In order to understand and predict volcanic events even better, a better understanding of the diverse underground processes involved is required. A new way to detect such processes, even if they are very subtle, is to use fibre optic cables as sensors. The analysis of light that is backscattered in them when the cables are deformed by vibrations, for example, has now made it possible for the first time to determine the volcanic signature of the Sicilian volcano Etna very precisely. An international team led by Philippe Jousset from the German Research Centre for Geosciences Potsdam (GFZ) and Gilda Currenti from the Italian Istituto Nazionale di Geofisica e Vulcanologia (INGV), among others, reported on this today in the journal Nature Communications. The method, known as Distributed Acoustic Sensing (DAS), was able to identify seismo-acoustic volcanic activity from a distance and map hidden near-surface volcanic structural features. With its high sensitivity and accuracy, it is proving to be a basis for improved volcano monitoring and hazard assessment.
The challenge of predicting volcanic eruptions
Understanding physical processes prior to and during volcanic eruptions has very much improved in recent years. However, it is still difficult to detect very subtle triggering mechanisms of volcanic phenomena with conventional observation methods such as seismometers. On the one hand, the accuracy of the measurement methods is not sufficient to detect and identify all processes within the volcano, and on the other hand, unknown underground structures distort the observed measurement signals. However, knowledge of even weak activities can be decisive when it comes to predicting and assessing the danger of volcanic eruptions. For example, at the Sicilian volcano Etna, the largest, most active and most visited volcano in Europe, with more than one million people living on its flanks and in its immediate vicinity. Etna's volcanic activity is characterised by frequent explosive eruptions with lava emissions.
Test of a new measurement method on the volcano Etna in Sicily
Philippe Jousset (GFZ), Gilda Currenti (INGV) and their colleagues have now investigated the suitability of fibre optic cables for measuring very weak seismic and volcanic activity. For this purpose, the team deployed a 1.3-kilometre-long fibre-optic cable a good 20 centimetres deep in a scoria layer on the volcano Etna at a distance of about 2 kilometres from the summit craters and measured the strain changes of the cable caused by the various volcanic activities.
The measuring principle with glass fibres
The so-called DAS principle was used for the measurement. DAS stands for "Distributed Acoustic Sensing". Successive light pulses are sent into an optical fibre via an interrogator using a laser. The light, which is partially backscattered by the natural "imperfections" of the fibre, is then analysed. The travel time of the light changes when the fibre deforms or stretches - for example, due to tiny ground movements, acoustic waves or temperature changes. In this way, such events can be detected for instance every metre all along a fibre and measured very precisely.
It was already known that by means of DAS telephone lines made of fibre optics can be used to record earthquakes: Since this has been demonstrated in Iceland in 2018 by GFZ researchers, monitoring seismic activity has been carried out at several places in the world – USA, Switzerland, Japan – and the technique has been applied in other geoscience applications, where ground motions or vibrations are to be measured.
The new fibre-optic method is suitable for the analysis of volcanoes
Now the researchers have demonstrated that the method is also suitable for the accurate analysis and monitoring of volcanoes. "The cable, deployed in a scoria layer, was capable of sensing strain changes associated to Etnean volcanic activity, such as volcanic explosions, small volcanic degassing, local volcano-tectonic earthquakes, as well as to atmospheric phenomena including hail and thunderstorms,” explains Philippe Jousset, lead author of the study and a scientist in the "Geophysical Imaging of the Subsurface" section at GFZ.
The DAS strain rate measurements were validated with measurements carried out with conventional sensors – geophones, broadband seismometers, infrasonic sensors. The locally dense measurements, unachievable with other methodologies, allow to detect and characterize both volcanic explosions as well as the non-linear interactions of the then propagating acoustic wave with the near-surface scoria deposits, triggering resonance phenomena in the subsurface. To quantify hidden subsurface structural features in the measured data and to detect and locate volcanic events with accuracy, standard volcano-seismology analysis, wave and strain propagation modelling tools, and techniques such as wave-field separation and reconstruction were applied. According to GFZ-scientist Benjamin Schwarz, who was also involved in the study, “the spatial resolution offered by fibre-optic strain measurements allows it to extract and amplify very small but important signals that were previously out of reach for quantitative analysis.”
"Our study demonstrates that DAS, with its high sensitivity and accuracy, can be used to efficiently monitor volcanic activity," Jousset sums up. "This is a new contribution that advances the understanding of volcanic processes. And we are convinced that this technique will become a standard for volcano monitoring in the years to come," Gilda Currenti anticipates.
Special advantage of fibre optics: most accurate measurements possible even from great distances
Thanks to its long-distance probing capabilities – currently at least several tens of kilometers –, an interrogator can be set-up in a remote place, making fibre optic observations easier and safer than conventional sensor arrays, which need telemetry, on-site power supply and regular maintenance. “Fibre-optic cables running from the volcano’s summit to remote locations would provide unique opportunities to deepen the understanding of ground response, including estimation of path effects and aiming at better understanding the origin of volcanic phenomena,” says Lotte Krawczyk, also one of the cable diggers and spokesperson of the PoF IV research program at Helmholtz. In addition, availability of fibre optic cable submarine infrastructure close to volcanic islands will be also of great help for studying otherwise largely inaccessible submarine magmatic processes.
Further information about the fibre optic sensing method can be found here.
Philippe Jousset, Gilda Currenti, Benjamin Schwarz, Athena Chalari, Frederik Tilmann, Thomas Reinsch, Luciano Zuccarello, Eugenio Privitera & Charlotte M. Krawczyk, 2022. Fibre optic distributed acoustic sensing of volcanic events. Nature Communications.DOI: 10.1038/s41467-022-29184-w
Dr. Philippe Jousset
Scientist in Section 2.2 Geophysical Imaging
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
Tel.: +49 331 288-1299
Prof. Dr. Charlotte Krawczyk
Programme Director PoF IV Helmholtz
Head of Section 2.2 Geophysical Imaging
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
Tel.: +49 331 288-1281