''Heritage buildings are often subjected to loading conditions that they were not exposed to in their earlier life span. Induced earthquakes in non-seismic regions caused by energy exploitation activities, or strains in the ground that are caused by the climate changes, are new phenomena that alter the usual loading situations for historical buildings.In this paper, monitoring results of a historical building in Groningen (Netherlands) in case of induced seismicity as well as climate change effects has been presented. Long-term monitoring results, detected cracks and relevance of the monitoring data are discussed. In the special case of Groningen, weak and agricultural soil properties dominate the structural response in the region. The gas extraction activities caused a soil subsidence in the giant Groningen Gas Field, resulting decameters of settlement in the entire area, thus an increase of the ground water level in respect to the ground surface. This is the reason why the heritage structures in the region are more vulnerable to soil-water-foundation interactions caused by climate change as compared to the time these heritage structures were constructed. The ground water monitoring as well as the interaction of soil movements with the structural response become important. The study presented here suggests ways on how to effectively monitor historical structures subjected to induced seismicity as well as harsh climate effects at the same time.It was shown here that the newly developed cracks on the structure were detected in a very narrow time window, coinciding with extreme drought and a small induced earthquake at the same time. One explanation provided here is that the soil parameters, such as shrinking of water-sensitive soil layers, in combination with small earthquakes, may cause settlements. The soil effects may superimpose with the earthquake effects eventually causing small cracks and damage. The effects of the climate change on historical buildings is rather serious, and structures on similar soil conditions around the world would need detailed monitoring of not only the structure itself but also the soil-foundation and ground water conditions.''
''On February 6th, 2023, two severe earthquakes struck southeastern Türkiye near the Syrian border. The first earthquake, Mw7.8, occurred at 04:17 local time in the East Anatolian Fault Zone near the city of Gaziantep. The second earthquake, Mw7.5, occurred approximately 9 h later at 13:24 local time near Elbistan County, in Kahramanmaraş province. These seismic events ruptured multiple segments of the East Anatolian Fault Zone (EAFZ), with rupture lengths exceeding 300 km, and deformation exceeding 5 m on both sides of the faults. In this study, we aim to analyze characteristics of the strong ground motion induced by the mainshocks, focusing on ground motion intensity measures such as the peak ground acceleration (PGA), the peak ground velocity (PGV), and the pseudo-acceleration response spectra (PSA). The first earthquake produced extremely high PGA values in both horizontal (> 2 g) and vertical (> 1 g) components. At near field distances, large PGVs are measured (> 180 cm/s) with more than 30 impulsive motions which may indicate source-related effects. Large spectral demands are also recorded for both earthquakes, partially underestimated by Ground Motion Models (GMMs), especially in the near-field. Specifically, we compare the PSA for horizontal directions with the design spectra provided by both the new and previous Turkish building codes. We also present building and ground damage observations that provide insights into the observed ground motions in the heavily damaged areas.''
The pipelines are buried structures. They move together with the soil during a seismic event. They are affected from ground motions. The project aims to find out the possible effects of Groningen earthquakes on pipelines of Loppersum and Slochteren.This project is devised for conducting an initial probe on the available data to see the possible actions that can be taken, initially on these two pilot villages, Loppersum and Slochteren, for detecting the potential relationship between the past damages and the seismic activity.Lifeline infrastructure, such as water mains and sewerage systems, covering our urbanised areas like a network, are most of the times, sensitive to seismic actions. This sensitivity can be in the form of extended damage during seismic events, or other collateral damages, such as what happened in Christchurch Earthquakes in 2011 in New Zealand when the sewerage system of the city was filled in with tonnes of sand due to liquefaction.Regular damage detection is one of key solutions for operational purposes. The earthquake mitigation, however, needs large scale risk studies with expected spatial distribution of damages for varying seismic hazard levels.
Krewerd is a small village in the North-East side of the Groningen Gas Field. It has 45 houses in total, 2 of which are included in the P50 risk zone and will therefore be assessed by National Coordinator Groningen (NCG). The rest of the houses are not in the priority list and will not be evaluated within 3 years, according to the existing plans of September 2019. It has been made clear by NCG that the usual engineering process, that includes all sorts of engineering calculations and procedures per NPR9998, cannot be followed in Krewerd. This is because the available engineering capacity is being used by NCG at its maximum, for the prior aim of accelerating the assessment and strengthening works in the P50 region. This project is prepared for presentation to NCG as an experimental project at Krewerd and is based on an initial document prepared by Fons Verheijen , a supportive document prepared by Otto Wassenaar , as well as the recent meeting by the two and Ihsan Engin Bal from Hanze. Furthermore, considering that the NCG is seeking an acceleration of the assessment procedure, the village Krewerd may play a role as a pilot.
The Krewerder way where residents are in control combined with accelerated assessment concerning earthquake damage seems to be a better way of tackling the reinforcement operation than the usual procedure (see project 'Experiment Krewerd') However, it is necessary to follow the experiment longer to be able to draw firm conclusions and to investigate how resilience develops over time on the level of individual residents and the community as a whole. This research projects targets this.Conclusions set in a report on how resilience develops over time on the level of individual residents and the community as a whole.The Krewerder way where residents are in control combined with accelerated assessment concerning earthquake damage seems to be a better way of tackling the reinforcement operation than the usual procedure (see project 'Experiment Krewerd') However, it is necessary to follow the experiment longer to be able to draw firm conclusions and to investigate how resilience develops over time on the level of individual residents and the community as a whole. This research projects targets this.
