Search results for " basin"

showing 10 items of 838 documents

Contribution of the largest events to suspended sediment transport across the USA

2010

This work analyses the contribution of the largest events to suspended sediment transport on the continental scale. The analysis is based on the United States Geological Survey (USGS) Suspended Sediment and Ancillary database. Data were obtained from 1314 catchments, comprising more than 2 500 000 daily events. The total number of days in the dataset amounts to 10 000 years. Catchments are of different sizes and belong to distinct climatic environments; they are distributed for the analysis according to USA hydrological divisions (HDs). The main objective of the research is to examine the effect of the n-largest event on the total suspended sediment load over recorded periods, and to discus…

HydrologyMediterranean climategeographygeography.geographical_feature_categoryDrainage basinSoil ScienceMagnitude (mathematics)SedimentDevelopmentCatchment hydrologyHydrology (agriculture)Geological surveyEnvironmental ChemistryEnvironmental scienceSediment transportGeneral Environmental ScienceLand Degradation & Development
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Flood events in Mediterranean ephemeral streams (ramblas) in Valencia region, Spain

2001

This article deals with flood events in Mediterranean ephemeral streams typical of the Valencia region. The combination of the basin physical characteristics steep slopes, sparse vegetation, thin soils and permeable rock. and intense, heavy and irregularly distributed rain, generates flash floods. Runoff generation is sudden, giving rise to flash floods with sharp, narrow hydrographs with short time lags. The high amount of runoff is, nevertheless, only a small fraction of the total rainfall, since the characteristics of the river basins are such that infiltration of large amounts of water occurs. Using daily hydrological data from the Rambla de la Viuda basin and 5-min data from both the B…

HydrologyMediterranean climategeographygeography.geographical_feature_categoryFlood mythHidrologiaDrainage basinStructural basinRunoff modelInfiltration (hydrology)Flash floodSurface runoffGeologyEarth-Surface ProcessesCATENA
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Empirical determination of the average annual runoff coefficient in the Mediterranean area

2014

Runoff estimation in ungauged basin is a challenge for the hydrological engineers and planners. For an y hydrological study on an ungauged basin, a methodology has to be appropriately selected for the determination of runoff at its outlet. Several meth ods have been used to estimate the basin runoff production. In this study the empirical Kennessey m ethod to determine average annual runoff coefficien t, RC, is tested on 61 Sicilian basins characterized b y different climate conditions, surface permeabilit y, mean slope and vegetation cover. A comparison between observed and calculated RC showed that a calibration of the Kennessey model could be necessary. The slight and not satisfying impr…

HydrologyMultidisciplinaryRunoff CoefficientRunoff curve numberStructural basinEmpirical determinationRunoff modelRunoff coefficientEmpirical ModelsStatisticsMediterranean areaEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliKennessey ModelSimple linear regressionSurface runoff
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Sediment origin and pedogenesis in the former mill pond basin of Turznice (north-central Poland) based on magnetic susceptibility measurements

2016

Abstract This paper aims to assess the usefulness of magnetic susceptibility measurements in pedological studies of mill pond sediments. The study area includes the former Turznice mill pond basin located in the south-eastern part of the Grudziądz Basin. Four soil profiles were selected within the transect located along the longitudinal axis of the basin. The following soil properties were determined in the collected samples: bulk density, particle size distribution, pH, content of carbonates, approximate content of organic matter (LOI), total organic carbon (TOC), total nitrogen (Nt), and the pseudo-total contents of metals (Fe, Mn, Cu, Zn, Pb, Ni, Cd). The obtained results were correlated…

HydrologyNorth centralGeography Planning and DevelopmentGeochemistrySediment04 agricultural and veterinary sciences010501 environmental sciencesStructural basin01 natural sciencesMagnetic susceptibilityGeophysicsPedogenesis040103 agronomy & agriculture0401 agriculture forestry and fisheriesMillGleysolsmill pond sedimentsheavy metalsGeology0105 earth and related environmental sciencesmagnetic susceptibilityBulletin of Geography: Physical Geography Series
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Hydrochemical evolution and environmental features of Salso River catchment, central Sicily (Italy)

2000

A hydrogeochemical study of the Salso River highlighted the chemical and isotopic space-time evolution along its flow path and the main contamination processes. Within the basin, three different hydrogeochemical facies have been individuated: (1) Ca-Mg-HCO3, (2) Ca-Mg-SO4 and (3) Na-Cl. The first facies reflects the chemical composition of the groundwaters hosted in the carbonate reliefs that belong to the Madonie Mountains. The second and the third facies are the result of the interaction processes between surface waters and the gypsum and salty clays, respectively. Two pollution sources have been also located in the basin downstream from the salt mine and downstream from a discharge area …

HydrologyPollutiongeographygeography.geographical_feature_categorymedia_common.quotation_subjectGeneral EngineeringDrainage basinStructural basinWater balanceFaciesEarth and Planetary Sciences (miscellaneous)General Earth and Planetary SciencesEnvironmental ChemistryEnvironmental scienceWater qualitySurface waterGroundwaterGeneral Environmental ScienceWater Science and Technologymedia_commonEnvironmental Geology
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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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A diachronic analysis of estuarine turbidity due to a flood following an extreme rainfall event

2011

During floods following rainfall events characterized by long return period, rivers bring to their mouths the higher concentration of sediments. This paper deals with a qualitative assessment of coastal water and turbidity load in estuarine waters as a consequence of an intense rainfall event occurred on the 16t h and 17 th September 2003 in the eastern part of Sicily. Although empirical relationships to estimate turbidity using remote sensing can be found in literature, however models parameters need to be calibrated through in situ measures acquired via intensive field campaigns. The algorithm used within this research was calibrated using field data acquired during three periods in 2008 …

HydrologyReturn periodgeographygeography.geographical_feature_categorySettore ICAR/03 - Ingegneria Sanitaria-AmbientaleFlood mythSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaDrainage basinEstuaryRemote Sensing Water qualityLand coverPlumeRiver mouthTurbiditySPIE Proceedings
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Testing a distributed approach for modelling sediment delivery

1998

Abstract Both the theoretical basis of a distributed approach to sediment delivery and its agreement with basin sediment yield measurements are tested. At first, by using morphological data of five Apulian and four Calabrian basins, the applicability of a theoretically-based relationship for evaluating the sediment delivery ratio of each morphological unit SDR h, into which a basin is divided, is verified. Using the morphological data of the nine investigated basins, the sediment delivery relationship, i.e. the relationship of the basin sediment delivery ratio SDR Wand SDR h, is tested. The analysis showed that the relationships, proposed by Ferro (1997), establishing the dependence of the …

HydrologySediment yieldTravel timeSedimentStructural basinTopographic mapScale (map)GeologyDrainage densityWater Science and Technology
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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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LONG TIME BEHAVIOR OF A SHALLOW WATER MODEL FOR A BASIN WITH VARYING BOTTOM TOPOGRAPHY

2002

We study the long time behavior of a shallow water model introduced by Levermore and Sammartino to describe the motion of a viscous incompressible fluid confined in a basin with topography. Here we prove the existence of a global attractor and give an estimate on its Hausdorff and fractal dimension.

HydrologyShallow water equations Global Attractor Fractal dimension dissipative systemWaves and shallow waterStructural basinSettore MAT/07 - Fisica MatematicaGeologyWaves and Stability in Continuous Media
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