Legacy BGS geothermal models: temperature at the base of the Upper Devonian Kinnesswood Formation and Stratheden Group (hot sedimentary aquifer resources) in the Midland Valley of Scotland

This raster dataset provides the maximum temperature in the Upper Devonian formations in the Midland Valley of Scotland. The reservoir temperature is modelled over the extent of the base of the Kinnesswood Formation and Stratheden Group, based on an updated geological model created by Kearsey, T.I., Receveur, M. and Monaghan, A.A., 2024. Modelled hot sedimentary aquifer geothermal potential of Upper Devonian strata in the Midland Valley of Scotland. The model is presented with high uncertainty.

Date (Publication): 2024

Citation identifier: http://data.bgs.ac.uk/id/dataHolding/13608363

Point of contact

Organisation name	Individual name	Electronic mail address	Role
British Geological Survey	Enquiries	enquiries@bgs.ac.uk	Distributor
British Geological Survey	Enquiries	enquiries@bgs.ac.uk	Point of contact

Maintenance and update frequency: Not planned

GEMET - INSPIRE themes, version 1.0

Geology

BGS Thesaurus of Geosciences

UK Location (INSPIRE)
Devonian
Aquifers
Geothermal energy
Sandstone reservoirs
Temperature

dataCentre

UK Location (INSPIRE)

Keywords

NERC_DDC

Access constraints: Other restrictions

Other constraints: Access constraints: no limitations.

Use constraints: License

Other constraints: Use constraints: this dataset is available to view under the Open Government Licence V3 ( https://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/) to encourage its use and re-use, subject to the following acknowledgement accompanying the reproduced BGS materials: 'Contains British Geological Survey materials © UKRI [year]'. Some of the data shown in the BGS view-only service layers are available to licence. The licence cost will generally be a licence administration fee, depending on the usage type and the area coverage of the dataset requested. Companies and other commercial organisations with an interest in reselling BGS data or developing value-added products and services based on BGS data will need a BGS data resellers licence. For more information, contact digitaldata@bgs.ac.uk.

Spatial representation type: Grid

Distance: 500 urn:ogc:def:uom:EPSG::9001

Language: English

Topic category

Geoscientific information

Geographic identifier: CENTRAL REGION (SCOTLAND) [id=147300]
British Geological Survey Gazetteer: Geographical hierarchy from Geosaurus 1979

Geographic identifier: Midland Valley Basin [id=1000334]
British Geological Survey Gazetteer: Geological gazetteer 2005

Begin date: 2024

End date: 2025

Unique resource identifier: OSGB 1936 / British National Grid (EPSG::27700)

Distribution format

Name	Version

Distributor contact

Organisation name	Individual name	Electronic mail address	Role
British Geological Survey	Enquiries	enquiries@bgs.ac.uk	Distributor

OnLine resource

Protocol	Linkage	Name
WWW:LINK-1.0-http--link	https://ukgtp.bgs.ac.uk	UK Geothermal Platform Web Map

OnLine resource

Protocol	Linkage	Name
WWW:LINK-1.0-http--link	https://ukgeothermalplatform.org	UK Geothermal Platform

Hierarchy level: Dataset

Other: dataset

Conformance result

Title: INSPIRE Implementing rules laying down technical arrangements for the interoperability and harmonisation of Geology

Date (Publication): 2011

Explanation: See the referenced specification

Pass: No

Conformance result

Title: 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

Date (Publication): 2010-12-08

Explanation: See http://eur-lex.europa.eu/LexUriServ/LexUriServ.do?uri=OJ:L:2010:323:0011:0102:EN:PDF

Pass: No

Statement: The potential geothermal energy source in the Midland Valley of Scotland was calculated as part of a first regional-scale estimate of the heat-in-place for the hot sedimentary aquifer in Scotland. The study considers the Kinnesswood Formation and Stratheden Group as the main target units (Upper Devonian in age) and includes the construction of an updated 3D geological model of depth and thickness, as well as values and assumptions used for the potential geothermal energy source estimation. The average geothermal gradient for the Upper Devonian units was calculated using a compilation of data from 79 boreholes, including temperature logs from deep hydrocarbon and coal-bed methane wells not included in previous analyses, long-term test reports, the UK Geothermal Catalogue (Burley et al. 1984; Rollin 1987), BGS reports (Browne et al., 1985), the UK Geoenergy Observatories boreholes (Monaghan et al. 2017), the Glenrothes geological well completion report and hard-copy logs of borehole temperatures. Newer LOG and BHT temperature data were corrected for the time since circulation. The maximum temperature (at the base Upper Devonian) was calculated based on the updated geological model, using the calculated geothermal gradient of 26.6 °C and assuming an average surface temperature of 8 °C.