Project I10 by Behnam Maleki Asayesh (University of Potsdam and GFZ Potsdam): Point process modelling of induced seismicity
Timescale: Oct. 2021 – Sept. 2024
PD Sebastian Hainzl, GFZ Potsdam
Prof. Matthias Holschneider University of Potsdam
apl. Prof. Gert Zöller, University of Potsdam
Natural seismicity is usually governed by some universal characteristics, e.g. exponentially distributed magnitudes with slope parameter around unity (Gutenberg-Richter law), and power-law decaying aftershocks (Omori law). Man-made seismicity, e.g. induced earthquakes resulting from fluid injection or gas production, often shows different characteristics. Moreover, fluid migration results in many cases in diffusive seismicity patterns in space and time without the well-known temporal clustering characteristics. While the traditional point process models based on Poisson processes or the Epidemic-Type-Aftershock-Sequences (ETAS) model are designed overall for natural seismicity, modelling approaches for earthquakes with strongly deviating characteristics are missing.
The first step in I10 will be the statistical analysis of various catalogues from man-made earthquakes (geothermal and fracking sites, gas fields, mines etc.) using families of potential distributions and parameter estimation techniques. Suitable pattern recognition techniques will help to quantify the spatio-temporal evolution of diffusive seismicity. Then appropriate point process models will be compared and extended in order to reproduce the main characteristics. Sophisticated processes of Cox and Levy type will also be considered for this aim. Non-stationarity can be modelled by extending the change-point methods from project I2 to more gradual changes. If specific distributions can be approximated sufficiently by normal distributions, tools of data assimilation and reproducing kernel Hilbert spaces might be applied.
We expect to obtain point process models which are suitable to describe seismicity that deviates from the typical Gutenberg-Richter- and Omori-type earthquakes. This will provide a better understanding of the underlying processes and the related hazard.
Dedicated Regional Cluster: no specific cluster