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dc.contributor.authorRojas-Zeledón, Ignacio José
dc.date.accessioned2018-02-16T16:20:36Z
dc.date.available2018-02-16T16:20:36Z
dc.date.issued2017
dc.identifier.urihttps://hdl.handle.net/2238/9387
dc.descriptionProyecto de Graduación (Licenciatura en Ingeniería Forestal) Instituto Tecnológico de Costa Rica, Escuela de Ingeniería Forestal, 2017.es
dc.description.abstractHydric erosion was studied under three forest stages of succession in Palo Verde National Park. Erosion and sedimentation rates were evaluated on three tropical dry forest stages of succession: early, intermediate, late and three slope conditions 20, 30 and 40% affected by the rain around Palo Verde lagoon in Guanacaste region, Bagaces-Costa Rica. The study area is characterized because of their clayey soils and proximity to chalky hills that overlap abruptly from sea level to 1000 m.a.s.l. approximately. It found significant differences between stages of succession, but not between the three different slope percentages. Under a maximum rain intensity average of 23 mm/15 min, the early stage succession is the highest sediment producer with an average value of 4.75 Mg/ha/year.es
dc.description.sponsorshipParque Nacional Palo Verdees
dc.language.isospaes
dc.publisherInstituto Tecnológico de Costa Ricaes
dc.subjectSedimentaciónes
dc.subjectSueloes
dc.subjectParque nacionaleses
dc.subjectBosqueses
dc.subjectHumedaleses
dc.titleErosión hídrica bajo tres estadios de sucesión de bosque dentro del Parque Nacional Palo Verde, Costa Ricaes
dc.typelicentiateThesises


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