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Abstract: . . . of groundwater in the centre of Dublin as a means to reduce consumption of energy derived from the combustion of fossil fuels. ERA report to Dept. of Energy. 266pp. Balling, N., Kristiansen, Breiner, N., Poulsen, K. D., Rasmussen, R., Saxov, S. 1981. Geothermal Measurements & SuTimeout. This is only a partial webpage . . . . . . Winter eeting, Uppsala, p153. Ball, D. 1991. The investigation to determine the extent and usability of groundwater in the centre of Dublin as a means to reduce consumption of energy derived from the combustion of fossil fuels. ERA report to Dept. of Energy. 266pp. Balling, N., Kristiansen, Breiner, N., Poulsen, K. D., Rasmussen, R., Saxov, S. 1981. Geothermal Measurements & SuTimeout. This is only a partial webpage . . . . . . Investigations of the UK heat flow field (1984-1987).Investigation of Geothermal Potential of the U.K., British Geological Survey, Keyworth. 44pp. Goodman, R., Jones, G.Ll., Kelly, J., Slowey, E., O’Neill, N. 2004. Geothermal Energy Exploitation in Ireland – Review of Current Status and Proposals for Optimising Future Utilisation. CSA report 3085/02.04 for SEI, July 2004. 93pp + XII Appendices Mitchell, W. I., (ed) 2004. The Geology of Northern Ireland, Our Natural Foundation. Geological Survey of Northern . . . . . . 9-19. Allen, A., Milenic, D., Sikora, P. 2003. Utilisation of the urban ‘heat island’ effect on shallow gravel aquifers as a source of low enthalpy hydro-geothermal energy. European Geothermal Congress, Hungary, 2003. 8pp. Page 77 Geothermal Energy – Northern Ireland Report No. 3194/01.05 September 2005 73 Andreescu, M. Burst, D., Demetrescu, C., Ene, M., Polonic, G. 1989. On the geothermal regime of the Moesian Platform and Getic Depression. Tectonophysics, 164, Amsterdam, p281- 286. Bach, B., Péter, . . . . . . Allen, A., Milenic, D., Sikora, P. 2003. Utilisation of the urban ‘heat island’ effect on shallow gravel aquifers as a source of low enthalpy hydro-geothermal energy. European Geothermal Congress, Hungary, 2003. 8pp. Page 77 Geothermal Energy – Northern Ireland Report No. 3194/01.05 September 2005 73 Andreescu, M. Burst, D., Demetrescu, C., Ene, M., Polonic, G. 1989. On the geothermal regime of the Moesian Platform and Getic Depression. Tectonophysics, 164, Amsterdam, p281- 286. Bach, B., Péter, T. Quality . . . . . . at 500m which included both measured and data calculated from geothermal gradients at 300m. It was considered that there was good correlation between the two data sets, but that the latter data set gave more detail and therefore this was used as the final map for the 500m level. At 500m depth across Ireland, a number of hot-spots are present in the data namely in west Clare, northwest Cavan, Fermanagh, Antrim and east Tyrone where values range from 21ºC - 40ºC, with the highest values in the Larne . . . --3000,6,250,3190,188115
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