AustralieFrV1, PascalFrancis, Corpus, bibRecord, 004428

Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia

Identifieur interne : 004428 ( PascalFrancis/Corpus ); précédent : 004427; suivant : 004429

Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia

Auteurs : T. W. Ellis ; S. Leguedois ; P. B. Hairsine ; D. J. Tongway

Source :

Australian journal of soil research [ 0004-9573 ] ; 2006.

RBID : Pascal:06-0238668

Descripteurs français

Pascal (Inist)
- Capture, Ruissellement plan incliné, Pente terrain, Versant, Ruissellement eau sol, Eau ruissellement, Agroforesterie, Eau surface, Gestion eau, Arbre, Sud est, Australie, Litière, Terrasse, Infiltration, Micro-terrasse, Bande boisée.

English descriptors

KwdEn :
- Agroforestry, Australia, Capture, Land slope, Litter, Overland flow, Runoff, Runoff water, Southeast, Water management, Wooded strip, infiltration, slopes, surface water, terraces, trees.

Abstract

We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

A01	`01`	`1`		`@0 0004-9573`
A02	`01`			`@0 ASORAB`
A03		`1`		`@0 Aust. j. soil res.`
A05				`@2 44`
A06				`@2 2`
A08	`01`	`1`	`ENG`	`@1 Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia`
A11	`01`	`1`		`@1 ELLIS (T. W.)`
A11	`02`	`1`		`@1 LEGUEDOIS (S.)`
A11	`03`	`1`		`@1 HAIRSINE (P. B.)`
A11	`04`	`1`		`@1 TONGWAY (D. J.)`
A14	`01`			`@1 CSIRO Land and Water, GPO Box 1666 @2 Canberra, ACT 2606 @3 AUS @Z 1 aut. @Z 2 aut. @Z 3 aut.`
A14	`02`			`@1 INRA Soil Science Research Unit, BP 20 619 Ardon @2 45 1666 Oliver @3 FRA @Z 2 aut.`
A14	`03`			`@1 CSIRO Sustainable Ecosystems, GPO Box 284 @2 Canberra, ACT 2601 @3 AUS @Z 4 aut.`
A20				`@1 117-125`
A21				`@1 2006`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 10723 @5 354000152983350040`
A44				`@0 0000 @1 © 2006 INIST-CNRS. All rights reserved.`
A45				`@0 1 p.1/4`
A47	`01`	`1`		`@0 06-0238668`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Australian journal of soil research`
A66	`01`			`@0 AUS`
C01	`01`		`ENG`	@0 We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.
C02	`01`	`2`		`@0 001E01P03`
C02	`02`	`X`		`@0 002A32B05`
C02	`03`	`2`		`@0 226C03`
C03	`01`	`X`	`FRE`	`@0 Capture @5 01`
C03	`01`	`X`	`ENG`	`@0 Capture @5 01`
C03	`01`	`X`	`SPA`	`@0 Captura @5 01`
C03	`02`	`X`	`FRE`	`@0 Ruissellement plan incliné @5 02`
C03	`02`	`X`	`ENG`	`@0 Overland flow @5 02`
C03	`02`	`X`	`SPA`	`@0 Chorreo plano inclinado @5 02`
C03	`03`	`X`	`FRE`	`@0 Pente terrain @5 03`
C03	`03`	`X`	`ENG`	`@0 Land slope @5 03`
C03	`03`	`X`	`SPA`	`@0 Pendiente terreno @5 03`
C03	`04`	`2`	`FRE`	`@0 Versant @5 04`
C03	`04`	`2`	`ENG`	`@0 slopes @5 04`
C03	`04`	`2`	`SPA`	`@0 Declive @5 04`
C03	`05`	`X`	`FRE`	`@0 Ruissellement eau sol @5 05`
C03	`05`	`X`	`ENG`	`@0 Runoff @5 05`
C03	`05`	`X`	`SPA`	`@0 Escorrentía suelo @5 05`
C03	`06`	`X`	`FRE`	`@0 Eau ruissellement @5 06`
C03	`06`	`X`	`ENG`	`@0 Runoff water @5 06`
C03	`06`	`X`	`SPA`	`@0 Escorrentía @5 06`
C03	`07`	`X`	`FRE`	`@0 Agroforesterie @5 07`
C03	`07`	`X`	`ENG`	`@0 Agroforestry @5 07`
C03	`07`	`X`	`SPA`	`@0 Agroforestal @5 07`
C03	`08`	`2`	`FRE`	`@0 Eau surface @5 08`
C03	`08`	`2`	`ENG`	`@0 surface water @5 08`
C03	`08`	`2`	`SPA`	`@0 Agua superficie @5 08`
C03	`09`	`X`	`FRE`	`@0 Gestion eau @5 09`
C03	`09`	`X`	`ENG`	`@0 Water management @5 09`
C03	`09`	`X`	`SPA`	`@0 Gestión del agua @5 09`
C03	`10`	`2`	`FRE`	`@0 Arbre @5 10`
C03	`10`	`2`	`ENG`	`@0 trees @5 10`
C03	`11`	`X`	`FRE`	`@0 Sud est @5 20`
C03	`11`	`X`	`ENG`	`@0 Southeast @5 20`
C03	`11`	`X`	`SPA`	`@0 Sureste @5 20`
C03	`12`	`2`	`FRE`	`@0 Australie @2 NG @5 21`
C03	`12`	`2`	`ENG`	`@0 Australia @2 NG @5 21`
C03	`12`	`2`	`SPA`	`@0 Australia @2 NG @5 21`
C03	`13`	`X`	`FRE`	`@0 Litière @2 NT @5 28`
C03	`13`	`X`	`ENG`	`@0 Litter @2 NT @5 28`
C03	`13`	`X`	`SPA`	`@0 Hojarasca @2 NT @5 28`
C03	`14`	`2`	`FRE`	`@0 Terrasse @5 29`
C03	`14`	`2`	`ENG`	`@0 terraces @5 29`
C03	`14`	`2`	`SPA`	`@0 Terraza @5 29`
C03	`15`	`2`	`FRE`	`@0 Infiltration @5 30`
C03	`15`	`2`	`ENG`	`@0 infiltration @5 30`
C03	`15`	`2`	`SPA`	`@0 Infiltración @5 30`
C03	`16`	`2`	`FRE`	`@0 Micro-terrasse @4 INC @5 68`
C03	`17`	`2`	`FRE`	`@0 Bande boisée @4 CD @5 96`
C03	`17`	`2`	`ENG`	`@0 Wooded strip @4 CD @5 96`
C03	`17`	`2`	`SPA`	`@0 Banda arbolada @4 CD @5 96`
C07	`01`	`2`	`FRE`	`@0 Australasie`
C07	`01`	`2`	`ENG`	`@0 Australasia`
C07	`01`	`2`	`SPA`	`@0 Australasia`
C07	`02`	`X`	`FRE`	`@0 Plante ligneuse @5 31`
C07	`02`	`X`	`ENG`	`@0 Woody plant @5 31`
C07	`02`	`X`	`SPA`	`@0 Planta leñosa @5 31`
N21				`@1 149`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

Format Inist (serveur)

NO :	PASCAL 06-0238668 INIST
ET :	Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia
AU :	ELLIS (T. W.); LEGUEDOIS (S.); HAIRSINE (P. B.); TONGWAY (D. J.)
AF :	CSIRO Land and Water, GPO Box 1666/Canberra, ACT 2606/Australie (1 aut., 2 aut., 3 aut.); INRA Soil Science Research Unit, BP 20 619 Ardon/45 1666 Oliver/France (2 aut.); CSIRO Sustainable Ecosystems, GPO Box 284/Canberra, ACT 2601/Australie (4 aut.)
DT :	Publication en série; Niveau analytique
SO :	Australian journal of soil research; ISSN 0004-9573; Coden ASORAB; Australie; Da. 2006; Vol. 44; No. 2; Pp. 117-125; Bibl. 1 p.1/4
LA :	Anglais
EA :	We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.
CC :	001E01P03; 002A32B05; 226C03
FD :	Capture; Ruissellement plan incliné; Pente terrain; Versant; Ruissellement eau sol; Eau ruissellement; Agroforesterie; Eau surface; Gestion eau; Arbre; Sud est; Australie; Litière; Terrasse; Infiltration; Micro-terrasse; Bande boisée
FG :	Australasie; Plante ligneuse
ED :	Capture; Overland flow; Land slope; slopes; Runoff; Runoff water; Agroforestry; surface water; Water management; trees; Southeast; Australia; Litter; terraces; infiltration; Wooded strip
EG :	Australasia; Woody plant
SD :	Captura; Chorreo plano inclinado; Pendiente terreno; Declive; Escorrentía suelo; Escorrentía; Agroforestal; Agua superficie; Gestión del agua; Sureste; Australia; Hojarasca; Terraza; Infiltración; Banda arbolada
LO :	INIST-10723.354000152983350040
ID :	06-0238668

Links to Exploration step

Pascal:06-0238668

Le document en format XML

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<front><div type="abstract" xml:lang="en">We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.</div>
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<fC01 i1="01" l="ENG"><s0>We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.</s0>
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<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Versant</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>slopes</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Declive</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Ruissellement eau sol</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Runoff</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Escorrentía suelo</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Eau ruissellement</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Runoff water</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Escorrentía</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Agroforesterie</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Agroforestry</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Agroforestal</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Eau surface</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>surface water</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Agua superficie</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Gestion eau</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Water management</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Gestión del agua</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Arbre</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>trees</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Sud est</s0>
<s5>20</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Southeast</s0>
<s5>20</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Sureste</s0>
<s5>20</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE"><s0>Litière</s0>
<s2>NT</s2>
<s5>28</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG"><s0>Litter</s0>
<s2>NT</s2>
<s5>28</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA"><s0>Hojarasca</s0>
<s2>NT</s2>
<s5>28</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Terrasse</s0>
<s5>29</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>terraces</s0>
<s5>29</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Terraza</s0>
<s5>29</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Infiltration</s0>
<s5>30</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>infiltration</s0>
<s5>30</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Infiltración</s0>
<s5>30</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Micro-terrasse</s0>
<s4>INC</s4>
<s5>68</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Bande boisée</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>Wooded strip</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Banda arbolada</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Plante ligneuse</s0>
<s5>31</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Woody plant</s0>
<s5>31</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Planta leñosa</s0>
<s5>31</s5>
</fC07>
<fN21><s1>149</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
<server><NO>PASCAL 06-0238668 INIST</NO>
<ET>Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia</ET>
<AU>ELLIS (T. W.); LEGUEDOIS (S.); HAIRSINE (P. B.); TONGWAY (D. J.)</AU>
<AF>CSIRO Land and Water, GPO Box 1666/Canberra, ACT 2606/Australie (1 aut., 2 aut., 3 aut.); INRA Soil Science Research Unit, BP 20 619 Ardon/45 1666 Oliver/France (2 aut.); CSIRO Sustainable Ecosystems, GPO Box 284/Canberra, ACT 2601/Australie (4 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Australian journal of soil research; ISSN 0004-9573; Coden ASORAB; Australie; Da. 2006; Vol. 44; No. 2; Pp. 117-125; Bibl. 1 p.1/4</SO>
<LA>Anglais</LA>
<EA>We describe a rainfall simulator experiment designed to measure the capture, by a fenced tree belt, of excess water generated as Hortonian flow from a pasture slope. Three rainfall events (48, 49, and 75 mm/h for 13, 30, and 30min, respectively) were applied, of which 15%, 29%, and 44%, respectively, ran off and drained onto the tree belt. The tree belt captured 100%, 32-68%, and 0-28% of the runoff from the 3 events, respectively. These captured runoff volumes represented 31-39%, 22-45%, and 0-29% increases in water supply to the trees, in addition to incident rainfall. Infiltration rates within the tree belt were up to 46% higher than in the pasture zone. This higher infiltration was mainly attributed to better soil surface conditions in the absence of stock and a 50-mm layer of tree litter. Overland flows within the tree belt formed tree litter into microterraces, which spread and slowed flows and allowed greater time for infiltration.</EA>
<CC>001E01P03; 002A32B05; 226C03</CC>
<FD>Capture; Ruissellement plan incliné; Pente terrain; Versant; Ruissellement eau sol; Eau ruissellement; Agroforesterie; Eau surface; Gestion eau; Arbre; Sud est; Australie; Litière; Terrasse; Infiltration; Micro-terrasse; Bande boisée</FD>
<FG>Australasie; Plante ligneuse</FG>
<ED>Capture; Overland flow; Land slope; slopes; Runoff; Runoff water; Agroforestry; surface water; Water management; trees; Southeast; Australia; Litter; terraces; infiltration; Wooded strip</ED>
<EG>Australasia; Woody plant</EG>
<SD>Captura; Chorreo plano inclinado; Pendiente terreno; Declive; Escorrentía suelo; Escorrentía; Agroforestal; Agua superficie; Gestión del agua; Sureste; Australia; Hojarasca; Terraza; Infiltración; Banda arbolada</SD>
<LO>INIST-10723.354000152983350040</LO>
<ID>06-0238668</ID>
</server>
</inist>
</record>

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	Serveur d'exploration sur les relations entre la France et l'Australie
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Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia

Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia

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