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Geothermal energy resources in ireland PGCert Geothermal Energy Technology University of Auckland Julian McDowell
Disclaimer The following presentation represents the views and opinions of the author. Reproduction of the slides and views within the presentation is not permitted without permission from the author. All information and data presented has been approved for use in the public domain. References can be provided upon request.
contents ,[object Object]
Geothermal setting
Shallow geothermal exploitation
Deep geothermal exploration
GT Energy – Newcastle, Dublin
Future Development,[object Object]
NE/SW fault trend
Extensive folding and faulting – Caledonian Orogeny
Magmatic Intrusions/Eruptions	- Granites – Devonian,400mya 	- Basalts – Cretaceous, 60mya ,[object Object]
Recent glaciations,[object Object]
Geothermal setting ,[object Object]
Shallow Geothermal:	-High potential for GSHP 	- temperate climate 	- high conductivities 	- 20MWth (WGC,2005) 	- 2009: 100MWth+ 	- shallow aquifers –urban  heat   	island ,[object Object],	- not on active plate boundary 	- no activity in last 60mya 	- average gradient 25-30◦C/km
Shallow Geothermal Resource Map Geothermal Resource Map of Ireland (CSA, SEI 2004):
Shallow geothermal Case study ,[object Object]
Palaeo-channel gravel aquifer,[object Object]
Lewis Gluckman Gallery (Arup, 2006)
Lewis Gluckman Gallery ,[object Object],- Cost saving against conventional cooling and heating : €12,000 (NZD$25,000) 	- Payback period : 14.6 years 	- CO2 emission reduction : 256t/year 	- Closely controlled temperature and humidity 	- Award winning design – architectural and environmental awards
Deep geothermal gradient Geothermal Resource Map of Ireland (CSA, SEI 2004): ,[object Object],Deep Geothermal Conclusions: ,[object Object]
Geothermal gradients : max.70-90oC at 2500m				max. 150C+ at 5000m ,[object Object]
Abundance of deep penetrating more recent faults and fractures in the South of Ireland results continuous leaking of heat to the surface – poor geothermal gradients
Carboniferous rocks act as good insulators of geothermal heat where fracturing is absent,[object Object]

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Geothermal energy resources in Ireland overview

Hinweis der Redaktion

  1. at the Causeway it eventually accumulated as a large lava lake in the bend of a river. With a depth of 90m, this lake was slow to cool. The lava in contact with the cold rock below quickly chilled and solidified, forming irregular miniature columns a few centimetres across. This base became an effective insulating layer and allowed the great homogeneous mass of the lava lake to cool slowly and evenly, developing regular stress patterns as it solidified. As contraction continued these patterns were expressed as evenly spaced cooling cracks that permeated the entire solidifying mass, creating thousands of mainly six-sided columns, about 30-40cm across