Search results for "erosion"

showing 10 items of 637 documents

IMPIEGO DEL RADIONUCLIDE 137CS PER LA STIMA DEI PROCESSI EROSIVI IN UN BACINO FORESTATO

2008

Il radionuclide cesio-137 (137Cs) è uno dei traccianti più utilizzati per stimare la perdita di suolo per erosione idrica. L'applicazione di questa tecnica alla scala di bacino richiede anzitutto l'acquisizione delle misure del radionuclide in punti distribuiti sulla superficie e l'utilizzo di modelli di conversione idonei a trasformare i valori di 137Cs in quantità di erosione netta o di deposito. La presente memoria si pone l'obiettivo di verificare l'affidabilità del modello di conversione esponenziale per stimare i processi erosivi in terreni interessati da coperture forestali. L'applicazione è stata condotta in un bacino sperimentale della Sila Greca per il quale sono disponibili alcun…

cesio 137erosione del suolo produzione di sedimenti bacini forestatiSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalierosione nettacalibrazione modello
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Six années de suivi du flux d'érosion éolienne sur un sol sableux cultivé au Sahel : Impacts des résidus de culture et de l'encroûtement

2013

In the Sahel, wind erosion occurs particularly in cultivated fields. This work was leaded at Banizoumbou in Niger where wind erosion fluxes have been measured for six years. The aims of this study was i) to monitor crop residues cover on traditional field and to quantify its influence on wind erosion ii) to characterize the impacts of soils crusting on erosion flux, iii) to characterize the impact of herbaceous strips on wind flux. Results showed that crop residues efficiently prevent cultivated fields from wind erosion during the dry season (January to April) and considerably reduce erosion fluxes at the beginning of the rainy season (May to July). Under a minimal crop residues cover rate …

champs cultivéscrop residuesVARIATION SAISONNIEREVENTSOL CULTIVEcampos cultivadoserosión eólicaerosion crustEROSION EOLIENNEérosion éolienneLUTTE ANTIEROSIVESahelcostras de erosiónwind erosion[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentcroûtes d’érosionVITESSEresiduos de cultivoRESIDU VEGETALrésidus de culture[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentPRATIQUE CULTURALEINDURATIONCROUTE D'ALTERATIONcultivated fieldsVARIATION PLURIANNUELLE
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Water-stable aggregates and organic matter pools in a calcareous vineyard soil under four soil-surface management systems

2006

. Vineyards in Champagne, France are generally situated on slopes where the soils are subject to erosion. Therefore it is important to find a soil-surface management practice that protects the soil against water erosion. We assessed the potential of mulches or grass covers to stabilize soil aggregates in a calcareous sandy loam from a vineyard in Champagne after 9 years under different management systems. Four different treatments were studied: (i) a bluegrass (Poa pratensis) surface cover between the vine rows (GC) with bare soil under the vines (R); two organic mulches of (ii) coniferous (CB) or (iii) poplar (PB) bark that covered the entire soil surface, and (iv) bare soil between the ro…

chemistry.chemical_classificationPoa pratensisbiologySoil Sciencebiology.organism_classificationVineyardPollutionAgronomychemistryLoamSoil waterBotanyErosionOrganic matterCalcareousMulchAgronomy and Crop ScienceSoil Use and Management
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Linking clay enrichment and sediment delivery processes

2002

Recent research has directed attention to the size distribution of eroded material because of its influence on deposition mechanics and in carrying capacity of pollutant materials. At first, in this paper the relationship between aggregate breakdown mechanism and erosion processes is briefly reviewed. Then the link between the clay enrichment ratio and the sediment delivery ratio at morphological unit scale is investigated. For 129 soil samples well distributed over the Sicilian Sparacia basin, the values for the experimental clay enrichment ratio calculated by the measured ultimate grain-size distributions are compared with the theoretical clay enrichment ratio values obtained by a procedu…

clay enrichment soil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Assessment of climate impacts on hydrology and geomorphology of semiarid headwater basins using a physically-based model.

2013

The response of watershed erosion rates to changes in climate is expected to be highly non-linear and thus demands for mechanistic approaches to improve our understanding of the underlying causes. In this study, the integrated geomorphic component tRIBS-Erosion of the physically-based, spatially distributed hydrological model, tRIBS, the TIN-based Real-time Integrated Basin Simulator, is used to analyze the sensitivity of small semi-arid headwater basins to projected climate conditions. Observed historic climate and downscaled realizations of general circulation models from CMIP3 inform the stochastic weather generator AWE-GEN (Advanced WEather GENerator), which is used to produce two clima…

climate change hydrology soil erosion phisically-based model
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Stochastic assessment of climate impacts on hydrology and geomorphology of semiarid headwater basins using a physically-based model

2015

Hydrologic and geomorphic responses of watersheds to changes in climate are difficult to assess due to projection uncertainties and nonlinearity of the processes that are involved. Yet such assessments are increasingly needed and call for mechanistic approaches within a probabilistic framework. This study employs an integrated hydrology-geomorphology model, the Triangulated Irregular Network-based Real-time Integrated Basin Simulator (tRIBS)-Erosion, to analyze runoff and erosion sensitivity of seven semiarid headwater basins to projected climate conditions. The Advanced Weather Generator is used to produce two climate ensembles representative of the historic and future climate conditions f…

climate impacts; erosion; geomorphology; modelingmodelingclimate impactgeomorphologyerosion
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Climatic changes and coastal erosion in Sicily

2009

climatic changes geomorphology coastal erosionSettore GEO/05 - Geologia Applicata
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Medium-term shoreline evolution of the mediterranean coast of Andalusia (SW Spain)

2015

Coastal environment is a dynamic system in which numerous natural processes are continuously actuating and interacting among them. As a result, geomorphologic, physical and biological characteristics of coastal environments are constantly changing. Such dynamic balance is nowadays seriously threatened by the strong and increasing anthropic pressure that favors erosion processes, and the associated loss of environmental, ecologic and economic aspects. Sandy beaches are the most vulnerable environments in coastal areas. The aim of this work was to reconstruct the historical evolution of the Mediterranean coastline of Andalusia, Spain. The investigated area is about 500 km in length and includ…

coast shoreline coastal erosion rate-of-change aerial photographsSettore GEO/05 - Geologia Applicata
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MEASURING FIELD RILL ERODIBILITY BY A SIMPLIFIED METHOD

2016

Many process-oriented erosion prediction models reproduce rill erosion as affected by site-specific parameters, as for example, rill erodibility, and thus, their practical application requires the measurement of these parameters or their estimate. The aim of this paper was establishing a method for indirectly measuring field rill erodibility. A simple mathematical approach based on a known soil detachment equation and accounting for the rill erosion dynamic process is applied. Field measurements carried out for seven natural rainfall events occurring at the plots of the Sparacia experimental station, southern Italy, are used for indirectly measuring the rill erodibility of the investigated …

concentrated flowsoil erosionfield measurementsSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalirill erodibilityrill erosion
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La vegetazione a protezione di processi di escavazione localizzata: risultati di uno studio sperimentale

2018

Diversi studi di letteratura mostrano come la vegetazione debba essere considerata un fattore chiave per analizzare i meccanismi di trasporto che si realizzano lungo un corso d’acqua naturale (Jarvela, 2002; Folkard, 2011). In particolare, la presenza di vegetazione sul fondo e/o sulle sponde del corso d’acqua contribuisce sia a stabilizzare i sedimenti che ad aumentare la resistenza al moto della corrente (Tsujimoto 1999; Nepf and Vivoni, 2000; Afzalimehr and Dey, 2009; Nepf, 2012), influenzando i processi di trasporto solido e i conseguenti fenomeni di erosione e di deposito lungo lo stesso corso d’acqua. In questo contesto, nel presente lavoro sono riportati alcuni risultati di uno studi…

corsi d'acqua erosione trasporto solido vegetazioneSettore ICAR/01 - Idraulica
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