Hydraulic conclusions from chemical considerations: groundwater in sedimentary environments in the central part of the Pannonian Basin, Hungary

Varsányi, Irén; Kovács, Lajos Ó; Balint, Andras

Hydraulic conclusions from chemical considerations: groundwater in sedimentary environments in the central part of the Pannonian Basin, Hungary | Conclusions hydrauliques à partir de considérations chimiques: les eaux souterraines d’environnements sédimentaires de la partie centrale du Bassin Pannonien, Hongrie Conclusiones hidráulicas a partir de consideraciones hidroquímicas: el agua subterránea en ambientes sedimentarios en la parte central de la Cuenca de Pannonian, Hungría 从化学角度得出的水力结论:匈牙利Pannonian流域中部沉积环境中的地下水 Hidraulikai következtetések kémiai megfontolások alapján: felszínalatti vizek üledékes környezetben (Pannon-medence középső része, Magyarország) Conclusões hidráulicas a partir de considerações químicas: água subterrânea em ambientes sedimentares na parte central da Bacia Panoniana, Hungria

2015

Varsányi, Irén | Kovács, Lajos Ó | Balint, Andras

Hydro-chemical and isotopic data from different aquifers in the Great Hungarian Plain (the central part of the Pannonian Basin) were evaluated down to a depth of 2,740 m. The chemical and isotopic composition of water is influenced by its origin and by chemical and mixing processes. The analytical data and chemical considerations, together with geology, pressure conditions and evolution history of the area, explain the evolution of the subsurface water. Most of the samples are of meteoric origin, but there were some samples with a non-meteoric contribution, as indicated by the water stable isotopes, and these were identified as seawater trapped during the sedimentation in Lake Pannon. The sea contribution is traceable by the shifts in δ¹⁸O and δ²H and the chemical composition of the water, and is explained with an upward-driving force. Chemical considerations and spatial variability of the dissolved components suggest that distinct water bodies, each with a specific origin and chemical evolution, can be separately identified. Although in the Quaternary layers there are water bodies that can be considered to display complete flow systems (from recharge to discharge), in most water bodies present infiltration was not identified. The lack of recent recharge to several water bodies in various places and depths suggests a separation of the recharge and the discharge that occurred not in space, but in time. A possible explanation of the cessation of recharge is a significant change in the hydraulic circumstances, probably the surface elevation.

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