2007
DOI: 10.1657/1523-0430(2007)39[25:ibvras]2.0.co;2
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Interactions between Vegetation, Roots, and Soil Stability in Restored High-altitude Ski Runs in the Alps

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Cited by 60 publications
(57 citation statements)
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References 45 publications
(38 reference statements)
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“…Accordingly, less organic matter has been found in the upper organo-mineral horizons (A) of the ski-slopes compared to the grasslands, suggesting either a lower organic matter accumulation, due to a lower biomass production in the ski-slope soil, or a stronger dilution of the former soil organic matter caused by mixing mineral and organo-mineral horizons during the ski-slope construction process. These results are in keeping with those reported in previous papers (Freppaz et al 2002;Gros et al 2004;Barni et al 2007;Pintar et al 2009;Pohl et al 2009;Martin et al 2010;Roux-Fouillet et al 2011). Moreover, most of the soil properties in both the ski-pistes and in the grasslands seemed to be closely related to elevation.…”
Section: Discussionsupporting
confidence: 92%
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“…Accordingly, less organic matter has been found in the upper organo-mineral horizons (A) of the ski-slopes compared to the grasslands, suggesting either a lower organic matter accumulation, due to a lower biomass production in the ski-slope soil, or a stronger dilution of the former soil organic matter caused by mixing mineral and organo-mineral horizons during the ski-slope construction process. These results are in keeping with those reported in previous papers (Freppaz et al 2002;Gros et al 2004;Barni et al 2007;Pintar et al 2009;Pohl et al 2009;Martin et al 2010;Roux-Fouillet et al 2011). Moreover, most of the soil properties in both the ski-pistes and in the grasslands seemed to be closely related to elevation.…”
Section: Discussionsupporting
confidence: 92%
“…Natural recovery, which depends on seed immigration from neighboring vegetation and/or more distant areas (Urbanska and Fattorini 2000), was nearly almost totally absent at Salati partly because of the pedo-turbation of the soil and the shallow soil depth found at the high elevation. These results confirm that the revegetation process of high altitude ski-pistes is difficult, slow and does not lead to a sustainable community (Barni et al 2007;Roux Fouillet et al 2011). The impact of ski-piste construction may be mitigated by hydroseeding, a useful technique to create a fast soil cover which can counteract erosion and reduce the negative visual impact of bare ground.…”
Section: Discussionmentioning
confidence: 61%
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“…Surface clearing consists of the clearing of woody vegetation from slopes (tall shrubs and trees) to provide open spaces for skiers. During construction through machine-grading, the natural vegetation cover and the topsoil are removed, most boulders are re-arranged to form the ski run bed, and coarse materials from lower horizons are mixed with finer upper soil and replaced to form the top layer [15]. These operations are implemented in order to reduce the thickness of snow required for safe and pleasurable skiing and they are mainly carried out during the summer.…”
Section: Ski Run Constructionmentioning
confidence: 99%
“…Barni et al [15] reviewed the main techniques involved in land modelling and observed that in most cases, this involves bulldozing, with the removal of considerable soil to a depth of up to 1 m. Freppaz et al [4] remarked that such disturbance can be seen as an anthropogenic pedoturbation. As a consequence, deeper horizons or unweathered parent material are exposed to the atmosphere and consequently to weathering processes.…”
Section: Effects On Soil Physical and Chemical Propertiesmentioning
confidence: 99%