Search results for " sistemazioni idraulico-forestali"

showing 10 items of 760 documents

Revisiting the Solid Flux Theory

2022

Several variations of the basic activated sludge process and of the related design procedures for final clarifiers have been developed, which are frequently based on the well-known solid flux theory (SFT). In this paper, by using the Lambert W function and a “virtual” solid flux corresponding to the Vesilind parameters’ ratio, the SFT is reformulated, and dimensionless groups are detected, which highly reduce the number of parameters that are involved in the final clarifiers’ design procedure. The derived dimensionless relationships and the corresponding plots have general validity since they can be applied to all the possible design/verification parameter combinatio…

final clarifierreduction hydrodynamic factorvalidationsolid flux theorydimensionless groupSettore CHIM/09 - Farmaceutico Tecnologico ApplicativoSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil Sciencesolid flux theory; final clarifier; dimensionless groups; reduction hydrodynamic factor; validationEarth-Surface ProcessesSoil Systems; Volume 6; Issue 4; Pages: 91
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Testing flow resistance equation for rill flow

2018

At first, in this paper a flow resistance equation for rill flow, deduced applying dimensional analysis and self-similarity theory, is presented. The incomplete self-similarity hypothesis is used for establishing the flow velocity distribution whose integration gives the theoretical expression of the Darcy-Weisbach friction factor. Then the deduced theoretical resistance equation, which is calibrated by some measurements of flow velocity, water depth, cross section area, wetted perimeter and bed slope carried out in 106 reaches of some rills modelled on an experimental plot, is tested using the literature data by Abrahams et al. (1996), Strohmeier et al. (2014) and Peng et al. (2015) for ri…

flow resistance plot measurements rill flow soil erosion velocity profileSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Effects of Boulder Arrangement on Flow Resistance Due to Macro-Scale Bed Roughness

2023

Flow resistance in gravel-bed channels is not only affected by the shape and size of the roughness elements, but also by their arrangement on the channel bed surface (position to flow streamlines, spacing between elements, and their protrusion from the channel bed). Many investigations proved that open channel flow resistance can be obtained by integrating the power velocity profile. For a macro-scale roughness condition, this study aims to investigate the effect of different boulder arrangements on flow resistance. First, for each arrangement, the equation relating Γ function of the power velocity profile, the Froude number, and the channel slope was calibrated using available measur…

flow velocity profileself-similarityflow resistance; gravel bed; boulder arrangement; dimensional analysis; flow velocity profile; self-similaritydimensional analysiGeography Planning and DevelopmentSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliboulder arrangementAquatic Scienceflow resistanceBiochemistrygravel bedWater Science and TechnologyWater; Volume 15; Issue 2; Pages: 349
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Experimental investigation of flow characteristics in vegetated channels

2006

flow velocity vegetation turbulenceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSettore ICAR/01 - Idraulica
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ESPERIMENTO DI SIMULAZIONE DELLA FORMAZIONE DEI RILL A SCALA DI PARCELLA

2016

Nella memoria sono riportati i risultati di un esperimento di simulazione della formazione del canale di un rill condotto in una parcella avente una dimensione 2x7 m2 ed una pendenza del 14% realizzata dal Dipartimento di Scienze Agrarie e Forestali dell’Università di Palermo. Una rete di solchi, costituita da due canali principali, è stata, dapprima incisa sul suolo manualmente e successivamente modellata utilizzando una corrente idrica limpida. Sui solchi modellati è stato effettuato, in corrispondenza di 11 sezioni trasversali della parcella, il rilievo delle caratteristiche geometriche e idrauliche utilizzando un profilometro. L’indagine ha inoltre previsto la realizzazione sia di un mo…

fotoricostruzione 3Derosione rilltecniche image-basedSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDEM.
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VERIFICA DI UNA TECNICA FOTOGRAFICA PER IL RILIEVO DELLA GEOMETRIA DI UN CANALE IN TERRA

2016

Nella memoria sono riportati i risultati delle verifiche di applicabilità di una tecnica image-based per il monitoraggio dei processi di erosione canalizzata. L’indagine, in particolare, ha avuto lo scopo di testare l’uso di modelli tridimensionali del terreno (DTM) ottenuti con l’impiego di un numero elevato di fotografie della stessa scena acquisite da differenti punti di vista (Tecnica “Structure-From Motion” SFM e “Multi-View-Stereo MVS). Il DTM tridimensionale (3D) è stato generato utilizzando il software open source Autodesk 123D Catch mentre per la creazione del Digital Elevation Model DEM (2.5D) è stato impiegato il software CloudCompare. Dei due canali in terra utilizzati nella spe…

fotoricostruzione 3Dtecniche image-basedDEMSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Primo contributo all'estensione di alcune serie climatiche siciliane mediante analisi di serie dendrocronologiche

2008

funzioni di rispostaSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestaliserie temporalidendroclimatologia
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Assessing dye-tracer technique for rill flow velocity measurements

2018

Abstract Rill erosion is considered one of the most important processes affecting soil because of the large amount of soil loss. The rill network acts as sediment source and is able to transport both rill flow-detached particles and those delivered from the interrill areas. Small flow depth in a rill and steep slope values of its bed affect significantly flow hydraulics. When rill flow velocity is measured using a dye-tracing method, the mean velocity is calculated by multiplying the measured surface velocity of the leading edge of the tracer plume by a correction factor. The main uncertainty of the dye-tracing technique stands in the relationship between mean and surface flow velocity. In …

geographyLeading edgegeography.geographical_feature_categoryCorrection factorDye methodHydraulics0208 environmental biotechnologyFlow (psychology)Soil science02 engineering and technologyDarcy–Weisbach equation020801 environmental engineeringPlumelaw.inventionRillFlow velocityFlow resistanceFlow velocitylawTRACERRill flowSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeologyEarth-Surface Processes
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Comment on “Effects of different tillage practices on the hydraulic resistance of concentrated flow on the loess plateau in China” by J. Sun et al

2020

Abstract For concentrated flows, which are characterized by small water depth and steep sloping beds, hydraulic conditions different from those typical of streams and rivers occur. In this study a new theoretically deduced flow resistance equation was tested using the experimental data by Sun et al. for three different tilled surfaces (Manual Dibbling, MD, Manual Hoeing, MH, and Contour Drilling, CD). At first, the profile parameter-relationship, which is the relationship between the velocity profile parameter Γ, the channel slope and the flow Froude number, was calibrated using rill flow data by Di Stefano et al. Then, the applicability of this relationship was tested by the measurements o…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesFlow (psychology)Soil science04 agricultural and veterinary sciencesSurface finish01 natural sciencesTillageRillsymbols.namesakeFlow velocity040103 agronomy & agricultureFroude numbersymbolsCalibrationSurface roughness0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliDimensional analysis Flow resistance Self-similarity Soil erosion Velocity profileGeology0105 earth and related environmental sciencesEarth-Surface Processes
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Impact of climate, soil properties and grassland cover on soil water repellency

2021

Abstract Numerous soil water repellency (SWR) studies have investigated the possible causes of this temporal phenomenon, yet there remains a lack of knowledge on the order of importance of the main driving forces of SWR in the context of changing environmental conditions under grassland ecosystems. To study the separate and combined effects of soil texture, climate, and grassland cover type on inducing or altering SWR, four sites from different climatic and soil regions were selected: Ciavolo (CI, IT), Csolyospalos (CSP, HU), Pwllpeiran (PW, UK), Sekule (SE, SK). The investigated parameters were the extent (determined by repellency indices RI, RIc and RIm) and persistence (determined by wat…

geographygeography.geographical_feature_categoryHydrophobic soilSoil textureSorptivitySoil ScienceSoil properties Soil water repellency Grass Length of dry periods Climate factors04 agricultural and veterinary sciences010501 environmental sciences01 natural sciencesSink (geography)GrasslandAgronomyHydraulic conductivitySoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil fertility0105 earth and related environmental sciences
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