Simulación del Flujo de Agua Subterránea en Acuíferos Usando Diferencias Finitas
In this work, a numerical method is presented to calculate the water storage within an aquifer, which is developed by presenting an algorithm to find the numerical solution of the water balance equation, which describes the behavior of the water flow within a porous material. First, the water balanc...
| Autor: | |
|---|---|
| Formato: | tesis de maestría |
| Estado: | Versión aceptada para publicación |
| Fecha de publicación: | 2020 |
| País: | Colombia |
| Recursos: | Universidad Nacional de Colombia |
| Repositorio: | Repositorio UN |
| Idioma: | español |
| OAI Identifier: | oai:repositorio.unal.edu.co:unal/78386 |
| Acesso em linha: | https://repositorio.unal.edu.co/handle/unal/78386 |
| Access Level: | acceso abierto |
| Palavra-chave: | 510 - Matemáticas::518 - Análisis numérico Aquifer Storage Flow Finite differences Water balance (Hydrology) Acuífero Almacenamiento Flujo Diferencias finitas Balance hídrico (Hidrología) |
| Resumo: | In this work, a numerical method is presented to calculate the water storage within an aquifer, which is developed by presenting an algorithm to find the numerical solution of the water balance equation, which describes the behavior of the water flow within a porous material. First, the water balance equation is deduced, then the deduction of the method is carried out to calculate the flow of groundwater in a heterogeneous and anisotropic aquifer in a transitory state, both for the 3-D and 2-D cases; It continues with the verification of certain properties that validate the method and ends by presenting some numerical examples. |
|---|