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| Content Provider | Springer Nature Link |
|---|---|
| Author | Reylds, D. A. Marimuthu, S. |
| Copyright Year | 2006 |
| Abstract | A conceptual model of the Lake Warden coastal wetlands system, Western Australia, was developed using hydraulic, chemical and stable isotopic data, and formed the basis for a groundwater flow model using the finite element numerical code (FEFLOW). The system to be modeled is complex. The surface water and groundwater within the wetlands system show varying salinity and isotopic composition over short distances and time frames. As a first step, the flow model was calibrated to observed groundwater levels measured since 2001 for both steady state and transient stresses. Particle tracking analysis was conducted to test the source areas of water discharging to the lakes within the wetlands system. The analysis was able to delineate the connectivity between the lakes in the wetland and the flow path. Enrichment of isotopic concentration is evident along a NE–SW transect and the data set provides a means for calibrating a detailed transport model. The study incorporates the varying deuterium composition of the water bodies directly into a transport model and a good match between observed and simulated temporal variations along the transect indicates that the model closely simulated the dynamics of water exchange between the lakes and groundwater within the system.Un modèle conceptuel du système Lac Warden, marécage côtier situé dans l’Ouest de l’Australie, a été réalisé à partir de données hydrauliques et chimiques dont les isotopes stables. Il a été utilisé comme base pour un modèle d’écoulement souterrain, réalisé avec un code numérique aux éléments finis (FEFLOW). Le système à modéliser est complexe. Dans le marécage, la salinité et la composition isotopique de l’eau de surface et de l’eau souterraine varient sur des distances et des pas de temps courts. Le modèle hydrogéologique a tout d’abord été calibré en régimes permanent et transitoire à partir des niveaux piézomètriques mesurés depuis 2001. Un suivi de trajectoire de particules, réalisé pour vérifier les zones de décharge des eaux souterraines dans les lacs du système marécageux, a permis d’identifier les connexions entre les lacs et de tracer les trajectoires d’écoulement. Une augmentation de la concentration isotopique le long d’une coupe transversale NE–SW est évidente et les données constituent un support pour la calibration d’un modèle de transport détaillé. La variation de la composition en deutérium dans les hydrosystèmes est prise en compte dans l’étude et directement intégrée dans le modèle de transport. Une bonne adéquation entre les variations temporelles simulées et observées le long de la coupe transversale indique que la dynamique des échanges d’eau entre les lacs et l’eau souterraine dans ce système a été assez bien simulée par le modèle.Se ha desarrollado un modelo conceptual del sistema de humedales costero del Lago Warden en el Occidente de Australia usando datos hidráulicos, químicos, y de isótopos estables el cual sirvió de base para un modelo de flujo de agua subterránea que usa el código numérico de elemento finito (FEFLOW). El sistema para el cual se elabora el modelo es complejo. El agua subterránea y superficial dentro del sistema de humedales muestra salinidad y composición isotópica variable en distancias y marcos de tiempo cortos. Como primer paso se calibró el modelo de flujo con niveles de agua subterránea medidos desde el año 2001 para regimenes permanentes y transitorios. Se llevó a cabo un análisis de búsqueda de partículas para evaluar las áreas fuente del agua que descarga a los lagos dentro del sistema de humedales. El análisis permitió delimitar la conectividad entre los lagos en el humedal y la trayectoria de flujo. El enriquecimiento de la concentración isotópica es evidente a lo largo de un levantamiento NE–SW y el grupo de datos aporta medios para calibrar un modelo detallado de transporte. El estudio incorpora la variación en composición de deuterio de los cuerpos de agua directamente en un modelo de transporte y una buena consistencia entre variaciones temporales, simuladas y observadas, a lo largo del levantamiento indican que el modelo simuló bastante bien la dinámica de intercambio de agua entre los lagos y el agua subterránea dentro del sistema. |
| Starting Page | 515 |
| Ending Page | 535 |
| Page Count | 21 |
| File Format | |
| ISSN | 14312174 |
| Journal | Hydrogeology Journal |
| Volume Number | 15 |
| Issue Number | 3 |
| e-ISSN | 14350157 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2006-11-14 |
| Publisher Institution | International Association of Hydrogeologists |
| Publisher Place | Berlin, Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Conceptual model Groundwater flow Coastal wetlands system FEFLOW Deuterium composition Waste Water Technology Water Pollution Control Water Management Aquatic Pollution Geology Hydrogeology |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth and Planetary Sciences Water Science and Technology |
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