Search results for " sistema."

showing 10 items of 1920 documents

Impact of climate, soil properties and grassland cover on soil water repellency

2021

Abstract Numerous soil water repellency (SWR) studies have investigated the possible causes of this temporal phenomenon, yet there remains a lack of knowledge on the order of importance of the main driving forces of SWR in the context of changing environmental conditions under grassland ecosystems. To study the separate and combined effects of soil texture, climate, and grassland cover type on inducing or altering SWR, four sites from different climatic and soil regions were selected: Ciavolo (CI, IT), Csolyospalos (CSP, HU), Pwllpeiran (PW, UK), Sekule (SE, SK). The investigated parameters were the extent (determined by repellency indices RI, RIc and RIm) and persistence (determined by wat…

geographygeography.geographical_feature_categoryHydrophobic soilSoil textureSorptivitySoil ScienceSoil properties Soil water repellency Grass Length of dry periods Climate factors04 agricultural and veterinary sciences010501 environmental sciences01 natural sciencesSink (geography)GrasslandAgronomyHydraulic conductivitySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil fertility0105 earth and related environmental sciences
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Discussion on 'Estimating depth-averaged velocities in rough channels'

2002

In this short communication the four estimate criteria of the depth-averaged local velocity proposed by Byrd et al. (Earth Surface Processes and Landforms, 2000, Vol. 25, pp. 167-173) are compared both with the three-point method of Bathurst and with the average velocity obtained by integrating the velocity profile (FPa2) suggested by Ferro and Pecoraro (Water Resources Research, 2000, vol. 36, pp. 2761-2770). The comparison was carried out using 84 velocity profiles measured by an acoustic Doppler velocimeter in a rectangular flume with a gravel bed. Copyright © 2002 John Wiley and Sons, Ltd.

geographygeography.geographical_feature_categoryLandformDepth averagedGeography Planning and DevelopmentEarth surfaceFlumeGravel bedRiemann averageVelocity profileEarth and Planetary Sciences (miscellaneous)Large-scale roughneSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeotechnical engineeringAcoustic Doppler velocimetryGeomorphologyGeologyEarth-Surface ProcessesEarth Surface Processes and Landforms
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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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A pedotransfer function for estimating the soil erodibility factor in Sicily

2009

The soil erodibility factor, K, of the Universal Soil Loss Equation (USLE) is a simple descriptor of the soil susceptibility to rill and interrill erosion. The original procedure for determining K needs a knowledge of soil particle size distribution (PSD), soil organic matter, OM, content, and soil structure and permeability characteristics. However, OM data are often missing and soil structure and permeability are not easily evaluated in regional analyses. The objective of this investigation was to develop a pedotransfer function (PTF) for estimating the K factor of the USLE in Sicily (south Italy) using only soil textural data. The nomograph soil erodibility factor and its associated firs…

geographygeography.geographical_feature_categorySoil textureMechanical EngineeringSoil organic matterlcsh:SBioengineeringSoil sciencelcsh:S1-972Industrial and Manufacturing EngineeringSoil gradationRilllcsh:AgricultureSoil erosion Soil erodibility Pedotransfer functionsUniversal Soil Loss EquationSoil structurePedotransfer functionErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalilcsh:Agriculture (General)Mathematics
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Experiments for testing soil texture effects on flow resistance in mobile bed rills

2018

Abstract In this paper a recently theoretically deduced rill flow resistance equation, based on a power-velocity profile, was tested experimentally on plots of varying slopes and soil texture in which mobile bed rills are incised. Measurements of flow velocity, water depth, cross section area, wetted perimeter and bed slope conducted in rill reaches incised on experimental plots, having different slope values (9, 14, 22, 24 and 26%) and soil texture (clay fraction ranging from 42 to 73%), and literature data were used to calibrate the flow resistance equation. In particular, the relationship between the velocity profile parameter Γ, the channel slope, the flow Froude number and texture frac…

geographygeography.geographical_feature_categorySoil textureRill hydraulic0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyPlot measurement020801 environmental engineeringRillWetted perimetersymbols.namesakeVelocity profileFlow resistanceFlow velocitySoil textureSoil waterSoil erosionFroude numbersymbolsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliTexture (crystalline)GeologyEarth-Surface ProcessesCATENA
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A full‐scale study of Darcy‐Weisbach friction factor for channels vegetated by riparian species

2021

In this article, an open channel flow resistance equation, deduced applying dimensional analysis and incomplete self-similarity condition for the flow velocity distribution, was tested using measurements carried out in a full-scale channel equipped with three types of riparian plants (Salix alba L., Salix caprea L. and Alnus glutinosa L.). In the experimental channel, having banks lined with boulders, the vegetation branches were anchored in a concrete bottom. For each species, the measurements were carried out with plants having different amounts of leaves, different plant density and plant area index. The relationship between the scale factor Γ of the velocity profile and the Froude numbe…

geographygeography.geographical_feature_categoryself-similaritySoil scienceScale factorDarcy–Weisbach equationopen channelOpen-channel flowsymbols.namesakevegetationdimensional analysiVegetation typevelocity profileFroude numbersymbolsmedicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalimedicine.symptomflow resistanceVegetation (pathology)ScalingWater Science and TechnologyMathematicsRiparian zoneHydrological Processes
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An automatic approach for rill network extraction to measure rill erosion by terrestrial and low‐cost unmanned aerial vehicle photogrammetry

2019

For an erosion event (October 2016) occurred at the Sparacia experimental area (Southern Italy), both terrestrial and low-altitude aerial surveys were carried out by consumer grade camera and quadcopter (low-cost unmanned aerial vehicle [UAV]) to measure rill erosion on two plots with steepness of 22% and 26%. Applying the structure from motion (SfM) technique, the three-dimensional digital terrain models (3D-DTMs) and the quasi three-dimensional models (2.5D-digital elevation model [DEM]) were obtained by the two surveys. Furthermore, 3D-DTM and DEM were built using the available aerial photographs (166) and adding 40 terrestrial photographs. For the first time, the convergence index was a…

geographygeography.geographical_feature_categorystructure from motionUAVMeasure (physics)terrestrial photogrammetryRill erosionplot measurementRillPhotogrammetrySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliExtraction (military)rill erosionGeologyWater Science and TechnologyRemote sensingHydrological Processes
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Comparing Physical Quality of Forest and Pasture Soils in a Sicilian Watershed

2011

Forest and pasture soils should have differing properties due, for example, to differing root characteristics or livestock trampling rates, but contradictory results are reported in the literature. The surface soil physical and hydraulic properties of five forest and pasture sites were determined in a Sicilian watershed. In general, forest soils had a significantly lower bulk density, b (by 17 to 35%), and a higher field saturated hydraulic conductivity, Kfs (by a factor of 3.4-11.5) than pasture soils. Differences between water retention characteristics of forest and pasture soils were low when high levels of organic matter, OM, content (> 7.1%) were detected for both land uses. The mean …

geographysoil physical qualityWatershedgeography.geographical_feature_categoryAgroforestrymedia_common.quotation_subjectSoil SciencePasturelanguage.human_languageSoil waterlanguageSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceQuality (business)SFH techniqueSicilianmedia_commonSoil Science Society of America Journal
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