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Run-on contribution to a Sahelian two-phase mosaic system : Soil water regime and vegetation life cycles

Identifieur interne : 006E02 ( PascalFrancis/Curation ); précédent : 006E01; suivant : 006E03

Run-on contribution to a Sahelian two-phase mosaic system : Soil water regime and vegetation life cycles

Auteurs : J. Seghieri [France] ; S. Galle [France]

Source :

RBID : Pascal:99-0431078

Descripteurs français

English descriptors

Abstract

An experiment was carried out from 1992 to 1995, in south-western Niger on a banded vegetation pattern which dominates on a laterite-capped plateau in the region. We quantified the changes in infiltration and vegetation in a thicket from which run-on from the upslope bare soil zone was artificially divested. A concrete wall (40 m long, 60 cm high, 20 cm thick, with a foundation 25 cm deep) was constructed at its upslope boundary. Infiltration was measured to a depth of 5,4 m by a neutron probe, and densities of annual plants were monitored along transects crossing perpendicularly a control thicket and the thicket deprived of run-on. Phenological phases and leaf water potential of the two dominant shrub species were recorded from stratified sampling according to their preferred location along the water resource gradient. Results indicated that run-on contributed the most to infiltration in the central zone, but the water content available to the annual plants (layer 0-10 cm) was not affected by run-on deprivation. Significant differences were found in the water content available to the shrubs (layer 0-100 cm) both between zones (upslope and central), and between thickets after the wall was built. However, in the thicket deprived of run-on, life cycle and physiology of the shrubs were severely disturbed upslope, while much smaller effects were observed in the centre. Surprisingly, within the study interval, run-on contribution was not found to be as essential to shrubs' life cycle at the location where it contributed the most to the infiltration.
pA  
A01 01  1    @0 1146-609X
A03   1    @0 Acta oecol. : (Montrouge)
A05       @2 20
A06       @2 3
A08 01  1  ENG  @1 Run-on contribution to a Sahelian two-phase mosaic system : Soil water regime and vegetation life cycles
A09 01  1  ENG  @1 Banded Vegetation Patterns
A11 01  1    @1 SEGHIERI (J.)
A11 02  1    @1 GALLE (S.)
A12 01  1    @1 TONGWAY (David) @9 introd.
A12 02  1    @1 SEGHIERI (Josiane) @9 introd.
A14 01      @1 IRD, B.P. 5045 @2 34032 Montpellier @3 FRA @Z 1 aut.
A14 02      @1 LTHE, B.P. 53 @2 38041 Grenoble @3 FRA @Z 2 aut.
A15 01      @1 "Gungahlin Homestead", CSIRO Wildlife and Ecology, GPO Box 284 @2 Canberra 2601 ACT @3 AUS @Z 1 aut.
A15 02      @1 IRD, B.P. 5045 @2 34032 Montpellier @3 FRA @Z 2 aut.
A20       @1 209-217
A21       @1 1999
A23 01      @0 ENG
A43 01      @1 INIST @2 12904 @5 354000086017920070
A44       @0 0000 @1 © 1999 INIST-CNRS. All rights reserved.
A45       @0 24 ref.
A47 01  1    @0 99-0431078
A60       @1 P
A61       @0 A
A64 01  1    @0 Acta oecologica : (Montrouge)
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C01 01    ENG  @0 An experiment was carried out from 1992 to 1995, in south-western Niger on a banded vegetation pattern which dominates on a laterite-capped plateau in the region. We quantified the changes in infiltration and vegetation in a thicket from which run-on from the upslope bare soil zone was artificially divested. A concrete wall (40 m long, 60 cm high, 20 cm thick, with a foundation 25 cm deep) was constructed at its upslope boundary. Infiltration was measured to a depth of 5,4 m by a neutron probe, and densities of annual plants were monitored along transects crossing perpendicularly a control thicket and the thicket deprived of run-on. Phenological phases and leaf water potential of the two dominant shrub species were recorded from stratified sampling according to their preferred location along the water resource gradient. Results indicated that run-on contributed the most to infiltration in the central zone, but the water content available to the annual plants (layer 0-10 cm) was not affected by run-on deprivation. Significant differences were found in the water content available to the shrubs (layer 0-100 cm) both between zones (upslope and central), and between thickets after the wall was built. However, in the thicket deprived of run-on, life cycle and physiology of the shrubs were severely disturbed upslope, while much smaller effects were observed in the centre. Surprisingly, within the study interval, run-on contribution was not found to be as essential to shrubs' life cycle at the location where it contributed the most to the infiltration.
C02 01  X    @0 002A14B04B
C03 01  X  FRE  @0 Humidité sol @5 01
C03 01  X  ENG  @0 Soil moisture @5 01
C03 01  X  SPA  @0 Humedad suelo @5 01
C03 02  X  FRE  @0 Cycle développement @5 02
C03 02  X  ENG  @0 Life cycle @5 02
C03 02  X  SPA  @0 Ciclo desarrollo @5 02
C03 03  X  FRE  @0 Dynamique végétation @5 03
C03 03  X  ENG  @0 Vegetation dynamics @5 03
C03 03  X  SPA  @0 Dinámica vegetación @5 03
C03 04  X  FRE  @0 Pluviométrie @5 04
C03 04  X  ENG  @0 Rainfall rate recording @5 04
C03 04  X  SPA  @0 Pluviometría @5 04
C03 05  X  FRE  @0 Zone semi aride @5 05
C03 05  X  ENG  @0 Semi arid zone @5 05
C03 05  X  SPA  @0 Zona semiárida @5 05
C03 06  X  FRE  @0 Climat tropical @5 06
C03 06  X  ENG  @0 Tropical climate @5 06
C03 06  X  SPA  @0 Clima tropical @5 06
C03 07  X  FRE  @0 Potentiel hydrique @5 07
C03 07  X  ENG  @0 Water potential @5 07
C03 07  X  SPA  @0 Potencial hídrico @5 07
C03 08  X  FRE  @0 Densité population @5 08
C03 08  X  ENG  @0 Population density @5 08
C03 08  X  SPA  @0 Densidad población @5 08
C03 09  X  FRE  @0 Spermatophyta @2 NS @5 10
C03 09  X  ENG  @0 Spermatophyta @2 NS @5 10
C03 09  X  SPA  @0 Spermatophyta @2 NS @5 10
C03 10  X  FRE  @0 Niger @2 NG @5 20
C03 10  X  ENG  @0 Niger @2 NG @5 20
C03 10  X  SPA  @0 Niger @2 NG @5 20
C03 11  X  FRE  @0 Phénologie @5 33
C03 11  X  ENG  @0 Phenology @5 33
C03 11  X  SPA  @0 Fenología @5 33
C03 12  X  FRE  @0 Stress hydrique @5 34
C03 12  X  ENG  @0 Water stress @5 34
C03 12  X  SPA  @0 Tension hídrica @5 34
C03 13  X  FRE  @0 Efficacité utilisation eau @5 35
C03 13  X  ENG  @0 Water use efficiency @5 35
C03 13  X  SPA  @0 Eficacia utilización agua @5 35
C07 01  X  FRE  @0 Afrique @2 NG
C07 01  X  ENG  @0 Africa @2 NG
C07 01  X  SPA  @0 Africa @2 NG
C07 02  X  FRE  @0 Plante herbacée @5 40
C07 02  X  ENG  @0 Herbaceous plant @5 40
C07 02  X  SPA  @0 Planta herbácea @5 40
C07 03  X  FRE  @0 Plante ligneuse @5 41
C07 03  X  ENG  @0 Woody plant @5 41
C07 03  X  SPA  @0 Planta leñosa @5 41
C07 04  X  FRE  @0 Afrique Ouest @2 NG @5 59
C07 04  X  ENG  @0 West Africa @2 NG @5 59
C07 04  X  SPA  @0 Africa occidental @2 NG @5 59
N21       @1 277

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Pascal:99-0431078

Le document en format XML

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<div type="abstract" xml:lang="en">An experiment was carried out from 1992 to 1995, in south-western Niger on a banded vegetation pattern which dominates on a laterite-capped plateau in the region. We quantified the changes in infiltration and vegetation in a thicket from which run-on from the upslope bare soil zone was artificially divested. A concrete wall (40 m long, 60 cm high, 20 cm thick, with a foundation 25 cm deep) was constructed at its upslope boundary. Infiltration was measured to a depth of 5,4 m by a neutron probe, and densities of annual plants were monitored along transects crossing perpendicularly a control thicket and the thicket deprived of run-on. Phenological phases and leaf water potential of the two dominant shrub species were recorded from stratified sampling according to their preferred location along the water resource gradient. Results indicated that run-on contributed the most to infiltration in the central zone, but the water content available to the annual plants (layer 0-10 cm) was not affected by run-on deprivation. Significant differences were found in the water content available to the shrubs (layer 0-100 cm) both between zones (upslope and central), and between thickets after the wall was built. However, in the thicket deprived of run-on, life cycle and physiology of the shrubs were severely disturbed upslope, while much smaller effects were observed in the centre. Surprisingly, within the study interval, run-on contribution was not found to be as essential to shrubs' life cycle at the location where it contributed the most to the infiltration.</div>
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<s5>34</s5>
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</fC03>
<fC03 i1="13" i2="X" l="FRE">
<s0>Efficacité utilisation eau</s0>
<s5>35</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG">
<s0>Water use efficiency</s0>
<s5>35</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA">
<s0>Eficacia utilización agua</s0>
<s5>35</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE">
<s0>Afrique</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG">
<s0>Africa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA">
<s0>Africa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE">
<s0>Plante herbacée</s0>
<s5>40</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG">
<s0>Herbaceous plant</s0>
<s5>40</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA">
<s0>Planta herbácea</s0>
<s5>40</s5>
</fC07>
<fC07 i1="03" i2="X" l="FRE">
<s0>Plante ligneuse</s0>
<s5>41</s5>
</fC07>
<fC07 i1="03" i2="X" l="ENG">
<s0>Woody plant</s0>
<s5>41</s5>
</fC07>
<fC07 i1="03" i2="X" l="SPA">
<s0>Planta leñosa</s0>
<s5>41</s5>
</fC07>
<fC07 i1="04" i2="X" l="FRE">
<s0>Afrique Ouest</s0>
<s2>NG</s2>
<s5>59</s5>
</fC07>
<fC07 i1="04" i2="X" l="ENG">
<s0>West Africa</s0>
<s2>NG</s2>
<s5>59</s5>
</fC07>
<fC07 i1="04" i2="X" l="SPA">
<s0>Africa occidental</s0>
<s2>NG</s2>
<s5>59</s5>
</fC07>
<fN21>
<s1>277</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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