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Soil-plant system development 9 to 136 years after marly gully beds rehabilitation (French Southern Alps)

Authors :
Erktan, Amandine
Cohen, M.
Zerouali, L.
Poulenard, J.
Cecillon, L.
Rey, F.
Ecosystèmes montagnards (UR EMGR)
Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
Université Paris Diderot - Paris 7 (UPD7)
UNIVERSITE DE SAVOIE FRA
Partenaires IRSTEA
Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)
Irstea Publications, Migration
Source :
Geophysical Research Abstracts, EGU General Assembly, EGU General Assembly, Apr 2014, Vienna, Austria. pp.1
Publication Year :
2014
Publisher :
HAL CCSD, 2014.

Abstract

International audience; Marly badlands, showing active eroded gullies and low soil fertility, are found in the French Southern Alps since around 250 years. Negative ecological, social and and economical consequences of such intense erosion historically promoted the ecological restoration of these terrains. In a small catchment of 390 ha (Saignon catchment, France), a first wave of restoration was run in 1876-78, mainly through Austrian black pine plantation on eroded gully sides. A second wave occurred in 2002 and focused on gullies partly vegetated on their sides but still showing active gully beds. Bioengineering works, made of barriers of Salix cuttings, were implanted in gully beds to increase sedimentation and in turn to re-initiate soil formation. This strategy proved to be efficient to retain sediment and to favor plant colonization. The aim of this study was to investigate soil fertility of sediment mounds retained in gully beds 9 to 136 years after their rehabilitation. To answer this question, we compared the topsoil (0-10 cm depth) chemical fertility of 6 gully beds restored in 2002 with bioengineering works to the one of 5 gully beds belonging to gullies stabilized by pine plantation 136 years ago. As a control, sediment mounds found in 15 bare gully beds were also studied. In each gully, basic soil characteristics of composite samples were assessed. Vegetative cover, plant richness and litter accumulation were also measured. We found that soil organic carbon and total nitrogen content significantly increased with the time since gully bed rehabilitation (4.3±0.4 / 12±1 / 21±2 g.kg-1 and 0.80±0.02 / 1.4±0.02 / 1.7±0.07 g.kg-1) for bare gully beds and gully beds rehabilitated 9 and 140 years ago, respectively. Carbonate content was lower in restored gullies (average value of 242±5 g.kg-1) compared to control ones (547±13 g.kg-1). These results suggest that pedogenesis was engaged in both sets of restored gullies (decarbonatation process). Available phosphorus was lowest in gully beds restored in 2002 (8.3±4 mg.kg-1; ANOVA test, p

Details

Language :
English
Database :
OpenAIRE
Journal :
Geophysical Research Abstracts, EGU General Assembly, EGU General Assembly, Apr 2014, Vienna, Austria. pp.1
Accession number :
edsair.dedup.wf.001..f68a93016d51ae5c51bb7b779a9fe8d7