Search results for " erosion"

showing 10 items of 356 documents

Testing flow resistance equation for rill flow

2018

At first, in this paper a flow resistance equation for rill flow, deduced applying dimensional analysis and self-similarity theory, is presented. The incomplete self-similarity hypothesis is used for establishing the flow velocity distribution whose integration gives the theoretical expression of the Darcy-Weisbach friction factor. Then the deduced theoretical resistance equation, which is calibrated by some measurements of flow velocity, water depth, cross section area, wetted perimeter and bed slope carried out in 106 reaches of some rills modelled on an experimental plot, is tested using the literature data by Abrahams et al. (1996), Strohmeier et al. (2014) and Peng et al. (2015) for ri…

flow resistance plot measurements rill flow soil erosion velocity profileSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Evaluating the Effectiveness of Forest Crop to Mitigate Erosion Using a Sediment Delivery Distributed Model

1998

In this paper sediment yield data, measured from 1978 to 1997 in a small experimental Calabrian basin reafforested with Eucalyptus trees (Eucalyptus occidentalis Engl.), and RUSLE (Revised Universal Soil Loss Equation) coupled with a sediment delivery distributed model are used to evaluate the antierosive effects of this forest cover. At first, the soil loss measureinents carried out in two experimental plots, located in the basin, are used to evaluate the crop and management factor C of RUSLE far Eucalyptus coppice. The reliability of the selected C factor value is verified by comparing, at an event scale, the measured and the calculated sediment yield values at the basin outlet. Then, a M…

forest antierosive effectivenessHydrologysoil erosionErosion controlSedimentForestrysediment deliverycrop factorUniversal Soil Loss EquationCrop factorErosionEnvironmental scienceSpatial variabilityWEPPCover crop
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Analisi multitemporale della linea di costa con tecniche di fotogrammetria area ed immagini QuickBird

2009

Il lavoro descrive l’attività svolta dal Dipartimento di Rappresentazione dell’Università di Palermo in cooperazione con la locale Agenzia Regionale per la Protezione dell’Ambiente (ARPA Sicilia) relativamente all’analisi multitemporale della linea di costa in Sicilia. L’analisi è stata condotta mediante la produzione e il confronto di ortofoto realizzate da foto aeree e da immagini satellitari ad alta risoluzione a partire dal 1955 fino al 2006. In particolare, vengono presentati i primi risultati conseguiti per una unità fisiografica costiera utilizzata come zona test per le verifiche delle precisioni conseguibili.

fotogrammetria ortofoto immagini satellitari erosione costiera monitoraggioSettore ICAR/06 - Topografia E Cartografia
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Assessing dye-tracer technique for rill flow velocity measurements

2018

Abstract Rill erosion is considered one of the most important processes affecting soil because of the large amount of soil loss. The rill network acts as sediment source and is able to transport both rill flow-detached particles and those delivered from the interrill areas. Small flow depth in a rill and steep slope values of its bed affect significantly flow hydraulics. When rill flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measured surface velocity of the leading edge of the tracer plume by a correction factor. The main uncertainty of the dye-tracing technique stands in the relationship between mean and surface flow velocity. In …

geographyLeading edgegeography.geographical_feature_categoryCorrection factorDye methodHydraulics0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyDarcy–Weisbach equation020801 environmental engineeringPlumelaw.inventionRillFlow velocityFlow resistanceFlow velocitylawTRACERRill flowSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeologyEarth-Surface Processes
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Modelling of piping collapses and gully headcut landforms: Evaluating topographic variables from different types of DEM

2021

Abstract The geomorphic studies are extremely dependent on the quality and spatial resolution of digital elevation model (DEM) data. The unique terrain characteristics of a particular landscape are derived from DEM, which are responsible for initiation and development of ephemeral gullies. As the topographic features of an area significantly influences on the erosive power of the water flow, it is an important task the extraction of terrain features from DEM to properly research gully erosion. Alongside, topography is highly correlated with other geo-environmental factors i.e. geology, climate, soil types, vegetation density and floristic composition, runoff generation, which ultimately inf…

geographyQE1-996.5geography.geographical_feature_category010504 meteorology & atmospheric sciencesAdvanced land observation satellite (ALOS)Water flowLandformCforestGully erosion susceptibility (GES)ElevationElastic netTerrainCubistGeologyVegetation010502 geochemistry & geophysics01 natural sciencesAdvanced Spaceborne Thermal Emission and Reflection RadiometerGeneral Earth and Planetary SciencesSurface runoffDigital elevation modelGeomorphologyDigital elevation model (DEM)Geology0105 earth and related environmental sciencesGeoscience Frontiers
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Comment on “Effects of different tillage practices on the hydraulic resistance of concentrated flow on the loess plateau in China” by J. Sun et al

2020

Abstract For concentrated flows, which are characterized by small water depth and steep sloping beds, hydraulic conditions different from those typical of streams and rivers occur. In this study a new theoretically deduced flow resistance equation was tested using the experimental data by Sun et al. for three different tilled surfaces (Manual Dibbling, MD, Manual Hoeing, MH, and Contour Drilling, CD). At first, the profile parameter-relationship, which is the relationship between the velocity profile parameter Γ, the channel slope and the flow Froude number, was calibrated using rill flow data by Di Stefano et al. Then, the applicability of this relationship was tested by the measurements o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFlow (psychology)Soil science04 agricultural and veterinary sciencesSurface finish01 natural sciencesTillageRillsymbols.namesakeFlow velocity040103 agronomy & agricultureFroude numbersymbolsCalibrationSurface roughness0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDimensional analysis Flow resistance Self-similarity Soil erosion Velocity profileGeology0105 earth and related environmental sciencesEarth-Surface Processes
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La reserva de semillas en una cuenca de "badlands" (Petrer, Alicante)

1992

In order to determine the influence of erosion in the absence of vegetation of badlands slopes, the seed content of the regolith and the seed removal by runoff in five storms were analyzed in an experimental catchment at Petrer (Alicante). Both, seed redistribution and seed loss were detected, but these seem to be insufficient to explain the lack of vegetation. It is hypothesized that besides the erosion process, factors such as pedoclimate, and chemical and physical properties of the regolith should be considered.

geographygeography.geographical_feature_categoryEcologySoil seed bankDrainage basinfood and beveragesForestrybadlandsVegetationalicante (spain)erosionRegolithlcsh:QH540-549.5ErosionSoil seed bank; badlands; erosion; Alicante (Spain)Environmental sciencelcsh:Ecologysoil seed bankSurface runoffAlicante (Spain)Ecology Evolution Behavior and SystematicsQH540-549.5
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Testing GIS-morphometric analysis of some Sicilian badlands

2014

Abstract Calanchi badlands are erosion landforms characterized by areas with scarce or absent vegetation, steep slopes, knife-edge divides and high erosion rates. They are originated by a combination of morphogenetic processes, partly similar to those shaping bigger fluvial landforms, and therefore can be considered as field “laboratories.” This paper presents the results of an investigation carried out in two badland sites located in Sicily, where the geometry of 25 calanchi has been characterized using Digital Elevation Models having a mesh size equal to 2 m. For each landform, a power length–volume relationship is established. This relationship demonstrates that length of calanchi channe…

geographygeography.geographical_feature_categoryLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaEphemeral keyDrainage basinFluvialVegetationCatchment hydrologySoil erosion Calanchi DEM GIS Hack's lawErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDigital elevation modelGeomorphologyGeologyEarth-Surface ProcessesCATENA
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A new empirical model for estimating calanchi Erosion in Sicily, Italy

2015

Abstract Calanchi (plural of calanco) are typical badland landforms of the Italian landscape. They consist of dense networks of V-shaped valleys, with a sparse or absent vegetation cover, which frequently develop on unconsolidated or poorly consolidated clayey deposits. In this paper, the dimensional analysis and the incomplete self-similarity theory were used to deduce a model relating the volume of sediments eroded from the calanchi area to a set of geometric attributes of their tributary areas. The morphometric characteristics of 209 calanchi basins were used to calibrate and validate the model. The predictive skill of the model was assessed by calculating the mean square error and the N…

geographygeography.geographical_feature_categoryLandformSettore GEO/04 - Geografia Fisica E GeomorfologiaSoil erosion Badlands Calanchi Dimensional analysis Self-similarity theory SicilyTributaryErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeomorphologyGeologyEarth-Surface ProcessesVegetation coverGeomorphology
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Variable scale effects on hillslope soil erosion during rainfall-runoff processes

2021

Abstract The variation of soil erosion across scales remains a controversial issue. A theoretical framework, coupling the normalized Green-Ampt equation for infiltration, 1D kinematic wave model for overland flow, and WEPP erosion modeling approaches for soil erosion, was used to explain and quantify the direct effect of scale on the soil erosion process. The results show that the relation between interrill erosion and slope length accords with a power-law decreasing trend, while the relation of rill erosion versus slope length shows a power-law increasing trend. Moreover, the power-law scaling of interrill erosion becomes more prominent with an increase of rainfall duration and intensity b…

geographygeography.geographical_feature_categorySoil scienceSoil typeInterrill and rill erosionWEPPScalingUSLE/RUSLEKinematic waveRillInfiltration (hydrology)UpscalingErosionEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliWEPPSurface runoffSediment transportEarth-Surface ProcessesSlope length
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