Search results for "LSL"

showing 10 items of 32 documents

A review of runoff generation and soil erosion across scales in semiarid south-eastern Spain

2011

Climate, lithology, soil and especially, intense land use/cover changes, make SE Spain very vulnerable to runoff generation and water erosion leading to loss of nutrients and organic matter and to infrequent but devastating floods, reservoir siltation and mass failures. This susceptibility has led to heavy economic investment and research efforts since the 1980s, making this region a worldwide reference for understanding the hydrology and geomorphology of semiarid ecosystems. Runoff and soil erosion have been intensively studied throughout the last decades in various natural ecosystems as well as in abandoned farmlands. Research has considered a wide range of methods and spatial and tempora…

HillslopeHydrologyConnectivityEcologyLand useRunoffSoil degradationCatchmentModellingSiltationScaleErosionSoil retrogression and degradationErosionEnvironmental scienceWEPPTemporal scalesSurface runoffSediment transportEcology Evolution Behavior and SystematicsEarth-Surface ProcessesJournal of Arid Environments
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Monitoring soil volume wetness in heterogeneous soils by electrical resistivity. A field-based pedotransfer function.: A field-based pedotransfer fun…

2014

11 pages; International audience; Modern irrigation techniques require accurate, rapid, cost-effective, spatial measurement of soil moisture. Electrical Resistivity Tomography (ERT) meets most of these requirements, but needs to be calibrated for each use because it is very sensitive to differences in soil characteristics. In this study, a pedotransfer function approach is used to remove the need for site-specific calibration, allowing ERT to be used directly to measure soil moisture. The study site was a hillslope vineyard, where eight calcaric-cambisol soil profiles were identified. From 2012 to 2013, 23 000 soil volume wetness measurements were acquired by Time Domain Reflectometry, and …

HillslopeSoil testSoil texture[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph][SDE.MCG]Environmental Sciences/Global Changes0207 environmental engineering[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil studySoil science[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]02 engineering and technologyElectrical Resistivity Tomography (ERT)[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil studyPedotransfer function[ SDU.STU.GP ] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Pedotransfer function[ PHYS.PHYS.PHYS-GEO-PH ] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Electrical resistivity and conductivityCation-exchange capacityElectrical resistivity tomography020701 environmental engineeringWater contentWater Science and TechnologyTime Domain Reflectometry (TDR)2. Zero hunger04 agricultural and veterinary sciences15. Life on land6. Clean water[ SDE.MCG ] Environmental Sciences/Global ChangesSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceGrapevineSoil moisture
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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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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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Quick and Slow Components of the Hydrologic Response at the Hillslope Scale

2016

It is widely recognized that the Hortonian mechanism of runoff generation occurs in arid and semi-arid regions, generally characterized by high rainfall intensity on soils exhibiting low infiltrabilities. Differently, in steeply sloping forested watersheds in humid climates, by infiltrating through a highly permeable upper soil horizon, water moves beneath the soil surface determining a slow response. However, in most real cases, for example when in arid regions mountain forested areas take place, both (quick and slow) runoff generation processes coexist and together contribute to the hydrologic hillslope response. In this paper, based on analytical solutions of the hydrologic response, ins…

HydrologySubsurface stormflowGamma probability density function0208 environmental biotechnologyhillslope scale overland flow subsurface stormflow instantaneous response function gamma probability density function02 engineering and technologySoil surfaceAgricultural and Biological Sciences (miscellaneous)Arid020801 environmental engineeringInstantaneous response functionOverland flowSoil waterEnvironmental scienceSoil horizonSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSlow responseHillslope scaleScale (map)Surface runoffIntensity (heat transfer)Water Science and TechnologyCivil and Structural Engineering
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Analysis of soil surface component patterns affecting runoff generation. An example of methods applied to Mediterranean hillslopes in Alicante (Spain)

2008

Spatial patterns of soil surface components (vegetation, rock fragments, crusts, bedrock outcrops, etc.) are a key factor determining hydrological functioning of hillslopes. A methodological approach to analyse the patterns of soil surface components at a detailed scale is proposed in this paper. The methods proposed are applied to two contrasting semi-arid Mediterranean hillslopes, and the influence of soil surface component patterns on the runoff response of the slopes was analysed. A soil surface components map was derived from a high resolution photo-mosaic obtained in the field by means of a digital camera. Rainfall simulation experimental data were used to characterise the hydrologica…

Hydrologygeographygeography.geographical_feature_categoryBedrockSoil surface componentsHydrographRunoff generationInfiltration (hydrology)Rock fragmentSoil waterSpatial ecologyHillslope processesCommon spatial patternPatternsSurface runoffGeologyEarth-Surface ProcessesGeomorphology
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Simplified Probabilistic-Topologic Model for Reproducing Hillslope Rill Network Surface Runoff

2015

AbstractThis work presents a simplified probabilistic-topologic model for reproducing rill network surface runoff on a square-plane hillslope. The model requires only two parameters: the first is related to the production capacity of overland flow of the hillslope, at the initial conditions of the process, and the second depends on the sinuosity of the rill network. From a hydrological point of view, the following parameters account for the effects that essentially delineate the hydrologic response of a natural hillslope: rainfall intensity, hillslope roughness, and slope. Obviously, the reliability of the model is pending experimental validation that has only just begun. However, a prelimi…

Hydrologygeographygeography.geographical_feature_categoryProbabilistic logicSurface finishSinuosityExperimental validationAgricultural and Biological Sciences (miscellaneous)RillHydrology (agriculture)Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSurface runoffsurface runoff cellular automata hillslopeGeologyIntensity (heat transfer)Water Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Variable power-law scaling of hillslope Hortonian rainfall–runoff processes

2019

Hydrological studies focused on Hortonian rainfall–run-off scaling have found that the run-off depth generally declines with the plot length in power-law scaling. Both the power-law proportional coefficient and the scaling exponent show great variability for specific conditions, but why and how they vary remain unclear. In the present study, the scaling of hillslope Hortonian rainfall–run-off processes is investigated for different rainfall, soil infiltration, and hillslope surface characteristics using the physically based cell-based rainfall-infiltration-run-off model. The results show that both temporally intermittent and steady rainfalls can result in prominent power-law scaling at the …

Hydrologysoil infiltrationhillslope surfaceRainfall runoffrainfallSoil infiltrationrun-onPower lawVariable (computer science)power-lawEnvironmental scienceRun-onScalingHortonian run-off scalingWater Science and Technology
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European traditional tomatoes galore: a result of farmers' selection of a few diversity-rich loci

2022

A comprehensive collection of 1254 tomato accessions, corresponding to European traditional and modern varieties, early domesticated varieties, and wild relatives, was analyzed by genotyping by sequencing. A continuous genetic gradient between the traditional and modern varieties was observed. European traditional tomatoes displayed very low genetic diversity, with only 298 polymorphic loci (95% threshold) out of 64 943 total variants. European traditional tomatoes could be classified into several genetic groups. Two main clusters consisting of Spanish and Italian accessions showed higher genetic diversity than the remaining varieties, suggesting that these regions might be independent seco…

LDQTLPhysiologySLCFruit morphologyMicrobiologiaPlant SciencePortes-lès-ValenceSLLquantitative trait locusSolanum lycopersicumsingle nucleotide polymorphismCrop evolution; diversification; fruit morphology; genome-wide association study; genotyping by sequencing; selection; single nucleotide polymorphismGWASLSLSolanum pimpinellifolium HM ClauseCrop evolutionFarmersSPSolanum lycopersicum var. cerasiformeTomàquets--Conreuminimum allele frequencyMAFPhenotypeDiversificationGenotyping by sequencinglong shelf-lifeGenome-wide association studydiversificationSNPselectionprincipal coordinate analysesGBSFrance Crop evolutionPolymorphism Single Nucleotidegenotyping by sequencingLife ScienceHumansPCoA:Enginyeria agroalimentària::Agricultura::Producció vegetal [Àrees temàtiques de la UPC]SelectionAllelesfruit morphologyGenetic VariationEcologia[SDV.BV.AP]Life Sciences [q-bio]/Vegetal Biology/Plant breedingPlant BreedingSolanum lycopersicum L. var. lycopersicumlinkage disequilibriumTomatoes--VarietiesGenome-Wide Association StudyJ Exp Bot
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Emerging contaminants related to the occurrence of forest fires in the Spanish Mediterranean

2017

Forest fires can be a source of contamination because, among others, of the use of chemicals to their extinction (flame retardants, FRs), or by the production of Polycyclic Aromatic Hydrocarbons (PAHs) derived from high temperature alteration of organic matter. Up to our knowledge, this study is the first to assess the direct (PAHs 16 on the USA EPA's priority list), and indirect [tri- to hepta- brominated diphenyl ethers (PBDEs), organophosphorus flame retardants (PFRs) and perfluoroalkyl substances (PFASs)] contamination related to forest fires. The abundance and distribution of these contaminants were monitored on two Mediterranean hillslopes, one burned and one unburned, near Azuébar (S…

Mediterranean climateCanopyEnvironmental Engineering010504 meteorology & atmospheric sciencesPBDEsPriority listForest fires010501 environmental sciences01 natural sciencesWildfiresPAHsAbundance (ecology)PFASsPFRsEnvironmental ChemistrySoil PollutantsOrganic matterPolycyclic Aromatic HydrocarbonsWaste Management and Disposal0105 earth and related environmental sciencesFlame Retardantschemistry.chemical_classificationConnectivitySedimentVegetationContaminationPollutionCoupled hillslopeschemistrySpainEnvironmental chemistryEnvironmental scienceEnvironmental Monitoring
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