HIDROGEOQUÍMICA Y PRODUCCIÓN DE MANANTIALES EN LAS FORMACIONES PACACUA Y PEÑA NEGRA
Guardat en:
| Autors: | , |
|---|---|
| Format: | artículo original |
| Estat: | Versión publicada |
| Data de publicació: | 2011 |
| Descripció: | The discharge of springs in Pacacua and Peña Negra Formation of Trinidad de Mora and Jericóde Desamparados, Costa Rica, was determined to be approximately 0.4 and 24.4 l/min. The water of the springsof the Pacacua Formation was classified as calcium-bicarbonate or magnesium-chloride and the water of thesprings of the Peña Negra Formation as calcium-bicarbonate or magnesium-bicarbonate. The zones of rechargefor the springs were defined in order to protect the groundwater resources in the future. |
| Pais: | Portal de Revistas UCR |
| Institution: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| Idioma: | Español |
| OAI Identifier: | oai:archivo.portal.ucr.ac.cr:article/8590 |
| Accés en línia: | https://archivo.revistas.ucr.ac.cr/index.php/geologica/article/view/8590 |