Search results for " erosion"

showing 10 items of 356 documents

Statistical distribution of soil loss and sediment yield at Sparacia experimental area, Sicily

2010

Abstract An analysis of the statistical distribution of event soil loss was carried out using the data collected in the period 1999–2008 at the microplots and plots of the Sparacia experimental area (Sicily, Italy). For a given microplot size, the analysis allowed to establish that the soil loss frequency distribution was skewed. Using the soil loss normalized by the event mean value, the analysis also showed that the frequency distributions corresponding to different microplot and plot sizes were overlapping, i.e. all distributions were extracted by the same statistical population. The developed analysis allowed to suggest that the soil loss of a given return period can be estimated using …

HydrologyReturn periodSoil erosion sediment yield measurements probability distributions extreme eventsStatistical populationErosionSedimentEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSpatial variabilityStructural basinFrequency distributionEarth-Surface Processes
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Analysis of rill step–pool morphology and its comparison with stream case

2021

In this paper, the morphology of step–pool features is analysed using rill measurements and literature data for streams. Close-range photogrammetry was used to carry out ground measurements on rills with step–pool units, shaped on a plot having slope equal to 14, 15, 22, 24 and 26%. Data were used to compare the relationships between H/L, in which H is the step height and L is the step length, and the mean gradient of the step–pool sequence, Sm, for streams or the slope of the step–pool unit, S, for rills. The relationship of H/L against Sm is widely used to test the occurrence of the maximum flow resistance condition in streams, which is associated with the range 1 ≤ (H/L)/Sm ≤ 2. Further …

HydrologyRillgeographyMorphology (linguistics)geography.geographical_feature_categoryGeography Planning and DevelopmentEarth and Planetary Sciences (miscellaneous)ErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSTREAMSGeologyEarth-Surface Processeserosion morphology rill soil erosion step–pool streams
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Scour around a Permeable Groin Combined with a Triangular Vane in River Bends

2019

River restoration refers to the environmental and ecological aspect of river engineering and aims to improve the natural habitat of a river system using eco-friendly methods. This paper introduces a new river restoration technique for bank protection and restoration of meander bends by combining a permeable groin with a triangular vane. Nine different combinations of permeable groins with triangular vane including three different effective lengths and three angles of vane were investigated in a 180 degrees mild laboratory flume bend in clear water conditions. Based on experimental tests, scour geometrical patterns were analyzed, classified, and compared with each other. This analysis showed…

HydrologyRiver engineeringBANK EROSION010504 meteorology & atmospheric sciences0207 environmental engineering02 engineering and technologySEDIMENT01 natural sciencesAgricultural and Biological Sciences (miscellaneous)HabitatSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDOWNSTREAM020701 environmental engineeringFLOW PATTERNSGeology0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringRESTORATION
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Effect of Vegetation on Fluvial Erosion Processes: Experimental Analysis in a Laboratory Flume

2013

Abstract The plane evolution of a meander wave is determined by the erosion processes at the banks. Particularly, the outer- bank is considerably vulnerable to the erosion processes. Indirect techniques, which act upon the reduction of the effect of the cross-circulation motion, have been recently proposed to limit the outer-bank erosion. This paper shows preliminary results on the role played by vegetation on cross-circulation motion. The analysis is conducted on the basis of experimental data collected in a large amplitude meandering channel constructed at the hydraulic laboratory of DICAM. Maps describing the cross-stream flow, both over the no-vegetated bed and over the vegetated bed, a…

HydrologyRivers meanders erosion secondary circulation vegetationFlow (psychology)FluvialVegetationerosionSettore ICAR/01 - IdraulicaFlumeRiversFlow velocityvegetationErosionMeanderGeneral Earth and Planetary SciencesmeandersGeomorphologysecondary circulationGeologyBank erosionGeneral Environmental ScienceProcedia Environmental Sciences
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Evaluation of the SEDD model for predicting sediment yield at the Sicilian experimental SPA2 basin

2007

In this paper a spatially distributed model of the hillslope sediment delivery processes, named the sediment delivery distributed (SEDD) model, is initially reviewed; the model takes into account the sediment delivery processes due to both the hillslope sediment transport and the effects of slope curvature. Then the rainfall and sediment yield events measured at the experimental SPA2 basin, in Sicily, are used both to calibrate the SEDD model and to verify the predictive capability of the distributed sediment delivery approach at event scale. For the SPA2 basin discretized into morphological units and stream tubes, the SEDD model is calibrated at event scale using the measurements carried o…

HydrologySediment yieldsoil erosionScale (ratio)Distributed element modelGeography Planning and DevelopmentSedimentPredictive capabilityStructural basinsediment yieldsediment deliveryexperimental basinEarth and Planetary Sciences (miscellaneous)CalibrationEnvironmental sciencedistributed modelSediment transportEarth-Surface ProcessesEarth Surface Processes and Landforms
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Effect of plot size on measured soil loss for two Italian experimental sites

2011

The objective of this investigation was to determine empirically the plot width and length effects on runoff volume, Ve, soil loss, Ae, and sediment concentration, Ce, by using data collected, at the temporal scale of the erosive event, on bare plots differing in width (2 to 8 m) and length (11 to 22 m) for two Italian stations (Masse, Umbria; Sparacia, Sicily). Mean results differed by a maximum factor of 1.6 for Ve, 1.8 for Ae and 1.2 for Ce when plots differing in width were compared and by a maximum factor of 1.4 for Ve, 1.2 for Ae and 1.3 for Ce when comparison between plot lengths was conducted. Differences between two plot widths or two plot lengths were not statistically significant…

HydrologySoil loSampling schemesoil erosionSoil ScienceSoil scienceLong term resultsSediment concentrationRunoff volumeerosion measurementSoil lossControl and Systems Engineeringplot lengthrainfall erosivitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalisoil erosion rainfall erosivity soil erodibilityplot widthPlot (narrative)Agronomy and Crop Sciencesoil erodibilityFood ScienceMathematicsBiosystems Engineering
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Analysis of soil loss data from plots of differing length for the Sparacia experimental area, Sicily, Italy

2010

Widely used models of the soil erosion process, such as the empirical universal soil loss equation (USLE) and revised USLE (RUSLE), suggest that soil loss, i.e. the mass of soil lost by water erosion per unit surface area, increases with slope length, λ, although contrasting experimental results may be found in the literature. Experiments were carried out at the Sparacia site, Sicily, to establish the influence of plot length on soil loss. This was tested using data characterised by a high number of replicated, bare plots of different lengths (0.25, 0.4, 1, 2, 5, 11, 22, 33 and 44 m), simultaneously operating in the 1999–2008 period. Event soil losses did not vary significantly with λ or ev…

HydrologySoil loSoil ScienceSedimentRill erosionSoil qualitySoil lossUniversal Soil Loss EquationControl and Systems EngineeringTemperate climateErosionbare plotsEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSurface runoffAgronomy and Crop ScienceFood Science
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Establishing a soil loss threshold for limiting rilling

2015

In this paper a frequency analysis of event soil loss measurements collected in the period 1999–2012 at the microplots and plots of the Sparacia Experimental Area in Sicily, southern Italy, was developed. The analysis was carried out using the annual maximum soil loss measurements normalized by the mean soil loss measured at a given temporal and spatial scale. The empirical frequency distribution of the normalized variable was well fitted by two Gumbel’s theoretical probability distributions discriminated by a value of the normalized variable equal to 2. This last value discriminates between the relatively low and frequent values of the normalized variable and the high and rare ones. The an…

HydrologySoil loss toleranceFrequency analysisScale (ratio)Soil erosion measurements Probability distributions Extreme events Soil loss tolerance RillingSoil scienceLimitinglaw.inventionSoil lossGumbel distributionlawSpatial ecologyEnvironmental ChemistryEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
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Response to ‘comment on “predicting event soil loss from bare plots at two Italian sites”’

2014

In this paper, a response to the comment by Dr. Kinnell on “Predicting event soil loss from bare plots at two Italian sites”’ (Bagarello et al., Catena 109, 96–102, 2013) is provided.

HydrologySoil losssoil erosionEvent (relativity)Environmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEarth-Surface Processes
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Concise review of interrill erosion studies in SE Spain (Alicante and Murcia): erosion rates and progress of knowledge from the 1980s

2005

From the 1980s onward studies on interrill soil erosion were intensified in SE Spain. The main achievements of the research carried out in the field areas of Alicante and Murcia concern: first, (1) the estimation of erosion rates directly in the field under a wide range of methodologies, different scales and different environmental conditions; (2) estimations based on existing models, such as the USLE, carried out for different subcatchments of the Segura and Júcar catchments; and (3) other parametric and physical event-based models have also been calibrated and validated. Second, the progress of the knowledge in understanding erosion mechanisms. New and reviewed concepts regarding mainly h…

HydrologySoutheast SpainSoil transportbusiness.industryEnvironmental resource managementSoil ScienceCommissionInterrill erosionDevelopmentErosion plotsRunoff generationSoil-erosion ratesERMESPolitical scienceErosion thresholdsErosionEnvironmental Chemistrymedia_common.cataloged_instanceChristian ministryEuropean unionbusinessSoil detachmentGeneral Environmental Sciencemedia_common
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