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Modelado de la dispersión mecánica mediante el método de los fenómenos de transporte advectivo, un primer paso
1Unit Subsurface and Groundwater Systems, Deltares, Utrecht, The Netherlands.
La dispersión mecánica en el flujo de aguas subterráneas se explica por la varianza de la velocidad, no por los gradientes de concentración. Un nuevo modelo introduce un parámetro de "desplazamiento de volumen dispersivo", que mejora la precisión de la simulación de plumas en acuíferos heterogéneos.
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