Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8894388 | Geoderma | 2018 | 11 Pages |
Abstract
As a result, the homogeneous hydrologic zones defined in VID may be used to recommend specific irrigation practices and as the basis for the application of distributed soil water movement models. These hydrologic properties may be applied directly as inputs to the models while the PTFs may allow for setting adequate parameters in nearby areas with similar soils from more readily available soil information (texture, organic matter and gypsum).
Keywords
SARIRFSSTAWCSSECCEGypsum contentLSDWUAVIDRMSEPTFDfEDFTECeWater user associationanalysis of the varianceANOVAbulk densityNumber of samplesPedotransfer functionsIrrigation return flowsleast significant differenceRoot mean square errorSalinityAvailable Water CapacityField capacityorganic matterAvailable water contentCalcium carbonate equivalentsodium absorption ratioWilting pointHydraulic conductivitySaturated hydraulic conductivity
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Jiménez-Aguirre M.T., Isidoro D., Usón A.,