AustralieFrV1, Main, Curation, bibRecord, 00A060

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

Identifieur interne : 00A060 ( Main/Curation ); précédent : 00A059; suivant : 00A061

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

Auteurs : T. W. Ellis [Australie] ; S. Leguedois [Australie, France] ; P. B. Hairsine [Australie] ; D. J. Tongway [Australie]

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.
Wicri :
- geographic : Australie.
- topic : Agroforesterie, Arbre.

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.

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Pascal:06-0238668

Le document en format XML

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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Capture of overland flow by a tree belt on a pastured hillslope in south-eastern Australia</title>
<author><name sortKey="Ellis, T W" sort="Ellis, T W" uniqKey="Ellis T" first="T. W." last="Ellis">T. W. Ellis</name>
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<author><name sortKey="Leguedois, S" sort="Leguedois, S" uniqKey="Leguedois S" first="S." last="Leguedois">S. Leguedois</name>
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<term>Australia</term>
<term>Capture</term>
<term>Land slope</term>
<term>Litter</term>
<term>Overland flow</term>
<term>Runoff</term>
<term>Runoff water</term>
<term>Southeast</term>
<term>Water management</term>
<term>Wooded strip</term>
<term>infiltration</term>
<term>slopes</term>
<term>surface water</term>
<term>terraces</term>
<term>trees</term>
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<term>Ruissellement plan incliné</term>
<term>Pente terrain</term>
<term>Versant</term>
<term>Ruissellement eau sol</term>
<term>Eau ruissellement</term>
<term>Agroforesterie</term>
<term>Eau surface</term>
<term>Gestion eau</term>
<term>Arbre</term>
<term>Sud est</term>
<term>Australie</term>
<term>Litière</term>
<term>Terrasse</term>
<term>Infiltration</term>
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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>
</front>
</TEI>
</record>

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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

Source :

Descripteurs français

English descriptors

Abstract

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

Links to Exploration step

Le document en format XML

Pour manipuler ce document sous Unix (Dilib)

Pour mettre un lien sur cette page dans le réseau Wicri