Please use this identifier to cite or link to this item: http://repositorio.unitau.br/jspui/handle/20.500.11874/2384
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dc.contributor.authorLopes L.N.pt_BR
dc.contributor.authorMartins E.pt_BR
dc.contributor.authorSantoro B.L.pt_BR
dc.contributor.authorSouza, Claudinei Fonsecapt_BR
dc.date.accessioned2019-09-12T16:37:11Z-
dc.date.available2019-09-12T16:37:11Z-
dc.date.issued2009-
dc.citation.volume14pt_BR
dc.citation.issue4pt_BR
dc.citation.spage564-
dc.citation.epage577-
dc.identifier.issn14137895-
dc.identifier.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-73549113336&partnerID=40&md5=c23bba9568ef3fffd479a670a470b9d7-
dc.identifier.urihttp://repositorio.unitau.br/jspui/handle/20.500.11874/2384-
dc.description.abstractKnowledge of water distribution in soil is of great importance to agriculture, since water is one of the factors that most influence the yield of crops. There are many techniques used to monitor soil water content. The time domain reflectometry (TDR) has been widespread among researchers because it presents several advantages, among which the determination in real time and possibility of automated readings. The main goal of this research was to evaluatethe water distribution in a profile of Red-Yellow Oxisol. Time domain reflectometry (TDR) probes were used to monitor the water distribution from drippers discharging at constant flow rates of 2, 4 and 8 L h-1 in soil. Considering results from different profiles, we observed greater water storage near the dripper decreasing gradually towards the wetting front. About one third of the applied water (33%) was stored in the first layer (0-0.10 m) for all experiments. Comparing different dripper flow rates, we observed higher water storage for 8 L h-1, with 30, 33 and 34% of applied water accumulating in the first layer (0-0.10m) for dripper flow rates of 2, 4 and 8 L h-1, respectively. The results suggest that based on the volume and frequency used in this experiment, it would be advantageous to apply small amounts of water at more frequent intervals to reduce deep percolation losses of applied water.en
dc.description.provenanceMade available in DSpace on 2019-09-12T16:37:11Z (GMT). No. of bitstreams: 0 Previous issue date: 2009en
dc.languagePortuguêspt_BR
dc.relation.ispartofIRRIGA-
dc.rightsAcesso Restritopt_BR
dc.sourceScopuspt_BR
dc.subject.otherTDRen
dc.subject.otherWater contenten
dc.subject.otherWetted soil volumeen
dc.subject.othercrop yielden
dc.subject.otherdischargeen
dc.subject.otherdrip irrigationen
dc.subject.otherexperimental studyen
dc.subject.otherOxisolen
dc.subject.otherpercolationen
dc.subject.othersoil wateren
dc.subject.otherwater contenten
dc.subject.otherwater storageen
dc.subject.otherwater supplyen
dc.subject.otherdrip irrigationen
dc.subject.otherOxisolen
dc.subject.othersoil wateren
dc.subject.othertime domain reflectometryen
dc.subject.otherwater contenten
dc.subject.otherwater supplyen
dc.titleWater distribution characterization in soil for drip irrigation [Caracterização da distribuição da água no solo para irrigação por gotejamento]en
dc.typeArtigo de Periódicopt_BR
dc.description.affiliationLopes, L.N., Universidade de Taubaté, Unitau, Taubaté, SP, Brazil-
dc.description.affiliationMartins, E., Departamento Engenharia Civil e Ambiental, Universidade de Taubaté, Unitau, Taubaté, SP, Brazil-
dc.description.affiliationSantoro, B.L., Departamento Engenharia Civil e Ambiental, Universidade de Taubaté, Unitau, Taubaté, SP, Brazil-
dc.description.affiliationSouza, C.F., Departamento de Recursos Naturais e Proteção Ambiental, Universidade Federal São Carlos, São Carlos, SP, Brazil-
dc.identifier.scopus2-s2.0-73549113336-
dc.contributor.scopus35275511000pt_BR
dc.contributor.scopus35734723400pt_BR
dc.contributor.scopus35115480400pt_BR
dc.contributor.scopus7102769563pt_BR
Appears in Collections:Artigos de Periódicos

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