SIMULATION OF THE GEOTHERMAL RESERVOIR OF THERMA - NIGRITA, CENTRAL MACEDONIA, GREECE


Published: Jul 27, 2016
Keywords:
3D modelling low enthalpy geothermal filed management FEFLOW
K. Kavouri
A. Arvanitis
C. Athanassoulis
M. Xenakis
Abstract

The geothermal field of Therma - Nigrita is among the most important low enthalpy fields in Greece. It is located at the SW part of the Strymon basin (Central Macedonia). The geothermal research at Nigrita was launched by IGME during 1980- 1982. Actually, it is exploited mainly for agricultural use and thermal spa. The geothermal field of Therma - Nigrita, officially characterized by Ministerial Decision, covers an area of 10 km², has a pressurized reservoir at 70-500 m depth, showing temperatures of 40-64°C and geothermal fluids containing large amounts of CO2. In this paper the development of a 3D model for the reservoir of Therma - Nigrita, is presented. For this purpose the FEFLOW code is employed which simulates fluid flow and heat transfer in the geothermal reservoir under transient state conditions. Following, three different management scenarios are tested for a ten-year period. The first scenario examines the evolution of the reservoir under no-exploitation conditions, the second one represents the current exploitation scheme and in the third scenario the production rates are doubled. According to the simulation results, the decrease in temperature is not expected greater than 1% for all scenarios, while the effect on hydraulic heads is significant for both scenarios 2 and 3.

Article Details
  • Section
  • Engineering Geology, Hydrogeology, Urban Geology
Downloads
Download data is not yet available.
References
Andritsos, N., Dalabakis, P., Karydakis, G., Kolios, N. and Fytikas, M., 2007. Update and
Characteristics of Low-Enthalpy Geothermal Applications in Greece, Proc. of the European
Geothermal Congress 2007, Unterhaching, Germany.
Arvanitis, A., Fytikas, M. and Dotsika, E., 1998. Geothermal conditions in Therma - Nigrita area
(Strymon basin, Northern Greece), Bull. Geol. Soc. Greece, XXXII/4, 229-242.
Bridger, D.W. and Allen, D.M., 2014. Influence of geologic layering on heat transport and storage
in an aquifer thermal energy storage system, Hydrogeology Journal, 22, 233-250.
Diersch, H.-J., 2014. FEFLOW. Finite Element Modeling of Flow, Mass and Heat Transport in
Porous and Fractured Media. Springer 2014 Springer-Verlag Berlin Heidelberg.
Dotsika, E., 1991. Utilisation du geothermometre isotopique sulfate-eau en milieux de haute
temperature sous influence marine potentielle: les systemes geothermaux de Grece, These en
Science, Univ. Paris-Sud, 184 pp.
Goldstein, B., Hiriart, G. and Tester, J., 2011. Great expectations for geothermal energy to 2100:
messages for now, GRCTrans, 35, 1175-1183
Karydakis, G., 1983. Study of the low enthalpy geothermal field in Therma - Nigrita area. Report
I.G.M.E., Athens, 46 pp.
Karydakis G., 2001. Geothermal exploration at the area Therma - Nigrita, Report I.G.M.E., Athens,
pp.
Karydakis, G., Arvanitis, A., Andritsos, N. and Fytikas, M., 2005. Low Enthalpy Geothermal Fields
in the Strymon basin (Northern Greece), Proc. of the World Geothermal Congress 2005,
Antalya, Turkey, 24-29 April, IGA & TGA, Paper Number 2615, 12 pp.
Lopez, S., Hamm, V. and LeBrun, M., 2010. 40years of Dogger aquifer management in Ile-de-
France, Paris Basin, France, Geothermics, 39, 339-356.
Most read articles by the same author(s)