Search results for "soil hydraulic propertie"

showing 10 items of 16 documents

Testing a Simplified Approach to Determine Field Saturated Soil Hydraulic Conductivity

2013

Abstract Interpreting and simulating hydrological processes need a large number of field saturated soil hydraulic conductivity, Kfs , data that should be collected with simple and rapid field experiments. A Simplified method based on a Beerkan Infiltration run (SBI method) was recently developed and tested successfully on Burundian soils. With the SBI method, a cylinder is inserted to a short depth into the soil and the infiltration time of a few small volumes of water repeatedly applied at the surface of the confined soil is measured. Calculating Kfs needs the slope of the linearized cumulative infiltration vs. time relationship and an estimate of the so called α* parameter. In this invest…

BEST (Beerkan Estimation of Soil Transfer parameters) procedureSoil scienceArea of interestSoil hydraulic propertiesSingle ring pressure infiltrometer.Infiltration (hydrology)Hydraulic conductivityMeasurement methodsSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliGeneral Earth and Planetary SciencesInfiltrometerSoil hydraulic properties Measurement methods BEST (Beerkan Estimation of Soil Transfer parameters) procedure Single ring pressure infiltrometerPondingGeneral Environmental ScienceMathematicsProcedia Environmental Sciences
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Determining Soil Hydraulic Properties Using Infiltrometer Techniques: An Assessment of Temporal Variability in a Long-Term Experiment under Minimum- …

2020

Conservation agriculture is increasingly accepted by farmers, but the modeling studies on agro-environmental processes that characterize these agricultural systems require accurate information on the temporal variability of the soil&rsquo

Geography Planning and Developmentlcsh:TJ807-830lcsh:Renewable energy sourcesSoil science010501 environmental sciencesManagement Monitoring Policy and Law01 natural sciencesAvailable water capacityField capacityMinimum tillageSoil managementHydraulic conductivityInfiltrometerlcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Renewable Energy Sustainability and the Environmentsoil hydraulic propertieslcsh:Environmental effects of industries and plantssaturated hydraulic conductivity04 agricultural and veterinary sciencesBulk densityTillageBEST procedure Saturated hydraulic conductivity SFH technique Soil hydraulic propertieslcsh:TD194-195040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceBEST procedureSFH techniqueSustainability
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Physical and hydraulic characterization of a clay soil at the plot scale

2010

Summary The soil physical and hydraulic properties have to be determined for interpreting and simulating many hydrological processes. An investigation was carried out to determine the physical and hydraulic characteristics of a clay soil at the plot scale. An intensive sampling of the surface soil layer of two plots of 4 × 11 m2 was carried out by measuring, for each plot, dry soil bulk density, ρb, and antecedent soil water content, θi, at 88 sampling points and field-saturated soil hydraulic conductivity, Kfs, at 176 sampling points. A wide range of Kfs values (0.7–5107 mm h−1) were measured by the Simplified Falling Head (SFH) technique. For each variable, the two plots yielded very simi…

Hydrological processeSampling (statistics)Soil physical propertieSoil scienceStandard deviationHydraulic conductivitySample size determinationSoil hydraulic propertiePlot scaleSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSpatial variabilityFrequency distributionWater contentWater Science and TechnologyMathematics
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USING A TRANSIENT INFILTROMETRIC TECHNIQUE FOR INTENSIVELY SAMPLING FIELD-SATURATED HYDRAULIC CONDUCTIVITY OF A CLAY SOIL IN TWO RUNOFF PLOTS

2012

Point measurement of soil properties allows to explain and simulate plot scale hydrological processes. An intensive sampling was carried out at the surface of an unsaturated clay soil to measure, on two adjacent plots of 4×11 m2 and two different dates (May 2007 and February-March 2008), dry soil bulk density, rb, and antecedent soil water content, qi, at 88 points. Field-saturated soil hydraulic conductivity, Kfs, was also measured at 176 points by the transient Simplified Falling Head technique to determine the soil water permeability characteristics at the beginning of a possible rainfall event yielding measurable runoff. The rb values did not differ significantly between the two dates b…

Hydrological processeSoil hydraulic propertiePlot scaleSoil physical propertieSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestali
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Testing infiltration run effects on the estimated water transmission properties of a sandy-loam soil

2016

Abstract Testing factors influencing determination of soil water transmission properties by an infiltrometer method helps better interpretation of the collected data and allows the development of appropriate sampling strategies for the intended use of the data. These factors include the soil water content at the start of the experiment, the height from which water is poured onto the soil surface, and the duration of the infiltration run. A sandy-loam soil was sampled with the BEST (Beerkan Estimation of Soil Transfer parameters) procedure of soil hydraulic characterization and two heights of pouring of water (0.03 and 1.5 m) under three different initial soil water content, θ i (0.12 ≤ θ i …

HydrologySoil test0208 environmental biotechnologySoil Science02 engineering and technologyRun duration020801 environmental engineeringInfiltration (hydrology)Hydraulic conductivitySoil hydraulic propertieLoamSoil waterSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental scienceBeerkan infiltration runInfiltrometerBEST procedureHeight of pouring of waterSurface runoffWater contentGeoderma
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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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INVESTIGATIONS ON INFILTRATION METHODS FOR AN IMPROVED SOIL HYDRAULIC CHARACTERIZATION

2020

Infiltration soil hydraulic properties saturated soil hydraulic conductivity surface hydrological processes BEST procedure for soil hydraulic characterization two-stage methodology height of water pouring effects soil sealing rainfall simulation beerkan infiltration experiment BEST algorithms laboratory investigation falling-head one dimensional infiltration simplified falling-head technique automatic infiltrometer Arduino parameterization of model for single-ring infiltration monitoring saturated hydraulic conductivity
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Fitting particle size distribution models to data from Burundian soils for the BEST procedure and other purposes

2009

Testing the Beerkan Estimation of Soil Transfer (BEST) soil particle size distribution (PSD) model is necessary to evaluate the applicability of the BEST procedure for characterising soil hydraulics. In this investigation, the fitting performance of the BEST PSD model was tested using a database of 114 Burundian soils with 14 measured particle size fractions for each soil sample, and also by considering a reduced number of measured particle size fractions for a sample. The fitting performance of the model developed by Fredlund et al. (2000) (FR model) was also considered for comparative purposes. On average, the BEST model yielded satisfactory results (i.e., mean relative error, E r ¯ = 3.9…

Particle-size distributionSoil textureBurundiSimulation modelingSoil ScienceDistribution (mathematics)Soil hydraulic propertieControl and Systems EngineeringApproximation errorParticle-size distribution modelSoil classificationStatisticsSoil waterParticle-size distributionSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSize fractionsParticle sizeAgronomy and Crop ScienceFood ScienceMathematicsBiosystems Engineering
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Improvement of BEST (Beerkan Estimation of Soil Transfer parameters) method for soil hydraulic characterization

Interpreting and modeling soil hydrological processes require the determination of the soil hydraulic characteristic curves, i.e. the relationships between volumetric soil water content, pressure head, and hydraulic conductivity. Using traditional methods to determine these properties is expensive and time consuming. Haverkamp et al. (1996) pioneered a specific method for soil hydraulic characterization known as the “Beerkan method”. An improved version of this methodology, called the Beerkan Estimation of Soil Transfer parameters (BEST) procedure, was developed by Lassabatère et al. (2006) to simplify soil hydraulic characterization. BEST considers certain analytic formulae for hydraulic c…

Saturated soil hydraulic conductivityBEST (Beerkan Estimation of Soil Transfer parameters) procedureSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil hydraulic properties
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Soil physical quality in a Sicilian agricultural area

2008

Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil physical quality Agricultural soils Land use Soil hydraulic properties
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