Résultats de la recherche (16 résultats)
- > Physical geography (supprimer)
Affinez votre recherche
Par Collection Par Auteur- DE BOODT, M. (2)
- BENYAMINI Y. (1)
- BERNARD, R. (1)
- BLACK, T. A. (1)
- CLARK, R. (1)
- COCHRANE, P. (1)
- COX, N. J. (1)
- DRAMIS, F. (1)
- FRENCH, H.M. (1)
- HARTMANN, R. (1)
- HATFIELD, J. L. (1)
- KEVEI, Mrs. (1)
- KOREJSA, M. M. (1)
- KOSTER, E.A. (1)
- PAREEK, O. P. (1)
- PARIS, J. F. (1)
- RICHTER, J. C. (1)
- SCHWING J. F. (1)
- SINGH, H. P. (1)
- THOMAS, E. C. (1)
- Physical geography (16)
- Agropédologie ; Belgique ; Bilan hydrique ; Conductivité hydraulique ; Cycle de l'eau ; Eau du sol ; Ecoulement ; Evapotranspiration ; Expérimentation ; Flux gravitaire ; Géographie physique ; Loi de Darcy ; Parcelle expérimentale ; Pédologie ; Technique de recherche (1)
- Alsace ; Dynamique ; France ; Géographie physique ; Géomorphodynamique ; Versant ; Vosges, massif ; Végétation (1)
- Appennino ; Dépôt de pente ; Géographie physique ; Géomorphodynamique ; Italie ; Marche ; Paléo-environnement ; Paléolithique ; Quaternaire ; Solifluxion ; Stratigraphie ; Umbria ; Versant (1)
- Australie ; Bioclimatologie ; Ecologie alpine ; Ecologie quantitative ; Géographie physique ; Haute montagne ; Montagne ; Physiologie végétale ; Physionomie des plantes ; Snowy Mountains ; Température foliaire ; Végétation (1)
- Australie ; Erosion des sols ; Géographie physique ; Queensland ; Ravinement ; Rigole ; Ruissellement ; Simulateur de pluie ; Transport solide ; Versant (1)
- Autocorrélation spatiale ; Eau de gravité ; Eau du sol ; Géographie physique ; Processus aléatoire ; Processus autorégressif ; Processus spatial ; Sol ; Statistique spatiale ; Structure spatiale ; Température du sol ; Variation spatiale (1)
- Averse ; Durée ; Géographie physique ; Infiltration ; Intensité ; Parcelle expérimentale ; Précipitation ; Sable ; Sable argileux ; Technique de recherche (1)
- Belgique ; Eau du sol ; Géographie physique ; Polder ; Précipitation ; Pédologie ; Variabilité temporelle (1)
- Bilan hydrique ; Bilan hydrologique ; Conductivité hydraulique ; Eau du sol ; Géographie physique ; Potentiel hydraulique ; Rétention de l'eau ; Sol ; Sol nu (1)
- Colline ; County Durham ; England ; Géographie physique ; Géomorphodynamique ; Mesure de terrain ; Mouvement de masse ; Royaume-Uni ; Série chronologique ; Versant (1)
- Croûte ; Cycle de l'eau ; Diminution ; Eau ; Eau du sol ; Erosion ; Erosion pluviale ; Géographie physique ; Hydraulique ; Hydrologie paramétrique ; Infiltration ; Infiltration potentielle ; Intensité d'averse ; Modèle ; Précipitation ; Sol ; Sol nu (1)
- Cryoclastie ; Cycle gel-dégel ; Erosion nivale ; Eté ; Géographie physique ; Géomorphodynamique ; Montagne ; Météorisation ; Neige ; Printemps ; Processus morphogénique ; Zone froide (1)
- Cryoclastie ; Falkland ; Géographie physique ; Périglaciaire ; Sol figuré ; Zone froide (1)
- Cycle de l'eau ; Equation d'Idso ; Evaporation physique ; Evaporation potentielle ; Géographie physique ; Sol (1)
- Diamètre des grains ; Ecoulement ; Eolien ; Erosion pluviale ; Expérimentation ; Fluviatile ; Granulométrie ; Géographie physique ; Géomorphodynamique ; Sédimentologie ; Sélectivité anormale ; Sélectivité normale ; Technique de recherche ; Transport solide ; Vitesse critique de charriage (1)
- Flore ; Formation herbacée ; Gphy ; Géographie physique ; Karst ; Phytogéographie ; Vallée karstique ; Versant ; Végétation (1)
- An assessment of soil movement time series from Brandon, County Durham, U. K. (1)
- Development of miniature sorted patterned ground following soil erosion in East Falkland, South Atlantic (1)
- Influence of plant physiognomy on leaf temperature on clear midsummer days in the Snowy Mountains, south-eastern Australia (1)
- Les Versants d'un cirque glaciaire des hautes Vosges: le Forlet. Une diversité de formes et d'évolution postglaciaire en relation avec le milieu végétal (1)
- Ob ekzogennom processe, nazyvaemom nivaciej. (Sur le processus exogène appelé érosion nivale) (1)
- Resistance to rill erosion : observations on the efficiency of rill erosion on a tilled clay soil under simulated rain and run-on water in Rill erosion. Processes and significance. (1)
- Some data about the composition of flora in karst dolines (1)
- The significance of stratified slope-waste deposits in the Quaternary of Umbria - Marche Apennines, Central Italy in Periglacial processes and landforms. (1)
- Test of an equation for evaporation from bare soil
- Estimating profile water storage from surface zone soil moisture measurements under bare field conditions
- Rainwater infiltration into a bare loamy sand
- Unsaturated water movement in two bare polder soils of Belgium
- Water storage in a bare and cropped sany loam soil
- Soil movement has been measured daily for almost a year on a 12o slope. Results show a pattern of alternating movements, with amplitudes substantially larger on bare earth than on grass. Time series exhibit short-term dependence with lags of one
- or two days and there are several instances where expansions and contractions can be related to individual precipitation events. A non linear and lagged relationship can be identified between daily precipitation and daily soil movement on bare earth
- Spatial variability of surface temperature along two transects of a bare soil
- Rainfall infiltration into bare soils
- Common and uncommon selectivity in the process of fluid transportation: field observations and laboratory experiments on bare surfaces in Aridic soils and geomorphic processes.
- In bare dolines grass associations seemingly homogeneous in their habitat and rich in number of species act as indicators of the specific ecological conditions of the various slopes. For the differences of species on the SW and NE slopes water
- This paper reports a study of rill development under simulated rain and run-on water on a bare, tilled soil on the eastern Darling Downs, Queensland. The development of rills on this soil relatively resistant to rilling is compared with that on two
- and indicate that in cool oceanic climates the distribution of frost-sorted patterns is controlled by the presence of bare ground on suitable regolith rather than by altitude.
- The phases of slope-waste accumulation are characterised by intense frost-shattering on bare slopes and subsequent reworking by gravity, slope-waste and solifluction. The oldest generation is represented by a small quantity of strongly cemented
- of bare rock surface near the snow| surface under the snow and air near the surface. The intensity of nivation, the rate of rock's destruction is controlled by amplitude and frequency of the temperatures fluctuations within the active layer near the snow's
- Are made out, on the one hand, slopes with accumulations of blocks. They are bare and of several types. The vegetation cannot settle here and develops only locally, mainly starting from the top of the slope, making use of the pecularities
- Leaf temperatures in seven physiognomic groups of plant species and surface temperatures of bare soil were measured at four sites between 940 m and 2,040 m above sea level in the Snowy Mountains of South-Eastern Australia. Maximum leaf-air