UnivTrevesV1, PascalFrancis, Corpus, bibRecord, 000096

Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes

Identifieur interne : 000096 ( PascalFrancis/Corpus ); précédent : 000095; suivant : 000097

Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes

Auteurs : J. B. Ries ; K. Andres ; S. Wirtz ; S. Tumbrink ; T. Wilms ; K. D. Peter ; M. Burczyk ; V. Butzen ; M. Seeger

Source :

Zeitschrift für Geomorphologie [ 0372-8854 ] ; 2014.

RBID : Francis:28944033

Descripteurs français

Pascal (Inist)
- Domaine aride, Domaine semi-aride, Dégradation des sols, Erosion des sols, Piétinement, Ovin, Caprin, Analyse quantitative, Pente de versant, Translocation, Fragment de roche, Parcelle expérimentale, Espagne, Andalucía, Méditerranéens, pays, Biogéomorphologie.

English descriptors

KwdEn :
- Andalusia, Arid area, Biogeomorphology, Experiment plot, Goat, Mediterranean States, Quantitative analysis, Rock fragment, Semi-arid area, Sheep, Slope gradient, Soil degradation, Soil erosion, Spain, Trampling.

Abstract

In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A06				`@2 3 @3 Suppl.`
A08	`01`	`1`	`ENG`	`@1 Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes`
A09	`01`	`1`	`ENG`	`@1 Past to present Quaternary landform change : natural and anthropogenic drivers`
A11	`01`	`1`		`@1 RIES (J.B.)`
A11	`02`	`1`		`@1 ANDRES (K.)`
A11	`03`	`1`		`@1 WIRTZ (S.)`
A11	`04`	`1`		`@1 TUMBRINK (S.)`
A11	`05`	`1`		`@1 WILMS (T.)`
A11	`06`	`1`		`@1 PETER (K.D.)`
A11	`07`	`1`		`@1 BURCZYK (M.)`
A11	`08`	`1`		`@1 BUTZEN (V.)`
A11	`09`	`1`		`@1 SEEGER (M.)`
A12	`01`	`1`		`@1 WUNDERLICH (J.) @9 ed.`
A12	`02`	`1`		`@1 HOUBEN (P.) @9 ed.`
A14	`01`			`@1 Dept. of Physical geography, FB VI - Geography/Geosciences, Trier Univ., Campus II @2 Trier @3 DEU @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut. @Z 5 aut. @Z 6 aut. @Z 7 aut. @Z 8 aut. @Z 9 aut.`
A15	`01`			`@1 Dept. of Physical Geography, Goethe-Univ. @2 Frankfurt am Main @3 DEU @Z 10 aut.`
A15	`02`			`@1 Dept. of Physical Geography, Univ. @2 Leiden @3 NLD @Z 11 aut.`
A20				`@1 23-45 @3 10 fig., 2 tabl.`
A21				`@1 2014`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 8829`
A44	`01`			`@0 8200 @1 Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2014`
A45				`@0 3 p.`
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C01	`01`		`ENG`	@0 In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved
C02	`01`	`G`		`@0 53148 @1 531III`
C02	`02`	`G`		`@0 531`
C03	`01`	`G`	`FRE`	`@0 Domaine aride @2 NI @5 01`
C03	`01`	`G`	`ENG`	`@0 Arid area @2 NI @5 01`
C03	`01`	`G`	`SPA`	`@0 Campo árido @2 NI @5 01`
C03	`02`	`G`	`FRE`	`@0 Domaine semi-aride @2 NI @5 02`
C03	`02`	`G`	`ENG`	`@0 Semi-arid area @2 NI @5 02`
C03	`02`	`G`	`SPA`	`@0 Campo semiárido @2 NI @5 02`
C03	`03`	`G`	`FRE`	`@0 Dégradation des sols @2 NI @5 03`
C03	`03`	`G`	`ENG`	`@0 Soil degradation @2 NI @5 03`
C03	`03`	`G`	`SPA`	`@0 Degradación de los suelos @2 NI @5 03`
C03	`04`	`G`	`FRE`	`@0 Erosion des sols @2 NI @5 04`
C03	`04`	`G`	`ENG`	`@0 Soil erosion @2 NI @5 04`
C03	`04`	`G`	`SPA`	`@0 Erosión de los suelos @2 NI @5 04`
C03	`05`	`G`	`FRE`	`@0 Piétinement @2 NI @4 INC @5 05`
C03	`05`	`G`	`ENG`	`@0 Trampling @2 NI @4 INC @5 05`
C03	`06`	`G`	`FRE`	`@0 Ovin @2 NI @5 06`
C03	`06`	`G`	`ENG`	`@0 Sheep @2 NI @5 06`
C03	`06`	`G`	`SPA`	`@0 Ovino @2 NI @5 06`
C03	`07`	`G`	`FRE`	`@0 Caprin @2 NI @5 07`
C03	`07`	`G`	`ENG`	`@0 Goat @2 NI @5 07`
C03	`07`	`G`	`SPA`	`@0 Caprino @2 NI @5 07`
C03	`08`	`G`	`FRE`	`@0 Analyse quantitative @2 NI @5 08`
C03	`08`	`G`	`ENG`	`@0 Quantitative analysis @2 NI @5 08`
C03	`08`	`G`	`SPA`	`@0 Análisis cuantitativo @2 NI @5 08`
C03	`09`	`G`	`FRE`	`@0 Pente de versant @2 NI @5 09`
C03	`09`	`G`	`ENG`	`@0 Slope gradient @2 NI @5 09`
C03	`09`	`G`	`SPA`	`@0 Inclinación de la vertiente @2 NI @5 09`
C03	`10`	`G`	`FRE`	`@0 Translocation @4 INC @5 10`
C03	`11`	`G`	`FRE`	`@0 Fragment de roche @2 NI @4 INC @5 11`
C03	`11`	`G`	`ENG`	`@0 Rock fragment @2 NI @4 INC @5 11`
C03	`12`	`G`	`FRE`	`@0 Parcelle expérimentale @2 NI @5 12`
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C03	`13`	`G`	`FRE`	`@0 Espagne @2 NG @5 13`
C03	`13`	`G`	`ENG`	`@0 Spain @2 NG @5 13`
C03	`13`	`G`	`SPA`	`@0 España @2 NG @5 13`
C03	`14`	`G`	`FRE`	`@0 Andalucía @2 NG @5 14`
C03	`14`	`G`	`ENG`	`@0 Andalusia @2 NG @5 14`
C03	`15`	`G`	`FRE`	`@0 Méditerranéens, pays @2 NG @5 15`
C03	`15`	`G`	`ENG`	`@0 Mediterranean States @2 NG @5 15`
C03	`15`	`G`	`SPA`	`@0 Países méditerranéos @2 NG @5 15`
C03	`16`	`G`	`FRE`	`@0 Biogéomorphologie @5 16`
C03	`16`	`G`	`ENG`	`@0 Biogeomorphology @5 16`
C03	`16`	`G`	`SPA`	`@0 Biogeomorfología @5 16`
C04	`01`	`G`		`@0 U2 @1 13!14!03,05,06,07`
C04	`02`	`G`		`@0 U2 @1 15!03,05,06,07!12,08,10,11`
C04	`03`	`G`		`@0 U1 @1 04!16,05,06,07!10,11,12,15`
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C06				`@0 FIS @0 TAS`

Format Inist (serveur)

NO :	FRANCIS 28944033 PRODIG-INTERGEO
ET :	Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes
AU :	RIES (J.B.); ANDRES (K.); WIRTZ (S.); TUMBRINK (S.); WILMS (T.); PETER (K.D.); BURCZYK (M.); BUTZEN (V.); SEEGER (M.); WUNDERLICH (J.); HOUBEN (P.)
AF :	Dept. of Physical geography, FB VI - Geography/Geosciences, Trier Univ., Campus II/Trier/Allemagne (1 aut., 2 aut., 3 aut., 4 aut., 5 aut., 6 aut., 7 aut., 8 aut., 9 aut.); Dept. of Physical Geography, Goethe-Univ./Frankfurt am Main/Allemagne (10 aut.); Dept. of Physical Geography, Univ./Leiden/Pays-Bas (11 aut.)
DT :	Publication en série; Niveau analytique
SO :	Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2014; Vol. 58; No. 3 Suppl.; Pp. 23-45; Bibl. 3 p.; 10 fig., 2 tabl.
LA :	Anglais
EA :	In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved
CC :	53148; 531
FD :	Domaine aride; Domaine semi-aride; Dégradation des sols; Erosion des sols; Piétinement; Ovin; Caprin; Analyse quantitative; Pente de versant; Translocation; Fragment de roche; Parcelle expérimentale; Espagne; Andalucía; Méditerranéens, pays; Biogéomorphologie
ED :	Arid area; Semi-arid area; Soil degradation; Soil erosion; Trampling; Sheep; Goat; Quantitative analysis; Slope gradient; Rock fragment; Experiment plot; Spain; Andalusia; Mediterranean States; Biogeomorphology
SD :	Campo árido; Campo semiárido; Degradación de los suelos; Erosión de los suelos; Ovino; Caprino; Análisis cuantitativo; Inclinación de la vertiente; Parcela experimental; España; Países méditerranéos; Biogeomorfología
LO :	INIST-8829
ID :	28944033

Links to Exploration step

Francis:28944033

Le document en format XML

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<s2>Trier</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
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<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
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<author><name sortKey="Seeger, M" sort="Seeger, M" uniqKey="Seeger M" first="M." last="Seeger">M. Seeger</name>
<affiliation><inist:fA14 i1="01"><s1>Dept. of Physical geography, FB VI - Geography/Geosciences, Trier Univ., Campus II</s1>
<s2>Trier</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
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<series><title level="j" type="main">Zeitschrift für Geomorphologie</title>
<title level="j" type="abbreviated">Z. Geomorphol.</title>
<idno type="ISSN">0372-8854</idno>
<imprint><date when="2014">2014</date>
</imprint>
</series>
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<seriesStmt><title level="j" type="main">Zeitschrift für Geomorphologie</title>
<title level="j" type="abbreviated">Z. Geomorphol.</title>
<idno type="ISSN">0372-8854</idno>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Andalusia</term>
<term>Arid area</term>
<term>Biogeomorphology</term>
<term>Experiment plot</term>
<term>Goat</term>
<term>Mediterranean States</term>
<term>Quantitative analysis</term>
<term>Rock fragment</term>
<term>Semi-arid area</term>
<term>Sheep</term>
<term>Slope gradient</term>
<term>Soil degradation</term>
<term>Soil erosion</term>
<term>Spain</term>
<term>Trampling</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Domaine aride</term>
<term>Domaine semi-aride</term>
<term>Dégradation des sols</term>
<term>Erosion des sols</term>
<term>Piétinement</term>
<term>Ovin</term>
<term>Caprin</term>
<term>Analyse quantitative</term>
<term>Pente de versant</term>
<term>Translocation</term>
<term>Fragment de roche</term>
<term>Parcelle expérimentale</term>
<term>Espagne</term>
<term>Andalucía</term>
<term>Méditerranéens, pays</term>
<term>Biogéomorphologie</term>
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<front><div type="abstract" xml:lang="en">In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved</div>
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<s3>Suppl.</s3>
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<fA08 i1="01" i2="1" l="ENG"><s1>Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes</s1>
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<fA09 i1="01" i2="1" l="ENG"><s1>Past to present Quaternary landform change : natural and anthropogenic drivers</s1>
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<fA11 i1="01" i2="1"><s1>RIES (J.B.)</s1>
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<fA11 i1="02" i2="1"><s1>ANDRES (K.)</s1>
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<fA11 i1="03" i2="1"><s1>WIRTZ (S.)</s1>
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<fA11 i1="04" i2="1"><s1>TUMBRINK (S.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>WILMS (T.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>PETER (K.D.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>BURCZYK (M.)</s1>
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<fA11 i1="08" i2="1"><s1>BUTZEN (V.)</s1>
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<fA11 i1="09" i2="1"><s1>SEEGER (M.)</s1>
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<fA12 i1="01" i2="1"><s1>WUNDERLICH (J.)</s1>
<s9>ed.</s9>
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<fA12 i1="02" i2="1"><s1>HOUBEN (P.)</s1>
<s9>ed.</s9>
</fA12>
<fA14 i1="01"><s1>Dept. of Physical geography, FB VI - Geography/Geosciences, Trier Univ., Campus II</s1>
<s2>Trier</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>7 aut.</sZ>
<sZ>8 aut.</sZ>
<sZ>9 aut.</sZ>
</fA14>
<fA15 i1="01"><s1>Dept. of Physical Geography, Goethe-Univ.</s1>
<s2>Frankfurt am Main</s2>
<s3>DEU</s3>
<sZ>10 aut.</sZ>
</fA15>
<fA15 i1="02"><s1>Dept. of Physical Geography, Univ.</s1>
<s2>Leiden</s2>
<s3>NLD</s3>
<sZ>11 aut.</sZ>
</fA15>
<fA20><s1>23-45</s1>
<s3>10 fig., 2 tabl.</s3>
</fA20>
<fA21><s1>2014</s1>
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<fC01 i1="01" l="ENG"><s0>In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved</s0>
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<s1>531III</s1>
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<fC03 i1="01" i2="G" l="FRE"><s0>Domaine aride</s0>
<s2>NI</s2>
<s5>01</s5>
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<s2>NI</s2>
<s5>01</s5>
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<fC03 i1="01" i2="G" l="SPA"><s0>Campo árido</s0>
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<s5>01</s5>
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<s5>02</s5>
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<fC03 i1="02" i2="G" l="ENG"><s0>Semi-arid area</s0>
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<fC03 i1="02" i2="G" l="SPA"><s0>Campo semiárido</s0>
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<fC03 i1="03" i2="G" l="FRE"><s0>Dégradation des sols</s0>
<s2>NI</s2>
<s5>03</s5>
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<fC03 i1="03" i2="G" l="ENG"><s0>Soil degradation</s0>
<s2>NI</s2>
<s5>03</s5>
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<fC03 i1="03" i2="G" l="SPA"><s0>Degradación de los suelos</s0>
<s2>NI</s2>
<s5>03</s5>
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<fC03 i1="04" i2="G" l="FRE"><s0>Erosion des sols</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="G" l="ENG"><s0>Soil erosion</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="G" l="SPA"><s0>Erosión de los suelos</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="G" l="FRE"><s0>Piétinement</s0>
<s2>NI</s2>
<s4>INC</s4>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="G" l="ENG"><s0>Trampling</s0>
<s2>NI</s2>
<s4>INC</s4>
<s5>05</s5>
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<fC03 i1="06" i2="G" l="FRE"><s0>Ovin</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="G" l="ENG"><s0>Sheep</s0>
<s2>NI</s2>
<s5>06</s5>
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<fC03 i1="06" i2="G" l="SPA"><s0>Ovino</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="G" l="FRE"><s0>Caprin</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="G" l="ENG"><s0>Goat</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="G" l="SPA"><s0>Caprino</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="G" l="FRE"><s0>Analyse quantitative</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="G" l="ENG"><s0>Quantitative analysis</s0>
<s2>NI</s2>
<s5>08</s5>
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<fC03 i1="08" i2="G" l="SPA"><s0>Análisis cuantitativo</s0>
<s2>NI</s2>
<s5>08</s5>
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<fC03 i1="09" i2="G" l="FRE"><s0>Pente de versant</s0>
<s2>NI</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="G" l="ENG"><s0>Slope gradient</s0>
<s2>NI</s2>
<s5>09</s5>
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<fC03 i1="09" i2="G" l="SPA"><s0>Inclinación de la vertiente</s0>
<s2>NI</s2>
<s5>09</s5>
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<fC03 i1="10" i2="G" l="FRE"><s0>Translocation</s0>
<s4>INC</s4>
<s5>10</s5>
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<fC03 i1="11" i2="G" l="FRE"><s0>Fragment de roche</s0>
<s2>NI</s2>
<s4>INC</s4>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="G" l="ENG"><s0>Rock fragment</s0>
<s2>NI</s2>
<s4>INC</s4>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="G" l="FRE"><s0>Parcelle expérimentale</s0>
<s2>NI</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="G" l="ENG"><s0>Experiment plot</s0>
<s2>NI</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="G" l="SPA"><s0>Parcela experimental</s0>
<s2>NI</s2>
<s5>12</s5>
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<fC03 i1="13" i2="G" l="FRE"><s0>Espagne</s0>
<s2>NG</s2>
<s5>13</s5>
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<fC03 i1="13" i2="G" l="ENG"><s0>Spain</s0>
<s2>NG</s2>
<s5>13</s5>
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<s2>NG</s2>
<s5>13</s5>
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<fC03 i1="14" i2="G" l="FRE"><s0>Andalucía</s0>
<s2>NG</s2>
<s5>14</s5>
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<fC03 i1="14" i2="G" l="ENG"><s0>Andalusia</s0>
<s2>NG</s2>
<s5>14</s5>
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<fC03 i1="15" i2="G" l="FRE"><s0>Méditerranéens, pays</s0>
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<s5>15</s5>
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<fC04 i1="04" i2="G"><s0>U1</s0>
<s1>01!02,03,10,11!05,06,07,15</s1>
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<server><NO>FRANCIS 28944033 PRODIG-INTERGEO</NO>
<ET>Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes</ET>
<AU>RIES (J.B.); ANDRES (K.); WIRTZ (S.); TUMBRINK (S.); WILMS (T.); PETER (K.D.); BURCZYK (M.); BUTZEN (V.); SEEGER (M.); WUNDERLICH (J.); HOUBEN (P.)</AU>
<AF>Dept. of Physical geography, FB VI - Geography/Geosciences, Trier Univ., Campus II/Trier/Allemagne (1 aut., 2 aut., 3 aut., 4 aut., 5 aut., 6 aut., 7 aut., 8 aut., 9 aut.); Dept. of Physical Geography, Goethe-Univ./Frankfurt am Main/Allemagne (10 aut.); Dept. of Physical Geography, Univ./Leiden/Pays-Bas (11 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2014; Vol. 58; No. 3 Suppl.; Pp. 23-45; Bibl. 3 p.; 10 fig., 2 tabl.</SO>
<LA>Anglais</LA>
<EA>In this study, the process dynamics of material disaggregation and translocation directly caused by trampling animals was quantified by means of experimental methods on test plots. Gerlach troughs were installed in order to quantify material mobilization in different directions. The slope angle and the running speed of the animals were varied. Additionally, the amount of material that was loosened by the hooves of the goats was measured. The translocation rates were surprisingly high and slope angles as well as running speed turned out to be important influencing factors. While rock movement occurred in all directions, most often the rock fragments were kicked forward downslope. Net mean downslope translocation rates varied between 1.5 cm and 6.6 cm corresponding with slope and the total number of rock fragments moved</EA>
<CC>53148; 531</CC>
<FD>Domaine aride; Domaine semi-aride; Dégradation des sols; Erosion des sols; Piétinement; Ovin; Caprin; Analyse quantitative; Pente de versant; Translocation; Fragment de roche; Parcelle expérimentale; Espagne; Andalucía; Méditerranéens, pays; Biogéomorphologie</FD>
<ED>Arid area; Semi-arid area; Soil degradation; Soil erosion; Trampling; Sheep; Goat; Quantitative analysis; Slope gradient; Rock fragment; Experiment plot; Spain; Andalusia; Mediterranean States; Biogeomorphology</ED>
<SD>Campo árido; Campo semiárido; Degradación de los suelos; Erosión de los suelos; Ovino; Caprino; Análisis cuantitativo; Inclinación de la vertiente; Parcela experimental; España; Países méditerranéos; Biogeomorfología</SD>
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Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes

Sheep and goat erosion ========ndash; experimental geomorphology as an approach for the quantification of underestimated processes

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