Estudio isotópico del acuífero de Lima
Filtrations 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....
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1993 |
| País: | Perú |
| Institución: | Instituto Peruano de Energía Nuclear |
| Repositorio: | IPEN-Institucional |
| Idioma: | español |
| OAI Identifier: | oai:repositorio.ipen.gob.pe:20.500.13054/151 |
| Acceso en línea: | https://hdl.handle.net/20.500.13054/151 |
| Access Level: | acceso abierto |
| Palabra clave: | Hidrología isotópica Acuíferos Aguas superficiales Tritio Ríos |
| Sumario: | Filtrations 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. |
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