Anthropogenic and natural ground deformation in the Hengill geothermal area, Iceland

• Published in: Journal of Geophysical Research: Solid Earth
• Main Authors: Juncu, D., Arnadottir, Th., Hooper, A., Gunnarsson, G.
• Other Authors: Nordic Volcanological Center, Institute of Earth SciencesUniversity of Iceland Reykjavík Iceland, COMET, School of Earth and EnvironmentUniversity of Leeds Leeds UK, OR—Reykjavík Energy Reykjavík Iceland
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: American Geophysical Union (AGU) 2017
• Subjects: Hengill; Nesjavellir; New Zealand; Iceland
• Online Access: http://hdl.handle.net/10754/678441; https://doi.org/10.1002/2016JB013626

We investigate crustal deformation due to the extraction of water and steam from a high-enthalpy geothermal reservoir; a common occurrence, yet not well understood. The cause of this deformation can be a change in pressure or in temperature in the reservoir, both of which can be caused by extraction or injection of geothermal fluids. Our study area, the Hengill mountains in SW Iceland, is an active volcanic center and a plate triple junction that hosts two power plants producing geothermal energy. This combination of natural and anthropogenic processes causes a complex displacement field at the surface. We analyze geodetic data—Global Navigation Satellite System and Interferometric Synthetic Aperture Radar—to obtain the surface velocity field, which we then simulate using an inverse modeling approach. We focus on the deformation around the geothermal power plants but need to model the regional tectonic and volcanic deformation as well, because the signals are overlapping. We find that plate motion and a deep contracting body can explain the broad scale signal in the area. Local deformation near the two power plants, Hellisheidi and Nesjavellir, can be explained by extraction of geothermal fluids. We estimate reservoirs extending from 0.6 to 3.0 km depth at Hellisheidi, and 1.0 to 3.0 km depth at Nesjavellir for observed pressure decrease rates of 0.25 MPa/yr and 0.1 MPa/yr, respectively. We find that the main cause for the subsidence in the geothermal area is the observed pressure drawdown. The authors would like to thank Einar Gunnlaugsson from Reykjavik Energy (RE) for providing production data from Hellisheidi and Nesjavellir; Bjarni Reyr Kristjánsson (RE) for discussions and advice regarding the geothermal power plant operations; RE and ÍSOR for GNSS data from the dense Hengill network; the Icelandic Meteorological Office (IMO) for operating the cGPS network in Iceland; Sigrún Hreinsdóttir (GNS, New Zealand) for global GNSS solutions; Tabrez Ali (University of Wisconsin, Madison, USA) for help and ideas ...