Search results for "Beerkan infiltration run"

showing 7 items of 7 documents

A simplified method based on Beerkan infiltration run

2013

A simplified method based on Beerkan infiltration run (SBI) to determine field saturated soil hydraulic conductivity

A simplified method based on Beerkan infiltration run (SBI)soil hydraulic conductivityA simplified method based on Beerkan infiltration run (SBI) soil hydraulic conductivity
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Estimation of hydrodynamic properties of a sandy-loam soil by two analysis methods of single-ring infiltration data

2022

Abstract Beerkan infiltration runs could provide an incomplete description of infiltration with reference to either the near steady-state or the transient stages. In particular, the process could still be in the transient stage at the end of the run or some transient infiltration data might be loss. The Wu1 method and the BEST-steady algorithm can be applied to derive soil hydrodynamic parameters even under these circumstances. Therefore, a soil dataset could be developed using two different data analysis methods. The hypothesis that the Wu1 method and BEST-steady yield similar predictions of the soil parameters when they are applied to the same infiltration curve was tested in this investi…

Data analysis methodSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliBeerkan infiltration runWu1 methodBEST methodologySoil hydrodynamic propertieJournal of Hydrology and Hydromechanics
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Hydrodynamic response of a loam soil after wetting with different methods

2023

Different points in a field can be wetted with different natural or artificial rainfall amounts and intensities. Therefore, a non-uniform soil wetting could occur during short-term monitoring of soil hydrodynamic parameters and its global effect on soil characterization is not easily predictable. For an initially dry loam soil, a sequence of three beerkan infiltration runs was performed at fixed sampling points in a period of two weeks. Immediately after the first beerkan run, the soil was perturbed by adding an additional water volume differing with the sampling point by the amount of water (0, 100 or 227 mm) and the application methodology (rainfall simulation, another beerkan run). As co…

Hydrodynamic propertieSoil disturbanceTemporal variabilityBeerkan infiltration runSoil water infiltration
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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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Run duration effects on the hydrodynamic properties of a loam soil estimated by steady-state infiltration methods

2020

Steady-state methods for the analysis of single-ring infiltration data are commonly applied. However, the duration of an infiltrometer experiment is often established quite subjectively based on the assumption that in general infiltration stabilizes rather quickly in the field. For a loam soil, the effect of the duration of a beerkan run on sorptivity, S, and saturated hydraulic conductivity, Ks, was tested by using the BEST (Beerkan Estimation of Soil Transfer parameters)-steady method and SSBI (Steady version of the Simplified method based on a Beerkan Infiltration run) method for data analysis. The standard experiment, based on a total of 15 water volumes each establishing an initial pon…

SSBI methodSteady state (electronics)0208 environmental biotechnologyexperimental protocolBioengineeringSoil science02 engineering and technologyIndustrial and Manufacturing Engineeringlcsh:Agriculturesoil sorptivitysaturated soil hydraulic conductivitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliBeerkan infiltration runlcsh:Agriculture (General)BEST-steadySSBI method.Mechanical Engineeringlcsh:S04 agricultural and veterinary scienceslcsh:S1-972020801 environmental engineeringInfiltration (hydrology)Duration (music)Loam040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental science
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Estimating saturated soil hydraulic conductivity by the near steady-state phase of a Beerkan infiltration test

2017

Abstract Single-ring infiltration experiments carried out in the field, such as the Beerkan runs, allow easy and inexpensive characterization of soil hydraulic properties, and specifically saturated soil hydraulic conductivity, Ks, by maintaining the functional connection of the sampled soil volume with the surrounding soil. However, a single infiltration experiment is not enough to determine Ks. The simplest way to obtain the necessary additional data is based on the assessment of the soil texture and structure characteristics. In this investigation, a simplified method, named SSBI (Steady version of the Simplified method based on a Beerkan infiltration run), was developed to estimate Ks b…

Soil textureField data0208 environmental biotechnologySoil ScienceSoil science04 agricultural and veterinary sciences02 engineering and technologyConductivitySteady-state infiltration020801 environmental engineeringInfiltration (hydrology)Saturated soil hydraulic conductivityHydraulic conductivitySoil water040103 agronomy & agricultureSoil volume0401 agriculture forestry and fisheriesSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInfiltrometerBeerkan infiltration runField methodMathematics
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Comparing two methods to perform a beerkan infiltration run in a loam soil at different dates

2023

<p>Performing beerkan infiltration runs with different heights of water pouring could help to obtain saturated soil sorptivity, <em>S</em>, and hydraulic conductivity, <em>K<sub>s</sub></em>, data usable to explain and simulate hydrological processes. However, most of the available information on the L (low height of water pouring, nearly 3 cm) - H (high height, 1-2 m) methodology refers to runs making use of a relatively limited number of water volumes and there is some sign that a few water volumes could yield an incomplete description of soil alteration phenomena induced by wetting. For a lo…

Water application procedureSurface hydrological processeSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil hydrodynamic parameterBeerkan infiltration runWater Science and TechnologyJournal of Hydrology
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