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10.1016/j.molliq.2019.111769
Isotropic-nematic transition parameters have been calculated for three different systems of ellipses characterized by their major to minor axis ratio κ = 3.
Isotropic-nematic transition parameters have been calculated for three different systems of ellipses characterized by their major to minor axis ratio κ = 3.
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10.1016/J.POLYMER.2018.11.041
5% SA located in entangled semi-dilute regime could induce the isotropic-nematic transition of GO at low concentration (.
5% SA located in entangled semi-dilute regime could induce the isotropic-nematic transition of GO at low concentration (.
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10.1088/1361-648X/aaf843
This phenomenon leads to a shift in the isotropic-nematic transition temperature.
This phenomenon leads to a shift in the isotropic-nematic transition temperature.
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10.1088/1361-648X/ab0394
Importantly, our relaxation method is able to follow the thermodynamic behavior provided by other non-phenomenological approaches; we predict the first order character of the isotropic-nematic transition, and we identify the uniaxial-biaxial transition as second order.
Importantly, our relaxation method is able to follow the thermodynamic behavior provided by other non-phenomenological approaches; we predict the first order character of the isotropic-nematic transition, and we identify the uniaxial-biaxial transition as second order.
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10.1016/j.cis.2019.102076
With increasing NCC concentration, the isotropic phase can undergo a transition to a liquid crystalline state (isotropic-nematic transition) or a transition to a dynamically arrested solid (liquid-solid transition).
With increasing NCC concentration, the isotropic phase can undergo a transition to a liquid crystalline state (isotropic-nematic transition) or a transition to a dynamically arrested solid (liquid-solid transition).
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10.1080/02678292.2019.1645366
In the attempt to go beyond a simple Onsager theoretical approach to understand the thermodynamic behavior of this system, we introduced some years ago a general theoretical description, which models the isotropic-nematic transition by properly taking into account molecular self-assembly, and we carefully verified the theoretical predictions against numerical simulations of patchy hard cylinders.
In the attempt to go beyond a simple Onsager theoretical approach to understand the thermodynamic behavior of this system, we introduced some years ago a general theoretical description, which models the isotropic-nematic transition by properly taking into account molecular self-assembly, and we carefully verified the theoretical predictions against numerical simulations of patchy hard cylinders.
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Keywords related to Isotropic
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Isotropic Resolution
Isotropic Composite
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Isotropic Functionally
Isotropic Hardening
Isotropic Magnetorheological
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Isotropic Spherical
Isotropic Micropolar
Isotropic Multi Layered
Isotropic Solid
Isotropic Energy
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Isotropic Invariant
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Isotropic Incompressible
Isotropic Nd Fe B
Isotropic Cylindrical
Isotropic Cosmologies
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Isotropic 3d
Isotropic Gaussian
Isotropic Rock
Isotropic Materials
Isotropic Phases
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Isotropic Liquids
Isotropic Formations
Isotropic Static
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Isotropic Harmonic
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Isotropic Nematic Phase
Isotropic Compression
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Keywords related to Transition
Crust Core Transition
Boundary Layer Transition
Order Disorder Transition
Upon Transition
Monolayer Transition
Inner Transition
Brill Transition
Light Transition
De Transition
Urgent Transition
Adsorbed Transition
Agroecological Transition
Speed Transition
Track Transition
Porous Transition
D2 Transition
Developmental Transition
Epidemiologic Transition
Solid Liquid Transition
Midlife Transition
Breaking Transition
Freedericksz Transition
Bandgap Transition
Fracture Transition
On Transition
Within Transition
Multi Component Transition
Digital Transition
Tectonic Transition
Dynamic Transition
4d Transition
Dimensional Transition
Wettability Transition
Net Zero Transition
Binary Transition
Crossover Transition
Folding Transition
Railway Transition
Biogeographic Transition
Sudden Transition
Molecular Transition
Pressure Induced Transition
Evolutionary Transition
Dormancy Transition
Mesolithic Neolithic Transition
Droplet Transition
Secondary Transition
Improving Transition
Spin Reorientation Transition
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Isotropic Nematic Transition
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