Abstract

Thermal energy from groundwater in abandoned, flooded, coal mines has the potential to make a significant contribution to decarbonization of heat and net-zero carbon emissions. In Glasgow, UK, a subsurface observatory has been constructed for mine water heat and heat storage research. We synthesize geological and mine water resource findings from a 4 year period of borehole planning, drilling, logging and testing. The heterogeneous bedrock is typical of the Scottish Coal Measures Group, whereas superficial deposits are more sand- and gravel-dominated than predicted. Mine water boreholes encountered workings in the Glasgow Upper, Glasgow Ell and Glasgow Main coal seams, proving water-filled voids, mine waste, fractured rock mass and intact coal pillars, with high yields on initial hydrogeological testing. Although the depth and extent of mine workings delineated on mine abandonment plans proved accurate, metre-scale variability was expected and proved in the boreholes. A mine water reservoir classification established from the observatory boreholes highlights the resource potential in areas of total extraction, stowage, and stoop and room workings. Because their spatial extent is more extensive across the UK than shafts or roadways, increasing the mine water energy evidence base and reducing exploration risk in these types of legacy workings is important. Supplementary material: Borehole reports and other datasets are available at https://ukgeos.ac.uk/data-downloads (mixture of over 20 DOI datasets and reports or data packs published openly on https://nora.nerc.ac.uk ; all material is deposited in the National Geoscience Data Centre).

Highlights

  • (e.g. HM Government 2018, 2020; Scottish Government 2020; CCC 2019) and whilst significant progress has been made in the decarbonisation of electricity (HM Government 2020), decarbonisation of heat presents a more difficult policy and implementation challenge (Abesser 2020; POSTNOTE 2020)

  • In 2019 48 GW of renewable electricity capacity was available in the UK representing 37 % of generation, whereas 90% of homes used fossil fuels for heating, cooking and hot water (HM Government 2020) with peak heat demand calculated at 170 GW

  • IPT Mine water reservoir classification R Borehole drilling at the Glasgow Observatory encountered a range of flooded mine workings from C open voids, loose and packed waste to fractured rock mass, that exert influence on the S hydrogeological properties and the recoverable mine water resource

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Summary

Discussion

IPT Mine water reservoir classification R Borehole drilling at the Glasgow Observatory encountered a range of flooded mine workings from C open voids, loose and packed waste to fractured rock mass, that exert influence on the S hydrogeological (hydraulic) properties and the recoverable mine water resource. E High yields were obtained from test pumping of a mining waste (stowage) reservoir classification C (Figure 10g) in GGA01 and with similar indications in GGA02 from an initial airlift during C construction These boreholes penetrate an area of total extraction area on the mine abandonment A plan, highlighting that depending on recharge and connectivity, there is resource potential in spatially extensive areas, away from shafts and roadways. If a room (void) or void and loosely packed waste R are encountered, make that the target interval for that borehole; C Areas marked on the mine abandonment plan as ‘total extraction’ penetrated a large S number of mine water reservoir classifications (open void, waste, fractured rock, clean collapse). Surface-based geophysical survey techniques may offer useful insights (e.g. microgravity, electromagnetic, magnetic, electrical resistivity tomography or ground penetrating radar surveys in Dennehy et al 2019), these were not utilised predrill in the Glasgow Observatory due to the building rubble and foundations in the thick made ground and 30 – 40 m thick superficial deposits

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