Search results for "Structural basin"

showing 10 items of 292 documents

Estimation of Evapotranspiration by Hargreaves Formula and Remotely Sensed Data in Semi-arid Mediterranean Areas

1997

Abstract A methodology is proposed for estimating evapotranspiration by Hargreaves formula and image analysis of remotely sensed data. At first, for a large sicilian basin (Belice basin), theactualevapotranspiration values are estimated by the energy balance equation, spectral data of two Landsat TM images and ground agrometereological measurements. Then theseactualevapotranspiration estimates and thereferenceevapotranspiration values obtained by a slightly modified Hargreaves formula, which incorporates the outgoing short-wave radiation and an albedo coefficient equal to 0·23, are used for calculating suitable crop coefficients. Finally, the minimum area of each land-use map unit, obtained…

HydrologyCrop coefficientPixelComputer Science::Computer Vision and Pattern RecognitionEvapotranspirationEnergy balanceEnvironmental scienceAquatic ScienceStructural basinAlbedoAridMultispectral pattern recognitionRemote sensingJournal of Agricultural Engineering Research
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Curve Number: Empirical Evaluation and Comparison with Curve Number Handbook Tables in Sicily

2014

The curve number (CN) method is widely used for estimating direct runoff depth from rainstorms. The procedure is on the basis of the parameter CN, a lumped expression of basin absorption and runoff potential, and a second parameter, initial abstraction (IA), which represents the interception, infiltration, and surface depression during the early part of a storm. The evaluation of CN in Sicily at a basin scale from rainfall-runoff multiday events is done using rainfall-runoff observations during the period 1940–1997 (mean record length of 20 years) in 61 Sicilian watersheds using three different methods: (1) the national engineering handbook, section 4 hydrology (NEH4) method (NEH4M) (the me…

HydrologyFlood mythStormStructural basinRunoff curve numberRunoff modelInfiltration (hydrology)Environmental ChemistryRunoff Curve Number method Curve number handbook tables Curve numberSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInterceptionSurface runoffGeologyGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
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Impact of climate variability, drainage and land-cover changes on hemiboreal streamflow

2017

ABSTRACTThe aim of the study was to determine the effects of climate variability, agricultural land drainage and afforestation of agricultural land on river discharge. The study was conducted in the Vienziemīte stream basin (6 km2), where discharge was monitored on a daily basis during the time period of 1946–2010. In the stream basin, natural afforestation of agricultural land began in the 1950s, and in the mid-1970s artificial drainage systems were installed in all agricultural land (70% of the total basin area). Climate variability and artificial drainage were the main factors observed to be affecting stream discharge. The changes were most evident in annual and seasonal mean, minimum an…

HydrologyHemiborealDischarge0208 environmental biotechnology02 engineering and technologyLand coverStructural basin020801 environmental engineeringAgricultural landStreamflowEnvironmental scienceAfforestationDrainageWater Science and TechnologyHydrological Sciences Journal
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Sediment Delivery Distributed (SEDD) Model

2000

Because eroded sediments are produced from different sources throughout a basin, it is often advantageous to model sediment delivery processes at basin scale using a spatially distributed approach....

HydrologyHydrological modellingfungiSedimentStructural basinhumanitiesErosionEnvironmental ChemistryEnvironmental scienceSediment transportScale modelBasin scalegeographic locationsGeneral Environmental ScienceWater Science and TechnologyCivil and Structural EngineeringJournal of Hydrologic Engineering
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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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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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