SPIN | Seismological Parameters and INstrumentation

Summary
The seismic wavefield carries the imprint of material it crossed. We now understand that seismic wavefields alter the material when they pass through it and that these changes are measurable. This is important, because the dynamic response of Earth’s material directly affects our societies: geomaterial alterations are associated with many natural hazards, such as volcanic eruptions, landslides, earthquakes, and the structural health of civil structures such as bridges and buildings. Traditional seismic sensors - global and regional networks of seismometers - provide us with high temporal resolution, but sparse spatial resolution.
Right now, new sensing technologies (fiber-optic cables (DAS), large-N arrays, rotation sensors) are emerging that can give us much more detailed spatial information about how the seismic wavefield behaves. This means that we can study changes in local material properties, and investigate complex behavior of materials as they deform under small strain. These sensing technologies are reaching a level of maturity where they can be incorporated into common seismological observation practice.
For this new era of seismological instrumentation and observation fundamentally new skills need to be developed. In SPIN, we will train the next generation of scientists to develop novel views about the dynamic behaviour of Earth materials, and in particular how to observe them with the revolutionary new sensing systems at hand. It is currently enigmatic how to combine these sensor types to optimize resolution power. This research and training will impact the way we understand solid Earth processes, how we interrogate the Earth’s geomechanical behavior, and the way we forecast natural hazards.
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More information & hyperlinks
Web resources: https://cordis.europa.eu/project/id/955515
Start date: 01-03-2021
End date: 31-08-2025
Total budget - Public funding: 4 087 891,80 Euro - 4 087 891,00 Euro
Cordis data

Original description

The seismic wavefield carries the imprint of material it crossed. We now understand that seismic wavefields alter the material when they pass through it and that these changes are measurable. This is important, because the dynamic response of Earth’s material directly affects our societies: geomaterial alterations are associated with many natural hazards, such as volcanic eruptions, landslides, earthquakes, and the structural health of civil structures such as bridges and buildings. Traditional seismic sensors - global and regional networks of seismometers - provide us with high temporal resolution, but sparse spatial resolution.
Right now, new sensing technologies (fiber-optic cables (DAS), large-N arrays, rotation sensors) are emerging that can give us much more detailed spatial information about how the seismic wavefield behaves. This means that we can study changes in local material properties, and investigate complex behavior of materials as they deform under small strain. These sensing technologies are reaching a level of maturity where they can be incorporated into common seismological observation practice.
For this new era of seismological instrumentation and observation fundamentally new skills need to be developed. In SPIN, we will train the next generation of scientists to develop novel views about the dynamic behaviour of Earth materials, and in particular how to observe them with the revolutionary new sensing systems at hand. It is currently enigmatic how to combine these sensor types to optimize resolution power. This research and training will impact the way we understand solid Earth processes, how we interrogate the Earth’s geomechanical behavior, and the way we forecast natural hazards.

Status

SIGNED

Call topic

MSCA-ITN-2020

Update Date

28-04-2024
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Horizon 2020
H2020-EU.1. EXCELLENT SCIENCE
H2020-EU.1.3. EXCELLENT SCIENCE - Marie Skłodowska-Curie Actions (MSCA)
H2020-EU.1.3.1. Fostering new skills by means of excellent initial training of researchers
H2020-MSCA-ITN-2020
MSCA-ITN-2020