tungstozincate Bridged by Co(Ⅱ) Complex Fragment

[CoII(phen)3]2[{(ZnW12O40)CoII(phen)2(H2O)}2CoII(trien)2(NaH2O)2]·3H2O was synthesized via hydrothermal technique and characterized with elemental analyses, IR spectroscopy, TGA-DTA, and variable temperature magnetic susceptibility. The compound crystallized in the monoclinic system with the space group P21/n, a=1.8210 nm, b=2.3592 nm, c=2.2932 nm, β=110.31o, V=9.239 nm3, Z=2, R1=0.0827. The compound consists of two coordination cations, three lattice water molecules, and a macroanion [{(ZnW12O40)Co(phen)2(...     

单轴压缩条件下溶蚀岩体力学特性数值试验研究

工程尺度的溶蚀岩体难以开展室内外力学试验,导致溶蚀岩体的力学参数获取存在困难,因此基于岩石矿物含量特征、室内力学试验和岩体结构面特征,采用三维颗粒流离散元法,通过建立等效孔隙型溶蚀岩体模型进行单轴压缩数值试验,进而分析其力学特性和变形破坏机制。研究表明：采用改进平行黏结模型,基于细观矿物特征,通过元胞自动机算法剔除颗粒可建立孔隙型溶蚀岩体模型;加载前期,岩体结构面首先快速破坏而产生以剪切为主的微裂纹;随加载进行,岩块内逐渐产生以拉裂纹为主的破坏,其微裂纹呈指数增加,而结构面微裂纹先激增后趋于稳定;相同轴向应变时,岩块内拉裂纹随溶蚀率增加而增加,而结构面剪切微裂纹减少;岩体的变形破坏分为结构面快速破坏、岩块弹性变形、岩块塑性变形和岩体完全破坏等4个阶段,其破坏形式随溶蚀率增加而从整体均匀性破坏转化为局部结构性破坏;溶蚀使岩体强度降低,溶蚀率与单轴抗压强度和变形模量分别呈反比和负指数函数关系。