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Results for “Crystal Growth”
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Crystal growth of Sr[subscript 2]Ir[subscript x]Ru[subscript 1-x]O[subscript 4] for x; 0.4
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Crystal growth, thermal, optical, magnetic and electrochemical properties of Mo2Ta2O11
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Projected Cost of Gallium Oxide Wafers from Edge-Defined Film-Fed Crystal Growth
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Reply to Comment on “A Mechanistic Understanding of Nonclassical Crystal Growth in Hydrothermally Synthesized Sodium Yttrium Fluoride Nanowires”
Comments are provided on the original article, highlighting areas of agreement and possible misunderstandings.
Crystal Growth of Alkali Uranyl Borates from Molten Salt Fluxes: Characterization and Ion Exchange Behavior of A 2 (UO 2 )B 2 O 5 (A = Cs, Rb, K)
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Enhancement of Crystal Growth in Molten Salts by a Cocrystallization Agent: Synthesis and Luminescent Properties of Ce 3+ - and Eu 2+ -Doped La 3 (SiS 4 ) 2 I
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Uncovering the effects of interface-induced ordering of liquid on crystal growth using machine learning
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Single-crystal growth and superconductivity in RbNi 2 Se 2
Herein we report the synthesis and characterization of RbNi 2 Se 2 , an analog of the iron chalcogenide superconductor Rb x Fe 2 Se 2 , via transport, angle-resolved photoemission spectroscopy, and density functional theory calculations. A superconducting transition at T c =1.20 K is identified. In the normal state, RbNi 2 Se 2 shows paramagnetic and Fermi-liquid behaviors. A large Sommerfeld coefficient yields an effective electron mass of m* ≈ 6m e . In the superconducting state, zero-field electronic specific-heat data C es can be described by a two-gap BCS model, indicating that RbNi 2 Se 2 is a possible multigap superconductor. Our density functional theory calculations and angle-resolved photoemission spectroscopy measurements demonstrate that RbNi 2 Se 2 exhibits relatively weak correlations and multiband characteristics, consistent with the multigap superconductivity.
Parity breaking at faceted crystal growth fronts during ice templating
Directional solidification of water-based solutions has emerged as a versatile technique to template hierarchical porous materials, but this nonequilibrium process remains incompletely understood. Here, in this study, we use phase-field simulations to shed light on the mechanism that selects the growth direction of the lamellar ice structure that templates those materials. Our results show that this selection can be understood within the general framework of spontaneous parity breaking, yielding quantitative predictions for the tilt angle of lamellae with respect to the thermal axis. The results provide a theoretical basis to interpret a wide range of experimental observations.
The Combined Effects of Mg2+ and Sr2+ on Calcite Crystallization, Growth, and Incorporation Behavior.
Abstract not provided.