Zobrazeno 1 - 10
of 36
pro vyhledávání: '"Véronique Auzet"'
Autor:
Thomas Grangeon, Rosalie Vandromme, Lai Ting Pak, Philippe Martin, Olivier Cerdan, Jean-Baptiste Richet, Olivier Evrard, Véronique Souchère, Anne-Véronique Auzet, Bruno Ludwig, Jean-François Ouvry
Publikováno v:
CATENA
CATENA, 2022, 214, pp.106257. ⟨10.1016/j.catena.2022.106257⟩
Catena
CATENA, 2022, 214, pp.106257. ⟨10.1016/j.catena.2022.106257⟩
Catena
International audience; The detrimental impacts of surface runoff and soil erosion, particularly in cultivated areas, call for the use of distributed runoff and soil erosion models with a view to supporting adapted catchment management strategies. Ho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::93d777a88364525ccab92e313805426f
https://hal.inrae.fr/hal-03645062/document
https://hal.inrae.fr/hal-03645062/document
Publikováno v:
Land Use Policy. 26:443-451
The inventory of muddy floods in France indicates that the occurrence of these events seriously increased in the North West and the East of the country. Muddy floods triggering can largely be explained by physical characteristics such as a hilly topo
Publikováno v:
Soil and Tillage Research
Soil and Tillage Research, Elsevier, 2009, 102 (1), pp.27-37. ⟨10.1016/j.still.2008.07.009⟩
Soil and Tillage Research, Elsevier, 2009, 102 (1), pp.27-37. ⟨10.1016/j.still.2008.07.009⟩
Conservation tillage (CT) constitutes one way to limit on- and off-site impacts of soil erosion. Literature analysis suggests that CT is more effective in reducing soil erosion than surface runoff. The effect on runoff mitigation may be rather limite
Publikováno v:
Earth Surface Processes and Landforms. 30:169-182
This paper explores a scale-adapted erosion mapping method which aims at a rapid assessment of field erosion and sediment transport pathways in catchments up to several square kilometres and compares the results with the output of a well-known erosio
Autor:
Louis-Marie Bresson, Rafael Angulo-Jaramillo, Thierry Bariac, Jean-Paul Gaudet, Anne-Véronique Auzet, Stéphanie Roulier
Publikováno v:
Soil Science. 167:201-210
In crusted soils, runoff and erosion at the surface are strongly controlled by soil infiltrability. An in situ hydrodynamic characterization of a cultivated crusted soil was conducted to define the factors that reduce infiltrability. Experiments were
Publikováno v:
Hydrological Processes
Hydrological Processes, Wiley, 1999, 13, pp.1621-1628
Hydrological Processes, Wiley, 1999, 13, pp.1621-1628
In the region of the basaltic plateau in Southern Brazil, problems of runoff and erosion on the deep ferrallitic soils are becoming increasingly recognized. Land use change from conventional tillage using disk plough to no-tillage on residues without
Autor:
Bruno Ambroise, Anne-Véronique Auzet
Publikováno v:
Earth Surface Processes and Landforms. 21:531-542
Soil creep, soil water tension and soil temperature were monitored at the Schildmatt experimental site over a 7 month period, in order to study the dynamics of creep movements measured with a specially designed strain gauge probe. The limited displac
Publikováno v:
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms, Wiley, 1995, 20, pp.759-767
Earth Surface Processes and Landforms, Wiley, 1995, 20, pp.759-767
Concentrated flow erosion is the dominant form of winter erosion in northern France. This study correlates the ephemeral rill and gully volumes measured in 20 cultivated catchments (4–95 ha) for three consecutive winters with the size of the potent
Publikováno v:
CATENA. 25:227-252
This study analyses the between-catchment variability of rill volumes produced by concentrated flow erosion during winter in the northern part of the Paris Basin. The working hypotheses were that (i) runoff concentrates along channels determined by t
Autor:
Anne-Véronique Auzet, Joël Humbert, Jean Mercier, Patrice Paul, Daniel Viville, Georges Najjar, Bruno Ambroise
Publikováno v:
Annales de Géographie. 104:64-87
The research catchments studied since 1975 by the C.E.R.E.G. in the Vosges mountains have permitted to precise the spatial and temporal variability of the main components of the water cycle and the controlling parameters in a temperate middle mountai