scholarly journals Ringwoodite rim around olivine core in shock-induced melt-vein of GRV 022321 chondrite: Transformation kinetics of olivine to ringwoodite

2021 ◽  
Author(s):  
Zhidong Xie ◽  
Thomas G. Sharp ◽  
Shuhao Zuo ◽  
Xiaochun Li
Keyword(s):  
Electron Microscopy ◽  
Raman Spectroscopy ◽  
Natural Occurrence ◽  
Controlled Growth ◽  
Rock Fragments ◽  
Nano Crystalline ◽  
Diffusion Controlled ◽  
State Diffusion ◽  
Crystallite Sizes ◽  
Electron Imaging

Abstract Here we report the natural occurrence of the ringwoodite rims around olivine cores in shock-induced melt veins of the Antarctic chondrite GRV 022321. Electron microprobe analysis (EMPA), Raman spectroscopy, Scanning electron microscopy (SEM) and Transmission electron microscopy (TEM) were used to examine the sample to better elucidate the mechanisms of transformation of the olivine to ringwoodite and Fe-Mg partitioning in olivine under the shock. The GRV 022321 is an L6 chondrite with a network of black veins enclosing abundant olivine host-rock fragments. Some of the enclosed fragments ranging from 5 µm to 100 µm in size have bright rims up to 20 µm wide, and a dark core under reflected light and backscatter electron imaging. Raman spectroscopy reveals that rims are made of ringwoodite, and cores are predominantly olivine. EMPA data show the ringwoodites in rims are richer in Fe (Fa46) than the olivine cores (Fa10-Fa23). The olivine cores have variable contrast in BSE images with the heterogeneities in fayalite content (Fa10 to Fa23) and a branching network of low-Fa olivine. FIB-TEM observations reveal that the ringwoodite rims are polycrystalline with crystallite sizes from 200 nm to 800 nm, while the olivine cores are also polycrystalline, but with smaller crystallites from 100 nm to 200 nm. Based on observation, we conclude that the original Fa23 olivine transformed to Fa10 olivine and Fa46 ringwoodite by a solid-state diffusion-controlled growth mechanism during shock, and the branching network of low-Fa olivine acted as long-range(up to 10µm)high-diffusion pathways for grain-boundary Fe-Mg interdiffusion through highly deformed nano-crystalline olivine to accommodate the diffusion-controlled growth of ringwoodite.

A complex corona between olivine and plagioclase from the Jotun Nappe, Norway, and the diffusion modelling of multimineralic layers

1992 ◽  
Vol 56 (385) ◽  
pp. 511-525 ◽  
Author(s):  
J. R. Ashworth ◽  
J. J. Birdi ◽  
T. F. Emmett
Keyword(s):  
Electron Microscopy ◽  
Diffusion Coefficients ◽  
Local Equilibrium ◽  
Mineral Layer ◽  
Small Diffusion ◽  
Phase Rule ◽  
Transmission Electron ◽  
Diffusion Controlled ◽  
State Diffusion

AbstractCoronas containing Ca-amphibole with aluminous minerals have been characterised optically and by scanning electron microscopy, analytical transmission electron microscopy and electron-probe microanalysis. The layers nearest to plagioclase are amphibole + epidote + kyanite, followed by amphibole + epidote + staurolite + spinel. These assemblages are consistent with waterundersaturated conditions, possibly at lower metamorphic grade than the commoner assemblage amphibole + spinel. Observed mineral proportions and compositions were used in a seven-layer model of steady-state, diffusion-controlled growth with local equilibrium. This model is not fully realistic, because the observed amphibole is strongly zoned from tschermakitic to actinolitic away from plagioclase, suggesting disequilibrium. However, the four-mineral layer has been successfully modelled assuming local equilibrium, with diffusion coefficients Lii larger for i = FeO and MgO than for SiO2, AlO3/2, CaO and FeO3/2. Retarded grain-boundary diffusion of the latter components is explicable by crystal-chemical effects. The number of minerals per layer is constrained by a modified form of the metasomatic phase rule of Korzhinskii, with the role of 'inert' components played by relatively immobile ones (having relatively small fluxes and relatively small diffusion coefficients).

Solid–state diffusion–controlled growth of the phases in the Au–Sn system

2017 ◽  
Vol 98 (1) ◽  
pp. 20-36 ◽  
Author(s):  
Varun A. Baheti ◽  
Sanjay Kashyap ◽  
Praveen Kumar ◽  
Kamanio Chattopadhyay ◽  
Aloke Paul
Keyword(s):  
Solid State ◽  
Solid State Diffusion ◽  
Controlled Growth ◽  
Diffusion Controlled ◽  
State Diffusion

scholarly journals The X-ray, Raman and TEM Signatures of Cellulose-Derived Carbons Explained

2022 ◽  
Vol 8 (1) ◽  
pp. 4
Author(s):  
Petros Kasaira Mubari ◽  
Théotime Beguerie ◽  
Marc Monthioux ◽  
Elsa Weiss-Hortala ◽  
Ange Nzihou ◽  
...  
Keyword(s):  
Electron Microscopy ◽  
Raman Spectroscopy ◽  
Structural Unit ◽  
X Ray Diffraction ◽  
X Ray ◽  
Characterization Techniques ◽  
Transmission Electron ◽  
Crystallite Sizes ◽  
Xrd Patterns ◽  
Average Size

Structural properties of carbonized cellulose were explored to conjugate the outcomes from various characterization techniques, namely X-ray diffraction (XRD), Raman spectroscopy, and high-resolution transmission electron microscopy. All these techniques have evidenced the formation of graphene stacks with a size distribution. Cellulose carbonized at 1000 and 1800 °C at a heating rate of 2 °C/min showed meaningful differences in Raman spectroscopy, whereas in XRD, the differences were not well pronounced, which implies that the crystallite sizes calculated by each technique have different significations. In the XRD patterns, the origin of a specific feature at a low scattering angle commonly reported in the literature but poorly explained so far, was identified. The different approaches used in this study were congruous in explaining the observations that were made on the cellulose-derived carbon samples. The remnants of the basic structural unit (BSU) are developed during primary carbonization. Small graphene-based crystallites inherited from the BSUs, which formerly developed during primary carbonization, were found to coexist with larger ones. Even if the three techniques give information on the average size of graphenic domains, they do not see the same characteristics of the domains; hence, they are not identical, nor contradictory but complementary. The arguments developed in the work to explain which characteristics are deduced from the signal obtained by each of the three characterization techniques relate to physics phenomena; hence, they are quite general and, therefore, are valid for all kind of graphenic materials.

scholarly journals Novel Lead-free biocompatible piezoelectric Hydroxyapatite (HA) – BCZT (Ba0.85Ca0.15Zr0.1Ti0.9O3) nanocrystal composites for bone regeneration

2019 ◽  
Vol 8 (1) ◽  
pp. 61-78 ◽  
Author(s):  
Chelli Sai Manohar ◽  
B Siva Kumar ◽  
Sai Pavan Prashanth Sadhu ◽  
Sai Krishna Srimadh ◽  
V Sai Muthukumar ◽  
...  
Keyword(s):  
Electron Microscopy ◽  
Raman Spectroscopy ◽  
Bone Regeneration ◽  
Bone Growth ◽  
Piezoelectric Coefficient ◽  
Operating Conditions ◽  
Lead Free ◽  
Hydrothermal Route ◽  
Nano Crystalline

Abstract BCZT (Ba0.85Ca0.15Zr0.1Ti0.9O3) is a recent class of lead-free ferroelectric material associated with high piezoelectric coefficient, making it suitable to inspire hydroxyapatite (HA)-BCZT ceramics for bone materials. Nano-crystalline hydroxyapatite (HA) synthesized using the hydrothermal route was characterized via FT-IR, Raman spectroscopy, X-ray powder diffraction (XRD), and Scanning Electron Microscopy (SEM). We also rationalized its formation as a function of operating conditions such as dwell time and temperature in this route. The nano-crystalline BCZT powder was synthesized via a sol-gel technique and its structural and morphological characterization were carried out using Raman Spectroscopy, XRD and Transmission Electron Microscopy (TEM). These investigations facilitated the optimization of HA-BCZT compositions and their electrical poling conditions to achieve enhanced piezoelectric effect. The composites (HA-BCZT) sintered at 1350∘C exhibited promising piezoelectric properties. We report the enhanced piezoelectric coefficient (d33) of 7±1 pC/N for 50% HA-BCZT which is significant as compared to that reported in the literature for ~98% BT (barium titanate) -HA composites. We highlight the role of Simulated Body Fluid (SBF) on the intriguing phase-change of Tricalcium Phosphate (TCP) obtained at this sintering temperature, to hydroxyapatite for its essential contribution to promote bone growth. We theoretically support the confirmed in vitro biocompatibility of these composites. Graphical abstract: Novel lead-free biocompatible piezoelectric HA-BCZT nanocrystal composites for accelerated Bone regeneration

Reconstruction of Two-Dimensional Projections of GP 32*I

1981 ◽  
Vol 39 ◽  
pp. 38-39
Author(s):  
H.A. Cohen ◽  
W. Chiu ◽  
J. Hosoda
Keyword(s):  
Electron Microscopy ◽  
Molecular Weight ◽  
Uranyl Acetate ◽  
Distilled Water ◽  
Acetate Solution ◽  
Two Dimensional ◽  
Parent Molecule ◽  
T4 Bacteriophage ◽  
Electron Imaging ◽  
Better Than

GP 32 (molecular weight 35000) is a T4 bacteriophage protein that destabilizes the DNA helix. The fragment GP32*I (77% of the total weight), which destabilizes helices better than does the parent molecule, crystallizes as platelets thin enough for electron diffraction and electron imaging. In this paper we discuss the structure of this protein as revealed in images reconstructed from stained and unstained crystals.Crystals were prepared as previously described. Crystals for electron microscopy were pelleted from the buffer suspension, washed in distilled water, and resuspended in 1% glucose. Two lambda droplets were placed on grids over freshly evaporated carbon, allowed to sit for five minutes, and then were drained. Stained crystals were prepared the same way, except that prior to draining the droplet, two lambda of aqueous 1% uranyl acetate solution were applied for 20 seconds. Micrographs were produced using less than 2 e/Å2 for unstained crystals or less than 8 e/Å2 for stained crystals.

scholarly journals New minerals tsangpoite Ca5(PO4)2(SiO4) and matyhite Ca9(Ca0.5□0.5)Fe(PO4)7 from the D'Orbigny angrite

2018 ◽  
Vol 83 (02) ◽  
pp. 293-313 ◽  
Author(s):  
Shyh-Lung Hwang ◽  
Pouyan Shen ◽  
Hao-Tsu Chu ◽  
Tzen-Fu Yui ◽  
Maria-Euginia Varela ◽  
...  
Keyword(s):  
Electron Microscopy ◽  
Raman Spectroscopy ◽  
Electron Diffraction ◽  
Grain Boundary ◽  
Electron Probe ◽  
Formation Mechanisms ◽  
Formula Unit ◽  
Micro Raman Spectroscopy ◽  
The Common ◽  
Oxygen Atoms

AbstractTsangpoite, ideally Ca5(PO4)2(SiO4), the hexagonal polymorph of silicocarnotite, and matyhite, ideally Ca9(Ca0.5□0.5)Fe(PO4)7, the Fe-analogue of Ca-merrillite, were identified from the D'Orbigny angrite meteorite by electron probe microanalysis, electron microscopy and micro-Raman spectroscopy. On the basis of electron diffraction, the symmetry of tsangpoite was shown to be hexagonal,P63/morP63, witha= 9.489(4) Å,c= 6.991(6) Å,V= 545.1(6) Å3andZ= 2 for 12 oxygen atoms per formula unit, and that of matyhite was shown to be trigonal,R3c, witha= 10.456 (7) Å,c= 37.408(34) Å,V= 3541.6 (4.8) Å3andZ= 6 for 28 oxygen atoms per formula unit. On the basis of their constant association with the grain-boundary assemblage: Fe sulfide + ulvöspinel + Al–Ti-bearing hedenbergite + fayalite–kirschsteinite intergrowth, the formation of tsangpoite and matyhite, along with kuratite (the Fe-analogue of rhönite), can be readily rationalised as crystallisation from residue magmas at the final stage of the D'Orbigny meteorite formation. Alternatively, the close petrographic relations between tsangpoite/matyhite and the resorbed Fe sulfide rimmed by fayalite + kirschsteinite symplectite, such as the nucleation of tsangpoite in association with magnetite ± other phases within Fe sulfide and the common outward growth of needle-like tsangpoite or plate-like matyhite from the fayalite–kirschsteinite symplectic rim of Fe sulfide into hedenbergite, infer that these new minerals and the grain-boundary assemblage might represent metasomatic products resulting from reactions between an intruding metasomatic agent and the porous olivine–plagioclase plate + fayalite-kirschsteinite overgrowth + augite + Fe sulfide aggregates. Still further thermochemical and kinetics evidence is required to clarify the exact formation mechanisms/conditions of the euhedral tsangpoite, matyhite and kuratite at the grain boundary of the D'Orbigny angrite.

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