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                    <gco:CharacterString>Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services</gco:CharacterString>
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            <gco:CharacterString>The theoretical potential 'recoverable heat' (Hrec) in the Upper Devonian formations in the Midland Valley of Scotland was calculated as part of a first regional-scale estimate of the deep geothermal potential of hot sedimentary aquifers in Scotland. The study considers the Kinnesswood Formation and Stratheden Group as the main target units, and includes the construction of an updated 3D geological model of depth and thickness. The theoretical potential 'recoverable heat' (Hrec) provides an estimate of the fraction of the 'heat-in-place' (HIP) that can be produced as thermal power (in kilowatts). It was calculated using the 3DHIP tool (Piris et al., 2021), which is based on the USGS volumetric HIP method developed by Muffler and Cataldi (1978). The values are theoretical due to lack of operational data for the UK. The method uses a Monte Carlo simulation to calculate the P50 probability distribution function for the Hrec based on the P50 distribution of the HIP derived from the 3D geological model, gridded at an XYZ spatial resolution of 500 x 500 x 50 m. Hrec was calculated assuming a recovery factor (R) of 0.1, a plant factor (Pf) of 0.95 (proportion of time a plant is likely to be operating), a geothermal project lifetime (Tlive) of 30 years, and a heat exchanger conversion factor of 0.85. The recoverable heat highly depends on the thickness of the aquifer, which is poorly constrained in some areas. Recovering the heat from the whole thickness of the aquifer is not likely to be technically possible, so these values are high, theoretical estimates.</gco:CharacterString>
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