AustralieFrV1, PascalFrancis, Corpus, bibRecord, 001F36

Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis

Identifieur interne : 001F36 ( PascalFrancis/Corpus ); précédent : 001F35; suivant : 001F37

Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis

Auteurs : Francisco J. Jimenez-Hornero ; Juan V. Giraldez ; Ana M. Laguna ; Tom Vanwalleghem

Source :

Geoderma : (Amsterdam) [ 0016-7061 ] ; 2010.

RBID : Pascal:11-0147621

Descripteurs français

Pascal (Inist)
- Végétation, Traceur, Transport, Analyse série temporelle, Système multifractal, Turbulence atmosphérique, Canal ouvert, Non linéarité, Méthode empirique, Caractère statistique, Transition phase, Modèle, Modélisation, Ecoulement canal découvert.

English descriptors

KwdEn :
- Atmospheric turbulence, Empirical method, Modeling, Multifractal system, Nonlinearity, Open channel, Open channel flow, Statistical character, models, phase transitions, time series analysis, tracers, transport, vegetation.

Abstract

Multifractal turbulence formalism has been used to describe the time series in simulated passive tracer transport in a vegetated open-channel, phenomenon characterized by a high temporal non-linear variability. A study of the empirical statistical moments scaling function for several scale ratios reveals the presence of a multifractal phase transition associated with one critical moment. The parameters of the universal multifractal model have been estimated using the double trace moment method. The theoretical statistical moments scaling was simulated by using the universal multifractal model showing an acceptable agreement with the corresponding empirical function. The universal multifractal parameters estimated here have different values to those reported for obstacle-free phenomena such as the atmospheric turbulence and passive scalar transport in turbulent oceanic flows.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A14	`01`			`@1 Department of Graphic Engineering and Geomatics, Gregor Mendel Building, Campus Rabanales, University of Cordoba @2 14071 Cordoba @3 ESP @Z 1 aut.`
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A15	`01`			`@1 Judith and David Coffey Chair, Faculty of Agriculture Food and Natural Resources, University of Sydney @2 Sydney 2006 @3 AUS @Z 4 aut.`
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C03	`14`	`X`	`FRE`	`@0 Ecoulement canal découvert @5 22`
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Format Inist (serveur)

NO :	PASCAL 11-0147621 INIST
ET :	Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis
AU :	JIMENEZ-HORNERO (Francisco J.); GIRALDEZ (Juan V.); LAGUNA (Ana M.); VANWALLEGHEM (Tom); TARQUIS (A. M.); BIRD (N. R. A.); PERRIER (E. M. A.); CRAWFORD (J. W.)
AF :	Department of Graphic Engineering and Geomatics, Gregor Mendel Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (1 aut.); Department of Agronomy and IAS CSIC, Leonardo da Vinci Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (2 aut.); Department of Applied Physics, Albert Einstein Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (3 aut.); Department of Agronomy, Leonardo da Vinci Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (4 aut.); Judith and David Coffey Chair, Faculty of Agriculture Food and Natural Resources, University of Sydney/Sydney 2006/Australie (4 aut.); Departamento de Matemática Aplicada, Universidad Politécnica de Madrid/28040 Madrid/Espagne (1 aut.); Department of Soil Science, Rothamsted Research/Harpenden, Herts, AL5 2JQ/Royaume-Uni (2 aut.); Unité de Recherches GEODES UR079, Centre IRD Ile de France/93143 Bondy/France (3 aut.)
DT :	Publication en série; Niveau analytique
SO :	Geoderma : (Amsterdam); ISSN 0016-7061; Coden GEDMAB; Pays-Bas; Da. 2010; Vol. 160; No. 1; Pp. 126-130; Bibl. 3/4 p.
LA :	Anglais
EA :	Multifractal turbulence formalism has been used to describe the time series in simulated passive tracer transport in a vegetated open-channel, phenomenon characterized by a high temporal non-linear variability. A study of the empirical statistical moments scaling function for several scale ratios reveals the presence of a multifractal phase transition associated with one critical moment. The parameters of the universal multifractal model have been estimated using the double trace moment method. The theoretical statistical moments scaling was simulated by using the universal multifractal model showing an acceptable agreement with the corresponding empirical function. The universal multifractal parameters estimated here have different values to those reported for obstacle-free phenomena such as the atmospheric turbulence and passive scalar transport in turbulent oceanic flows.
CC :	002A32; 001E01P03; 001E01N01; 226C03; 226A01
FD :	Végétation; Traceur; Transport; Analyse série temporelle; Système multifractal; Turbulence atmosphérique; Canal ouvert; Non linéarité; Méthode empirique; Caractère statistique; Transition phase; Modèle; Modélisation; Ecoulement canal découvert
ED :	vegetation; tracers; transport; time series analysis; Multifractal system; Atmospheric turbulence; Open channel; Nonlinearity; Empirical method; Statistical character; phase transitions; models; Modeling; Open channel flow
SD :	Vegetación; Trazador; Transporte; Sistema multifractal; Turbulencia atmosférica; Canal abierto; No linealidad; Método empírico; Carácter estadístico; Transición fase; Modelo; Modelización; Flujo canal descubierto
LO :	INIST-3607.354000194339950140
ID :	11-0147621

Links to Exploration step

Pascal:11-0147621

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<fC03 i1="01" i2="2" l="ENG"><s0>vegetation</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Vegetación</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Traceur</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>tracers</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Trazador</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Transport</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>transport</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Transporte</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Analyse série temporelle</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>time series analysis</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Système multifractal</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Multifractal system</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Sistema multifractal</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Turbulence atmosphérique</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Atmospheric turbulence</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Turbulencia atmosférica</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Canal ouvert</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Open channel</s0>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Canal abierto</s0>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Non linéarité</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Nonlinearity</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>No linealidad</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Méthode empirique</s0>
<s5>12</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Empirical method</s0>
<s5>12</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Método empírico</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Caractère statistique</s0>
<s5>13</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Statistical character</s0>
<s5>13</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Carácter estadístico</s0>
<s5>13</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Transition phase</s0>
<s5>16</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>phase transitions</s0>
<s5>16</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Transición fase</s0>
<s5>16</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Modèle</s0>
<s5>18</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>models</s0>
<s5>18</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Modelo</s0>
<s5>18</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Modélisation</s0>
<s5>19</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Modeling</s0>
<s5>19</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Modelización</s0>
<s5>19</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Ecoulement canal découvert</s0>
<s5>22</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Open channel flow</s0>
<s5>22</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Flujo canal descubierto</s0>
<s5>22</s5>
</fC03>
<fN21><s1>094</s1>
</fN21>
</pA>
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<server><NO>PASCAL 11-0147621 INIST</NO>
<ET>Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis</ET>
<AU>JIMENEZ-HORNERO (Francisco J.); GIRALDEZ (Juan V.); LAGUNA (Ana M.); VANWALLEGHEM (Tom); TARQUIS (A. M.); BIRD (N. R. A.); PERRIER (E. M. A.); CRAWFORD (J. W.)</AU>
<AF>Department of Graphic Engineering and Geomatics, Gregor Mendel Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (1 aut.); Department of Agronomy and IAS CSIC, Leonardo da Vinci Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (2 aut.); Department of Applied Physics, Albert Einstein Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (3 aut.); Department of Agronomy, Leonardo da Vinci Building, Campus Rabanales, University of Cordoba/14071 Cordoba/Espagne (4 aut.); Judith and David Coffey Chair, Faculty of Agriculture Food and Natural Resources, University of Sydney/Sydney 2006/Australie (4 aut.); Departamento de Matemática Aplicada, Universidad Politécnica de Madrid/28040 Madrid/Espagne (1 aut.); Department of Soil Science, Rothamsted Research/Harpenden, Herts, AL5 2JQ/Royaume-Uni (2 aut.); Unité de Recherches GEODES UR079, Centre IRD Ile de France/93143 Bondy/France (3 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Geoderma : (Amsterdam); ISSN 0016-7061; Coden GEDMAB; Pays-Bas; Da. 2010; Vol. 160; No. 1; Pp. 126-130; Bibl. 3/4 p.</SO>
<LA>Anglais</LA>
<EA>Multifractal turbulence formalism has been used to describe the time series in simulated passive tracer transport in a vegetated open-channel, phenomenon characterized by a high temporal non-linear variability. A study of the empirical statistical moments scaling function for several scale ratios reveals the presence of a multifractal phase transition associated with one critical moment. The parameters of the universal multifractal model have been estimated using the double trace moment method. The theoretical statistical moments scaling was simulated by using the universal multifractal model showing an acceptable agreement with the corresponding empirical function. The universal multifractal parameters estimated here have different values to those reported for obstacle-free phenomena such as the atmospheric turbulence and passive scalar transport in turbulent oceanic flows.</EA>
<CC>002A32; 001E01P03; 001E01N01; 226C03; 226A01</CC>
<FD>Végétation; Traceur; Transport; Analyse série temporelle; Système multifractal; Turbulence atmosphérique; Canal ouvert; Non linéarité; Méthode empirique; Caractère statistique; Transition phase; Modèle; Modélisation; Ecoulement canal découvert</FD>
<ED>vegetation; tracers; transport; time series analysis; Multifractal system; Atmospheric turbulence; Open channel; Nonlinearity; Empirical method; Statistical character; phase transitions; models; Modeling; Open channel flow</ED>
<SD>Vegetación; Trazador; Transporte; Sistema multifractal; Turbulencia atmosférica; Canal abierto; No linealidad; Método empírico; Carácter estadístico; Transición fase; Modelo; Modelización; Flujo canal descubierto</SD>
<LO>INIST-3607.354000194339950140</LO>
<ID>11-0147621</ID>
</server>
</inist>
</record>

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Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis

Exploring the effects of the vegetation on passive tracer transport by using the multifractal analysis

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