Search results for "soil water"

showing 10 items of 840 documents

Combined use of eddy covariance and sap flow techniques for partition of ET fluxes and water stress assessment in an irrigated olive orchard

2013

Correct estimation of crop actual transpiration plays a key-role in precision irrigation scheduling, since crop growth and yield are associated to the water passing through the crop. Objective of the work was to assess how the combined use of micro-meteorological techniques (eddy covariance, EC) and physiological measurements (sap flow, SF) allows a better comprehension of the processes involving in the Soil–Plant–Atmosphere continuum. To this aim, an experimental dataset of actual evapotranspiration, plant transpiration, and soil water content measurements was collected in an olive orchard during the midseason phenological period of 2009 and 2010. It was demonstrated that the joint use of …

HydrologyPhenologyWater stressSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiafungiEddy covarianceOlivefood and beveragesSoil ScienceEddy covarianceEddy covariance; Flux partition; Olive; Sap flow; Water stressCrop coefficientFlux partitionSap flowEvapotranspirationSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceDNS root zoneOrchardAgronomy and Crop ScienceEarth-Surface ProcessesWater Science and TechnologyTranspirationAgricultural Water Management
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Anthropogenic processes in the evolution of a soil chronosequence on marly-limestone substrata in an Italian Mediterranean environment

2007

Due to anthropic pressure, many areas of the world are affected by a process of soil “entisolization” that leads to the formation of “anthropogenic soils”. In order to investigate Man's role in soil evolution, a survey was carried out in Southeastern Sicily (Italy), where, for years, there have been wide farming areas with anthropogenic soils. A chronosequence of anthropogenic soils in a vineyard area, cultivated for 22 years, was investigated. The first stage of the chronosequence was made by the original soils which, in the study area, had been undisturbed till the 1980's. These soils, classified as Entic Haploxerolls under the American Soil Taxonomy (ST) or Calcaric Kastanozem according …

HydrologyRegosolWRB classificationChronosequenceAmerican Soil TaxonomySoil ScienceKastanozemsAnthropogenic processeSoil chronosequenceVineyardAnthrosolSoil waterSoil horizonEntisolGeologyUSDA soil taxonomyGeoderma
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The influence of geomorphological position and vegetation cover on the erosional and hydrological processes on a Mediterranean hillslope

1998

Soil erosion and runoff rates are assumed to be highly dependent on slope position. However, little knowledge exists about the hydrogeomorphological processes at the pedon scale that support this idea. In order to assess the hydrological and erosional behaviour of soils at different slope positions, simulated rainfall experiments (55 mm was applied during one hour) were carried out on a south-facing slope with underlying limestone in south-east Spain. In the mean terms, the erosion rates (9 g m2 hr−1) and the runoff coefficients (12%) were very low at the scale of measurement (0·25 m2). The slope position does not affect erosion rates when the measurements are carried out under extreme dry …

HydrologyReturn periodMediterranean climateSoil waterErosionSoil horizonInfiltration (HVAC)Surface runoffGeologyVegetation and slope stabilityWater Science and TechnologyHydrological Processes
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Applying the bootstrap technique for studying soil redistribution by caesium-137 measurements at basin scale

2000

Abstract The use of the bootstrap technique to estimate the reference level of137 Cs in an uneroded site is tested. The analysis is developed using 137Cs measurements made in a small experimental Sicilian basin. In the reference area the 137Cs activity is normally distributed with a known sample mean value, m equal to 94.4 mBq cm−2. The influence of137 Cs reference site sampling was determined generating samples having a fixed size, N and six different values of the sample coefficient of variation, CV, by a Monte Carlo technique. Then, for each size N, the probability distribution of the mean μ of the sequences generated by Monte Carlo technique is defined. The soil redistribution is determ…

HydrologySample size determinationCoefficient of variationMonte Carlo methodSoil waterErosionProbability distributionSampling (statistics)Soil scienceSpatial distributionWater Science and TechnologyMathematics
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THE IMPACT OF FIRE ON REDISTRIBUTION OF SOIL ORGANIC MATTER ON A MEDITERRANEAN HILLSLOPE UNDER MAQUIA VEGETATION TYPE

2010

Soil organic matter (SOM) changes affect the CO2 atmospheric levels and is a key factor on soil fertility and soil erodibility. Fire affects ecosystems and the soil properties due to heating and post-fire soil erosion and degradation processes. In order to understand fire effects on soil organic carbon (SOC) balance research was undertaken on a fire-prone ecosystem: the Mediterranean maquia. The spatial distribution of SOC was measured in a Burnt site 6 months after a wildfire and in a Control site. Samples were collected at two different depths (0–3 and 3–10 cm) and SOC was determined. The results show that 41·8 per cent of the SOC stock was lost. This is due to the removal of the burnt ma…

HydrologySoil biodiversitySoil organic matterSoil SciencemediterraneanashSoil scienceSoil carbonDevelopmentsoil organic carbon (SOC)SpainSoil retrogression and degradationSoil waterVegetation typeEnvironmental ChemistryEnvironmental sciencemaquiaSoil fertilitySurface runofffireGeneral Environmental Science
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Comparison of aggregate stability indices for soil classification and assessment of soil management practices

1989

Summary In view of soil structure analysis and land-use and management history evaluation, several mechanical indices of soil structure were tested on 13 Italian soils. From the wet and dry sieving aggregate distributions, a pseudo-textural aggregation index (Ipta) and a mechanical aggregation index (Ima)) were determined and compared with other soil structure stability indices based on single-sieve analysis. The single-sieve indices S and WSI were good correlated with Ipta and Ima, showing the possibility of substituting the time-consuming aggregate-size distribution determinations. All the soil structure indices were correlated with selected semi-permanent soil characteristics. Soil struc…

HydrologySoil managementSoil structureAggregate (composite)Pedotransfer functionSoil waterGeneral EngineeringEnvironmental scienceRegression analysisSoil classificationSoil sciencecomplex mixturesStability (probability)Soil Technology
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The impact of natural and anthropogenic factors on groundwater quality in an active volcanic/geothermal system under semi-arid climatic conditions: T…

2017

Abstract A comprehensive hydrogeochemical study of the cold and thermal groundwaters of the presently quiescent volcanic system at Methana was undertaken that involved collecting 71 natural water samples. Methana is a peninsula in Peloponnesus, Greece whose arid climate and hydrological situation is similar to that of the nearby small islands of the Aegean Sea. Similarly, the chemical and isotopic compositions of its water are dominated by the mixing of seawater with meteoric water both through direct intrusion and meteoric recharge. However, the simple mixing trends at Methana are modified by water–rock interaction processes, enhanced by the dissolution of endogenous CO2, which lead to str…

HydrologySoil salinitySalinization0208 environmental biotechnologyGeochemistry02 engineering and technologyGroundwater recharge010501 environmental sciencesStable isotope01 natural sciencesArid020801 environmental engineeringSalinityGeochemistry and PetrologySoil waterTrace elementVolcanic aquiferMeteoric waterEconomic GeologySeawaterTrace metalHydrogeochemistryGeology0105 earth and related environmental sciencesJournal of Geochemical Exploration
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Application and evaluation of the SWAP model for simulating water and solute transport in a cracking clay soil

2005

In Sicily, the increasing scarcity of quality water is leading to irriga- from salinization (Crescimanno et al., 2004). tion with saline water in soils having a considerable susceptibility to In Sicily, the increasing scarcity of good quality water cracking. Irrigation systems involving high application rates are used coupled with intensive use of soil under semiarid to arid in these irrigated areas, and bypass flow during irrigation is thus climatic conditions, is leading to irrigation with saline prevalent. Adoption of management practices accounting for cracking water on soils having a high shrink-swell potential and is therefore necessary to prevent salinization and land degradation. su…

HydrologySoil salinityWater flowSoil ScienceSoil qualityLeaching modelVGM van Genuchten-MualemPedotransfer functionHydraulic conductivitySoil waterSWAP Soil-Water-Atmosphere-Plant environment;VGM van Genuchten-MualemEnvironmental scienceWater contentSWAP Soil-Water-Atmosphere-Plant environment
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Assessing soil moisture regimes with traditional and new methods

2002

Soil moisture regime classes are required by U.S. soil taxonomy and other classification systems. Soil moisture regimes are based on long-term daily data of soil water content, which are as a rule estimated by means of models. International Commitee on Soil Moisture and Temperature Regimes (ICOMMOTR) has proposed classifying pedoclimate on the basis of biweekly water potential. This study was conducted to validate the use of the Erosion-Productivity Impact Calculator (EPIC) model in assessing soil water content of experimental fields placed in different European pedoclimatic conditions, to compare the pedoclimatic classification obtained with EPIC with those produced by the traditional Bill…

HydrologySoil seriesPedotransfer functionUsticSoil waterSoil ScienceEnvironmental scienceSoil scienceDeserts and xeric shrublandsWater contentLeaching modelUSDA soil taxonomy
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Soil aggregate stability in three Mediterranean environments

1996

Abstract This paper considers the effect of vegetation on soil aggregate stability in three different Mediterranean landscapes in Southeast Spain. Soils on limestone, marls and clays, with two levels of vegetation cover at each north-facing slopes of the study areas, were investigated. Three aggregate stability tests (CND, TDI and UD) based on the drop impact and ultrasonic dispersion methods and the Emerson dispersion test were performed. The results of the experiments show the positive influence of vegetation on aggregate stability. However, vegetation is less important than lithology in influencing soil aggregate stability. Soil depth and moisture also affect aggregation, but the relatio…

HydrologySoil structureSoil waterGeneral EngineeringEnvironmental scienceSoil morphologyVegetationDispersion (geology)Soil typeWater contentVegetation and slope stabilitySoil Technology
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