Anthropogenic or not?
A recently published paper in Science, written by a team of the Swiss Seismological Service at ETH Zurich and collaborators from the Engineering Geology group at ETH, GFZ Potsdam and the Glasgow University, explores the potential link between a magnitude 5.5 earthquake in South Korea and a nearby geothermal project.
The earthquake, which occurred on 15 November 2017, injured about 80 people and caused damage to numerous buildings in the city of Pohang. If proven to be anthropogenic, it would be the largest earthquake known to have been associated with the exploitation of deep geothermal energy.
Seismograms of induced earthquakes are generally indistinguishable from those of natural earthquakes. Therefore, investigations focus on a range of indicators, taking into account the location of earthquakes, their depths, and the history of stimulation activities conducted underground. By analyzing publically available continuous waveform and geodetic data from satellites, the paper contributes to the understanding of the nature of the event.
Mainshock close to geothermal site
The study shows that the mainshock and its largest aftershocks occurred within 2 km distance or less of the geothermal site. Furthermore, they are located within 1.5 km distance of an induced event, which occurred in April 2017 during one of the underground stimulation operations. These locations are confirmed by a Korean study, which has been simultaneously published in Science.
In general, the closer an earthquake sequence is located to a geothermal site and to previous related seismic activity, as well as the sooner it happens after underground operations, the greater the chance of being related to it. The mainshock and the 46 aftershocks detected between 15 and 30 November 2017 all occurred at depths of 3 to 7 kilometres.
Such depths are unusually shallow when compared to previously registered natural events in the area. The analysis of satellite data illustrates that the mainshock displaced the surface of the earth permanently by up to 4 cm, indicating that the activated, and previously unknown fault, is a steeply dipping and very shallow thrust fault that passes directly beneath the bottom hole section.
These indications combined lead to the conclusion that a connection between the magnitude 5.5 earthquake in South Korea and the nearby geothermal project is plausible. However, the mainshock occurred about two months after the last stimulation activities. So far, there is no quantitative model available that relates the injection activities conducted to the occurrence of this event.
Expert commission examins evidence
The Korean government has appointed an independent expert commission to examine all pieces of evidence and to evaluate if the event was triggered or induced by the nearby stimulation activities. To our understanding, the commission will (re-)analyze all available data and models, including microseismicity data, injection volumes, reservoir pressures, and detailed hydrological and geological data, which are essential to understand the relation between the injection operations and the earthquake sequence.
The Swiss Seismological Service (SED) at ETH Zurich has first informed the public in November 2017 about the Pohang earthquake in the context of the release of a best practice report on induced seismicity. At the same time, Geo-Energie Suisse AG had notified the canton of Jura, where currently the only EGS-style deep geothermal project in Switzerland has applied for a construction permit. In consequence, the canton instructed Geo-Energie Suisse AG to evaluate potential implications for the planned Haute-Sorne geothermal project.
Deeper understanding needed
"Such strong earthquakes in connection with deep geothermal projects have not yet occurred worldwide. However, it is known that other technical interventions that led to stress changes in the ground caused similarly large shocks. A deeper understanding of what was happening in Pohang is essential if geothermal energy is to be produced safely and sustainably in the future", says Stefan Wiemer, head of Swiss Seismological Service at ETH Zurich.
ETH Zurich is intensively involved in research in this field. On the one hand through controlled experiments in underground laboratories in Grimsel or soon in the Bedretto Tunnel, on the other hand through the development and validation of adaptive control systems that evaluate all available information in real time and continuously include it in the risk assessment.
More information:
phys.org/news/2018-04-evidence … hang-earthquake.html
Provided by ETH Zurich