Search results for "soil erosion"

showing 10 items of 149 documents

Soil Erosion and Deposition Rate Inside an Artificial Reservoir in Central Italy: Bathymetry versus RUSLE and Morphometry

2022

This study, using different direct and indirect methodologies, evaluated the sedimentation rate in an artificial reservoir in central Italy. This reservoir is regionally representative and was built in the 1960s for hydroelectric purposes; it has experienced a strong decrease in trap efficiency and a loss of over 70% of the stored water volume. Direct measurements of the lake bottom bathymetry, carried out in 2006 and 2015, and 3D reconstructions performed in a GIS environment, made it possible to calculate the volume of filling material and to verify an increasing trend in the sedimentation rate since 2006. The sample reservoir denudation rate was compared with that obtained using the Revi…

Global and Planetary ChangeEcologyartificial reservoirsSettore GEO/04 - Geografia Fisica E GeomorfologiaRUSLEsoil erosion rate; trap efficiency; RUSLE; sediment connectivity; sediment yield; artificial reservoirssoil erosion ratetrap efficiencysediment connectivitySettore GEO/05 - Geologia Applicatasediment yieldNature and Landscape ConservationLand
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EXPERIMENTAL STUDY OF RILL FLOW RESISTANCE AT PLOT SCALE

2021

I processi erosivi costituiscono un rilevante problema ambientale con impatto anche di tipo socioeconomico. Infatti, questi processi determinando l’asportazione degli strati superficiali di suolo, causano la riduzione della fertilità e produttività del suolo, e hanno un considerevole impatto sulla biodiversità. La perdita di suolo dovuta all’erosione idrica è un fenomeno naturale ed inevitabile, che può divenire intollerabile in condizioni particolari che spesso dipendono da fattori antropici (Di Stefano e Ferro, 2016). I processi di erosione idrica sono generalmente caratterizzati dall’erosione interrill o rill. Nelle aree interrill, caratterizzate da correnti overland, il processo erosivo…

HYDRAULICSRILLSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPLOTSOIL EROSIONFLOW RESISTANCE
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Using a physically-based model, tRIBS-Erosion, for investigating the effects of climate change in semi-arid headwater basins.

2013

Soil erosion due to rainfall detachment and flow entrainment of soil particles is a physical process responsible for a continuous evolution of landscapes. The rate and spatial distribution of this phenomenon depend on several factors such as climate, hydrologic regime, geomorphic characteristics, and vegetation of a basin. Many studies have demonstrated that climate-erosion linkage in particular influences basin sediment yield and landscape morphology. Although soil erosion rates are expected to change in response to climate, these changes can be highly non-linear and thus require mechanistic understanding of underlying causes. In this study, an integrated geomorphic component of the physic…

Hydrology Soil erosion Climate change
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Effects of climate, land cover and topography on soil erosion risk in a semiarid basin of the Andes

2016

Understanding soil erosion processes in the Ecuadorian Andes with a tropical wet-dry climate and a variable topography, is fundamental for research on agriculture sustainable, environmental management, as well as for a stable water supply for the local populations. This work proposes method to estimate soil erosion risk in the semiarid Catamayo basin with limited data. The results show that the rainfall distribution and the erosivity along with the rugged topography, followed by the land cover (C-factor), are the most important factors to estimate soil erosion risk. The soil erodibility is the most important factor in the dry season for agricultural areas and where the ground cover is spars…

Hydrology010504 meteorology & atmospheric sciencesAgroforestrySoil biodiversityClimatedrylandlandform04 agricultural and veterinary sciencesVegetationLand cover01 natural sciencesC-factorSoil retrogression and degradation040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceDryland salinityWEPPSurface runoffSoil conservationsoil erosion riskEcuadorian Andes0105 earth and related environmental sciencesEarth-Surface ProcessesCATENA
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MANUAL SAMPLING AND TANK SIZE EFFECTS ON THE CALIBRATION CURVE OF PLOT SEDIMENT STORAGE TANKS

2004

In many experimental soil erosion plots, runoff is collected and carried by a conveyance system to a sequence of storage tanks. If the soil loss is measured by collecting, after mixing, samples of the stored suspension, then a calibration curve between the actual mean concentration (C) and the measured concentration (Cm) in the storage tank occurs. The aim of this article was to evaluate experimentally the factors affecting the relationship between C and Cm. For a sandy loam soil, the replicated measurements of Cm (20 samples) for two values of the actual concentration (C = 5 and 25 g/L) showed that the variability of the measurements of Cm is low and confirmed the reliability of a calibrat…

HydrologyCalibration curveLoamStorage tankCalibrationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSampling (statistics)SedimentSurface runoffAgricultural and Biological Sciences (miscellaneous)Calibration Sediment concentration Soil erosion measurement Soil erosion plotWater levelTransactions of the ASAE
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Carbon input threshold for soil carbon budget optimization in eroding vineyards

2016

Abstract Previous studies have documented that, relative to conventional tillage (CT), alternative soil management (reduced tillage, mulching, or cover crops) decreases soil erosion and increases soil organic matter (SOM) in vineyards. These previous studies, however, failed to consider the loss of soil organic carbon (SOC) with erosion that could occur with the adoption of agro-environmental measures (AEM) in a semiarid environment. Accordingly, the aims of this study were to determine whether changes in SOC content under AEM management are always positive and to develop a conceptual model for estimating the “SOC threshold”. The SOC threshold was defined as that level of SOC in an AEM-mana…

HydrologyConventional tillageSoil organic matterAgro-environmental measureSoil ScienceSoil science04 agricultural and veterinary sciencesSoil carbon010501 environmental sciencesAgro-environmental measure; Degradation; Organic carbon; Soil erosion; Soil Science01 natural sciencesSettore AGR/02 - Agronomia E Coltivazioni ErbaceeMinimum tillageSoil managementTillageDegradation040103 agronomy & agricultureErosionSoil erosion0401 agriculture forestry and fisheriesEnvironmental scienceCover cropOrganic carbon0105 earth and related environmental sciences
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Comparing theoretically supported rainfall-runoff erosivity factors at the Sparacia (South Italy) experimental site

2018

Interpreting rainfall‐runoff erosivity by a process‐oriented scheme allows to conjugate the physical approach to soil loss estimate with the empirical one. Including the effect of runoff in the model permits to distinguish between detachment and transport in the soil erosion process. In this paper, at first, a general definition of the rainfall‐runoff erosivity factor REFe including the power of both event runoff coefficient QR and event rainfall erosivity index EI30 of the Universal Soil Loss Equation (USLE) is proposed. The REFe factor is applicable to all USLE‐based models (USLE, Modified USLE [USLE‐M] and Modified USLE‐M [USLE‐MM]) and it allows to distinguish between purely empirical m…

HydrologyRainfall runoffplot measurements rainfall‐runoff erosivity soil erosion USLE‐M0208 environmental biotechnology040103 agronomy & agricultureSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0401 agriculture forestry and fisheriesEnvironmental science04 agricultural and veterinary sciences02 engineering and technology020801 environmental engineeringWater Science and TechnologyHydrological Processes
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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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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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