Serveur d'exploration sur les relations entre la France et l'Australie

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

Consistent closure schemes for statistical models of anisotropic fluids

Identifieur interne : 008E15 ( Main/Exploration ); précédent : 008E14; suivant : 008E16

Consistent closure schemes for statistical models of anisotropic fluids

Auteurs : Martin Kröger [Suisse] ; Amine Ammar [France] ; Francisco Chinesta [France]

Source :

RBID : Pascal:08-0281326

Descripteurs français

English descriptors

Abstract

We propose a rational approach to approximating the various alignment tensors. It preserves the correct symmetry and leads to consistent results. For the case of uniaxial nematic fluids, the decoupling approximation for a tensor of rank n involves (n - 2)/2 scalar functions Sn(S2) in terms of a scalar argument S2, with Sn (0) = 0 and Sn (1) = 1. Nothing else can be concluded about the mathematical relationship between moments of the distribution function, and in particular, all consistent decoupling approximations for fourth-order moment in terms of second-order moments can be characterized by a single S4(S2) function. We propose using the simple model dependent convex shaped equilibrium relationship between S4 and S2 to characterize new (and simple) decoupling approximations K-I and K-II for the biaxial (including uniaxial) phase. In order to test the new against earlier proposed approximations rigorously, and to discuss consistency issues, we solve the Hess-Doi Fokker-Planck equation for nematic and nematic-discotic liquid crystals efficiently for a wide range of (2300 distinct) possible conditions including mixed shear and elongational flows, diverse field strengths, and molecular shapes. As a result, we confirm the closures K-I and K-II with correct tensorial symmetry; they are valid under arbitrary conditions to high precision, exact in the isotropic and totally aligned phases, improve upon earlier parameter-free closures in particular in the temperature regime T∈ [0.6, ∞] x TNI with the nematic-isotropic transition temperature TNI (or alternatively, for mean-field strengths U ∈ [0, 8]). K-II performs as good as the so-called Bingham closure, which usually requires 30 empirical coefficients, while K-I and K-II are essentially parameter-free, and their quality can be expected to be insensitive to the particular model.


Affiliations:


Links toward previous steps (curation, corpus...)


Le document en format XML

<record>
<TEI>
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en" level="a">Consistent closure schemes for statistical models of anisotropic fluids</title>
<author>
<name sortKey="Kroger, Martin" sort="Kroger, Martin" uniqKey="Kroger M" first="Martin" last="Kröger">Martin Kröger</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Polymer Physics, ETH Zurich, Department of Materials, Wolfgang-Pauli-Str. 10</s1>
<s2>8093 Zürich</s2>
<s3>CHE</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
<country>Suisse</country>
<placeName>
<settlement type="city">Zurich</settlement>
<region nuts="3" type="region">Canton de Zurich</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Ammar, Amine" sort="Ammar, Amine" uniqKey="Ammar A" first="Amine" last="Ammar">Amine Ammar</name>
<affiliation wicri:level="1">
<inist:fA14 i1="02">
<s1>Laboratoire de Rhéologie, UMR 5520 CNRS-UJF-INPG, 1301 Rue de la Piscine, BP 53 Domaine Universitaire</s1>
<s2>38041 Grenoble</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
</inist:fA14>
<country>France</country>
<wicri:noRegion>38041 Grenoble</wicri:noRegion>
<placeName>
<settlement type="city">Grenoble</settlement>
<region type="region" nuts="2">Auvergne-Rhône-Alpes</region>
<region type="old region" nuts="2">Rhône-Alpes</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Chinesta, Francisco" sort="Chinesta, Francisco" uniqKey="Chinesta F" first="Francisco" last="Chinesta">Francisco Chinesta</name>
<affiliation wicri:level="1">
<inist:fA14 i1="03">
<s1>LMSP UMR 8106 CNRS-ENSAM-ESEM, 151 Boulevard de l'Hôpital</s1>
<s2>75013 Paris</s2>
<s3>FRA</s3>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>France</country>
<wicri:noRegion>75013 Paris</wicri:noRegion>
<placeName>
<settlement type="city">Paris</settlement>
<region type="région" nuts="2">Île-de-France</region>
</placeName>
</affiliation>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">INIST</idno>
<idno type="inist">08-0281326</idno>
<date when="2008">2008</date>
<idno type="stanalyst">PASCAL 08-0281326 INIST</idno>
<idno type="RBID">Pascal:08-0281326</idno>
<idno type="wicri:Area/PascalFrancis/Corpus">003540</idno>
<idno type="wicri:Area/PascalFrancis/Curation">002B08</idno>
<idno type="wicri:Area/PascalFrancis/Checkpoint">003339</idno>
<idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">003339</idno>
<idno type="wicri:doubleKey">0377-0257:2008:Kroger M:consistent:closure:schemes</idno>
<idno type="wicri:Area/Main/Merge">009753</idno>
<idno type="wicri:Area/Main/Curation">008E15</idno>
<idno type="wicri:Area/Main/Exploration">008E15</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title xml:lang="en" level="a">Consistent closure schemes for statistical models of anisotropic fluids</title>
<author>
<name sortKey="Kroger, Martin" sort="Kroger, Martin" uniqKey="Kroger M" first="Martin" last="Kröger">Martin Kröger</name>
<affiliation wicri:level="1">
<inist:fA14 i1="01">
<s1>Polymer Physics, ETH Zurich, Department of Materials, Wolfgang-Pauli-Str. 10</s1>
<s2>8093 Zürich</s2>
<s3>CHE</s3>
<sZ>1 aut.</sZ>
</inist:fA14>
<country>Suisse</country>
<placeName>
<settlement type="city">Zurich</settlement>
<region nuts="3" type="region">Canton de Zurich</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Ammar, Amine" sort="Ammar, Amine" uniqKey="Ammar A" first="Amine" last="Ammar">Amine Ammar</name>
<affiliation wicri:level="1">
<inist:fA14 i1="02">
<s1>Laboratoire de Rhéologie, UMR 5520 CNRS-UJF-INPG, 1301 Rue de la Piscine, BP 53 Domaine Universitaire</s1>
<s2>38041 Grenoble</s2>
<s3>FRA</s3>
<sZ>2 aut.</sZ>
</inist:fA14>
<country>France</country>
<wicri:noRegion>38041 Grenoble</wicri:noRegion>
<placeName>
<settlement type="city">Grenoble</settlement>
<region type="region" nuts="2">Auvergne-Rhône-Alpes</region>
<region type="old region" nuts="2">Rhône-Alpes</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Chinesta, Francisco" sort="Chinesta, Francisco" uniqKey="Chinesta F" first="Francisco" last="Chinesta">Francisco Chinesta</name>
<affiliation wicri:level="1">
<inist:fA14 i1="03">
<s1>LMSP UMR 8106 CNRS-ENSAM-ESEM, 151 Boulevard de l'Hôpital</s1>
<s2>75013 Paris</s2>
<s3>FRA</s3>
<sZ>3 aut.</sZ>
</inist:fA14>
<country>France</country>
<wicri:noRegion>75013 Paris</wicri:noRegion>
<placeName>
<settlement type="city">Paris</settlement>
<region type="région" nuts="2">Île-de-France</region>
</placeName>
</affiliation>
</author>
</analytic>
<series>
<title level="j" type="main">Journal of non-newtonian fluid mechanics</title>
<title level="j" type="abbreviated">J. non-newton. fluid mech.</title>
<idno type="ISSN">0377-0257</idno>
<imprint>
<date when="2008">2008</date>
</imprint>
</series>
</biblStruct>
</sourceDesc>
<seriesStmt>
<title level="j" type="main">Journal of non-newtonian fluid mechanics</title>
<title level="j" type="abbreviated">J. non-newton. fluid mech.</title>
<idno type="ISSN">0377-0257</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass>
<keywords scheme="KwdEn" xml:lang="en">
<term>Closure model</term>
<term>Distribution functions</term>
<term>Ferromagnetic fluid</term>
<term>Fokker-Planck equation</term>
<term>Liquid crystals</term>
<term>Liquid nematic transformation</term>
<term>Magnetorheological fluid</term>
<term>Mathematical models</term>
<term>Nematic crystals</term>
<term>Orientational order</term>
<term>Rational approximation</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr">
<term>Ordre orientationnel</term>
<term>Fonction distribution</term>
<term>Modèle mathématique</term>
<term>Equation Fokker Planck</term>
<term>Transformation liquide nématique</term>
<term>Fluide ferromagnétique</term>
<term>Approximation rationnelle</term>
<term>Modèle fermeture</term>
<term>Cristal liquide</term>
<term>Cristal nématique</term>
<term>Fluide magnétorhéologique</term>
</keywords>
</textClass>
</profileDesc>
</teiHeader>
<front>
<div type="abstract" xml:lang="en">We propose a rational approach to approximating the various alignment tensors. It preserves the correct symmetry and leads to consistent results. For the case of uniaxial nematic fluids, the decoupling approximation for a tensor of rank n involves (n - 2)/2 scalar functions S
<sub>n</sub>
(S
<sub>2</sub>
) in terms of a scalar argument S
<sub>2</sub>
, with S
<sub>n</sub>
(0) = 0 and S
<sub>n</sub>
(1) = 1. Nothing else can be concluded about the mathematical relationship between moments of the distribution function, and in particular, all consistent decoupling approximations for fourth-order moment in terms of second-order moments can be characterized by a single S
<sub>4</sub>
(S
<sub>2</sub>
) function. We propose using the simple model dependent convex shaped equilibrium relationship between S
<sub>4</sub>
and S
<sub>2</sub>
to characterize new (and simple) decoupling approximations K-I and K-II for the biaxial (including uniaxial) phase. In order to test the new against earlier proposed approximations rigorously, and to discuss consistency issues, we solve the Hess-Doi Fokker-Planck equation for nematic and nematic-discotic liquid crystals efficiently for a wide range of (2300 distinct) possible conditions including mixed shear and elongational flows, diverse field strengths, and molecular shapes. As a result, we confirm the closures K-I and K-II with correct tensorial symmetry; they are valid under arbitrary conditions to high precision, exact in the isotropic and totally aligned phases, improve upon earlier parameter-free closures in particular in the temperature regime T∈ [0.6, ∞] x T
<sub>NI</sub>
with the nematic-isotropic transition temperature T
<sub>NI</sub>
(or alternatively, for mean-field strengths U ∈ [0, 8]). K-II performs as good as the so-called Bingham closure, which usually requires 30 empirical coefficients, while K-I and K-II are essentially parameter-free, and their quality can be expected to be insensitive to the particular model.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>France</li>
<li>Suisse</li>
</country>
<region>
<li>Auvergne-Rhône-Alpes</li>
<li>Canton de Zurich</li>
<li>Rhône-Alpes</li>
<li>Île-de-France</li>
</region>
<settlement>
<li>Grenoble</li>
<li>Paris</li>
<li>Zurich</li>
</settlement>
</list>
<tree>
<country name="Suisse">
<region name="Canton de Zurich">
<name sortKey="Kroger, Martin" sort="Kroger, Martin" uniqKey="Kroger M" first="Martin" last="Kröger">Martin Kröger</name>
</region>
</country>
<country name="France">
<region name="Auvergne-Rhône-Alpes">
<name sortKey="Ammar, Amine" sort="Ammar, Amine" uniqKey="Ammar A" first="Amine" last="Ammar">Amine Ammar</name>
</region>
<name sortKey="Chinesta, Francisco" sort="Chinesta, Francisco" uniqKey="Chinesta F" first="Francisco" last="Chinesta">Francisco Chinesta</name>
</country>
</tree>
</affiliations>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Asie/explor/AustralieFrV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 008E15 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 008E15 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Asie
   |area=    AustralieFrV1
   |flux=    Main
   |étape=   Exploration
   |type=    RBID
   |clé=     Pascal:08-0281326
   |texte=   Consistent closure schemes for statistical models of anisotropic fluids
}}

Wicri

This area was generated with Dilib version V0.6.33.
Data generation: Tue Dec 5 10:43:12 2017. Site generation: Tue Mar 5 14:07:20 2024