DBPapers
DOI: 10.5593/SGEM2014/B12/S2.128

UPDATE ON STATIONARY TEMPERATURE MODEL ON CARBONATES DOMINATED, STRATIFIED, LOW ENTHALPY HYDROGEOTHERMAL SYSTEM OF THE BESENOVA ELEVATION, N. SLOVAKIA

B. Fricovsky, L. Tometz, L. Vizi, J. Stiakova
Wednesday 1 October 2014 by Libadmin2014

References: 14th International Multidisciplinary Scientific GeoConference SGEM 2014, www.sgem.org, SGEM2014 Conference Proceedings, ISBN 978-619-7105-08-7 / ISSN 1314-2704, June 19-25, 2014, Book 1, Vol. 2, 1003-1010 pp

ABSTRACT
The Bešeňová elevation is exploited since 1979, however, modeling of geothermal field modeling aimed at vertical distribution of geothermic settings only. Here, deep reservoir temperatures are used to calculate overheating- a controlling factor on reservoir convection onset. Even in neither region of the system the critical condition of Ra > Rc and Nu > Nc is reached, implementation of tolerance (δRa < 3 and δNu < 0,03) points on minor convection onset possibility in the central, production zone.

Keywords: Bešeňová elevation, heat flux, overheating, reservoir temperature