Estudio isotópico del acuífero de Lima

dc.creatorSebastián, Carlos
dc.creatorRojas, Rubén
dc.creatorPlata, A.
dc.creatorRuíz, J.C.
dc.creatorPlata, A.
dc.creatorRojas, Rubén
dc.creatorRuíz, J.C.
dc.creatorSebastián, Carlos
dc.date.accessioned2014-04-29T17:58:02Z
dc.date.accessioned2023-05-24T15:14:03Z
dc.date.available2014-04-29T17:58:02Z
dc.date.available2023-05-24T15:14:03Z
dc.date.created2014-04-29T17:58:02Z
dc.date.issued1993-08
dc.identifierRojas R, Plata A, Ruíz JC, Sebastián C. Estudio isotópico del acuífero de Lima. Revista Peruana de Física. 1993; Volumen IV, No. 1 p. 31-36.
dc.identifierhttps://hdl.handle.net/20.500.13054/151
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6442904
dc.description.abstractFiltrations from Rimac and Blanco rivers and Graton Tunnel (on the Rimac basin, 80 km from Lima. and 2500 m sea level) were studied using artificial tracers and superficial water analysis. Graton tunnel has a 3-5 m3/s volume. Domestic and industrial demand of Lima (7 million inhabitants) is 22 m3/s. Preliminary results suggest that Graton tunnel filtrations do not originate on Rimac or Blanco rivers, but in regions at 4600 m sea level. Detected tritium suggests that water filtrated in Graton tunnel is modern.
dc.languagespa
dc.publisherLima
dc.publisherPE
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceInstituto Peruano de Energía Nuclear
dc.sourceRepositorio Institucional del Instituto Peruano de Energía Nuclear
dc.subjectHidrología isotópica
dc.subjectAcuíferos
dc.subjectAguas superficiales
dc.subjectTritio
dc.subjectRíos
dc.titleEstudio isotópico del acuífero de Lima
dc.typeinfo:eu-repo/semantics/article


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