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By Otto Rentz, Dominik Most, Anke Eber

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The tertiary subsidence of the basin led to a new sedimentary period. A new Miocene time emersion was followed by an alluvial filling. In the Rhine Graben, three aquifers are likely to provide sufficiently hot water to produce electricity. They are from the bottom up (Figure 1): The Buntsandstein (lower Triassic), made of sandstone interfilled with clay. The Muschelkalk (mid Triassic), composed of clayey and sandy limestones and dolomites. The 'Grande Oolithe' (Bajocian and Bathonian), made of oolithic limestones, clayey at the base.

G. in dena, 2005), which have to be taken care of: More extreme load situations are faced in the grid, necessitating grid extensions. e. more reserve capacities are needed. The less predictable residual load curve requires more frequent start-up procedures of conventional power stations and causes a decreasing efficiency due to more frequent partial load operation (higher specific fuel consumption) and due to the increasing provision of balancing power necessary. Average production costs in the conventional plant portfolio rise (passed on to consumers as rising prices on the competitive market) as workload decreases due to the required higher flexibility of power plants and the necessary reserve capacities.

Potential of Deep Aquifers for Geothermal Electricity Production in Alsace 29 The described methodology was implemented in an ArcGIS-based application, with options to be translated and adapted to other areas and other data sources : the study presented here is now being extended to the other suitable French regions. In order to evaluate more precisely the relevance of geothermics in France, other aspects have to be taken into account. In particular, the final cost of electricity is a criterion that can not be ignored : the total costs and the internal energy demand of a geothermal plant have then to be evaluated more precisely.

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