基础成分配比对白云鄂博尾矿微晶玻璃结构及性能的影响

以白云鄂博二次选后尾矿和粉煤灰为主要原料,采用熔融法制备得到了CaO-MgO-Al2O3-SiO2系尾矿微晶玻璃.制备流程包括熔融、退火、核化及晶化过程.其中玻璃熔融温度为1450℃,核化温度为720℃,晶化温度为850℃.利用XRD研究了基础玻璃成分配比对微晶玻璃结构的影响.结果表明基础玻璃成分配比直接决定微晶玻璃的主晶相形成.随着基础玻璃成分配比的变化,微晶玻璃可能形成辉石相、钙长石相、镁铁尖晶石相或磁铁矿相.当其他元素固定,CaO/MgO和CaO/Al2O3比值的减小会导致微晶玻璃由辉石相转变为镁铁尖晶石相和钙长石相.而当SiO2/CaO比值大于2时,主晶相则由辉石相转变为磁铁矿相.DTA测试结果表明CaO有利于析晶温度的降低,而MgO、Al2O3和SiO2相对提高了析晶温度.力学性能测试表明抗折强度、密度、耐酸碱度与微晶玻璃主晶相有直接关系.主晶相为辉石相的微晶玻璃具有更高的抗折强度、密度和耐酸性.     

Fe2O3对纳米晶尾矿微晶玻璃结构及性能的影响

以铁尾矿和金尾矿为主要原料,采用熔融法制备了添加0 ～ 20wt; Fe2O3的CaO-MgO-Al2O3-SiO2(CMAS)系纳米晶尾矿微晶玻璃,利用差示扫描量热分析(DSC)、X射线衍射分析(XRD)、红外光谱(IR)、扫描电镜(SEM)和综合力学性能仪等测试手段,研究了Fe2O3含量对该体系微晶玻璃显微结构及性能的影响.实验结果表明:随着Fe2O3含量的增加,样品的晶化温度和玻璃化转变温度逐渐降低;且Fe2O3可促进主晶相透辉石相(Mg0.6Fe0.2Al0.2) Ca(Si1.5Al1.5)O6的形成;同时Fe2O3能够有效减小透辉石相平均晶粒尺寸;另外,微晶玻璃的密度、显微硬度和耐碱性随晶粒尺寸的减小而增加,而抗折强度和耐酸性随晶粒尺寸的减小而降低.     

烧结法制备高炉渣CMAS系统微晶玻璃的研究

利用高炉渣及其它辅助原料制备基础玻璃,采用一步烧结法制备主晶相为辉石的CaO-MgO-Al2O3-SiO2(CMAS)微晶玻璃.综合运用DSC,XRD以及场发射扫描电子显微镜等测试手段,分析热处理制度对高炉渣CMAS微晶玻璃的析晶行为及性能的影响.结果表明:随着热处理温度上升,微晶玻璃的主晶相均为辉石,次晶相均为长石,晶相析出量增加,微晶玻璃的体积密度及抗折强度均呈现先增后减趋势.随着热处理时间增加,微晶玻璃的体积密度及抗折强度均呈现下降趋势.当热处理温度为1020 ℃,晶化时间30 min时,样品的机械性能最好,体积密度为2.690 g·cm-3,抗折强度为67.00 MPa.     

Fe2O3对CaO-Al2O3-MgO-SiO2系微晶玻璃析晶及断裂特性的影响

采用熔融法,利用纯化学试剂制备了CaO-A12O3-MgO-SiO2 (CAMS)系微晶玻璃,利用DTA、XRD、拉曼光谱仪等研究了Fe2O3对微晶玻璃析晶特性的影响规律,微晶玻璃的物化性能由抗折强度、杨氏模量、剪切模量、泊松比、维氏硬度等进行评价.结果表明,微晶玻璃的析晶特性随着Fe2 O3含量的增加而增强,对应母体玻璃中首先出现富铁相,进而促进辉石主晶相的析出.微晶玻璃的断裂特性及裂纹扩展方式均随析晶度的提高得到明显改善.但过量的Fe2O3添加则对微晶玻璃的析晶特性无明显影响,反而降低了玻璃相的致密性.微晶玻璃的耐酸性、抗折强度、杨氏模量及剪切模量均呈现先增加后降低的趋势,微晶玻璃的Fe2 O3含量为6.6wt;时综合性能最优.     

熔融法转炉钢渣微晶玻璃的结构与性能研究

利用转炉钢渣制备出高性能的微晶玻璃,可有效提高其附加值,同时具有环保效益.本文以转炉钢渣为主要原料,通过组分设计,改变其掺人量,制备出了相应的基础玻璃与微晶玻璃.并通过XRD、DSC、FTIR、SEM以及抗折强度、密度、表面硬度等进行表征,获得了如下结果:转炉钢渣的掺量在45wt; ～ 55wt;之间变化时,均可以制备出微晶玻璃.随着CaO/SiO2的增加,有利于促进玻璃析晶,与此同时,会促进在架状结构的霞石晶相中析出聚粒状的二次晶相普通辉石.普通辉石晶相的析出不利于抗折强度的增长,但对密度和硬度均有所提高.当钢渣掺量为50wt;时,微晶玻璃的最高抗折强度为198.89 MPa,显微硬度为772 MPa,密度为2.86 g/cm3.     

Pr2O3对含Cr2O3辉石系矿渣微晶玻璃晶化行为的影响

以白云鄂博西尾矿和粉煤灰为主要原料,分别制备了添加0,2.0wt;,4.0wt;和6.0wt; Pr2O3的辉石系矿渣微晶玻璃;综合采用基于DSC/DTA结果的析晶活化能Ek、Avrami指数以及粘流活化能Eη和背散射电子SEM显微形貌分析研究了Pr2O3对析晶的影响.结果表明在所研究范围内,Pr2O3含量的提高在整体上抑制了辉石相的析出.其原因除了与富Pr颗粒相对辉石相在析晶过程中的“钉扎”有关外,还与Pr2O3含量提高后使基础玻璃网络聚合程度加大,从而增大了辉石相形成所需离子扩散的阻力有关.     

铁含量及价态对白云鄂博尾矿微晶玻璃析晶特性及性能的影响

以白云鄂博尾矿及粉煤灰等固体废弃物为主要原料,采用熔融法、经退火、核化及晶化热处理制备得到了以辉石为主晶相的CaO-MgO-Al2O3-SiO2 (CMAS)系尾矿微晶玻璃.利用化学分析方法测定了不同氧化铁及碳含量对微晶玻璃中Fe3+/Fe2+的影响;利用XRD、DTA、SEM等研究了不同氧化铁及碳含量对微晶玻璃结构及析晶特性的影响.结果表明,不同氧化铁添加量对微晶玻璃中Fe3+/Fe2影响很小,因此对微晶玻璃的析晶特性无本质影响.而随着还原碳粉的加入,Fe3+/Fe2与未加碳粉相比减小明显,微晶玻璃中FeO质量分数的增加极大地提高了微晶玻璃的析晶特性.但过量的碳粉加入导致单质铁的析出,反而降低了微晶玻璃的析晶能力.上述析晶特性的变化直接影响到微晶玻璃的耐酸度及抗折强度.     

熔融法制备金尾矿微晶玻璃及性能研究

以金尾矿为主要原料,采用熔融法制备CaO-Al2O3-SiO2系微晶玻璃.利用差热分析(DSC)、X射线衍射分析(XRD)、扫描电镜(SEM)等分析手段对所制备的微晶玻璃进行了分析测试与表征,并研究了不同晶化温度对制得微晶玻璃的物相组成、微观结构及性能的影响.结果表明:在850～ 950℃下,随着晶化温度的提高,所制备微晶玻璃的性能均提高.确定较佳的晶化制度为950℃保温3h,所制备微晶玻璃的热膨胀系数、抗折强度及密度分别为68.7×10-7/℃,122 MPa和2.836 g/cm3.     

Al2O3对辉石质陶瓷烧结性能的影响

以钢渣尾泥为原料制备了辉石质陶瓷,并通过对陶瓷制品物理性能测试和XRF、XRD、SEM分析,研究了Al2O3组分对辉石质陶瓷烧结过程结构演变过程及陶瓷物理性能的影响规律.研究表明,随着烧结温度升高,陶瓷中铝离子首先参与形成钙长石,并随着钙长石晶相消失而进入液相;部分铝离子进一步扩散,使得透辉石相转变为固溶铝离子的普通辉石相.在本实验条件下,氧化铝含量较低的样品具有较高的烧结温度(1210℃)和较高的强度(93.74 MPa).氧化铝含量的增加使陶瓷形成较多的玻璃相和内部微裂纹,从而降低其力学性能.     

熔制坩埚对CaO-Al2O3-MgO-SiO2系矿渣微晶玻璃结构与性能的影响

以白云鄂博二次选后尾矿、高炉渣和粉煤灰为主要原料,采用熔融法分别在氧化铝坩埚和石墨坩埚熔制制得CaO-Al2O3-MgO-SiO2 (CAMS)系微晶玻璃,利用DSC、XRD、SEM、EDS、ICAP、XPS等测试手段,研究了不同坩埚熔制对微晶玻璃成分、显微结构及性能的影响.研究表明:高温玻璃熔液对氧化铝坩埚的侵蚀作用及石墨坩埚的还原作用,使基础玻璃中Al2O3和Fe2O3含量发生较大变化,氧化铝坩埚熔制制备的基础玻璃有一个析晶峰,温度为905 ℃,对应的微晶玻璃主晶相为含铁透辉石Ca(Mg,Al) (Si,Al)2O6,而石墨坩埚熔制制备的基础玻璃出现两个析晶峰,温度分别为866℃和805℃,对应的微晶玻璃主晶相透辉石Ca(Mg,Al) (Si,Al)2O6和次晶相柯石英SiO2,由于以上原因导致制备的微晶玻璃在显微结构及理化性能上也存在一定的差异.     

On the inhomogeneity of the transition surface layer of the solid core of the earth

Different geophysical data and conclusions of theoretical models, which can give information about the behavior of the solid and liquid cores of the Earth as well as about the existence of a transition layer as a temperature-hysteresis region at a relatively weak first-order phase transition, are compared. It is concluded that liquid inclusions inevitably exist in this region; these inclusions are involved (due to the complex convective processes occurring in the liquid core) in the transport of light materials from some areas of the solid-core surface. The porosity and permeability of the transition layer determine the seismic acoustic inhomogeneities in these areas, which contact the convective flows in the liquid core. In particular, this explains the well-known ??east-west?? effect. Obviously, the model of the crystalline core is not the only possible alternative for a model of a core with a metallic glasslike structure.     

On the role of the porous shell of the solid core of the earth in the anomalous heat and mass flow to the mantle

The model of the pressure-induced first-order phase transition of a metal melt to the metallicglass state considers a thermodynamically nonequilibrium porous near-surface shell of the solid core of the Earth, which contacts cyclonic vortices in the liquid core. Anomalous flows of heat and light-material mass to the mantle from the solid core at these contact points are calculated. These anomalous flows are shown to be comparable with the observed ones under the assumption of a rapid increase in the melt viscosity at pressures of 1–10 Mbar, which is characteristic of a solid core. In this case, the porous layer permeability may be very low.     

Influence of the Crystal Structure of the Nucleus on the Morphology of t-ZnO Tetrapods

Crystallography Reports - A new approach to simulating the morphology of hierarchical nanocrystals has been proposed on the example of ZnO nanotetrapods. Within this approach, twinning is...     

Features of the magnetic state of the layered Fe-V nanostructure of the superconductor-ferromagnet type

The magnetic state of the V(39 nm)/20 [V(3 nm)/Fe(3 nm)] nanostructure has been investigated by polarized neutron reflectometry in the temperature range from 1.6 to 30 K in magnetic fields from 0.2 to 15 kOe. The data obtained indicate that the superconductivity of vanadium layers may affect magnetic ordering both over the depth of the structure and in its plane.     

Study of the influence of the rare-earth elements on the properties of lead iodide

Lead iodide (PbI₂) shows excellent electronic properties for detection of ionizing radiation. We report the introduction of rare-earth elements and other elements as admixtures during synthesis to study their influence on the quality of single crystals. Synthesized material as well as single crystals have been characterized by measurements of electrical resistivity and low-temperature photo luminescence and index of refraction. The structural quality with respect to polytypes was analysed by electron back scatter diffraction. Makyoh topography was applied for surface studies.     

Effect of the temperature on the TMOS sono-hydrolysis and a study of the structure of the resulting aged sonogels

The effect of temperature on the oxalic acid catalyzed sono-hydrolysis of tetramethoxysilane (TMOS) was studied by means of a heat flux calorimetric method. The activation energy of the process was measured as (24.5 ± 0.8) kJ/mol in the temperature range between 10 and 50 °C. The structural characteristics of the resulting sonogels, after long period of aging in saturated conditions, were studied by means of small angle X-ray scattering. The structure can be described as formed by ∼2.7 nm mean size mass fractal-like aggregates (clusters) of primary silica particles of ∼0.3 nm mean size, all imbibed in a liquid phase. The average mass fractal dimension of the clusters was found to be 2.58. The primary particle density was estimated as 2.23 g/cm³, in good agreement with the value frequently quoted for fused silica. The volume fraction of the clusters in the saturated sonogels was estimated as about 28%. The moment in which the meniscus of the liquid phase penetrates into the clusters under rapid evaporation process has been detected by an inflection in the first derivative of the curve of weight loss in a simple thermogravimetric test.     

A new example for the applicability of the relationship between the particle size and the kinetic of the crystal growth

Experiments have been made with PbCrO₄ precipitating system in a batch type tank. In the experiments the speeds of stirring and the residence times were changed. The particle size distribution of precipitates formed has been determined. The rate determining mechanism of the crystal growth were evaluated by two different methods (NIELSEN method and method elaborated in our institute). The two methods used have indicated the same informations about the rate determining processes. It also has been stated that the coagulation does not disturb the selection of the suitable growing mechanism.     

Ordering of cations in the voids of the anionic framework of the crystal structure of catapleiite

The pseudohexagonal crystal structure of the mineral catapleiite Na_1.5Ca_0.2[ZrSi₃(O,OH)₉] · 2(H₂O,F) from the Zhil’naya Valley in the central part of the Khibiny alkaline massif (Kola Peninsula, Russia) is studied by X-ray diffraction (XCalibur-S diffractometer, R = 0.0346): a = 20.100(4), b = 25.673(5), and c = 14.822(3) Å; space group Fdd2, Z = 32, and ρ_calcd = 2.76 g/cm³. Fluorine atoms substituting part of H₂O molecules in open channels of the crystal structure have been found for the first time in the catapleiite composition by microprobe analysis. The pattern of distribution of Na and Ca atoms over the voids of the mixed anionic framework consisting of Zr-octahedra and three-membered rings of Si-tetrahedra accounts for the pronounced pseudoperiodicity along the a and c axes of the pseudohexagonal unit cell and for the lowering of crystal symmetry to the orthorhombic one. It is shown that part of the hydrogen atoms of water molecules is statistically disordered; their distribution correlates with the pattern of the population of large eight-vertex polyhedra by Na and Ca atoms.