Search results for "MAZ"

showing 10 items of 3205 documents

USING A TRANSIENT INFILTROMETRIC TECHNIQUE FOR INTENSIVELY SAMPLING FIELD-SATURATED HYDRAULIC CONDUCTIVITY OF A CLAY SOIL IN TWO RUNOFF PLOTS

2012

Point measurement of soil properties allows to explain and simulate plot scale hydrological processes. An intensive sampling was carried out at the surface of an unsaturated clay soil to measure, on two adjacent plots of 4×11 m2 and two different dates (May 2007 and February-March 2008), dry soil bulk density, rb, and antecedent soil water content, qi, at 88 points. Field-saturated soil hydraulic conductivity, Kfs, was also measured at 176 points by the transient Simplified Falling Head technique to determine the soil water permeability characteristics at the beginning of a possible rainfall event yielding measurable runoff. The rb values did not differ significantly between the two dates b…

Hydrological processeSoil hydraulic propertiePlot scaleSoil physical propertieSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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High resolution remote estimation of soil surface water content by a thermal inertia approach

2009

Summary The spatial distribution of soil surface water content in a bare soil was evaluated by a thermal inertia approach from high resolution visible/near infrared (VIS/NIR) and thermal infrared (TIR) airborne data. Given that the relationship between the thermal inertia and the soil water content strongly depends on the accurate estimation of the soil thermal conductivity, two different empirical models were applied to estimate it. Remotely estimated water contents were tested with time domain reflectometry (TDR) measurements collected on a 110 × 90 m 2 bare field in coincidence with airborne over-flights. The thermal conductivity model by Johansen (1975) produced more accurate estimates …

Hydrology (agriculture)Thermal conductivitySoil thermal propertiesThermal inertia Soil water content Surface temperature Soil thermal conductivitySoil waterEnvironmental scienceMineralogySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliConductivityReflectometryWater contentSurface waterWater Science and Technology
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SCS Curve Number and Green-Ampt Infiltration Models

2019

Soil Conservation Service curve number (SCS-CN) and Green-Ampt (GA) infiltration models are probably the most applied equations in practical hydrology to compute the amount of direct runoff from rainfall. Both models are very simple, require few parameters, and present drawbacks and advantages. The empirical CN model concentrates the infiltration effect in the curve number and in the so-called soil hydrological groups, which have been widely characterized for different soil types, land cover, and antecedent soil moisture conditions (ASMCs), although the latter was considered ambiguous, whereas soil hydrological characteristics, including ASMC, are taken into account for the simplified physi…

Hydrology010504 meteorology & atmospheric sciencesGreen-Ampt model0208 environmental biotechnologySCS-CN model02 engineering and technologyRunoff curve numberinfiltration01 natural sciences020801 environmental engineeringAMPTInfiltration (hydrology)medicineSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental ChemistryEnvironmental scienceSurface runoff0105 earth and related environmental sciencesGeneral Environmental ScienceWater Science and TechnologyCivil and Structural Engineeringmedicine.drugJournal of Hydrologic Engineering
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Probability Distribution of Peak Discharge at the Hillslope Scale Generated by Hortonian Runoff

2016

In this work, the probability distribution of peak discharge at the hillslope bottom is determined hypothesizing a prevalent Hortonian mechanism of runoff production for a given rainfall duration. As is well known, the probability distribution of peak discharge depends on the probability of both the rainfall event as well as that of the antecedent soil moisture conditions. In particular, the probability of the rainfall event is calculated according to the familiar rainfall duration-intensity-frequency approach, whereas the ecohydrological method from the literature is used here to define the probability of the antecedent soil moisture conditions. The latter depends on a set of parameters de…

Hydrology010504 meteorology & atmospheric sciencesScale (ratio)0208 environmental biotechnologySoil science02 engineering and technology01 natural sciencesAgricultural and Biological Sciences (miscellaneous)020801 environmental engineeringDischarge prorwhiiiiy distributionEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliHydrologic response Hillslope scale Discharge probability distribution Ecohydrological approachSurface runoffFeuhydrological approachHydrologie response: Hillslope scale0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural Engineering
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Comparing different application procedures of the water drop penetration time test to assess soil water repellency in a fire affected Sicilian area

2019

Abstract The Water Drop Penetration Time (WDPT) technique was applied in two subsequent years (2016 and 2017) to check surface soil water repellency (SWR) in a Sicilian mountain area affected by a wildfire on June 2016. A total of 93 sites were sampled and from 3 to 100 droplets were used to characterize a site. The detected SWR varied with the severity of the wildfire, being practically absent in the unburnt control area and slight to extreme in the burnt areas. The percentage of extremely repellent sites increased with wildfire severity. SWR vanished one year after the passage of the fire in sites where fire severity was moderate but it persisted in the case of a severe wildfire. In gener…

Hydrology010504 meteorology & atmospheric sciencesWater drop penetration time test04 agricultural and veterinary sciencesPenetration (firestop)Spatial distribution01 natural sciencesField samplingSoil water040103 agronomy & agricultureControl area0401 agriculture forestry and fisheriesEnvironmental scienceSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSmall-scale spatial variabilitySoil hydrophobicity0105 earth and related environmental sciencesEarth-Surface Processes
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Tropical Andean forest derives calcium and magnesium from Saharan dust

2008

[1] We quantified base metal deposition to Amazonian montane rain forest in Ecuador between May 1998 and April 2003 and assessed the response of the base metal budget of three forested microcatchments (8–13 ha). There was a strong interannual variation in deposition of Ca [4.4–29 kg ha−1 a−1], Mg [1.6–12], and K [9.8–30]). High deposition changed the Ca and Mg budgets of the catchments from loss to retention, suggesting that the additionally available Ca and Mg was used by the ecosystem. Increased base metal deposition was related to dust outbursts of the Sahara and an Amazonian precipitation pattern with trans-regional dry spells allowing for dust transport to the Andes. The increased base…

HydrologyAtmospheric ScienceGlobal and Planetary Changegeographygeography.geographical_feature_categoryAmazonianDrainage basinRainforestMineral dustAtmospheric sciencesEnvironmental ChemistryEnvironmental scienceEcosystemPrecipitationDeposition (chemistry)Base metalGeneral Environmental ScienceGlobal Biogeochemical Cycles
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MANUAL SAMPLING AND TANK SIZE EFFECTS ON THE CALIBRATION CURVE OF PLOT SEDIMENT STORAGE TANKS

2004

In many experimental soil erosion plots, runoff is collected and carried by a conveyance system to a sequence of storage tanks. If the soil loss is measured by collecting, after mixing, samples of the stored suspension, then a calibration curve between the actual mean concentration (C) and the measured concentration (Cm) in the storage tank occurs. The aim of this article was to evaluate experimentally the factors affecting the relationship between C and Cm. For a sandy loam soil, the replicated measurements of Cm (20 samples) for two values of the actual concentration (C = 5 and 25 g/L) showed that the variability of the measurements of Cm is low and confirmed the reliability of a calibrat…

HydrologyCalibration curveLoamStorage tankCalibrationSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceSampling (statistics)SedimentSurface runoffAgricultural and Biological Sciences (miscellaneous)Calibration Sediment concentration Soil erosion measurement Soil erosion plotWater levelTransactions of the ASAE
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Overland Flow Times of Concentration for Hillslopes of Complex Topography

2016

The time of concentration is an important parameter for predicting peak discharge at the basin outlet and for designing urban infrastructure facilities. In studying the hillslope response, employing hydraulic equations of flow, the shape of the hillslope geometry has often been assumed as rectangular and planar. However, natural hillslopes have complex topographies whose shapes are characterized by irregularly spaced contour lines. Recently, kinematic wave time of concentration has been derived for rectangular and curved parallel hillslopes. This paper extends this work to hillslopes of complex planform geometry, considering the degree of divergence or convergence of the hillslope. The exte…

HydrologyComplex topography0208 environmental biotechnologyUrban infrastructure02 engineering and technologyStructural basinAgricultural and Biological Sciences (miscellaneous)020801 environmental engineeringSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSurface runoffGeomorphologyTime of concentrationGeologyHillslope hydrology Overland flow Convergent and divergent hillslopes Concave and convex profileWater Science and TechnologyCivil and Structural Engineering
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Experimental Modeling of Submerged Pivot Weir

2020

An inclined rectangular overflow structure, also called a pivot weir, consists of a rectangular plate, angled downstream from the vertical, that can be used as an upstream water level control device. A pivot weir is submerged when the upstream water level is influenced by the downstream flow depth. In this paper, to investigate factors influencing submerged flow conditions, an extensive experimental program including 251 experimental trials was carried out using weir inclination angles of 39.6°, 53°, 85°, and 90° and weir heights ranging from 0.263 to 0.312 m. A formula to distinguish between free and submerged flow conditions was developed using the Π theorem of dimensional analysis and th…

HydrologyDownstream (manufacturing)WeirSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliUpstream (networking)Dimensional analysis Incomplete self-similarity Overflow gate Stage-discharge formula Submerged flow condition Threshold condition Wavy flow conditionAgricultural and Biological Sciences (miscellaneous)GeologyWater Science and TechnologyCivil and Structural EngineeringWater level
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Predicting event soil loss from bare plots at two Italian sites

2013

Abstract Including runoff in USLE-type empirical models is expected to improve plot soil loss prediction at the event temporal scale and literature yields encouraging signs of the possibility to simply estimate runoff at these spatial and temporal scales. The objective of this paper was to develop an estimating procedure of event soil loss from bare plots (length = 11–44 m, slope steepness = 14.9–16.0%) at two Italian sites, i.e. Masse, in Umbria, and Sparacia, in Sicily, having a similar sand content (5–7%) but different silt (33% at Sparacia, 59% at Masse) and clay (62% and 34%, respectively) contents. A test of alternative erosivity indices for the Masse station showed that the best perf…

HydrologyEmpirical modellingSoil scienceSiltSoil water erosion Soil loss prediction Empirical models USLE-MUSLE-MMSoil lossEmpirical modelSoil loss predictionEmpirical modelsErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliUSLE-MUSLE-MMEnvironmental scienceSoil water erosionTemporal scalesSurface runoffScale (map)Earth-Surface ProcessesEvent (probability theory)CATENA
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