dc.contributorMinella, Jean Paolo Gomes
dc.contributorhttp://lattes.cnpq.br/3194231720402587
dc.contributorGubiani, Paulo Ivonir
dc.contributorhttp://lattes.cnpq.br/7251203817503318
dc.contributorBoeni, Madalena
dc.contributorhttp://lattes.cnpq.br/2751273298495891
dc.creatorSchneider, Fabio José Andres
dc.date.accessioned2018-08-22T12:15:26Z
dc.date.accessioned2019-05-24T20:48:58Z
dc.date.available2018-08-22T12:15:26Z
dc.date.available2019-05-24T20:48:58Z
dc.date.created2018-08-22T12:15:26Z
dc.date.issued2017-02-24
dc.identifierhttp://repositorio.ufsm.br/handle/1/14074
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/2843748
dc.description.abstractThe runoff generation over fields with no-tillage agriculture management remains being a problem with environment, social and economic impacts. The purpose of this research was evaluate the capacity of a physic based and distributed model (LISEM) to simulate the generation and propagation of the runoff over hillslopes cultivated with no tillage system during monitored rainfall events. The field experiment is located in Júlio de Castilhos, central region of Rio Grande do Sul state, on Fepagro - State Foundation for Agricultural Research. Was investigated the Lisem model capacity to simulate the generation and propagation of the runoff over different areas, four of them with approximately 0.5 ha with different soil and cover management systems, and one with approximately 2.5 ha with presence of ephemeral channels. From most of the rainfall events monitored during 2015 and 2016 years, five was chosen that generated runoff over all fields to calibrate the model parameters, two of them considered of low magnitude, two of high magnitude and one of extreme high magnitude. The calibration of the model was designed by changing the saturate soil hydraulic conductivity, initial soil water content, surface Manning’s coefficient and aleatory roughness of the soil, to fit the peak of flow discharge, total volume discharge and hydrograph shape. In general, the model performed well on simulate the runoff dynamics, especially the extreme high magnitude rainfall event, responsible for the most of environment impacts, water and soil losses. LISEM model can be an option in studies to better understanding the hydrological process behavior of the runoff generation, and as a decision tool in recommendations of more efficient practices to excess runoff control, contributing to decrease the water erosion, soil losses and improving the soil and water quality.
dc.publisherUniversidade Federal de Santa Maria
dc.publisherBrasil
dc.publisherAgronomia
dc.publisherUFSM
dc.publisherPrograma de Pós-Graduação em Ciência do Solo
dc.publisherCentro de Ciências Rurais
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International
dc.subjectEscoamento superficial
dc.subjectPlantio direto
dc.subjectEncostas
dc.subjectModelagem
dc.subjectLISEM
dc.subjectRunoff
dc.subjectNo-tillage
dc.subjectHillslope
dc.subjectModeling
dc.titleModelagem matemática do escoamento superficial na escala de encosta sob plantio direto
dc.typeTesis


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