Search results for " sistemazioni idraulico-forestali"

showing 10 items of 760 documents

MONITORAGGIO DEI PROCESSI EROSIVI NELL’AREA SPERIMENTALE DI SPARACIA

2014

Processi erosivi campionatore campionamento della perdita di suolo ersoione rill erosione iterrillSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
researchProduct

SULLA APPLICABILITÀ DELLA USLE-MM PER LA STIMA DISTRIBUITA DELLA PRODUZIONE DI SEDIMENTI

2010

Nella memoria è presentata una nuova versione del modello distribuito SEDD (SEdiment Delivery Distributed model) che accoppia la RUSLE o la USLE-MM con un criterio spazialmente distribuito per la stima dei processi di trasferimento delle particelle erose all’interno di un bacino idrografico. In particolare, viene proposta l’applicazione a scala di bacino di un fattore di erosività, che tiene conto anche del processo di deflusso a scala di versante, e di un fattore di erodibilità del suolo determinati utilizzando le misure parcellari condotte nell’area sperimentale di Sparacia in Sicilia. Il modello è stato calibrato utilizzando le misure dei deflussi liquidi e solidi effettuate nei bacini s…

Produzione di sedimentiUSLE-MMSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliErosione idrica
researchProduct

Utilizzo di modelli bimodali per la descrizione della curva di ritenzione idrica del suolo

2013

L’approfondimento dell’influenza della struttura sulle caratteristiche di ritenzione idrica del suolo può contribuire alla risoluzione dei problemi legati all’eterogeneità del mezzo poroso ed anche alla quantificazione della qualità fisica del suolo. In particolare, nei suoli naturali strutturati, la presenza di un dominio dei pori strutturali (porosità inter-aggregati) e di un dominio dei pori matriciali (porosità intra-aggregati) può essere descritta mediante un’espressione della curva di ritenzione idrica di tipo bi-modale. L’indagine ha riguardato 40 suoli siciliani, per i quali è stato applicato alle misure sperimentali di ritenzione idrica il modello bimodale proposto da Dexter et al.…

Proprietà idrauliche del suolo Curva di ritenzione Modelli bimodaliSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliCurva di ritenzione idrica del suolo modelli bimodali
researchProduct

Closure to "Deducing a drain spacing formula by applying dimensional analysis and self-similarity theory" by Vito Ferro

2017

This paper is a closure of the discussions to the paper "Deducing a drain spacing formula by applying dimensional analysis and self-similarity theory"

Pure mathematicsSelf-similarityClosure (topology)CalculusSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliAgricultural and Biological Sciences (miscellaneous)drain dimensional analysis self-similarityWater Science and TechnologyCivil and Structural EngineeringMathematics
researchProduct

STIMA DELLA RADIAZIONE SOLARE GIORNALIERA IN SICILIA MEDIANTE I DATI DI TEMPERATURA MASSIMA E MINIMA

2009

RADIAZIONE SOLARESICILIASettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliHARGREAVES-SAMANI
researchProduct

A new strategy to assure compliance with soil loss tolerance at a regional scale

2023

The relevant erosive effects of extraordinary rainfall events due to climate change require establishing soil conservation strategies to prevent damages due to hydrogeological instability. The “tolerable” soil loss, i.e., the maximum soil loss compatible with sustainable soil use, represents a quantitative target to establish the effectiveness of actions to control soil erosion. In this paper, a new approach to defining the condition corresponding to a tolerable soil loss is proposed. At first, using the statistical analysis of the measured annual values of the rainfall erosivity factor, the cover and management factor CT, for which the maximum tolerable soil loss is equal to the annual soi…

Rainfall erosivity factorSoil loss toleranceCover and management factorSoil erosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliRegional analysisEarth-Surface ProcessesCATENA
researchProduct

Modeling Rainfall Erosivity by Measured Drop-Size Distributions

2015

AbstractThe study of the detachment of soil particles due to rainfall erosivity requires knowledge of the energetic characteristics of the precipitation. In this paper, following a review of both the drop-size distribution (DSD) proposed by one researcher and the corresponding relationship for evaluating the kinetic power of rainfall, the reliability of that researcher’s DSD using the size distributions of raindrops detected by an optical disdrometer installed at Palermo (Sicily) is experimentally tested. Finally, an experimental verification of both the relationship proposed by two separate research teams for evaluating the specific and unit rainfall kinetic energy is carried out.

Rainfall kinetic energyDrop sizeDisdrometerMeteorologyEnvironmental ChemistryEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliPrecipitationDrop size distribution Ulbrich‘s distribution Kinetic energy Rainfall erosivityKinetic energyGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineering
researchProduct

Modelling the frequency distribution of inter-arrival times from daily precipitation time-series in North-West Italy

2018

Abstract The discrete three-parameter Lerch distribution is used to analyse the frequency distribution of inter-arrival times derived from 26 daily precipitation time-series, collected by stations located throughout a 28,000 km2 area in North-West Italy (altitudes ranging from 113 m to 2,170 m a.s.l.). The precipitation regime of these Alpine regions is very different (latitude 44.5 to 46.5 N) from the typical Mediterranean precipitation regime of the island of Sicily (latitude 37 to 38 N), where the Lerch distribution has already been tested and whose results are compared. In order to verify the homogeneity of the precipitation time series, the Pettitt test was preliminarily performed. In …

Rainfall regimeSeries (stratigraphy)Water scarcity010504 meteorology & atmospheric sciencesInter-arrival timesbusiness.industry0208 environmental biotechnologyDistribution (economics)Dry spells02 engineering and technology01 natural sciences020801 environmental engineeringinter-arrival times Lerch probability distribution rainfall regime water scarcity wet spells and dry spellsDry spells; Inter-arrival times; Lerch probability distribution; Rainfall regime; Water scarcity; Wet spellsNorth westClimatologySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceWet spellsPrecipitationbusinessLerch probability distribution0105 earth and related environmental sciencesWater Science and TechnologyHydrology Research
researchProduct

Flow resistance of overland flow on a smooth bed under simulated rainfall

2020

In this paper a recently theoretically deduced flow resistance equation, based on a power-velocity profile, was tested using laboratory measurements by Yoon and Wenzel for an overland flow on a smooth bed under rainfall. These measurements of the Darcy-Weisbach friction factor, corresponding to a wide range of the flow Reynolds number (191–5700), were carried out for an overland flow under a simulated rainfall characterized by different intensity values ranging from 13 to 381 mm h−1. At first, the available measured values of flow velocity, water depth, cross sectional area, wetted perimeter and bed slope were used to calibrate the relationship between the velocity profile parameter Γ, the …

RainfallDimensional analysi010504 meteorology & atmospheric sciencesFlow (psychology)01 natural sciencessymbols.namesakeWetted perimeterOverland flowVelocity profileFroude numberRange (statistics)Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali0105 earth and related environmental sciencesEarth-Surface ProcessesTurbulenceReynolds number04 agricultural and veterinary sciencesMechanicsSelf-similarityFlow velocityFlow resistance040103 agronomy & agriculturesymbols0401 agriculture forestry and fisheriesGeologyIntensity (heat transfer)
researchProduct

La formula razionale rivisitata

2019

The Rational Formula (RF), also known as CIA formula, is probably the most applied equation in practical hydrology to compute the peak discharge, due to its simplicity and effective compromise between theory and data availability. The RF assumes the linearity of the hillslope response, neglects the time to ponding and the antecedent soil moisture condition (ASMC), concentrates the infiltration effect in the runoff coefficient (C) which estimation is highly controversial, since it is based on qualitative indications. This paper proposes an advanced rational formula that makes it possible to derive the peak discharge at the hillslope scale, where the above assumptions are relaxed and which de…

Rational formula kinematice wavw model Green-Ampt model runoff coefficientSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
researchProduct