Ground motions induced by pore pressure changes at the Szentes geothermal area, SE Hungary
| Autor: | Békési, E., Fokker, P.A., Candela, T., Szanyi, J., van Wees, J.-D., Tectonics, Experimental rock deformation |
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| Přispěvatelé: | Tectonics, Experimental rock deformation |
| Jazyk: | angličtina |
| Rok vydání: | 2022 |
| Předmět: |
InSAR
Pore water pressure Sustainability and the Environment Renewable Energy Sustainability and the Environment Data assimilation Geomechanical modeling Szentes geothermal field (Hungary) Economic Geology Renewable Energy Petrology Geotechnical Engineering and Engineering Geology Geothermal gradient Geology |
| Zdroj: | Geothermal Energy, 10(1), 1. Springer Science + Business Media |
| ISSN: | 1992-2000 2195-4771 |
| Popis: | The long-term sustainable exploitation of geothermal resources requires cautious planning and regulation. Exploitation in excess of natural recharge can result in reservoir pressure decline, causing a decrease in production rates. Furthermore, such “overexploitation” of geothermal reservoirs may lead to compaction and land subsidence. Understanding of such phenomena is critical for the assessment of societal-environmental risks, but can also be used for optimization by constraining reservoir processes and properties.Excessive thermal water volumes have been extracted from porous sedimentary rocks in the Hungarian part of the Pannonian Basin. Thermal water production in Hungary increased significantly from the early 70’s. Regional-scale overexploitation of geothermal reservoirs resulted in basin-scale pressure drop in the Upper Pannonian sediments, leading to compaction and ground subsidence.We investigated surface deformation at the Szentes geothermal filed, SE Hungary, where the largest pressure decline occurred. We obtained data from the European Space Agency’s ERS and Envisat satellites to estimate the ground motions for the periods of 1992-2000 and 2002-2010. We applied inverse geomechanical modelling to understand the compaction behaviour of the reservoir system and to estimate the subsurface properties. We constrained the model parameters using the Ensemble Smoother with Multiple Data Assimilation, which allowed us to incorporate large amounts of surface movement observations in a computationally efficient way. The model requires pressure time series as input parameters, therefore, the lack of regular pressure measurements in geothermal wells of Szentes resulted in significant uncertainties. Still, we managed to identify a potential delay in pressure drop and subsidence, implying a time-decay compaction behaviour of the reservoir system, and we arrived at realistic estimates for the compaction coefficient of the reservoir. The improved parametrization enables better forecasting of the reservoir behaviour and facilitates the assessment of future subsidence scenarios. This study thus demonstrates the effectiveness of InSAR-based ground motion data and inverse geomechanical modelling for the monitoring of geothermal reservoirs and the establishment of a sustainable production scheme. |
| Databáze: | OpenAIRE |
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