Abstract
The Permo-Triassic Sherwood Sandstone Group is an important aquifer with potential for both shallow and deep geothermal energy use in the UK. This study investigates the hydrogeological properties of the shallow buried Sherwood Sandstone Group in Northern Ireland, with a focus on its porosity, using borehole nuclear magnetic resonance (BNMR) and petrophysical models (Archie and Waxman-Smits). BNMR and downhole geophysical logging (resistivity, EC, temperature and natural gamma) were carried out on three boreholes drilled into the lower Sherwood Sandstone Group aquifer at depths of about 100 m on Queen's University Belfast campus. The results showed that the porosity calculated from BNMR and the Waxman-Smits model are comparable, demonstrating the relationship between BNMR and petrophysical-derived porosity. The average porosity of the Sherwood Sandstone Group at this location ranges between 14.9 % and 17.6 %, with maximum values ranging between 33.7 % and 40.4 %. However, the results from the Archie model are significantly larger than those of BNRM, confirming its unsuitability for lithologies containing clays, even in small amounts. This study confirms storage capacities in the lower Sherwood Sandstone Group that make it suitable for ATES systems.
| Original language | English |
|---|---|
| Pages (from-to) | 189-197 |
| Number of pages | 9 |
| Journal | Advances in Geosciences |
| Volume | 65 |
| DOIs | |
| Publication status | Published - 18 Mar 2025 |
Bibliographical note
The authors appreciate the technical assistance of the Geological Survey of Northern Ireland and Advanced Logic Technology (ALT) in providing access to WellCAD software. We also thank Joseph Ireland for assisting with the data collection and three anonymous reviewers who provided valuable comments.Data Availability Statement
Code and data availabilityThe BNMR and Petrophysical models porosity results are provided in the Supplement. The MATLAB code for visualising these data can be provided by the contact author upon request.
Supplement
The supplement related to this article is available online at https://doi.org/10.5194/adgeo-65-189-2025-supplement.
Funding
This research has been supported by the UK Research and Innovation through the Natural Environment Research Council (NERC) QUADRAT Doctoral Training Programme (DTP) (grant no. R1079NBE/40386285).
| Funders | Funder number |
|---|---|
| Natural Environment Research Council | R1079NBE/40386285 |