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A Compact Weighing Lysimeter to Estimate the Water Infiltration Rate in Agricultural Soils

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dc.contributor 271445 es_ES
dc.coverage.spatial Global es_ES
dc.creator Ávila Dávila, Laura
dc.creator Soler Méndez, Manuel
dc.creator Bautista Capetillo, Carlos Francisco
dc.creator González Trinidad, Julian
dc.creator Junez Ferreira, Hugo Enrique
dc.creator Robles Rovelo, Cruz Octavio
dc.creator Molina Martínez, José Miguel
dc.date.accessioned 2021-12-14T18:05:16Z
dc.date.available 2021-12-14T18:05:16Z
dc.date.issued 2021-01
dc.identifier info:eu-repo/semantics/publishedVersion es_ES
dc.identifier.issn 2073-4395 es_ES
dc.identifier.uri http://ricaxcan.uaz.edu.mx/jspui/handle/20.500.11845/2875
dc.description.abstract Infiltration 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.iso eng es_ES
dc.publisher MDPI es_ES
dc.relation https://www.mdpi.com/2073-4395/11/1/180 es_ES
dc.relation.ispartof https://doi.org/10.3390/agronomy11010180 es_ES
dc.relation.uri generalPublic es_ES
dc.rights Attribution-NonCommercial-ShareAlike 3.0 United States *
dc.rights.uri http://creativecommons.org/licenses/by-nc-sa/3.0/us/ *
dc.source Agronomy 2021, 11, 180. es_ES
dc.subject.classification CIENCIAS FISICO MATEMATICAS Y CIENCIAS DE LA TIERRA [1] es_ES
dc.subject.other soil moisture es_ES
dc.subject.other water balance es_ES
dc.subject.other vertical movement es_ES
dc.subject.other water mass es_ES
dc.subject.other rainfall es_ES
dc.subject.other drainage es_ES
dc.title A Compact Weighing Lysimeter to Estimate the Water Infiltration Rate in Agricultural Soils es_ES
dc.type info:eu-repo/semantics/article es_ES


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