Search results for "soil"

showing 10 items of 3493 documents

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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Statistical distribution of soil loss and sediment yield at Sparacia experimental area, Sicily

2010

Abstract An analysis of the statistical distribution of event soil loss was carried out using the data collected in the period 1999–2008 at the microplots and plots of the Sparacia experimental area (Sicily, Italy). For a given microplot size, the analysis allowed to establish that the soil loss frequency distribution was skewed. Using the soil loss normalized by the event mean value, the analysis also showed that the frequency distributions corresponding to different microplot and plot sizes were overlapping, i.e. all distributions were extracted by the same statistical population. The developed analysis allowed to suggest that the soil loss of a given return period can be estimated using …

HydrologyReturn periodSoil erosion sediment yield measurements probability distributions extreme eventsStatistical populationErosionSedimentEnvironmental scienceProbability distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSpatial variabilityStructural basinFrequency distributionEarth-Surface Processes
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Analysis of rill step–pool morphology and its comparison with stream case

2021

In this paper, the morphology of step–pool features is analysed using rill measurements and literature data for streams. Close-range photogrammetry was used to carry out ground measurements on rills with step–pool units, shaped on a plot having slope equal to 14, 15, 22, 24 and 26%. Data were used to compare the relationships between H/L, in which H is the step height and L is the step length, and the mean gradient of the step–pool sequence, Sm, for streams or the slope of the step–pool unit, S, for rills. The relationship of H/L against Sm is widely used to test the occurrence of the maximum flow resistance condition in streams, which is associated with the range 1 ≤ (H/L)/Sm ≤ 2. Further …

HydrologyRillgeographyMorphology (linguistics)geography.geographical_feature_categoryGeography Planning and DevelopmentEarth and Planetary Sciences (miscellaneous)ErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSTREAMSGeologyEarth-Surface Processeserosion morphology rill soil erosion step–pool streams
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Moving Ahead from Assessments to Actions by Using Harmonized Risk Assessment Methodologies for Soil Degradation

2010

Almost all developed countries use risk assessment methodologies (RAMs) for the evaluation of risks related to soil degradation, viz. soil organic matter decline, erosion, landslides, salinization and/or compaction. However and for various reasons, seldom the use of such RAMs seldom results in actual measures to combat soil degradation in practice. In this study the current status of RAMs in EU-27 was evaluated and factors hampering the implementation of action plans were explored. To do so we used a so-called risk assessment chain, which describes the five successive steps of any risk assessment for soil threats viz., (1) notion of the threat, (2) data collection, (3) data processing, (4) …

HydrologyRisk perceptionData collectionSoil salinitybusiness.industrySoil retrogression and degradationSoil organic matterEnvironmental resource managementCredibilityLand degradationEnvironmental scienceRisk assessmentbusiness
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Defining minimum runoff length allows for discriminating biocrusts and rainfall events

2021

This study was started in the context of the research projects PECOS (REN2003-04570/GLO) and PREVEA (CGL2007-63258/BOS) , both funded by the Spanish National Plan for RD&I and by the European ERDF Funds (European Regional Development Fund) , and continued during the project SCIN (Soil Crust In-terNational, PRI-PIMBDV-2011-0874, European project of ERA-NET BIODIVERSA, the Spanish team being funded by the Spanish Ministry of Economy and Competitiveness) . The work was finally supported and culminated by the DINCOS project (CGL2016-78075-P, Spanish State Programme for Scientific Research) and by the European ERDF Funds (Euro-pean Regional Development Fund) . Consuelo Rubio's partici-pation was…

HydrologyRunoff connectivityTabernas DesertInfiltrationEnvironmental scienceBiological soil crustBiologia dels sòlsEcologíaSurface runoffSemiaridLength slope factorTaberans Desert
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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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Testing the long term applicability of USLE-M equation at a olive orchard microcatchment in Spain

2016

Abstract Universal Soil Loss Equation USLE-based erosion models have been used extensively to complement erosion measurements, to understand the interactions of the different geophysical features into erosion processes and to assess adequate alternative management practices and scenarios analyses. Despite its proved usefulness on different land-uses around the world, there is an urgent need to set up simple tools which do not require an advanced management expertise in terms of both choose of model parameters and calculation ability and which are accurate particularly at the event scale. In this paper the suitability of the Modified USLE (USLE-M) model at the event and the annual scale were…

HydrologyScale (ratio)USLE-M model RUSLE olive orchard crop factor soil losses sediment delivery0208 environmental biotechnologySediment02 engineering and technology020801 environmental engineeringTerm (time)Universal Soil Loss EquationCrop factorErosionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceNash–Sutcliffe model efficiency coefficientEarth-Surface ProcessesEvent (probability theory)CATENA
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Evaluation of the SEDD model for predicting sediment yield at the Sicilian experimental SPA2 basin

2007

In this paper a spatially distributed model of the hillslope sediment delivery processes, named the sediment delivery distributed (SEDD) model, is initially reviewed; the model takes into account the sediment delivery processes due to both the hillslope sediment transport and the effects of slope curvature. Then the rainfall and sediment yield events measured at the experimental SPA2 basin, in Sicily, are used both to calibrate the SEDD model and to verify the predictive capability of the distributed sediment delivery approach at event scale. For the SPA2 basin discretized into morphological units and stream tubes, the SEDD model is calibrated at event scale using the measurements carried o…

HydrologySediment yieldsoil erosionScale (ratio)Distributed element modelGeography Planning and DevelopmentSedimentPredictive capabilityStructural basinsediment yieldsediment deliveryexperimental basinEarth and Planetary Sciences (miscellaneous)CalibrationEnvironmental sciencedistributed modelSediment transportEarth-Surface ProcessesEarth Surface Processes and Landforms
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Hydrogeological hazards and weather events: Triggering and evolution of shallow landslides

2014

Abstract Landslides are the most intense and serious manifestations of the degradation of slopes and they are the main causes of geological hazard when they, directly or indirectly, involving towns and infrastructures. They are a global environment problem; there are several examples that have produced untold damages and loss of human lives in many parts of the world. In 1920 the landslides mobilization, as a result of a strong earthquake in China, in the province of Kansu, killed 200,000 people; in 1938 fast debris flow, triggered by heavy rainfalls in Japan, caused the death of 600 people; in 1963 in Italy the Vajont disaster caused the death of 1,899 people, as a result of a landslide lo…

HydrologySettore GEO/04 - Geografia Fisica E GeomorfologiaSoil ScienceLandslideHydrogeological instabilityHazardDebris flowCultural heritageGeo-environmental Hydrogeological instability Urban planningGeo-environmental hazardUrban planningUrban planninglcsh:TA1-2040Geologic hazardslcsh:Engineering (General). Civil engineering (General)Agronomy and Crop ScienceEnvironmental planningGlobal environmental analysisSpatial planningGeologyNature and Landscape ConservationWater Science and TechnologyInternational Soil and Water Conservation Research
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A field assessment of the Simplified Falling Head technique to measure the saturated soil hydraulic conductivity

2012

Abstract The Simplified Falling Head (SFH) technique to measure field saturated soil hydraulic conductivity, Kfs, has received little testing or comparison with other techniques. Different experiments were carried out to i) determine the effect of ring size on the measured conductivity; ii) compare the SFH and Pressure Infiltrometer (PI) techniques in a clay loam soil; and iii) evaluate the approach used in the SFH methodology to estimate the α* parameter. Sampling a relatively large number of sites allowed to detect statistically significant relationships between the Kfs values obtained with rings differing in diameter (0.15 and 0.30 m, respectively). The ring size effect was substantial (…

HydrologySimplified Falling Head techniqueField assessmentSoil ScienceSoil scienceField saturated soil hydraulic conductivityConductivityInfiltration (hydrology)Hydraulic conductivityLoamSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInfiltrometerMeasurement techniqueOrder of magnitudePondingMathematicsGeoderma
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