Abstract
Lowering of the piezometric-head due to pumping to protect mines from water-inrushes can create an extensive cone of depression. As a result of this, the directions of ground water flow in the surrounding aquifers can be changed, which can be sensitively indicated by the changes in water-temperature. In the bauxite deposits of Hungary the regular temperature measurements in the piezometric boreholes and observation wells, makes it possible to monitor, in combination with other methods, the hydrological structure of the surrounding rock mass.
Similar content being viewed by others
References
Devenyi P. et al. (1983), Geothermal Conditions of Hungary, Geophysical Transactions, MAELGI, Budapest, Vol. 29, No. 1, pp. 19–30.
L. Alfoldi, T. Bocker and A. Lorberer (1977), ‘Hydrogeological Characteristics of the Hungarian Carbonate Fissured Warm Water Reservoirs’, Magyarorszag Heviz Kutjai III, Vituki, Budapest, pp 17–28.
L. Bodry (1981), ‘Geothermal Model of the Earth's Crust in the Pannonian Basin Technophysics 72, pp 61–73
Juhasz, J (1977), ‘Hydrogeology’, Akademiai kiodo, Budapest
L. Stegena (1987), ‘Praktische Geothermische Untersuchungen in Ungarn’, Annales Univ. Sci. Budapestiensis de L. Eotovos Nom, Sectio Geol., 1, pp 79–87.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Hegedus-Koncz, M., Nandori, G. & Gaspar, L. Hydrogeological and geothermal changes in karstic reservoirs due to mine dewatering. Mine Water and the Environment 11, 45–54 (1992). https://doi.org/10.1007/BF02919581
Issue Date:
DOI: https://doi.org/10.1007/BF02919581