Search results for "hydraulic conductivity"

showing 10 items of 115 documents

Field testing parameter sensitivity of the two-term infiltration equation using differentiated linearization

2003

Knowledge of soil hydraulic conductivity in the vadose zone is important in many agronomic, engineering and environmental areas. Transient tension infiltrometer experiments can be used to estimate the hydraulic conductivity, K0, corresponding to a given pressure head by the single-test (TST) method that uses the coefficients C1 and C2 of the two-term infiltration equation. The “Differentiated Linearization” (DL) method has been proposed to estimate these coefficients when a layer of contact material is used for the experiment. A field test of the DL and TST methods was conducted on a sandy loam and a clay soil. Eliminating the early-time influence of the contact layer was easy when the sorp…

Capillary actionSorptivitySoil hydraulic conductivitySoil SciencePressure headInfiltration (hydrology)Hydraulic conductivitytension infiltrometerLoamVadose zoneSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInfiltrometerGeotechnical engineeringMathematics
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Accuracy of Saturated Soil Hydraulic Conductivity Estimated from Numerically Simulated Single‐Ring Infiltrations

2019

The single-ring pressure infiltrometer (PI) method is widely used to determine saturated soil hydraulic conductivity, K s , directly in the field. The original and still most common way to analyze the data makes use of the steady-state model developed by the Canadian School in the 90s and two (two-ponding-depth, TPD, approach) or more (multiple-ponding-depth, MPD, approach) depths of ponding. The so-called Wu method based on a generalized infiltration equation allows analysis of the transient infiltration data collected by establishing a single ponding depth of water on the infiltration surface. This investigation, making use of simulated infiltration runs for initially unsaturated sand to …

lcsh:GE1-350lcsh:GeologySaturated soil hydraulic conductivityData analysis proceduresMaterials scienceHydraulic conductivitySingle-ring pressure infiltrometerlcsh:QE1-996.5Settore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSoil ScienceComposite materialRing (chemistry)lcsh:Environmental sciencesVadose Zone Journal
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On Infiltration and Infiltration Characteristic Times

2022

In his seminal paper on the solution of the infiltration equation, Philip (1969), https://doi.org/10.1016/b978-1-4831-9936-8.50010-6 proposed a gravity time, tgrav, to estimate practical convergence time and the time domain validity of his infinite time series expansion, TSE, for describing the transient state. The parameter tgrav refers to a point in time where infiltration is dominated equally by capillarity and gravity as derived from the first two (dominant) terms of the TSE. Evidence suggests that applicability of the truncated two-term equation of Philip has a time limit requiring higher-order TSE terms to better describe the infiltration process for times exceeding that limit. Since …

Science & TechnologyEROSIONsorptivityHYDRAULIC CONDUCTIVITYINFILTROMETERInfiltrationEnvironmental Sciences & EcologyPARAMETERSSOILMODELPhysical SciencesLimnology[SDE]Environmental Sciencesddc:550Water ResourcesEQUATIONSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliWATERsteady statetime domain validityMarine & Freshwater BiologyLife Sciences & Biomedicinehydraulic conductivityEnvironmental SciencesWater Science and Technology
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Source shape and data analysis procedure effects on hydraulic conductivity of a sandy-loam soil determined by ponding infiltration runs

2017

Performing ponding infiltration runs with non-circular sources could represent a good means to sample completely an area of interest. Regardless of the shape of the source, predicting the expected reliability of the collected data by infiltrometers should facilitate soil hydraulic characterisation and also allow a more conscious use of the field data. The influence of the shape of the infiltration source (i.e., circular or square) and the analysis procedure of the steady-state infiltration data on the saturated hydraulic conductivity, Ks, of a sandy-loam soil was tested in this investigation. Circular and square surfaces sampled with the pressure infiltrometer (PI) yielded similar estimates…

Yield (engineering)infiltration source shape0208 environmental biotechnologyBioengineeringSoil science02 engineering and technologyIndustrial and Manufacturing Engineeringlcsh:AgricultureHydraulic conductivitySimplified falling head techniquesaturated soil hydraulic conductivitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInfiltrometerGeotechnical engineeringlcsh:Agriculture (General)PondingMathematicssimplified falling head technique.Mechanical Engineeringlcsh:SPressure infiltrometer04 agricultural and veterinary scienceslcsh:S1-972020801 environmental engineeringVolumetric flow rateInfiltration (hydrology)LoamPressure infiltrometer. Saturated soil hydraulic conductivity. Infiltration source shape. Simplified falling head technique.Soil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesJournal of Agricultural Engineering
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Influence of stress-level due to self-weight on the hydraulic conductivity of permeable concrete for geotechnical applications

2022

Permeable concrete is effectively used in many fields of civil and environmental engineering, including some geotechnical applications such as drainage piles, deep drainage trenches, and as a permeable backfill material for retaining walls. The principal requirements that a pervious concrete must have for geotechnical applications are those that simultaneously guarantee enough hydraulic conductivity and good filter properties against internal erosion of the soil in which the drains are realised. These requirements can be effectively achieved through special mix-designs in which a non-negligible amount of sand is added to the aggregates, unlike the permeable concretes used for example in the…

Stress levelSettore ICAR/07 - GeotecnicaHydraulic conductivityPermeable concreteComputers in Earth SciencesGeotechnical Engineering and Engineering GeologySafety Risk Reliability and QualityGeomechanics for Energy and the Environment
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The effect of alternating different water qualities on accumulation and leaching of solutes in a Mediterranean cracking soil

2002

The relevance of bypass flow on water flow, solute or pesticide transport is becoming increasingly recognized. Recent investigations proved that soil salinization may be influenced by bypass flow, i.e. the rapid transport of water and solutes via macropores and/or shrinkage cracks to subsoil and groundwater. This paper explores the role of bypass flow in the process of accumulation and leaching of solutes, as well as of sodium, in a Mediterranean cracking soil irrigated with saline/sodic waters. The results of bypass flow experiments performed on undisturbed soil cores showed that leaching of solutes occurred in concomitance with bypass fluxes when a low salinity solution was alternated wit…

Soil salinitySoil testWater flowcrackingSoil sciencesalinizationcomplex mixturesirrigationclay soilsuitspoelenLeaching (agriculture)salt movementWater Science and TechnologyHydrologymodelLaboratorium voor Bodemkunde en geologieMacroporescheurvormingbypass flowSoil physicsLaboratory of Soil Science and Geologypredictionzware kleigrondenfieldLeaching modelleachingSoil watermiddellandse-zeegebiedverziltingirrigatiehydraulic conductivitymediterranean regionGeologystructured clay soilHydrological Processes
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Development and analysis of the Soil Water Infiltration Global database

2018

27 Pags.- 11 Tabls.- 8 Figs. © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.

Condutividade Hidráulica[SDV]Life Sciences [q-bio]0208 environmental biotechnology02 engineering and technologySilt910computer.software_genreSoilRING INFILTROMETERS900 Geschichte und Geografie::910 Geografie Reisen::910 Geografie ReisenHydraulic conductivityELECTRICAL-CONDUCTIVITYAgricultural landddc:550Meteorology & Atmospheric SciencesSATURATED HYDRAULIC CONDUCTIVITYGeosciences Multidisciplinarydatabaselcsh:Environmental sciences2. Zero hungerlcsh:GE1-350DatabaseIN-SITUlcsh:QE1-996.5Geology04 agricultural and veterinary sciencesPE&RCPedo-transfer functions6. Clean waterInfiltration (hydrology)HYDROPHYSICAL PARAMETERS[SDE]Environmental SciencesPhysical SciencesINFILTRATION GLOBAL DATABASEHidrologiaHydraulic conductivityPHYSICAL-PROPERTIESSANDY SOILTENSION INFILTROMETEREcology and EnvironmentPedotransfer functionPEDOTRANSFER FUNCTIONSLife ScienceSOIL INFILTRATION MEASUREMENTSLand surface modelsInfiltration (hydrology)Soil Water Infiltration Global databaseANALYSIS OF THE SOIL WATERScience & TechnologyLand useInfiltration15. Life on land020801 environmental engineeringInfiltraçãolcsh:GeologySoloInfiltration Land surface models Land use Pedo-transfer functionsSWIGAgriculture and Soil ScienceData qualityITC-ISI-JOURNAL-ARTICLEEarth and Environmental SciencesINFILTROMETER MEASUREMENTSLand useSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesGeneral Earth and Planetary SciencesEnvironmental scienceHydrologyITC-GOLDcomputer
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Testing Soil Encasing Materials for Measuring Hydraulic Conductivity of a Sandy-Loam Soil by the Cube Methods

2008

The Cube Method (CM) and the Modified Cube Method (MCM) were developed for measuring vertical (K v ) and horizontal (K h ) saturated hydraulic conductivity of a single soil sample. By these methods, a cube of soil is carved out in situ and a suitable material is applied to enclose the cube in a tightly fitting casing before moving the sample to the laboratory. Problems may be associated with the use of gypsum, originally used to encase soil. The suitability of molten wax and expandable polyurethane foam to encase a soil cube was tested for a sandy-loam soil. Wax-treated samples yielded lower conductivity results than untreated samples by a maximum factor of 3.7. The observed discrepancies w…

WaxMaterials scienceGypsumSoil testSoil ScienceMineralogyConductivityengineering.materialSoil compaction (agriculture)Hydraulic conductivityLoamvisual_artvisual_art.visual_art_mediumengineeringSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliSaturated soil hydraulic conductivity cube methods expandable polyurethane foamComposite materialCasingSoil Science Society of America Journal
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Hydrological and hydraulic behaviour of a surface flow constructed wetland treating agricultural drainage water in northern Italy.

2020

Abstract A surface flow constructed wetland (SFCW) treating agricultural drainage water was investigated with the aim to detect modifications in hydrological and hydraulic characteristics after more than a decade of operation. Ponded infiltration tests were conducted to estimate the saturated hydraulic conductivity, Ks, of the surface soil layer at the point scale. At the global scale, infiltration rate, i, was computed from the water balance to detect leakages from the pervious wetland surface. Tracer tests were conducted to analyse the existence of preferential flow inside the system and to estimate its hydraulic retention time (HRT). Clogging phenomena occurred given a mean Ks value of 3…

HydrologygeographyEnvironmental Engineeringgeography.geographical_feature_category010504 meteorology & atmospheric sciencesHydraulic retention timeInfiltration010501 environmental sciencesInfiltration (HVAC)Inlet01 natural sciencesPollutionSaturated hydraulic conductivityCloggingWater balanceHydraulic conductivityConstructed wetlandSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental ChemistryEnvironmental scienceSurface flow constructed wetlandDrainageWaste Management and DisposalHydraulic retention time0105 earth and related environmental sciencesThe Science of the total environment
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Changes in soil hydrodynamic parameters during intermittent rainfall following tillage

2023

The changes in the soil hydrodynamic properties following soil tillage were investigated in rainfall simulation trials of intermittent rain at the Masse experimental station (Soil Erosion LABoratory, SERLAB) in central Italy. The experiments were designed to build a database as representative as possible of situations that may occur in nature. The data collected during the experiments were used to determine the saturated soil hydraulic conductivity, Ks, the soil sorptivity at the antecedent soil–water matric potential Ψi, S, and the flow-weighted mean pore size at Ψi, λm. It was also verified if the energy content of total rainfall after tillage explained the short-term temporal variability…

Soil porosity SorptivityHydraulic conductivity Infiltration process Soil sealingHydraulic conductivitySoil sealingSoil porositySorptivityHydraulicSorptivitySettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliInfiltration processconductivityInfiltration proceEarth-Surface Processes
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