Search results for "infiltration"

showing 10 items of 291 documents

Impairment of TGF-β signaling in T cells increases susceptibility to experimental autoimmune hepatitis in mice

2002

In autoimmune hepatitis, strong TGF-beta1 expression is found in the inflamed liver. TGF-beta overexpression may be part of a regulatory immune response attempting to suppress autoreactive T cells. To test this hypothesis, we determined whether impairment of TGF-beta signaling in T cells leads to increased susceptibility to experimental autoimmune hepatitis (EAH). Transgenic mice of strain FVB/N were generated expressing a dominant-negative TGF-beta type II receptor in T cells under the control of the human CD2 promoter/locus control region. On induction of EAH, transgenic mice showed markedly increased portal and periportal leukocytic infiltrations with hepatocellular necroses compared wit…

Genetically modified mouseCellular immunityPhysiologyT-LymphocytesEnzyme-Linked Immunosorbent AssayMice TransgenicAutoimmune hepatitisBiologyMiceImmune systemTransforming Growth Factor betaPhysiology (medical)medicineAnimalsHomeostasisCells CulturedAutoimmune diseaseHepatitisB-LymphocytesHepatologyGastroenterologyT lymphocyteBlotting Northernmedicine.diseaseImmunohistochemistryHepatitis AutoimmunePhenotypeNeutrophil InfiltrationImmunologySignal transductionSignal TransductionAmerican Journal of Physiology-Gastrointestinal and Liver Physiology
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Soil moisture changes after land abandonment in the Central Spanish Pyrenees

2001

14 páginas, 3 tablas, 6 figuras.

Geography (General)geography.geographical_feature_categoryLand useGeography Planning and DevelopmentForestryEnvironmental Science (miscellaneous)Seasonalitymedicine.diseaseShrublandInfiltration (hydrology)GeographyEarth and Planetary Sciences (miscellaneous)medicineG1-922Plant coverSurface runoffWater content
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Beerkan Estimation of Soil Transfer parameters (BEST) across soils and scales

2019

Abstract Theories and models used in soil hydrological sciences rely on the knowledge of the spatially and temporally variable soil hydraulic properties, i.e. the water retention and hydraulic conductivity curves. Obtaining reliable experimental information on these curves for an area of interest is not easy and it still remains a challenge for soil scientists. In 2006, a simple and physically based methodology was proposed to completely characterize the soil using a single ring infiltration experiment in the field and determination of soil particle size distribution, initial and final soil water content and dry soil bulk density. This methodology, named BEST – Beerkan Estimation of Soil Tr…

Heterogeneous soil010504 meteorology & atmospheric sciencesSoil textureHydraulic conductivity0207 environmental engineeringDual-permeability soilSoil science02 engineering and technology01 natural sciencesSealed soilHydraulic conductivityDry soilSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali020701 environmental engineeringComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesWater Science and TechnologyBEST methodInfiltrationArea of interest15. Life on landBulk density6. Clean waterWater repellencyInfiltration (hydrology)Soil waterEnvironmental science[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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Hydrodynamic response of a loam soil after wetting with different methods

2023

Different points in a field can be wetted with different natural or artificial rainfall amounts and intensities. Therefore, a non-uniform soil wetting could occur during short-term monitoring of soil hydrodynamic parameters and its global effect on soil characterization is not easily predictable. For an initially dry loam soil, a sequence of three beerkan infiltration runs was performed at fixed sampling points in a period of two weeks. Immediately after the first beerkan run, the soil was perturbed by adding an additional water volume differing with the sampling point by the amount of water (0, 100 or 227 mm) and the application methodology (rainfall simulation, another beerkan run). As co…

Hydrodynamic propertieSoil disturbanceTemporal variabilityBeerkan infiltration runSoil water infiltration
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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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Role of rock fragment cover on runoff generation and sediment yield in tilled vineyards

2017

Summary The soil in conventional Mediterranean vineyards is an active and non-sustainable source of sediment and water. Lack of vegetation cover, small soil organic matter content and intense ploughing result in large rates of erosion in a millennia-old tillage system. There is a need for soil conservation strategies that enable sustainability of wine and grape production; therefore, it is essential to measure the rates and to investigate the processes and factors of soil erosion. This study evaluated factors that can reduce soil losses in traditional Mediterranean vineyards. The investigation was carried out with 96 rainfall simulation experiments at the pedon scale (0.24 m2) to measure so…

Hydrology010504 meteorology & atmospheric sciencesSoil organic matterSoil ScienceSoil science04 agricultural and veterinary sciencescomplex mixtures01 natural sciencesNo-till farmingInfiltration (hydrology)Soil retrogression and degradation040103 agronomy & agricultureErosion0401 agriculture forestry and fisheriesEnvironmental scienceWEPPSurface runoffSoil conservation0105 earth and related environmental sciencesEuropean Journal of Soil Science
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Modeling the probability distribution of peak discharge for infiltrating hillslopes

2017

Hillslope response plays a fundamental role in the prediction of peak discharge at the basin outlet. The peak discharge for the critical duration of rainfall and its probability distribution are needed for designing urban infrastructure facilities. This study derives the probability distribution, denoted as GABS model, by coupling three models: (1) the Green-Ampt model for computing infiltration, (2) the kinematic wave model for computing discharge hydrograph from the hillslope, and (3) the intensity-duration-frequency (IDF) model for computing design rainfall intensity. The Hortonian mechanism for runoff generation is employed for computing the surface runoff hydrograph. Since the antecede…

Hydrology0208 environmental biotechnologyHydrograph02 engineering and technology020801 environmental engineeringRunoff modelFlumeKinematic waveInfiltration (hydrology)Gamma distributionProbability distributionEnvironmental scienceSurface runoffWater Science and TechnologyWater Resources Research
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Effect of climate on surface flow along a climatological gradient in Israel: a field rainfall simulation approach

1998

Abstract A climatological gradient was selected in Israel to examine the effects of climate on surface flow and soil erosion. The gradient is composed of eight study areas located between the Dead Sea and the Galilee Mountains. Mean annual rainfall ranges from 100 mm year −1 in the driest site to 900 mm year −1 in the wettest site. Simulated rainfall experiments were performed in order to determine the main hydrological and erosional parameters. Data were recorded in 36 different plots after showers of 50 mm h −1 rain intensity and 45–60 min duration. In the arid sites ( −1 ) abundant runoff appeared on the soil surface very quickly, and the infiltration rates were very low. Erosion rates, …

HydrologyEcologySoil waterErosionEnvironmental scienceHydrographInfiltration (HVAC)Surface runoffAridSurface waterEcology Evolution Behavior and SystematicsPondingEarth-Surface ProcessesJournal of Arid Environments
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Ecohydrological adaptation of soils following land abandonment in a semi-arid environment

2010

Representative land use types were selected in southeast Spain to investigate the redistribution of soil water in relation to vegetation development and land abandonment.Simulated rainfall experiments were performed during 2 days on each of the four selected surfaces: ploughed, a 3-year fallow field, a 12-year abandoned field with shrubs and a semi-natural field with Stipa tenacissima tussocks. Each experiment consisted of five runs of artificial rain. Soil moisture dynamics were measured by time domain reflectometry (TDR), as well as runoff and ponding on the plot surface. Also the movement of the wetting front was measured after each run.On the ploughed field, ponding and local runoff wer…

HydrologyEcologyved/biologyved/biology.organism_classification_rank.speciesSoil scienceAquatic ScienceAridInfiltration (hydrology)Soil waterEnvironmental scienceSoil horizonSurface runoffWater contentEcology Evolution Behavior and SystematicsPondingEarth-Surface ProcessesStipa tenacissimaEcohydrology
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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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