HIDROGEOQUÍMICA Y PRODUCCIÓN DE MANANTIALES EN LAS FORMACIONES PACACUA Y PEÑA NEGRA
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| Nhiều tác giả: | , |
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| Định dạng: | artículo original |
| Trạng thái: | Versión publicada |
| Ngày xuất bản: | 2011 |
| Miêu tả: | 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. |
| Quốc gia: | Portal de Revistas UCR |
| Tổ chức giáo dục: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| Ngôn ngữ: | Español |
| OAI Identifier: | oai:archivo.portal.ucr.ac.cr:article/8590 |
| Truy cập trực tuyến: | https://archivo.revistas.ucr.ac.cr/index.php/geologica/article/view/8590 |