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ERE5.4

EDI
Underground Thermal Energy Storage, applications and associated processes in porous and fractured aquifers

Thermal, hydraulic and mechanical processes in aquifers are of increasing interest for hydrogeological analysis for development of innovative field and laboratory experiments. Both in research and in practice, accurate characterization of subsurface flow and heat transport, observations of induced or natural variations of the thermal regime. The seasonal and long-term development of thermal and mechanical conditions in aquifers, and heat transfer across aquifer boundaries are focus points. This also includes the role of groundwater in the context of geothermal energy use for predicting the long-term performance of geothermal systems (storage and production of heat), and integration in urban planning. There are many ongoing research projects studying heat as a natural or anthropogenic tracer, and which try to improve thermal response testing in aquifers. Such techniques are of great potential for characterizing aquifers, flow conditions, and crucial transport processes, such as mechanical dispersion. Understanding the interaction of hydraulic, thermal and mechanical processes is a major challenge in modern hydrogeology. Deep underground constructions, tunnels, CO2 storage, hydro- and enhanced geothermal applications are prominent subjects. We invite contributions that deliver new insight into advances in experimental design, reports from new field observations, as well as demonstration of sequential or coupled modeling concepts. The session aims to provide an overview of the current and future research in the field, covering any temporal or spatial scale, and seeks to address both separate and coupled processes.

Thermal Energy Storage is a key component for an efficient and low-carbon energy balance. TES allows a flexibility of storage volume and storage time, and represents a cross-sector technology. As it is coupling heat, cooling energy, and electricity, which still belong in most cases to completely different market sectors, there is currently a marginal integration among the operators.
The aim of this session is to increase the understanding on how the existing gap on efficiency issues (energy balance and losses), social acceptance, and how to best adress the technical obstacles concerning the Underground Thermal Energy Storage (UTES) technologies themselves (high complexity of geological configurations forcing different approaches to the issue) or how to integrate renewable energy sources (e.g. geothermal, solar, thermal, …) with UTES technologies .

Convener: Martin Bloemendal | Co-conveners: Bastian WelschECSECS, Peter Bayer, Kathrin Menberg, Claire BossennecECSECS, Stijn BeerninkECSECS
Presentations
| Mon, 23 May, 15:55–18:20 (CEST)
 
Room -2.31

Mon, 23 May, 15:10–16:40

Chairpersons: Peter Bayer, Claire Bossennec

15:55–16:05
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EGU22-4198
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ECS
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solicited
Lukas Seib et al.

Geothermal energy and thermal energy storages can significantly reduce the consumption of fossil energy resources by storing large amounts of heat in the subsurface, which is especially valuable when dealing with fluctuating renewable energy sources. Crystalline rocks with low hydraulic conductivity are a suitable target for such storage systems due to reduced convective heat losses. In the frame of the research project SKEWS (Seasonal Crystalline Borehole Thermal Energy Storage), a medium deep borehole thermal energy storage demonstrator with four 750 m deep borehole heat exchangers will be built at the Technical University of Darmstadt, Germany. In the preparation phase of this project, an extensive geophysical, petrophysical and structural dataset is gathered for the characterization of the project site’s subsurface.

This multi-disciplinary dataset is used for the creation of a first-order finite element method (FEM) model of the storage reservoir for thermo-hydraulic modelling. The input data includes a large petrophysical dataset for crystalline rocks and a stress-dependent Discrete Fracture Network (DFN) for the hydraulic characterization of the fractured granodioritic basement rock. For numerical analysis of the storage operation cycles, a novel co-simulation approach, using the FEM suite FEFLOW and the Modelica library MoSDH, is used to consider the interconnection between the subsurface heat-exchangers and the surface heating grid. This approach allows for detailed FEM modelling of the subsurface, while being able to take the complexity of the surface heating network into account at the same time. The model will be updated continuously by additional data during the building process of the pilot and the following experiments, to generate a highly detailed and validated numerical model of a heat storage system in a granodioritic reservoir. Ultimately, the presented workflow can serve for the accurate prediction of the performance of upscaled systems and therefore support a well-founded design process of this novel storage technology.

How to cite: Seib, L., Bossennec, C., Julian, F., Bastian, W., Frey, M., and Sass, I.: Numerical modeling of a granodioritic MD-BTES test-site, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-4198, https://doi.org/10.5194/egusphere-egu22-4198, 2022.

16:05–16:10
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EGU22-9581
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ECS
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Highlight
Stijn Beernink et al.

To reduce worldwide greenhouse gas (GHG) emissions, fossil fuels are being replaced by renewable energy in a rapid tempo. As a result, the energy system becomes more decentralized with e.g. PV systems as a source for local multi-energy systems, with aim to become as self-sustainable as possible. This is challenging because these systems often rely on an intermittent energy source (production mainly in summer), which is not aligned with energy demand (mainly in winter). One solution for this problem is the combination of power-to-heat (PtH) with High Temperature Aquifer Thermal Energy Storage (HT-ATES), which allows for flexible and effective utilisation and storage of available green electricity to match the availability and demand of sustainable electricity. Currently, insights in the practical potential of this solution and methods for effective integration of PtH and HT-ATES in multi-energy systems are lacking. Therefore, we assessed methods to improve the integration and control of a HT-ATES system and tested varying ways of integration for a local decentralized multi-energy system. To this end, we expanded and integrated a multi-energy system model with a numerical hydro-thermal model to dynamically simulate the functioning of the integrated HT-ATES. The impact of key design parameters (heat pump size, storage temperature, cut-off temperature) on overall energy performance and the effect of different methods for integration of the local energy system were simulated and analysed. 

Results show that the integration of HT-ATES with PtH allows for providing the local energy system with 100% of the yearly heat demand with a 25% smaller heat pump than without HT-ATES. Also, compared to Pth without storage, the yearly energy use pattern changes dramatically to match the availability of renewable electricity. An inventive mode of operation was designed which allows for lowering the threshold temperature of the HT-ATES by an innovative integration of the heat pump. This mode of operation increases the HT-ATES performance and decreases the overall costs of heat production. Overall, this study shows that the integration of HT-ATES in a multi-energy system is suitable to cost-effectively match annual heat demand and supply, and to increase local sustainable energy use. Solutions like these show high potential to decentralize energy production/use, to decrease pressure on the power grid and to increase total renewable energy use.

How to cite: Beernink, S., van der Roest, E., van der Hoek, J. P., Hartog, N., and Bloemendal, M.: High Temperature ATES in combination with power-to-heat: maximizing renewable energy use for a local energy system, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9581, https://doi.org/10.5194/egusphere-egu22-9581, 2022.

16:10–16:15
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EGU22-12564
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ECS
Stefan Heldt and Sebastian Bauer

High temperature Aquifer Thermal Energy Storage (HT-ATES) is one option to compensate for the seasonal mismatch between supply and demand in a renewable dominated heating sector. The thermal impacts to be expected by a planned HT-ATES plant can be predicted by numerical modelling, which is necessary for the development of monitoring concepts, legal authorization and economical assessments. One aspect of numerical pre-investigations, which was mostly disregarded by previous studies, is the assessment of thermal impacts in layers above the storage formation, which are heated conductively by the warm well. Furthermore, a quantification of the related heat losses and the implications on storage efficiency need to be considered.

The thermohydraulic processes induced by the HT-ATES are numerically simulated by a radially symmetric model neglecting ambient groundwater flow. The model includes the discretised warm ATES well, which reaches to a depth of ≈250 m and the surrounding geological layers. The geology and the operational scheme are based on a typical setting representative for northern Germany. The simplified operational scheme consists of half a year injection and half a year extraction, repeated for 50 years, with an injection temperature of 85 °C, varying return flow temperatures and an initial subsurface temperature of 13 °C. The thermal properties of the well casing are varied in a sensitivity study to estimate the influence of different material choices.

The model results show, that a temperature increase of 5 °C propagates 7 m radially in cohesive layers around the well in the first year of operation. After 50 years, temperature increases of 5 °C or more are found within a distance of about 40 m, 30 °C within about 13 m and 50 °C within about 2 m. Density-driven buoyancy flow is observed in cohesionless layers, leading to heat accumulation near the top of these layers. The heat consequently propagates significantly further there than in the cohesive formations, e.g. a temperature increase of 5 °C propagates maximally 121 m from the well in 50 years. The conductive heat loss to the overlaying formations through the well casing is 2 % of the injected heat. The such derived estimation of thermal impacts in overlaying formations is conservative, since ambient groundwater flow is neglected, which would result in lower temperatures due to advective heat transport away from the well. The heat loss, however, would be larger with groundwater flow, since this would reduce temperatures around the well and thus increase the temperature gradients and the conductive heat transport. Material choices of the well material may increase or decrease the heat losses and thus the thermal impacts.

How to cite: Heldt, S. and Bauer, S.: Thermal Impact of High Temperature Aquifer Thermal Energy Storage on Overlying Layers, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-12564, https://doi.org/10.5194/egusphere-egu22-12564, 2022.

16:15–16:20
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EGU22-856
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ECS
Christoph Bott and Peter Bayer

Efficient thermal energy storage concepts are key for achieving the ambitious international climate targets. Implemented in thermal energy networks with a high contribution made by volatile renewable energy sources, large-scale applications for sensible heat and cold storage are favourable. They compensate for short-term fluctuations in the energy demand profiles, and they enable solar energy harvested in summer to be recovered for use in winter. Especially when pre-existing infrastructure facilities (e.g., basin installations from disused industrial, water treatment, and stormwater retention facilities) are reused as framework structures for thermal energy storage devices, environmental boundary conditions are often adverse. This is, for example, due to interference with near-subsurface aquifers or due to a suboptimal geometry of the given storage structure. For identifying strengths and weaknesses of a storage facility, and for technological optimization, simulation of thermal processes is vital. By this, the role of subsurface heterogeneity and slowly evolving transient thermal conditions in the storage device as well as in the ambient ground can be analysed. Thus, different degrees of utilisation, potential lateral energy losses or gains, and ultimately the economic viabilities of potential solutions can be evaluated. Most of the existing modelling applications do not address these issues in full detail. In fact, previous studies revealed that originally predicted efficiencies and amortization periods are often not achieved. This can be attributed to insufficiently represented boundary conditions (e.g., steady and uniform ambient temperatures at all exterior storage interfaces) or to rigorous simplifications by symmetric modelling techniques (no possibility to implement asymmetric processes, e.g., groundwater flow in surrounding subsurface).

In our study, we use a new numerical model to represent hydrogeological processes around ground-based thermal storage devices at high resolution and in different respects. In a series of generic scenarios, we focus on fundamental parameters of groundwater and environmental conditions, such as different groundwater levels and flow velocities, and we inspect the influence of various thermophysical (thermal conductivity/storage capacity) and hydraulic material parameters (e.g., porosity, permeability). With these, we analyse effects on storage utilisation rates, thermal losses, and temperature conditions in the surrounding area. Finally, we provide insight into previously neglected influencing factors and offer improvement strategies for the planning and implementation of large-scale, closed, seasonal thermal energy storage systems.

How to cite: Bott, C. and Bayer, P.: Modelling environmental interactions of large-scale, closed seasonal thermal energy storage systems, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-856, https://doi.org/10.5194/egusphere-egu22-856, 2022.

16:20–16:25
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EGU22-6763
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ECS
Ji-Young Baek et al.

Tracer experiments have been carried out for various scales to enhance the understanding of transport processes in porous media. The comparison between multi-tracers behaviors could provide insights in using tracers for the aquifer characterization. Especially, the comparison of heat and solute transports has been drawing attention in recent studies based on the similarity of governing equations. However, the difference between influences of particle sizes on heat and solute transport processes has yet to be clarified. In this study, to investigate the impacts of mean grain size (d50) difference on solute and heat transports, laboratory heat, and solute tracer experiments were conducted using two grain sizes of sand (d50 = 0.50, and 0.76 mm). Obtained experimental data were analyzed by mathematical models and those results were compared at 7 different flow conditions for two different mean grain sizes. Compared to other experimental data conducted with various particle sizes, normalized thermal dispersion coefficients showed a wider range of values to the different particle sizes under the same Pèclet number than normalized solute dispersion coefficients, even though the heat transport occurred in smaller Pèclet numbers. These results could indicate that the influence of particle size difference could be more critical in thermal dispersion coefficients.

Acknowledgements

This work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIP) (No. 2017R1A2B3002119). This work was also supported by Korea Environment Industry & Technology Institute(KEITI) through "Activation of remediation technologies by application of multiple tracing techniques for remediation of groundwater in fractured rocks" funded by Korea Ministry of Environment (MOE)(Grant number:20210024800002/1485017890). This work was also supported by the Institute for Korea Spent Nuclear Fuel (iKSNF) and National Research Foundation of Korea (NRF) grant funded by the Korean government (Ministry of Science and ICT, MSIT) (Grant number: 2021M2E1A1085200).

 

How to cite: Baek, J.-Y., Park, B.-H., and Lee, K.-K.: Influence of Particle Sizes on Solute and Heat Transport Interpretation, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-6763, https://doi.org/10.5194/egusphere-egu22-6763, 2022.

Mon, 23 May, 17:00–18:30

Chairpersons: Claire Bossennec, Stijn Beernink

17:00–17:05
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EGU22-531
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ECS
Cécile Ducrocq et al.

Crustal deformation allows us to monitor and understand critical properties of exploited geothermal systems around the world. The Hellisheiði high-temperature geothermal field (in 2011: 303MWe and 133MWth) in SW Iceland has been previously studied using Global Navigation Satellite Systems (GNSS) and Interferometry Synthetic Aperture Radar (InSAR) data between 2011 and 2015. These studies characterized the subsidence rate related to the extraction of fluids in the Hellisheiði area, as well as a 4-month uplift at the start of injection of geothermal fluids in the Húsmúli area. This uplift was accompanied by significant seismicity culminating with two ML >3.5 earthquakes felt in the surrounding region.

We carry out further analysis of GNSS and InSAR data between 2011 and 2019 that show a total of three uplift events, separated by periods of subsidence or little deformation in the Húsmúli area. The deformation episodes seem to correlate with heightened seismic activity despite the continued decrease of injected mass flow rate in the original injection boreholes.

Here we use a finite element poroelastic model (COMSOL Multiphysics) to relate the extraction and injection of the adjacent Hellisheiði and Húsmúli areas to the ground deformation within the same time span. We assume that the boreholes can be represented by three point-injector sources: one of negative mass flow rate in Hellisheiði, and two of positive mass flow rates in (west and east) Húsmúli. The three sources are necessary to explain the deformation observed between 2011 and 2019. The poroelastic model presents insights into the temporal response of geothermal systems from extraction/injection, changes in exploitations and variability in permeability all of which induce heightened strain and stress in the fractured Húsmúli region. We investigate if poroelastic effects may be responsible for triggering transient earthquake swarms and to what degree poroelasiticy can explain the spatially and temporally complex uplift and subsidence. We suggest this study offers new insights into the Hellisheiði geothermal system that are transferable to geothermal systems around the world.

How to cite: Ducrocq, C., Heimisson, E. R., Geirsson, H., Árnadóttir, T., Axelsson, G., Hjörleifsdóttir, V., and Drouin, V.: Temporal deformation in the Hellisheiði geothermal field and its adjacent Húsmúli injection field explained by poroelastic modelling, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-531, https://doi.org/10.5194/egusphere-egu22-531, 2022.

17:05–17:10
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EGU22-3659
Victor Bense et al.

Aquitard hydraulic properties are notoriously difficult to assess, yet accurate aquitard hydraulic conductivity estimates are critical to quantify recharge and discharge to and from semi-confined aquifer systems via hydraulic head gradients. Such flux quantification is required to evaluate the risks of aquifer exploitation by groundwater abstraction and aquifer vulnerability to surface contamination. In this study, we consider a regionally important aquitard and compare existing hydraulic conductivity estimates obtained through traditional methods to those inferred from long-term hydraulic head monitoring and thermally-derived vertical groundwater fluxes (0.04--0.25 m/y). We estimate the fluxes using numerical modeling to analyse the propagation of decadal climate signals into temperature-depth profiles and fitting the simulated and observed inflection point depths (minimum temperature). Results reveal that climate-disturbed temperature-depth profiles paired with multi-level head data can yield accurate vertical fluxes and aquitard hydraulic conductivities. This approach for characterizing groundwater systems and quantifying flows to and from sedimentary aquifers is more efficient but yields results that are comparable to conventional methods.

How to cite: Bense, V., Kruijssen, T., van der Ploeg, M., and Kurylyk, B.: Inferring aquitard hydraulic conductivity using transient temperature-depth profiles impacted by ground surface warming, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3659, https://doi.org/10.5194/egusphere-egu22-3659, 2022.

17:10–17:15
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EGU22-5084
Ulrich Steiner et al.

The storage of low-temperature heat in the near surface underground is already widely used worldwide, whereas only little attempts of storing of higher temperatures have been made so far. However, this can become increasingly important in the heat transition strategy by contributing with this technology to medium and peak load supply. Previous works have demonstrated that a large part of the required thermal energy can be efficiently stored in former oil reservoirs in Tertiary sediments of the URG. The advantage of using depleted oil reservoirs as HT-ATES is that they have a lower overall project risk due to the knowledge of the subsurface from the exploration history and that the geological and geophysical data, which are mostly available, allow a more reliable forecast of efficiency and development costs.

KIT in Karlsruhe has now planned the "Deepstor" HT-ATES research infrastructure for its Northern Campus. The site is adjacent to the former Leopoldshafen oil field and can draw on a large amount of data from boreholes for assessment prior to drilling. The targeted reservoirs is the several meters in thickness consisting of fine-grained calcareous sandstones from the Oligocene Froidfontaine Formation at a depth of approx. 1,300 meters.

The baseline of this study is the interpretation of petrophysical data such as resistivity-, sonic-, gamma and SP-logs to derive hydrogeological and geothermal parameters in 15 deep wells in vicinity of the planned drilling site. An integrated data analysis is performed with simulations to gain a quantitative understanding of the fluid and heat flow of the HT-ATES site and to predict the storage and recuperation capacity. Poro-perm values from core material are used to calibrate the results. The aim is a statistically based assessment of the storage site for planning and cost estimation of the research infrastructure.

This work should provide further insights for the future development of geothermal heat storage and enable the integration of a HT-ATES in the KIT campus.

How to cite: Steiner, U., Ang, N., Bauer, F., and Schill, E.: Characterization of Oligocene Oil Reservoir Sandstones for High Temperature Aquifer Thermal Energy Storage (HT-ATES) in the Upper Rhine Graben (URG), SW Germany, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5084, https://doi.org/10.5194/egusphere-egu22-5084, 2022.

17:15–17:20
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EGU22-5610
Peter Bayer et al.

Under natural conditions the thermal signature at the Earth´s surface equilibrates with the geothermal heat flux. Given that downward propagation of heat by conduction and advection is magnitudes lower than the daily and seasonal variation at the surface, these short-phased patterns impart a dampened and long-phased temperature response in the shallow subsurface. While climate change manifests in temperature trends that correlate at decade scale this signature is integrated by the slow heat transfer in gradual subsurface warming. In many places land use and small scale anthropogenic structures overprint the thermal response of the subsurface to climate change at the surface. In our contribution we present evidence of subsurface warming in natural and anthropogenic settings for different case studies in Central Europe. Repeated temperature depth logs reveal that in natural environments shallow subsurface temperature rise is trailing when compared to the rise in surface temperature and diminishes towards greater depths (e.g. +0.35 K per decate at the surface, +0.28 at 20 m, and +0.09 at 60 m below ground level for 32 wells in Bavaria). While in general a coherent pattern is found for different locations in natural environments, site-specific trends have a high spread (e.g. +0.36±0.44 K per decade for 227 wells in Austria) and temperature can also be dependent on vertical or lateral groundwater flow in the region. In built-up areas temperature rise in the subsurface is characterised by a higher variance and often exceeds the rise of surface temperature. Especially in dense urban areas ground temperature is elevated indicating local extreme temperature rises that are magnitudes higher than temperature rise at the surface. The high variance originates partially from the scarcity of reliable and long-term monitoring. Monitoring data typically lacks either depth or time resolution as temperature is either continously logged at a single-depth, erratically measured as depth profile, or measured at the surface during groundwater quality measurements.

How to cite: Bayer, P., Benz, S. A., Menberg, K., Blum, P., Noethen, M., and Hemmerle, H.: Subsurface warming trends in response to climate change and local heat sources in Central Europe, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5610, https://doi.org/10.5194/egusphere-egu22-5610, 2022.

17:20–17:25
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EGU22-5795
Alejandro García-Gil et al.

The use of shallow geothermal energy (SGE) resources in oceanic volcanic environments entails additional challenges when compared to continental sedimentary/plutonic settings. The efficiency of shallow geothermal heat exchangers heavily depends on the geology and hydrogeology of the terrain where are placed. Volcanic rocks in small oceanic islands (<5,000 km2) are the result of volcanism, erosion, and tectonic collapse. All these processes conform highly heterogeneous formations with complex hydrogeology whose thermal response to shallow geothermal systems requires a good understanding of heat transfer in such environments. The SAGE4CAN project will concentrate on SGE resource assessment taking into account heterogeneity characteristic of volcanic formations, both at local and insular scale. To this end, the Canary Islands are selected as representative volcanic oceanic islands, to define SGE implementation barriers including but not limited to (1) heterogeneities of thermal properties intrinsic to volcanic formations (volcanic dikes, red layers, landslides, etc.), (2) heat advection in the context of complex groundwater flow in the unsaturated (dominate in midlands and highlands) as well as in the saturated medium (coast), (3) enhanced geothermal gradients, (4) transient effects of urban and volcanic activity, (5) heating and cooling demand, (6) shallow geothermal energy installations design and optimization, as well as (7) energy transition strategies in energy-dependent islands. The SGE4CAN project will investigate novel approaches to overcome such boundary conditions of oceanic volcanic islands in the estimation of the renewability of the resources, developing novel procedures to conduct cost-efficient and open-access Thermal Response Tests (TRTs), investigate the performance of existent SGE systems, assessing environmental impacts associated with SGE use. The knowledge generated from this project will be used on its final stage to identify adequate strategies for the integration of SGE into heating and cooling policies and action plans, as well as to raise awareness about the technology so that it gets recognition.

 

How to cite: García-Gil, A., Santamarta, J. C., Mejías Moreno, M., Baquedano, C., Garrido Schneider, E., Alonso Sánchez, T., Rey Ronco, M. Á., Sánchez-Navarro, J. Á., Marazuela, M. Á., Andreu Gallego, A., and Tiscar Cervero, J. M.: The SAGE4CAN project: The use of shallow geothermal energy from oceanic volcanic islands , EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5795, https://doi.org/10.5194/egusphere-egu22-5795, 2022.

17:25–17:30
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EGU22-7500
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ECS
Christian Wenzlaff et al.

High Temperature - Aquifer Thermal Energy Storage (HT-ATES) offers a promising opportunity for climate-neutral heat supply in urban areas due to their high storage capacity and the possibility of direct integration into the regional district heating system. The assessment of the storage potential of HT-ATES requires reliable numerical models of the corresponding storage formation. To analyse the potential of the Lower Muschelkalk (Middle Triassic) as HT-ATES horizon, an unstructured 3D finite element model of the natural gas storage facility in Berlin/Spandau was developed. At this site, two porous layers (average porosity of 22 %) of oolithic grainstones characterize the target formation with a total thickness of about 30 m and a natural reservoir temperature of 32 °C in a depth of 535 m below ground surface. Beside lab analysis of core samples and fluid samples from the site, slug-withdrawal tests were performed in summer 2021 to identify hydraulic key parameters for the numerical simulations. The results indicate a productivity between 0.5 and 1.2 l/s/bar with reservoir permeability between 250 and 700 mD allowing maximum flow rates between 55 and 135 m³/h. In this study, we present a complete workflow from geological characterisation, lab analysis and field testing to detailed numerical HT-ATES simulations. Furthermore, we compare the storage potential based on different data sources such as solar heating systems and district heating networks. First results from the numerical simulations with storage volumes between 15,000 m³ (solar heating system) and 400,000 m³ (district heating system) show promising mean efficiency values between 60 % and 90 % within 25 years of operation. The hydraulic tests and the underlying numerical simulations indicate that the Lower Muschelkalk is suitable for HT-ATES.

How to cite: Wenzlaff, C., Winterleitner, G., Virchow, L., Regenspurg, S., Thielke, C., and Blöcher, G.: Assessing the geological potential of the Lower Muschelkalk as High Temperature - Aquifer Thermal Energy Storage (HT-ATES) horizon in Berlin (Germany), EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-7500, https://doi.org/10.5194/egusphere-egu22-7500, 2022.

17:30–17:35
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EGU22-9128
Martin Bloemendal et al.

Aquifer thermal energy storage (ATES) is a technology to provide energy-efficient heating and cooling to buildings by storage of warm and cold water in aquifers. In regions with large demand for ATES, ATES adoption has led to congestion problems in aquifers. The aquifer utilisation and the recovery of thermal energy stored in aquifers can be increased by reducing the distance between wells of the same temperature. Hence, this approach is implemented in practice, but the understanding of how this affects both the recovery efficiency and the needed pumping energy is missing.

In this research, the effect of well placement on the performance of individual systems is quantified using numerical modelling. Results show an increase in performance of individual systems when the thermal zones of wells of the same temperature are combined. The relative increase of the thermal recovery efficiency is 12% for average-sized systems with a storage volume of 250,000 m3/year, and 25% for small systems (50,000 m3/year). Performance of the combined system improves because the surface area of the thermal zone of the combined system, over which thermal losses occur, is smaller than the sum of the surface areas of the individual systems. Performance improvement is larger for systems with small storage volumes and long well screens. The optimal distance between wells of the same temperature is 0.5 times the thermal radius, following the trade-off between an increase of the thermal recovery efficiency and an increase in pumping energy. The distance between wells of opposite temperature must be larger than 3 times the thermal radius to avoid negative interaction.

How to cite: Bloemendal, M., Duijff, R., and Bakker, M.: Thermal and hydraulic effects due to interaction between aquifer thermal energy storage systems, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9128, https://doi.org/10.5194/egusphere-egu22-9128, 2022.

17:35–17:40
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EGU22-11755
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ECS
Adela Ramos Escudero and Martin Bloemendal

Aquifer Thermal Energy Storage (ATES) is a technology that provides sustainable and cheap space heating and cooling. Its successful application is directly dependent on the presence of a suitable aquifer and local climatic conditions.

In Spain, there is not yet a mature market for ATES. There are no specific standards or norms and hardly any practical guidelines have been developed. This work presents a methodology that assesses the potential for ATES in Spain using subsurface and climatic data processed with GIS. The method identifies aquifers with possible thermal use and areas where the climatic conditions are favorable for ATES for the residential sector. Based on these conditions, urban areas located in favorable areas are identified. Their associated population allows making an approximation of the ATES market size in Spain. Results show that 38% of the aquifers in Spain show potential for ATES and 63% of large urban areas in Spain are located in such areas. Also, 50% of the population lives in areas where the residential sector appears to be suitable for ATES based on climatic conditions.

How to cite: Ramos Escudero, A. and Bloemendal, M.: GIS-based Aquifer Thermal Energy Storage (ATES) systems potential assessment in Spain, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-11755, https://doi.org/10.5194/egusphere-egu22-11755, 2022.

17:40–17:45
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EGU22-734
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ECS
Claire Bossennec et al.

Geothermal energy and thermal energy storage are essential components in balancing a decarbonated future energy supply. The north-eastern shoulder of the Upper Rhine Graben (URG), with its Variscan basement belonging to the Mid-German Crystalline High, is a potential target area for heat storage projects. Ganodioritic units in the city area of Darmstadt provide suitable thermo-mechanical properties to implement a Medium Deep Borehole heat exchanger Thermal Energy Storage (MD-BTES). This study focuses on the structural architecture of such crystalline units, representing a heterogeneous fracture and fault network. An approach combining geophysical characterisation and the analysis of surface fracture network analogue is performed to quantify the dimensions and topology of such a fracture network in the subsurface.

Two 2D seismic profiles helped to characterise the deep subsurface structures of the BTES demo site area and to localise the boundaries between the unweathered basement, the weathered basement, and the overlying sedimentary layers. The weathered basement and Permian volcano-sedimentary and Quaternary fluviatile units build the near-surface groundwater aquifer. This shallow aquifer requires a detailed investigation, performed through electrical resistivity mapping, near-surface S-wave refraction seismic survey, ground-penetrating radar lines and radon emanations profiles, combined with shallow geotechnical drillings. Selected surface analogues are located in the northern Odenwald Massif, the most extensive outcropping section of the Mid-German Crystalline High. The first analogue is a pit located 150 m apart from the BTES demo site. The second is the Mainzer Berg quarry in the Sprendlinger Horst, at a 12 km westbound distance, which belongs to Variscan granodioritic and granitic units with similar properties. Derived from these analogues, the fracture length distribution follows the power-law with an exponent about -2. The main relevant orientations identified are trending N030°E -N040°E, N090°E -N100°E, N120°E -N130°E and N165°E, with an overall fracture density of 3.06 frac.m-1 for the demo site subsurface. Additionally, the connectivity of the fracture network is heterogeneous due to clustering. Such clustering also affects weathered horizons, which constitute the near-surface groundwater aquifer.

These fracture network properties are then implemented into sub-surface semi-artificial discrete fracture network (DFN) models to quantify at the first-order the flow properties of such heat storage rocks. This approach allows a successful characterisation of the BTES site, improves the local reservoir model accuracy and ensures an optimal assessment of the storage system behaviour.

How to cite: Bossennec, C., Seib, L., Frey, M., Burschil, T., Buness, A. H., Welsch, B., and Sass, I.: Geophysical and structural characterisation of a granodioritic MD-BTES test-site, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-734, https://doi.org/10.5194/egusphere-egu22-734, 2022.

17:45–17:50
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EGU22-9212
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ECS
Chris Boeije et al.

The formation of free gas bubbles (degassing) is a major issue during production of geothermal fluids. These often contain substantial amounts of dissolved gasses, such as CO2, CH4 and N2. Lower pressures in the region surrounding the production well can cause dissolved gas to come out of the solution. This can have detrimental effects on the production and generally on the operation, such as corrosion of the facilities or reduced water production as the gas limits the space where the water can flow. This study aims to improve the understanding of the conditions under which free gas nucleates, including determination of the bubble point pressure and temperature and the rate at which bubbles form during depressurization.

The focus of this study is on CO2 degassing from high salinity brines. We report a series of well-controlled depressurization experiments in a pressure cell that allows for visual monitoring of the degassing process. The cell is filled with brine saturated with dissolved CO2 at high pressure and temperature. The pressure within the cell can be reduced in a reproducible manner thus allowing for repeatable experiments. A high-speed camera paired with a uniform LED light source is used to record the degassing process. The pressure in the cell is monitored using a transducer synchronized with the camera. The resulting images were analysed using an in-house MATLAB code, which allows for determination of the bubble point pressure and rate of bubble formation. Experiments were performed at high pressure (up to 200 bar) and temperature (up to 200 °C) using a fixed CO2 concentration of 200 mmol/L (i.e. 8.8 g/L). Two saline brine solutions are used to assess the influence of the salt concentration on the bubble nucleation process: a low salinity (1 M NaCl) and a high salinity (1.5 M CaCl2 + 2 M NaCl) solution.

A model based on the geochemical software PHREEQC was also developed to predict the solubility of CO2 in high salinity geothermal brines. This model allows for simulating the degassing behaviour at the same conditions as those used in the experiments. From these simulations, the theoretical bubble point pressure and temperature can be estimated along with the rate of gas exsolution during a depressurization process. As there are several alternative equation-of-states for CO2 in solution with brines, a comparative matching of the depressurization experiments with individual formulations is presented.

How to cite: Boeije, C., Weinzierl, W., Zitha, P., and Pluymakers, A.: Degassing kinetics of high salinity geothermal fluids, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9212, https://doi.org/10.5194/egusphere-egu22-9212, 2022.

17:50–17:55
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EGU22-12929
Philip Vardon et al.

In conjunction with a deep geothermal project which is being implemented on the TU Delft campus in the Netherlands, a high temperature aquifer thermal energy storage (HT-ATES) is being considered. An initial feasibility study suggests that this could significantly reduce CO2 emissions from heating and be financially beneficial. As part of the research associated with the implementation of the geothermal well, a 500 m deep monitoring and exploration well has been drilled to further investigate two target layers for HT-ATES and to allow for scientific records before, during and after the production phase of the geothermal project. With this drilling, the potential for HT-ATES of multiple layers is investigated by means of innovative exploration methods. An extensive set of downhole geophysical logging tools was used, many cores from both consolidated and unconsolidated layers were taken and a pumping test was carried out in the deepest layer. This work presents an initial overview of the work carried out and provides insights into the initial results of this innovative exploration drilling. The Delft geothermal project is therefore a great example of a beneficial interplay of economic and societal interest (i.e. city heating, CO2-neutral campus) and scientific innovation.

How to cite: Vardon, P., Bloemendal, M., Beernink, S., Hartog, N., Barnhoorn, A., Schmiedel, T., Abels, H., and Laumann, S.: Exploration of high temperature aquifer thermal energy storage in Delft (The Netherlands), EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-12929, https://doi.org/10.5194/egusphere-egu22-12929, 2022.

17:55–18:00
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EGU22-9263
Maria Klepikova et al.

Fracture surface topography exhibits long-range spatial correlations resulting in a heterogeneous aperture field. This leads to the formation, within fracture planes, of preferential flow channels controlling flow and transport processes. We have investigated numerically the influence of the statistical properties of the aperture field and upscaled hydraulic behavior on heat transport in rough rock fractures with realistic geometries. Similarly to the rough fracture's hydraulic behaviour, we find that its heat transport behaviour deviates from the conventional parallel plate fracture model with increasing fracture closure and/or decreasing correlation length.  We demonstrate that the advancement of the thermal front is typically slower in rough fractures compared to smooth fractures having the same mechanical aperture. In contrast with previous studies that neglect temporal and spatial temperature variations in the rock matrix, we find that the thermal behavior of a rough-walled fracture can, under field-relevant conditions, be predicted from a parallel plate model with an aperture equal to the rough fracture's effective hydraulic aperture. The practical implication of our finding is that thermal exchanges at the scale of a single fracture is controlled by the effective hydraulic transmissivity. Provided that thermal properties of the host rock are known, this implies that (1) geothermal efficiency can be computed at field sites using hydraulic characterization alone, and predicted using well-known low-dimensional hydraulic parameterizations in terms of effective hydraulic properties and (2) heat tracer tests are reliable for inferring effective fracture transmissivity.

How to cite: Klepikova, M., Méheust, Y., Roques, C., and Linde, N.: Heat transport by flow through rough rock fractures, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9263, https://doi.org/10.5194/egusphere-egu22-9263, 2022.

18:00–18:05
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EGU22-9562
Andreas Englert and Peter Bayer

Understanding of subsurface flow and transport is of major interest supporting optimal design for several societal relevant technologies, such as waste disposals, geothermal or groundwater production facilities. To advance measurement and modeling techniques and refine them for practical applications, we further developed the fractured aquifer test site Rock Garden at the Martin Luther University Halle. The Rock Garden test site is situated beneath the courtyard of the Faculty of Natural Sciences III and is 60 m x 60 m in size. Fractured Rotliegend series of conglomerates, sand- and siltstones are investigated at the site by 6 drillings. A central borehole (B3) is 40 m in depth and developed as an open borehole between 15 m - 40 m below surface. Five boreholes are developed as groundwater observation wells of about 20 m depth and are equipped with filter screens between 10 m - 20 m below surface. Natural groundwater levels are on average about 3 m below surface and vary about 0.5 m around this value. The average gradient varies as a function of time between 0.3 % and 0.5 %, direction east northeast. A first pumping test in B3 unraveled hydraulic connection to all of the five surrounding boreholes. The effective transmissivities are of the order of 10-5 m2/s and storativities are of the order of 10-4. To understand hydraulically active fractures or fracture zones and their connection to the rock matrix at the Rock Garden site, a first flowmeter experiment was performed in well B3. Under natural conditions no flowmeter signals have been detected suggesting vertical ambient flow to be smaller than 7 cm/min. Under pumping conditions, the flowmeter signals suggest diffuse horizontal inflow from conglomerate lenses (about 80 % of the total inflow) and discrete horizontal inflow from fractures in clay and siltstones (about 20 % of the total inflow). To characterize these fractured and porous zones in detail, we plan performing hydraulic and tracer tomography at the Rock Garden test site in the near future.

How to cite: Englert, A. and Bayer, P.: Rock Garden test site – hydraulics in porous fractured media, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9562, https://doi.org/10.5194/egusphere-egu22-9562, 2022.

18:05–18:10
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EGU22-9780
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ECS
Rubén Vidal and Maarten W Saaltink

Aquifer Thermal Energy Storage (ATES) is a technology that injects heat into aquifers during low energy demand and extracts it during high demand. ATES generates variation of temperature in the underground that can lead to chemical reactions. These reactions can affect the efficiency of ATES and modify the groundwater chemistry and the properties of soils and rocks. We present a novel method that allows calculation of complex numerical models and understanding the thermo-hydro-chemical processes in ATES in a simple way. Aqueous and mineral reactions must be assumed in equilibrium.  The method decouples the chemistry from the thermo-hydraulic processes. The chemical part of the method consists of chemical batch calculations in which minerals dissolve/precipitate and water chemistry varies as a result of changing temperature. The thermo-hydraulic part consists of calculating temperature and spatial and temporal derivatives of temperature. From this, chemical composition of groundwater and precipitation/dissolution rates of minerals can be calculated straightforwardly.

We have applied the method to a HEATSTORE benchmark case, which is inspired by an ATES pilot project located in Bern, Switzerland. We used PHREEQC for the chemical calculations and for the thermo-hydraulic modelling we used the finite element code CODE_BRIGHT. The results permit us to understand better the reactive transport processes in the aquifer (which we divided into mixing, heat retardation and heat conduction), changes in the porosity of the rocks and the precipitation and dissolution of minerals.

 

Acknowledgements: This work was financed by the ERANET project HEATSTORE (170153-4401). This project has been subsidized through the ERANET cofund GEOTHERMICA (Project n. 731117), from the European Commission, RVO (the Netherlands), DETEC (Switzerland), FZJ-PTJ (Germany), ADEME (France), EUDP (Denmark), Rannis (Iceland), VEA (Belgium), FRCT (Portugal), and MINECO (Spain). Also, the first author is supported by a grant from the Department of Research and Universities of the Generalitat de Catalunya (2021 FI_B 00940).

How to cite: Vidal, R. and Saaltink, M. W.: A novel method for thermo-hydro-chemical models for Aquifer Thermal Energy Storage, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-9780, https://doi.org/10.5194/egusphere-egu22-9780, 2022.

18:10–18:15
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EGU22-11934
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ECS
Geraldine Regnier et al.

Aquifer Thermal Energy Storage (ATES) has significant potential to provide large-scale seasonal cooling and heating in the built environment, offering a low-carbon alternative to fossil fuels. To deliver safe and sustainable ATES deployments, accurate numerical modelling tools must be used to predict flow and heat transport in the targeted aquifers. However, numerical simulation of ATES systems is very challenging, due to the associated high computational cost of capturing fluid flow and heat transport at a high resolution and importance of accurately modelling complex geological heterogeneity.

Here, we present a novel approach to simulate ATES, based on the use of surface-based geologic models (SBGM), a double control-volume finite element method, and unstructured tetrahedral meshes with dynamic mesh optimisation (DMO). Previous use of DMO for a range of porous media flow applications has allowed an important reduction in the cost of numerical simulations. DMO allows the resolution of the mesh to vary over time and space to satisfy a user-defined solution precision for selected fields, refining where the solution fields are complex and coarsening elsewhere. SBGM allows accurate representation of complex geological heterogeneity and efficient application of DMO, essential for accurate simulation of ATES without excessive computational cost. 

We demonstrate application of these methods in two low-temperature ATES scenarios: a homogeneous aquifer, and a heterogeneous fluvial aquifer containing meandering, channelised sandbodies separated by mudstones. For both cases, cold and warm water are injected alternatively over 6-month periods via a well doublet. We demonstrate that DMO reduces the required number of mesh elements by a factor of up to 22 and simulation time by a factor of up to 15, whilst maintaining the same accuracy as an equivalent fixed mesh. DMO significantly reduces the computational cost of ATES simulations in both homogeneous and heterogeneous aquifers. This offers significant advantages compared to conventional methods in assessing the impact of uncertain geologic heterogeneity on ATES operation and efficiency, and in optimising individual and multiple ATES deployments.

How to cite: Regnier, G., Salinas, P., Jacquemyn, C., and Jackson, M. D.: Numerical modelling of Aquifer Thermal Energy Storage systems with Surface-Based Geologic modelling and Dynamic Mesh Optimisation, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-11934, https://doi.org/10.5194/egusphere-egu22-11934, 2022.

18:15–18:20
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EGU22-12456
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ECS
Alberto Previati et al.

Low enthalpy geothermal applications such as ground coupled heat pumps (GCHP) and groundwater heat pumps (GWHP) are an attractive low-carbon solution for heating and cooling of buildings. Their efficiency depends on the subsurface thermal properties (e.g. thermal conductivity, heat capacity) and the hydrogeological/thermal regimes (e.g. groundwater flow, depth of the water table, temperature profile). The geothermal potential is an indicator used to quantify and compare the ability to exchange heat with the subsurface/groundwater according to specific technologies. Even though it has no unique definition, it is often obtained as a combination of the subsurface hydrogeological/thermal properties and the thermal regime and, by means of GIS techniques it can be spatialized to obtain geothermal potential maps.

The subsurface thermal properties vary in space according to the geological setting, while the hydrogeological and thermal regimes can vary both in space and time according to the fluid and heat budgets of the aquifers. However, despite few studies consider the variability of the geothermal potential in time due to possible variations of the hydrogeological and thermal regimes, it is essential to evaluate the efficiency of geothermal systems in a changing environment such as subsurface urban heat islands. The hydrogeological/thermal regimes are not stationary, especially beneath big cities where land and subsurface uses control the elevation of the water table and the shallow subsurface thermal regime. Moreover, the heating and cooling demand of buildings may vary due to climate change effects such as global warming and atmosphere urban heat island.

The potential to exchange heat with the subsurface in the Milan metropolitan area was estimated from hydrogeological and thermal regimes simulated by a fluid-flow/heat-transport city-scale numerical model, calibrated on the current state. Several scenarios were generated changing the boundary conditions according to projected changes of (I) the air temperature (based on RCP 2.6, 4.5 and 8.5 scenarios), (II) the groundwater head, (III) the land use/city size and (IV) the geothermal uses (based on the increment of installations and changes of the thermal demand), to estimate the changes and the seasonal variability of the subsurface temperature at different depths in different zones of the city. Finally, the future variations of the thermal potential were estimated for heating and cooling seasons combining the scenarios-projected subsurface temperatures with the hydrogeological and thermal properties, also considering the variation of heating and cooling thermal loads.

How to cite: Previati, A., Silvestri, V., Frattini, P., and Crosta, G. B.: Evaluating the sustainability of low enthalpy geothermal applications in a subsurface heat island, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-12456, https://doi.org/10.5194/egusphere-egu22-12456, 2022.