DETERMINACIÓN DE LA VELOCIDAD DE LOS GASES EN EL SUBSUELO MEDIANTE UN MÉTODO BASADO EN LAS VARIACIONES DE LA CONCENTRACIÓN DEL GAS RADÓN
Wedi'i Gadw mewn:
| Awdur: | |
|---|---|
| Fformat: | artículo original |
| Statws: | Versión publicada |
| Dyddiad Cyhoeddi: | 2011 |
| Disgrifiad: | In this paper a theoretic model is proposed to calculate the gas velocity in the subsoil based onradon concentration variations. The general transport equation for radon in a homogeneous soil with constantporosity is assumed. The diffusion coefficient and the gas velocity being constant. In order to illustrate the mo-del, three geological areas were considered: the Irazú and Arenal volcanoes, situated in the volcanic range inCosta Rica, and the Agua Caliente fault located in San José, Costa Rica. |
| Gwlad: | Portal de Revistas UCR |
| Sefydliad: | Universidad de Costa Rica |
| Repositorio: | Portal de Revistas UCR |
| Iaith: | Español |
| OAI Identifier: | oai:archivo.portal.ucr.ac.cr:article/8542 |
| Mynediad Ar-lein: | https://archivo.revistas.ucr.ac.cr/index.php/geologica/article/view/8542 |