The occurrence of felt earthquakes due to gas production in Groningen has initiated
numerous studies and model attempts to understand and quantify induced seismicity in this …

The increase in number and strength of shallow induced seismicity connected to the
Groningen gas field since 2003 and the occurrence of a ML 3.6 event in 2012 started the …

In different subsurface energy technologies, traffic light systems (TLSs) have been
implemented for limiting the strength of induced seismicity. Despite their widespread …

We implement a Coulomb rate‐and‐state approach to explore the nonlinear relation
between stressing rate and seismicity rate in the Groningen gas field. Coulomb stress rates …

Over 320 induced earthquakes with magnitude M≥ 1.5, including 38 with M≥ 2.5 in the
Groningen gas field, the Netherlands, are statistically analysed, and their societal impacts …

Recently, growing earthquake activity in the northeastern Netherlands has aroused
considerable concern among the 600,000 provincial inhabitants. There, at 3 km deep, the …

The Groningen gas field in the Netherlands has a significant level of induced seismicity; this
seismicity is attributed to fluid withdrawal not fluid injection. This is one of the most …

The Groningen gas field in the Netherlands experienced an immediate reduction in seismic
events in the year following a massive cut in production. This reduction is inconsistent with …

The intermittent storage of hydrogen in subsurface porous media such as depleted gas
fields could be pivotal to a successful energy transition. Numerical simulations investigate …

In the Netherlands, over 190 gas fields of varying size have been exploited, and 15% of
these have shown seismicity. The prime cause for seismicity due to gas depletion is stress …