Utilización de los SRM en la obtención de parámetros y en la preparación de modelos de sistemas hidrogeológicos
DOI:
https://doi.org/10.21701/bolgeomin.118.3.006Palabras clave:
agua subterránea, evaluación de parámetros hidrogeológicos, SRM, zona no saturada, zona saturadaResumen
En este trabajo se presenta, en primer lugar, una revisión de los parámetros hidrogeológicos que pueden obtenerse a partir de los SRM, explicando seguidamente la forma en que pueden utilizarse los datos de SRM para su cálculo, así como las limitaciones existentes. En este sentido, se presentan los parámetros de almacenamiento y flujo de los acuíferos, enfatizando la viabilidad de la utilización de los SRM en su obtención, y los límites existentes en la conversión de los valores obtenidos en un SRM en datos hidrogeológicos. En segundo lugar, se analiza el uso integrado de los parámetros de almacenamiento y flujo en aplicaciones de hidroestratigrafía del subsuelo, pasando seguidamente a discutir el valor potencial que tienen los SRM para la investigación de la zona vadosa, con especial énfasis en su adecuación para la evaluación de las variaciones de la humedad con la profundidad en la zona no saturada. Finalmente, se analiza la capacidad específica del método SRM, que proporciona valores integrados provenientes de un gran volumen del subsuelo, en el contexto de integración de datos hidrogeológicos y su aplicabilidad como método para proporcionar datos para modelos de distribución de agua subterránea.
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