Please use this identifier to cite or link to this item: http://ricaxcan.uaz.edu.mx/jspui/handle/20.500.11845/2875
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dc.contributor271445es_ES
dc.coverage.spatialGlobales_ES
dc.creatorÁvila Dávila, Laura-
dc.creatorSoler Méndez, Manuel-
dc.creatorBautista Capetillo, Carlos Francisco-
dc.creatorGonzález Trinidad, Julian-
dc.creatorJunez Ferreira, Hugo Enrique-
dc.creatorRobles Rovelo, Cruz Octavio-
dc.creatorMolina Martínez, José Miguel-
dc.date.accessioned2021-12-14T18:05:16Z-
dc.date.available2021-12-14T18:05:16Z-
dc.date.issued2021-01-
dc.identifierinfo:eu-repo/semantics/publishedVersiones_ES
dc.identifier.issn2073-4395es_ES
dc.identifier.urihttp://ricaxcan.uaz.edu.mx/jspui/handle/20.500.11845/2875-
dc.description.abstractInfiltration estimation is made by tests such as concentric cylinders, which are prone to errors, such as the lateral movement under the ring. Several possibilities have been developed over the last decades to compensate these errors, which are based on physical, electronic, and mathematical principles. In this research, two approaches are proposed to measure the water infiltration rate in a silty loam soil by means of the mass values of a lysimeter weighing under rainfall conditions and different moisture contents. Based on the fact that with the lysimeter it is possible to determine acting soil flows very precisely, then with the help of mass conservation and assuming a downward vertical movement, 12 rain events were analyzed. In addition, it was possible to monitor the behavior of soil moisture and to establish the content at field capacity from the values of the weighing lysimeter, from which both approach are based. The infiltration rate of these events showed a variable rate at the beginning of the rainfall until reaching a maximum, to descend to a stable or basic rate. This basic infiltration rate was 1.49 ± 0.36 mm/h, and this is because soils with fine textures have reported low infiltration capacity. Four empirical or semi-empirical models of infiltration were calibrated with the values obtained with our approaches, showing a better fit with the Horton’s model.es_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.relationhttps://www.mdpi.com/2073-4395/11/1/180es_ES
dc.relation.ispartofhttps://doi.org/10.3390/agronomy11010180es_ES
dc.relation.urigeneralPublices_ES
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/3.0/us/*
dc.sourceAgronomy 2021, 11, 180.es_ES
dc.subject.classificationCIENCIAS FISICO MATEMATICAS Y CIENCIAS DE LA TIERRA [1]es_ES
dc.subject.othersoil moisturees_ES
dc.subject.otherwater balancees_ES
dc.subject.othervertical movementes_ES
dc.subject.otherwater masses_ES
dc.subject.otherrainfalles_ES
dc.subject.otherdrainagees_ES
dc.titleA Compact Weighing Lysimeter to Estimate the Water Infiltration Rate in Agricultural Soilses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
Appears in Collections:*Documentos Académicos*-- UA Cien. y Tec. de la Luz y la Mat. (LUMAT)

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