Abstract
Sea-water intrusion is actively contaminating fresh groundwater reserves in the coastal aquifers of the Pioneer Valley, north-eastern Australia. A three-dimensional sea-water intrusion model has been developed using the MODHMS code to explore regional-scale processes and to aid assessment of management strategies for the system. A sea-water intrusion potential map, produced through analyses of the hydrochemistry, hydrology and hydrogeology, offsets model limitations by providing an alternative appraisal of susceptibility. Sea-water intrusion in the Pioneer Valley is not in equilibrium, and a potential exists for further landward shifts in the extent of saline groundwater. The model required consideration of tidal over-height (the additional hydraulic head at the coast produced by the action of tides), with over-height values in the range 0.5–0.9 m giving improved water-table predictions. The effect of the initial water-table condition dominated the sensitivity of the model to changes in the coastal hydraulic boundary condition. Several salination processes are probably occurring in the Pioneer Valley, rather than just simple landward sea-water advancement from “modern” sources of marine salts. The method of vertical discretisation (i.e. model-layer subdivision) was shown to introduce some errors in the prediction of water-table behaviour.
Résumé
L’intrusion de l’eau de mer est en train de contaminer activement les réserves d’eau souterraine potable dans les aquifères côtiers de la vallée de Pioneer au nord-est de l’Australie. Un modèle en trois dimensions de l’intrusion de l’eau de mer a était réalisé en utilisant le code MODHMS pour étudier les processus à l’échelle régionale et faciliter l’évaluation de stratégies de gestion du système. Une carte piézomètrique de l’intrusion de l’eau de mer, réalisée grâce à l’étude de l’hydrogéochimie, l’hydrologie et l’hydrogéologie, compense les limites du modèle en permettant une évaluation alternative de la vulnérabilité. L’intrusion de l’eau de mer dans la vallée de Pioneer n’est pas en équilibre et un potentiel existe pour des déplacements plus à l’intérieur des terres de l’étendue des eaux souterraines salées. Le modèle devait prendre en compte les surélévations dues aux marées (la charge hydraulique supplémentaire au niveau de la côte produite par l’action des marées), avec des valeurs de surélévations de l’ordre de 0.5–0.9 m entraînant de meilleures prédictions du niveau de la nappe. L’effet de l’état initial de la nappe était prédominant sur la sensibilité du modèle par rapport aux changements de la condition hydraulique aux limites au niveau de la côte. Plusieurs processus de salinisation doivent probablement avoir lieu dans la vallée de Pioneer et non pas uniquement une simple avancée d’eau de mer dans les terres à partir de sources “modernes” de sels marins. La méthode de la discrétisation verticale (subdivision en couches dans le modèle) s’est révélée être à l’origine d’erreurs dans la prédiction du comportement de la nappe.
Resumen
La intrusión de agua de mar está contaminando las reservas de agua subterráneas de agua dulce en los acuíferos costeños en Pioneer Valley, noreste de Australia. Se ha desarrollado un modelo tridimensional de intrusión de agua de mar mediante el uso de código MODHMS para explorar procesos de escala regional y para asistir la evaluación de estrategia para el manejo del sistema. Un mapa de potencial de intrusión de agua de mar, producido mediante el análisis de hidroquímica, hidrología e hidrogeología balancea las limitaciones del modelo al proporcionar una asesoría alternativa de susceptibilidad. En Pioneer Valley la intrusión de agua del mar no está en equilibrio y existe el potencial de movimiento en la extensión de agua subterranea salada desde el mar hacia la tierra. El modelo requirió considerar la carga hidráulica adicional en la costa producida por la acción de las mareas (sobre-altura de la marea), con una sobre-altura en el rango de 0.5–0.9 m, locual produjo mejores predicciones de la mesa de agua. El efecto de la condición inicial de la mesa de agua dominaba la sensitividad del modelo a cambios en la condición de límite hidráulico de la costa. Es probable que múltiples procesos de salinización estén ocurriendo en Pioneer Valley, en lugar de un avance simple de agua de mar hacia la tierra de fuentes “modernas” de sales marinas. Se observó que el método de discretización vertical (subdivisión de capas del modelo) introduce algunos errores en las predicciones de cambios en el comportamiento de la mesa de agua.
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Acknowledgements
The authors wish to gratefully acknowledge the Queensland Department of Natural Resources and Mines (NR&M) for providing funding for this project. The authors are thankful for technical assistance provided by NR&M Water Assessment staff and for the assistance with MODHMS given by Dr Sorab Panday. We also thank three anonymous reviewers for their helpful comments.
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Werner, A.D., Gallagher, M.R. Characterisation of sea-water intrusion in the Pioneer Valley, Australia using hydrochemistry and three-dimensional numerical modelling. Hydrogeol J 14, 1452–1469 (2006). https://doi.org/10.1007/s10040-006-0059-7
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DOI: https://doi.org/10.1007/s10040-006-0059-7