醇-水混合溶剂中双亲水嵌段共聚物对CaCO3粒子形貌的调控

合成形态、大小及结构受到人为调控的无机材料是现代材料科学的一个重要研究方向, 通过生物模拟方法可望实现各类有机添加剂及模板对无机物形貌与结构的有效调控[1,2]. 近年来, 一类新型的无机晶体生长调控剂--双亲水嵌段共聚物[3]已成功地用于多种无机粒子形貌的有效调控. 双亲水嵌段共聚物由2个与无机表面亲和作用不同的亲水链段构成, 在其水溶液中, 已实现了具有一系列特殊形貌的碳酸钙[4~6]、磷酸钙[7]及硫酸钡[8]粒子的生物模拟合成. 人们已陆续报道了在多种有机添加剂及模板作用下典型的生物矿物CaCO3的生物模拟合成[9,10]. 我们曾系统地研究了水溶液中双亲水嵌段共聚物对CaCO3粒子形貌的调控作用[6],最近又在双亲水嵌段共聚物-表面活性剂混合溶液中合成出具有新颖形貌(如空壳状等)的CaCO3粒子[11]. 本文考察了醇-水混合溶剂中双亲水嵌段共聚物对CaCO3粒子形貌的调控作用, 初步揭示了溶剂特性对该调控作用的显著影响.     

镁铝型水滑石水热合成

水滑石是一类具有特殊结构的层状无机材料 .具有可调变的组成及独特的结构和性能 ,在离子交换、吸附分离、催化、医药等领域得到广泛应用 [1～ 4 ] .特别是水滑石类材料所具有的选择性、红外吸收性和离子交换性等一些特殊性能 ,使其作为新型无机功能材料已应用于 PE农膜 (保温剂 )和 PVC(无毒热稳定剂 )等高分子材料中 ,显示了独特的性能[5] .作为无机功能材料 ,水滑石在复合材料中的应用必然涉及其粒子尺寸和分布 ,因此对水滑石晶化规律的研究非常重要 .水滑石成熟的合成方法是共沉淀法[6] ,如单滴法、双滴法 .由于沉淀粒子是渐次产生 ,…     

超分子化合物｛[8-hydroxyquinolineH]_4~(4+)·[SiW_(12)O_(40)]~(4-)·2H_2O｝的水热合成、晶体结构及热稳定性

近些年来,合成和研究开发新型结构的有机鄄无机配合功能性材料日益成为人们关注的热点[1￣3]。金属杂多酸盐以其独特的分子结构及理化性质,已经成为构造新型分子功能材料的重要无机构筑块,作为电子受体的金属杂多酸盐可以与有机π电子给体如TTF、ET和有机金属茂合物结合,形成有机鄄无机复合物。该类化合物在光、电、磁、催化和超导领域有潜在的应用前景[4￣6],它们的结构不同,性质各异,其中一些具有超分子结构[7]。本研究通过水热合成法,合成了一种未见报道的Keggin结构硅钨酸盐超分子化合物｛[8鄄hydroxyquinolineH]44·+[SiW12O40]4·…     

双亲水嵌段共聚物存在下特殊形貌的BaC2O4晶体合成

近年来 ,无机新型材料已经广泛应用于各个技术领域 ,而对于所合成材料的大小和形貌的调控已经成为该材料能够应用于催化、药物、电子、陶瓷、染料和化妆品等领域的一个关键因素[1 ] .利用水溶性有机添加剂作为晶体生长的诱导剂来控制无机晶体的形貌和晶型已有很多报道 .例如 :多种生物分子[2～ 5] 和普通合成的大分子添加剂[6] 对 Ca CO3 晶体在成核、晶化和生长过程中的晶型和形貌有着明显的控制作用 .近年来 ,双亲水嵌段共聚物的功能型高分子 (DHBC) [7]已经发展成为能够有效控制无机晶化过程的新型晶体生长的调控剂 .这类高分子通常是…     

利用室温固态反应制备球霰石型CaCO3粒子

合成形态、大小及结构可人为调控的无机材料是现代材料科学的重要研究方向[1]. 借助于各类有机添加剂及模板剂的调控作用, 可利用溶液合成方法制备出形貌与结构受到有效调控的无机粒子[2,3]. 室温固态化学反应已被成功地应用于多种无机纳米粒子[4]及纳米线[5]的合成, 并显示出高效、节能、无污染和操作简便等优点, 因而在材料合成领域具有应用前景[6].     

"面包圈"状高有序度大孔径介孔分子筛SBA-15的合成

介孔材料因其高度有序的大孔径、较佳的催化吸附性能、良好的电磁性质及易于剪裁而引起人们极大的兴趣[1～9].人们已相继合成了介孔氧化硅薄膜[3,10]、球[12]、空心球[4,13]和纤维[12～15]等,并设法控制中孔材料晶体外貌[3～9,15～21].最近,我们报道了利用多相组装和无机晶体(如NaCl,LiCl)作大孔结构导向剂的方法[16],合成了人造"珊瑚"状介-大孔氧化硅膜[13].Lin等[17]用共表面活性剂法在丁醇存在下合成了多组有序结构的介孔氧化硅空心球; Shio等[21]在完全溶解的硅酸钠和阳离子表面活性剂溶液中,合成了细棒状介孔氧化硅粉末.本文报道一种控制介孔材料颗粒外貌和形状的新方法,即共溶剂法,并以此法合成了高有序度、大孔径、 "面包圈"状介孔氧化硅SBA-15.这种新材料有望在微加工、催化、生物分离、电子器件的矿化、色谱载体等方面得到应用[1～9].     

离子液体中制备无机材料

离子液体作为潜在的“绿色”溶剂,具有许多传统溶剂无法比拟的优异性能,在有机合成、催化、液液分离和萃取等领域引起了广泛的研究。而在离子液体领域无机材料的制备是一个较新的发展分支,现已利用其合成出多种具有独特结构和性能的无机材料。本文就离子液体在无机材料制备方面的应用及发展趋势进行了综述。目前,对于制备无机材料,离子液体主要是作为电解液、表面活性剂或溶剂,本文介绍了其在应用中的优缺点,并指出该领域未来的发展趋势是离子热合成和集模板-溶剂-反应物于一身的离子液体反应。     

活性聚苯乙烯膜诱导碳酸钙异相成核结晶

0引言生物矿物材料(如骨、牙齿、贝壳等)的优异性能[1]使得无机材料的仿生合成(又称有机模板合成)成为近年来研究的热点之一[2]。该合成技术的优点是,通过有机物分子与无机离子的相互作用,能够在温和的条件下合成出具有多级结构、特殊形貌和优异性能的有机/无机复合材料。CaCO3     

离子液体在无机纳米材料合成上的应用

室温离子液体作为一种新型的绿色环保溶剂,在无机纳米材料合成中的应用引起越来越多研究者的注意。目前,已经利用室温离子液体合成出了纳米多孔材料、纳米粒子和中空球、一维纳米材料等。与传统的溶剂相比,离子液体在合成过程中体现出了很多优势,且合成的产物也不同,为无机纳米材料的合成开辟了一条新途径。本文就近年来国内外相关研究进展,对离子液体在无机纳米材料合成中的应用进行综述。     

无机纳米稀土发光材料的制备方法*

无机纳米稀土发光材料作为一种重要的发光材料,由于具有独特的光、电和化学性质,使其在高性能磁体、发光器件、显示、生物标记、光学成像和光学治疗等方面得到了广泛的应用。稀土发光材料的这些性质与材料的尺寸和形状密切相关,近年来研究者已经利用多种合成方法制备了不同形状的纳米稀土发光材料,包括纳米线、纳米棒、纳米管、纳米纤维和纳米片等。本文综述了无机纳米稀土发光材料的几种常用的制备方法,包括水热/溶剂热法、有机/无机前驱体热分解法和超声辅助合成法等,评述了这些方法的优缺点,并结合课题组在无机纳米稀土发光材料制备方面的工作,对无机纳米稀土发光材料制备方法的发展进行了展望。     

Thermochemistry of decomposition of manganese(II) oxalate dihydrate

Differential scanning calorimetry (DSC) has been used to determine the enthalpy of dehydration of manganese(II) oxalate dihydrate and the enthalpies of decomposition in nitrogen and in oxygen of the anhydrous oxalate. The thermodynamic data have been related to the activation energies reported in kinetic studies and to the mechanisms proposed for the thermal decomposition and oxidation processes.     

Titrimetric, coulometric and spectrophotometric determination of manganese following perchloric acid oxidation in the presence of pyrophosphate

Manganese is oxidized quantitatively to a violet, tervalent pyrophosphate in a boiling mixture of equal parts of perchloric acid and phosphoric add. This Mn(III) can be titrated potentiometrically or coulometrically with iron(II); it can also be measured spectrophotometrically. If the titrimetric method is carried out with titanium (III) or chromium(II), iron can also be titrated immediately after the manganese. The methods were applied to a new reference sample, ISU 600 Manganiferous Iron Ore, and to manganese ore, spiegeleisen, ferromanganese, and rail steel. Manganese(II) oxalate dihydrate has been reinvestigated as a primary standard and is highly recommended.     

The influence of sample cells for differential thermal analysis in controlled atmospheres

DTA curves for the thermal decomposition of uranyl oxalate trihydrate and ammonium vanadyl oxalate dihydrate, using different DTA instruments, are compared. It is shown that widely differing and misleading results can be obtained by an incorrect choice of sample cell. The anomalous effects are discussed in terms of the geometry of the sample holders and the consequent ease of removal of product gases and accessibility of the reactant gas.It is recommended that uranyl oxalate trihydrate could be used to assess the conditions of flow-rate, sample size, etc., necessary to achieve correct atmosphere control with a given DTA cell.     

Characterisation and thermal analysis of vanadium(II) oxalate

The synthesis, compositional formula and mode of thermal decomposition of a compound for which there existed only a single literature reference [1] have been investigated in this work.The product of the aqueous phase reaction between vanadium(II) ions and oxalate ions at lowpH has been identified: vanadium(II) oxalate dihydrate, VC₂O₄·2H₂O, has been characterised by thermal methods of analysis supported by a range of complementary analytical techniques.The findings of a previous author [1] have been confirmed and extended in this work. In addition, a synthetic procedure for the preparation of gram quantities of vanadium(II) oxalate dihydrate, VC₂O₄·2H₂O, is reported here for the first time.The oxalate compound prepared was found to be remarkably stable in relation to aerial oxidation, unlike other representative solid state compounds of the vanadium(II) oxidation state. Vanadium(II) oxalate dihydrate may, therefore, serve as an important intermediate in the future synthesis of other vanadium(II) compounds.We would wish to thank Mr. S. Sutcliffe, University College Salford, for providing the Thermal Analysis data and also Mr. S. Unsworth, Magnesium Electron, Clifton, Manchester, for providing the XRD data.     

FT-Raman spectroscopy of lichens on dolomitic rocks: an assessment of metal oxalate formation

The FT-Raman spectra of five epilithic lichen taxa growing on dolomite and magnesium-rich carbonate rocks have been analysed and interpreted for the key molecular marker bands associated with calcium oxalate monohydrate (whewellite), calcium oxalate dihydrate (weddelite) and magnesium oxalate dihydrate. From the results, it can be concluded that the biomineral product of lichen biodeterioration involves the calcareous part of the substratum only; no trace of magnesium oxalate has been found in the Raman spectra. Two of the species, Lecanora sulfurea and Aspicilia calcarea, produce calcium oxalate monohydrate exclusively, but Dirina massiliensis f. sorediata, D. massiliensis f. massiliensis and Tephromela atra produce significant quantities of the dihydrate. An explanation is advanced for the exclusive accumulation of calcium oxalate into the lichen thallus despite the significant presence of magnesium ions.     

Thermal decomposition of oxalates. Part 15. Effect of container material on DTA results for thermal decomposition of magnesium oxalate

During the study of the thermal decomposition of magnesium oxalate dihydrate certain anomalies were noted. It was found that even in the presence of oxygen the decarboxylation peak was endothermic except in the presence of a catalyst. In a platinum crucible results were found to be different from those in a porcelain crucible due to the platinum acting effectively as a catalyst.     

Thermal decomposition of hydrated iron(II) oxalate and manganese(II) oxalate in vacuum

The thermal decomposition of hydrated iron(II) oxalate and manganese(II) oxalate under high vacuum conditions (10^–5 mm Hg) has been studied by differential thermal analysis. The decomposition in vacuum of iron(II) oxalate is exothermic, while that of manganese(II) oxalate is endothermic. An explanation is offered for this behaviour.The financial support by National Bureau of Standards, U.S.A., through a PL-480 scheme is gratefully acknowledged.     

草酸镁二水合物的非等温热分解动力学

The thermal decomposition of the magnesium oxalate dihydrate in a static air atmosphere was investigated by TG-DTG techniques. The intermediate and residue of each decomposition were identified from their TG curve. The kinetic triplet, the activation energy E, the pre-exponential factor A and the mechanism functionsf（a） were obtained from analysis of the TG-DTG curves of thermal decomposition of the first stage and the second stage by the Popesou method and the Flynn-Wall-Ozawa method.     

The use of thermal analysis in determination of some urinary calculi of calcium oxalate

The human urinary calculi are mainly constituted by calcium oxalate, magnesium ammonium phosphate hexahydrate, and uric acid. The ions or molecules are easily characterized by wet chemical methods. The difficulties appear in the differentiation of the hydrates of calcium oxalate (monohydrate COM or Whewellite, and dihydrate COD or Weddelite). A high level of COD in the urinary stones leads, often, inflammation, sharp pain and blood in urine. In the worse cases, they must be extracted by surgical way. The identification of the main components of urinary calculi, the knowledge of the true number of water molecules bounded to the calcium oxalate, and the determination of each hydrate in the mixture, are the interests of this memory. The thermal analysis (simultaneous DTA-TG) was applied on thirty-three urinary calculi. The determination of the calcium oxalate hydrates was confirmed by calorimetry (DSC). This revised version was published online in July 2006 with corrections to the Cover Date.     

A Raman spectroscopic study of thermally treated glushinskite--the natural magnesium oxalate dihydrate

Raman spectroscopy has been used to study the thermal transformations of natural magnesium oxalate dihydrate known in mineralogy as glushinskite. The data obtained by Raman spectroscopy was supplemented with that of infrared emission spectroscopy. The vibrational spectroscopic data was complimented with high resolution thermogravimetric analysis combined with evolved gas mass spectrometry. TG-MS identified two mass loss steps at 146 and 397 degrees C. In the first mass loss step water is evolved only, in the second step carbon dioxide is evolved. The combination of Raman microscopy and a thermal stage clearly identifies the changes in the molecular structure with thermal treatment. Glushinskite is the dihydrate phase in the temperature range up to the pre-dehydration temperature of 146 degrees C. Above 397 degrees C, magnesium oxide is formed. Infrared emission spectroscopy shows that this mineral decomposes at around 400 degrees C. Changes in the position and intensity of the CO and CC stretching vibrations in the Raman spectra indicate the temperature range at which these phase changes occur.