Search results for "Soil surface"

showing 10 items of 28 documents

Eco-geomorphological connectivity and coupling interactions at hillslope scale in drylands: Concepts and critical examples

2020

The diagnosis of land degradation requires a deep understanding of ecosystem functioning and evolution. In dryland systems, in particular, research efforts must address the redistribution of scarce resources for vegetation, in a context of high spatial heterogeneity and non-linear response. This fact explains the prevalence of eco-hydrological perspectives interested in runoff processes and, the more recent, focused on connectivity as an indicator of system resource optimisation. From a geomorphological perspective and reviewing the concepts of eco-hydro-geomorphological interactions operating in ecosystems, this paper explores the effects of erosion on vegetation configuration through two …

0106 biological sciencesProcess-patternGeospatial analysis010504 meteorology & atmospheric sciencesContext (language use)computer.software_genre010603 evolutionary biology01 natural sciencesFeedbackEcosystemSoil surface armouringEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesRunoff connectivityEcologybusiness.industryScale (chemistry)Environmental resource managementVegetationHillslope-channel couplingScaleSpatial heterogeneityLand degradationEnvironmental sciencebusinessSurface runoffcomputerGeografiaJournal of Arid Environments
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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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Using Beerkan experiments to estimate hydraulic conductivity of a crusted loamy soil in a Mediterranean vineyard

2019

Abstract In bare soils of semi-arid areas, surface crusting is a rather common phenomenon due to the impact of raindrops. Water infiltration measurements under ponding conditions are becoming largely applied techniques for an approximate characterization of crusted soils. In this study, the impact of crusting on soil hydraulic conductivity was assessed in a Mediterranean vineyard (western Sicily, Italy) under conventional tillage. The BEST (Beerkan Estimation of Soil Transfer parameters) algorithm was applied to the infiltration data to obtain the hydraulic conductivity of crusted and uncrusted soils. Soil hydraulic conductivity was found to vary during the year and also spatially (i.e., ro…

Water en LandgebruikHydraulic conductivity0207 environmental engineeringSoil science02 engineering and technologyVineyardVineyardSoilBodemSoil Water and Land UseHydraulic conductivitySoil surface crustSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali020701 environmental engineeringPondingWater Science and TechnologyFluid Flow and Transfer ProcessesConventional tillageMechanical EngineeringWater and Land Use04 agricultural and veterinary sciencesHydraulic engineeringPE&RCBodem Water en LandgebruikTillageInfiltration (hydrology)LoamWater infiltration measurementSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceWater infiltration measurementsBEST procedureTC1-978
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Evaluating roughness effects on C-band AMSR-E observations

2014

International audience; The usefulness of microwave remote sensing to retrieve near-surface soil moisture has already been demonstrated in many studies. However, obtaining high quality estimates of soil moisture is influenced by many effects from soil, vegetation and atmosphere; one of the key parameters is surface roughness. This research focusses on a semi-empirical method to evaluate the roughness effects from space borne observations. Global maps of roughness effects are evaluated at C-band from AMSR-E measurements.

010504 meteorology & atmospheric sciencesC band[SDE.MCG]Environmental Sciences/Global Changes0211 other engineering and technologiessoil surface roughnessAMSR-E02 engineering and technologySurface finish01 natural sciences13. Climate actionEnvironmental sciencesoil moisture[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processing021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensing2014 IEEE Geoscience and Remote Sensing Symposium
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Soil hydraulic properties determined by infiltration experiments and different heights of water pouring

2014

Abstract Establishing the dependence of the soil hydraulic characterization carried out by an infiltration experiment on the procedure used to apply water on the confined soil surface may help to better interpret the collected data and also to develop more accurate strategies for soil hydraulic characterization. Soil was sampled at four Sicilian sites with both the Simplified Falling Head (SFH) technique and the Beerkan Estimation of Soil Transfer parameters (BEST) procedure and two heights of water application (0.03 and 1.5 m). The most appropriate BEST algorithm to analyze the data was determined and the effect of the height of water pouring on the measured soil hydraulic properties was e…

HydrologyWater applicationHydraulic conductivitySoil hydraulic propertieSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil ScienceEnvironmental scienceSFH techniqueBEST procedureSoil surfaceInfiltration (HVAC)Geoderma
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Effect of cultivation techniques on the hydrodynamic and mechanical behaviour of the "Lauragais-terreforts"

1993

The effect of various seed bed preparations on hydrodynamic and mechanical parameters was studied experimentally by simulated rainfall on clayeyloamy soils Lauragais, which had developed on chalky molasse on a slope greater than 12 %. The level of soaked up rain ("pluie d'imbibition", Pi) is closely connected to the inital degree of saturation of the soil ; it varies from 10 to 24 mm when the soil is humid and increases when the soil is dry (14 to 47 mm). But when the soil surface is crusted the Pi is less and seems to be no longer controlled by the degree of water in the soil. Treatments with fine structural elements show the fewest possibilities of infiltration during the soaking up stage…

Drop (liquid)Degree of saturationSoil scienceSoil surfaceSoil saturationMolasseInfiltration (hydrology)EVOLUTION DES SOLS SOUS CULTUREINFILTRATIONSTRUCTURE DU SOLSoil waterEnvironmental scienceEROSION HYDRIQUESIMULATION DE PLUIESurface runoff
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Interacción de procesos geomórficos y distribución de componentes de la superficie del suelo en relación a la evolución de los abarrancamientos de Ta…

2009

Este artículo se ha desarrollado en el contexto de los proyectos: REN2003-045707GLO(PECOS); CGL2007-63258/BOS(PREVEA) y CGL2006-11619(PROBASE), financiados por la CICYT en el marco del Plan Nacional I+D+I

Surface (mathematics)Geography (General)geographygeography.geographical_feature_categoryRelation (database)business.industryLandformGeography Planning and DevelopmentDistribution (economics)Soil surfaceEnvironmental Science (miscellaneous)Spatial distributionField (geography)Factores de la erisiónBadlandsEarth and Planetary Sciences (miscellaneous)G1-922businessDigital elevation modelComponentes superficiales del sueloGeomorphologyGeology
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El método mejorado del tocón (ISUM) permite evaluar procesos de erosión del suelo en plantas injertadas utilizando medidas topográficas in situ

2021

[EN] Policymakers, stakeholders and rural inhabitants must be aware of the relevance of soil erosion as an irreversible landdegradation process. This is key to achieve the land degradation neutrality challenge and the sustainability of humankindand natural ecosystems. Agricultural areas are being affected by soil erosion threatening soil quality and, subsequently,food security. Therefore, it is necessary to develop new techniques and methods visually friendly and easy to be accessedto survey and assess the soil erosion concerns. ISUM (Improve Stock Unearthing Method) is a well-contrasted procedureto estimate and map soil mobilisation and erosion rates. To achieve this goal, using the plant …

In situCartographyEarth observationGeografía del sueloAgriculturaSoil scienceAgricultureCultural HeritageMapping techniques3D ModellingGeophysicsSuperficie del sueloTécnicas cartográficasSoil surfaceEnvironmental scienceCartografíaGeocomputingEnvironmental applicationsStock (geology)GeodesySoil geography
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A simple field method to measure the hydrodynamic properties of soil surface crust

2013

The hydraulic resistance of the surface crust was determined by a combination of two infiltrometric techniques: first, a surface measurement of steady-state infiltration rate is conducted by a mini-disk tension infiltrometer (MDI); then, the surface crust is removed, its thickness is measured, and a ponded infiltration test is performed at the same site. The Beerkan Estimation of Soil Transfer parameters (BEST) method is applied to estimate the hydraulic properties of the underlying soil provided the particlesize distribution and the bulk density are known. Under the assumption of a unit gradient of hydraulic head below the soil crust, the pressure head at the interface crust-soil is derive…

soil surface crust mini disk tension infiltrometer BEST procedureBEST procedure; Mini disk tension infiltrometer; Soil surface crust; Industrial and Manufacturing Engineering; Mechanical Engineering; BioengineeringWater flowMechanical Engineeringlcsh:SBioengineeringCrustInfiltration (HVAC)lcsh:S1-972Industrial and Manufacturing Engineeringlcsh:AgricultureHydraulic headSoil surface crustHydraulic conductivityMini disk tension infiltrometerSoil crustLoamSoil surface crust mini disk tension infiltrometer BEST procedure.InfiltrometerGeotechnical engineeringBEST procedurelcsh:Agriculture (General)MathematicsJournal of Agricultural Engineering
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