Fracture of LiF-MgF2 Precipitated Composites

The precipitation reaction in LiF-MgF₂ solid solutions was successfully used to toughen this composite. Incoherent, stable, rod-shaped MgF₂ precipitates were produced in the LiF matrix by quenching and aging treatments. They increased the fracture toughness of the system to >12 times that of undoped LiF single crystals. The maximum toughness was observed with 3 wt% MgF₂ after quenching and aging at 280°C for°300 min. The large toughness increase is attributed to pulling out of the incoherent MgF₂ rods and microcracking ahead of the primary crack.     

Chemical Interaction Between LiF and MgAl2O4 Spinel During Sintering

Reactions between LiF and MgAl₂O₄ at temperatures up to 1500°C are examined with a variety of tools, including differential scanning calorimetry, thermo-gravimetric analysis, X-ray diffraction, and scanning electron microscopy. LiAlO₂ and MgF₂ are found to be the active reaction products at these temperatures. A transient liquid phase comprising MgF₂ and LiF forms at intermediate temperatures, but then is consumed at higher temperatures during the reformation of MgAl₂O₄. If processed as an uncompacted powder mixture, all of the initial LiF in the system eventually vaporizes at temperatures exceeding 1300°C. A new reaction sequence relevant to the densification of LiF-doped MgAl₂O₄ spinel is proposed.     

Fluoride Model Systems: II, The Binary Systems CaF2–BeF2, MgF2–BeF2, and LiF–MgF2

Data obtained by quenching, thermal, and high-temperature X-ray techniques are presented for the three binary systems CaF₂–BeF₂, MgF₂–BeF₂, and LiF–MgF₂. The systems CaF₂–BeF₂ and MgF₂–BeF₂ are presented as weakened models of the systems ZrO₂–SiO₂ and TiO₂–SiO₂, respectively. The compound CaBeF₄ is a model of ZrSiO₄ (zircon). New data obtained for the system LiF–MgF₂ explain many discrepancies among the results of previous authors. Solid solution is almost complete between LiF and MgF₂ at elevated temperatures, but a small gap occurs at the eutectic (735°C.) with extensive exsolution at lower temperatures.     

Preparation of Whisker β-Spodumene Glass–Ceramics

β-spodumene glass–ceramics with a whisker-like microstructure were prepared from the following materials (in wt%): 64.5 SiO₂, 18.0 Al₂O₃, 4.2 Li₂O, 4 ZrO₂, and 8 MgF₂. Scanning electron microscope (SEM) analysis showed that phase separation in the base glass leads to the formation of a primary crystal phase of MgF₂ that promotes the formation of spherical β-spodumene. Whisker spodumene crystals surrounded by spherical crystals are observed at 720°C after 1 h, and the whisker crystals grow at the cost of spherical crystals with increasing temperature and time. The flexural strengths of the glass–ceramics reach a maximum of 228 MPa after heat treatment at 850°C for 1 h.     

Sintering of MgF2-LiF Solid Solutions

The influence of additions of 0, 2, 3.5, and 5% LiF on the sintering kinetics of MgF₂ were studied using microcylindrical samples on a hot-stage microscope. The sintering rate of MgF₂ was markedly enhanced, doubling at 650°C when the LiF was increased from 3.5 to 5 mol%. An approximate model is suggested explaining the observed sintering enhancement based on the increased concentration of fluorine ion vacancies.     

Purification, Growth of Single Crystals, and Selected Properties of MgF2

A modified Bridgman-Stockbarger method was used to grow single crystals of MgF₂ weighing about 200 g. The purity of the charge material was critical. Purification was achieved by first drying technical-grade MgF₂ and then vaporizing in vacuum. Spectral transmission of the single crystals was measured; in comparison with CaF₂, MgF₂ was slightly less transparent in the infrared region and had about the same transparency in the ultraviolet region. Modulus-of-rupture values were also obtained in several orientations. No plastic flow was observed.     

Discontinuous Dissolution of Iron Aluminate Spinel in the Al2O3–Fe2O3 System

When sintered 85Al₂O₃–15Fe₂O₃ (in wt%) specimens consisting of corundum grains and spinel particles were annealed at temperature where only a corundum phase was stable, phase transformation of spinel into metastable FeAIO₃ and subsequently complete dissolution of the metastable phase occurred together with the migration of grain boundaries at the surface of the specimens. Since the grain boundary migration was induced by grain boundary diffusion of Fe₂O₃ from the transforming and dissolving particles, the boundary migration by temperature decrease corresponds to a discontinuous dissolution of the spinel particles and a chemically induced grain boundary migration by temperature change. Inside the specimens, however, the transformation—dissolution and the grain boundary migration were suppressed because of unavailable accommodation of the volume expansion due to the transformation.     

Phase Equilibria and Structural Species in MgF2-MgO, MgF2-CaO, and MgF2-Al2O3 Systems

Partial equilibrium phase diagrams for the systems MgF₂-MgO, MgF₂-CaO, and MgF₂-Al₂O₃ were determined by differential thermal analysis. Simple eutectics were observed at 8.5 mol% MgO and 1228°± 3°C in the MgF₂-MgO system, at 7.5 mol% CaO and 1208°± 3°C in the MgF₂-CaO system, and at 2.5 mol% Al₂O₃ and 1250°± 3°C in the MgF₂-Al₂O₃ system. On the basis of agreements between the activities calculated by the Clausius-Clapeyron equation and Temkin's model using the present data, the eutectic melt consists of Mg²⁺, F^-, and O^2- ions in the MgF₂-MgO system; Mg²⁺, Ca²⁺, F^-, and O^2- ions in the MgF₂-CaO system; and Mg²⁺, Al³⁺, F^-, and AlO_2¯ ions in the MgF₂-Al₂O₃ system. Well-defined long needles of MgO in the MgF₂-MgO system, less defined needles of CaO in the MgF₂-CaO system, and Al₂O₃ grains in the MgF₂-Al₂O₃ system were observed by optical microscopy.     

Low-Temperature Firing and Microwave Dielectric Properties of Ca[(Li1/3Nb2/3)0.84Ti0.16]O3−δ Ceramics for LTCC Applications

The effects of LiF and ZnO–B₂O₃–SiO₂ (ZBS) glass combined additives on phase composition, microstructures, and microwave dielectric properties of Ca[(Li_1/3Nb_2/3)_0.84Ti_0.16]O_3−δ (CLNT) ceramics were investigated. The LiF and ZBS glass combined additives lowered the sintering temperature of CLNT ceramics effectively from 1150° to 880°C. The main diffraction peaks of all the specimens split due to the coexistence of the non-stoichiometric phase (A) and stoichiometric phase (B), which all possess CaTiO₃-type perovskite structures. The transformation from A into B became accelerated with the increase of LiF or ZBS content. ZBS glass restrained the volatilization of lithium salt, which greatly affected the microstructures and microwave dielectric properties. CLNT ceramics with 2 wt% LiF and 3 wt% ZBS sintered at 900°C for 2 h show excellent dielectric properties: ɛ_r=34.3, Q × f =17 400 GHz, and τ_f=−4.6 ppm/°C. It is compatible with Ag electrodes, which makes it a promising ceramic for low-temperature cofired ceramics technology application.     

Scattering-Loss Mechanism in CaF2-Film-Assisted Diffusion Bonding of MgF2 Ceramics

The present study examined the bonding of MgF₂ ceramics by hot-pressing. A layer of CaF₂ 2 to ∼3 μm thick was used as an agent to decrease the bonding temperature and to avoid breaching. The principal factors influencing transmission loss were the cellular growth in the MgF₂ layer, which caused about a 5% loss in transmittance, and grain growth in the films, as well as voids caused by the lattice mismatch, which, together with the formation of a recrystallization zone, caused about a 20% loss in transmittance. Grain growth in the CaF₂ film was not the main cause of the scattering loss. The effect of the grain growth in the MgF₂ matrix on transmittance was calculated as about 5%. Compositional fluctuations along the interfaces also had an important influence on scattering loss. For the sample that bonded at 650°C after 5 h, under a pressure of 430 kg/cm² (42 MPa), the crystalline solubility limit of CaF₂ in MgF₂ was measured at ∼l7at.%.     

Subsolidus Equilibria in the System MgO–GeO2–MgF2

Four MgO-GeO₂-MgF₂ compounds, analogous to the humite minerals, were synthesized by solid state reaction by substituting germanium for silicon. The 43 selected compositions were sintered at 800° to 1200°C. Solid state compatibility relations were established from petrographic and X-ray diffraction analyses. The optical properties and characteristic X-ray diffraction data for the four MgO-GeO₂-MgF₂ compounds were determined, and 2MgO.GeO₂ MgF₂, 4MgO.2GeO₂ MgF₂, and 6MgO.3GeO₂ MgF₂ were indexed by Ito's method.     

Coherent Precipitation in the System MgO-Al2O3-Cr2O3

An isothermal section of the ternary system MgO–Al₂O₃-Cr₂O₃ was determined at 1700°± 15°C to delineate the stability field for spinel crystalline solutions (cs). Crystalline solutions were found between the pseudobinary joins MgAl₂O₄–Cr₂O₃ and MgCr₂O₄-Al₂O₃, and the binary join MgAl₂O₄-MgO. The first two crystalline solutions exhibit cation vacancy models while the latter can probably be designated as a cation interstitial model. Precipitation from spinel cs may proceed directly to an equilibrium phase, (Al_1-xCr_x)₂O₃, with the corundum structure or through a metastable phase of the probable composition Mg(Al_1-xC_r)₂₆O₄₀. The composition and temperature limits were defined where the precipitation occurs via metastable monoclinic phases. The coherency of the metastable monoclinic phase with the spinel cs matrix can be understood by considering volume changes with equivalent numbers of oxygens and known crystallographic orientation relations. Electron probe and metallographic microscope investigations showed no preferential grain boundary precipitation.     

Effect of Sol-Gel Mixing on Mullite Microstructure and Phase Equilibria in the α-Al2O3-SiO2 System

Starting powders containing 72 wt% Al₂O³ and 28 wt% SiO₂, were prepared by sol-gel methods classified as colloidal and polymeric. Compacts fired at 1700°C showed significant differences in microstructure. The specimens formed with the colloidal powder had mullite grains of prismatic shape and a liquid phase; with polymeric powder, mullite grains were granular with no liquid phase present. It is shown that the mullite grains in the first case are higher in AI₂O₃ content, resulting in an excess of SiO₂ which is the base for the liquid phase. In the second case, the mullite grains have the same Al₂O₃ content as the starting powders. The presence of a liquid phase in the first case is considered to be metastable, resulting from the nature of the starting materials and processing conditions employed.     

Sol–Gel Processed Y-PSZ Ceramics with 5 wt% Al2O3

Y-PSZ ceramics with 5 wt% Al₂O₃ were synthesized by a sol–gel route. Experimental results show that powders of metastable tetragonal zirconia with 2.7 mol% Y₂O₃ and 5 wt% Al₂O₃ can be fabricated by decomposing the dry gel powder at 500°C. Materials sintered in an air atmosphere at 1500°C for 3 have high density (5.685 g/cm³), high content of metastable tetragonal zirconia (>96%), and high fracture toughness (8.67 MPa.m^1/2). Compared with the Y-PSZ ceramics, significant toughening was achieved by adding 5 wt% Al₂O₃.     

Characterization and Stabilization of Metastable Tetragonal ZrO2

Fine single-domain and polydomain particles of tetragonal ZrO₂ were prepared by hydrothermal and heat treatment of ZrO₂· n H₂O. The particles were characterized by X-ray diffraction, electron microscopy, NMR, mass spectrometry, and ir spectroscopy. The main impurity in the samples was 1 to 2 wt% OH⁻ ions, most of which were concentrated on the particle surfaces or at domain boundaries; some were also distributed in the lattice. Fine single-domain tetragonal particles were strain-free, but polydomain particles had large strains. The single-domain tetragonal particles were transformed much more easily than the polydomain particles by mechanical treatment. The stablization of metastable tetragonal ZrO₂ cannot be explained adequately by the surface-energy theory. An explanation based on the concept of a martensitic transformation may be more reasonable.     

Stability Relations of Magnesium Metasilicate Polymorphs

The observed stability relations of enstatite, protoenstatite, and clinoenstatite were in good agreement with the findings of earlier workers. Polycrystalline preparations of MgSiO₃ polymorphs were synthesized with the aid of small additions of MgF₂ or LiF as mineralizers. At 1042°± 3°C, enstatite, the stable low-temperature modification, inverts to protoenstatite, the stable high-temperature modification. The metastable transition between protoenstatite and clinoenstatite occurs at 865°± 5°C, the rate of transformation of polycrystalline protoenstatite to clinoenstatite being dependent on type and amount of mineralizer used, degree of compaction of sample, firing temperature, rate of cooling, degree of grinding at room temperature, and time at room temperature. Under certain conditions, a 1 to 2 mole % substitution of Mn²⁺ for Mg²⁺ inhibits the inversion of protoenstatite to either stable enstatite or metastable clinoenstatite below about 1042°C. Metastable clinoenstatite was never found to invert to the stable enstatite modification below the metastable inversion temperature of clinoenstatite to protoenstatite at 865°C. Above this temperature but below 1042°C, it inverts to protoenstatite which in turn inverts to enstatite. The aggregate linear thermal expansion coefficients of enstatite, protoenstatite, and clinoenstatite between 300° and 700° C were respectively 120 × 10⁻⁷, 98 × 10⁻⁷, and 135 × 10⁻⁷°C⁻¹.     

Microstructural Characterization of ZrO2 Particles Prepared by Reaction of Gaseous ZrCl4 with Fe2O3

The microstructure of ZrO₂ fine particles produced by a novel synthesis method at 450° and 950°C has been studied. The fundamentals of the synthesis method, which involves both chemical and diffusion phenomena, are presented. The method is based on mass transport through the gaseous phase between metallic zirconium and Fe₂O₃ powder. The mass-transporting chemical species are zirconium and iron chlorides. This article focuses on the microstructure and structure of ZrO₂ particles formed by the reaction between gaseous ZrCl₄ and solid Fe₂O₃, which is a relevant reaction step that occurs during the synthesis process. The resulting ZrO₂ crystals grown on Fe₂O₃ particles have been analyzed using transmission electron microscopy. Microstructural characterization has been complemented by X-ray diffractometry analysis. Tetragonal-ZrO₂ is produced at 450°C and monoclinic-ZrO₂ single crystals are produced at 950°C.     

New Uniformly Porous CaZrO3/MgO Composites with Three-Dimensional Network Structure from Natural Dolomite

Porous CaZrO₃/MgO composites with a uniform three-dimensional (3-D) network structure have been successfully synthesized using reactive sintering of highly pure mixtures of natural dolomite (CaMg(CO₃)₂) and synthesized zirconia powders with LiF additive. Equimolar dolomite and zirconia powders doped with 0.5 wt% LiF were cold isostatically pressed at 200 MPa and sintered at 1100–1400°C for 2 h in air. Through the liquid formation via LiF doping, strong necks were formed between constituent particles before completion of the pyrolysis of dolomite, resulting in the formation of a 3-D network structure. During and after the formation of the network structure, CO₂ was given off to form a homogeneous open-pore structure. The pore-size distribution was very narrow (with pore size ∼ 1 μm), and the porosity was controllable (e.g., ∼30%–50%) by changing the sintering temperature. The porous composites can be applied as filter materials with good structural stability at high temperatures.     

Crystallization and Seeding Effect in BaAl2Si2O8 Gels

Two sol-gel routes have been used to prepare celsian (BaAl₂Si₂O₈) precursors. The crystallization behaviors of unseeded gels and the gels seeded with 5 wt% feldspar, rutile, LiAISi₂O₂, and ZrO₂ crystals as well as SrAl₂Si₂O₈ gel have been studied using X-ray diffraction (XRD), scanning electron microscopy (SEM), and thermal gravimetric and differential thermal analyses (TGA and DTA). It was found that metastable hexacelsian, rather than the preferred monoclinic celsian, was the major crystallization product in the two unseeded gels. Seeding largely enhanced the crystallization of monoclinic celsian, but the mechanisms involved were different for seeding with different crystals. SrAl₂Si₂O₈ gel and ZrO₂ crystals acted as normal heterogeneous centers and had little catalytic effect on monoclinic celsian crystallization. Feldspar and rutile crystals worked as epitaxial substrates for monoclinic celsian and produced pure monoclinic celsian in some temperature regions. LiAISi₃O₈ seeds lowered the glass transition temperature of the immediately adjacent gel matrix and led to the crystallization of pure monoclinic celsian.     

Phase Equilibria in the System Na2SiO3-Li2SiO3

Phase equilibria were studied for the system Na₂SiO_:rLi₂SiO₃. The 2 end-member metasilicates show limited mutual solid solubility with the (Na_2-χLi_χ)SiO₃ solid solutions being particularly extensive at solidus temperatures (0 x 1.06). Ordering of the latter solid solution occurs at the NaLiSiO_;) composition with a_supercellx= 6a_subcell During cooling of the solid solutions, metastable phase transformations occur; a twinned monoclinic metastable phase, low (Na, Li)₂SiO₃, has been characterized.