TTE92
Monitoreo de gases volcánicos: análisis de emisiones de dióxido de azufre…
ABSTRACT
The Láscar volcano, located in the Central Andes, is the most active volcanic system
in northern Chile. Its activity began before the last glacial period (40-50 ka) and continues to
this day with minor explosions every 2-3 years. As the main character, Láscar presents
constant degassing at its summit, therefore, to understand its origin and current fluctuation,
an analysis of sulfur dioxide (SO 2 ) emissions was performed, with data measured during four
years (2017-2021) by DOAS instrument of the Volcanological Observatory of the Southern
Andes (OVDAS).
The SO2 emissions database, associated with wind speed and the number of
measurements made by the instrument, were analyzed according to the type of activity and
volcanic alert presented by the volcano during the study period. From this, three periods of
interest were identified: (1) pre-yellow alert: August 2017 to February 2018, (2) yellow alert:
March to August 2018, and (3) post-yellow alert: September 2018 to August 2021; which
conclude a state of passive degassing fluctuating between 275 to 1.142 t/d of SO 2 . However,
from the graphs made, an oscillatory pattern was identified with maximum amplitude during
the austral winter, increase in measurements without detecting SO 2 , and anomalies above
2.000 t/d of SO 2 , which when linked to other precursor parameters of volcanic activity (height
of the outgassing column, surface thermal volcanic activity, and the number of seismic events
type Volcano-Tectonic Long-Period and Screw type) allowed generating a comprehensive
multi-parametric analysis. Thus, it was identified that hydrothermal activity, seasonal
change, and magma ascent dynamics influence volcanic SO 2 emission, generating three
degassing patterns: (1) Low SO 2 volcanic-hydrothermal degassing, (2) SO 2 emissions
influenced by wind velocity, and (3) SO 2 emissions in response to magmatic activity.
In summary, the eruptive activity of the Láscar volcano identified during March 2018
and March 2019, would start with a deep seismic activity to then develop shallow volcanic
activity where SO 2 amounts above 2.429 t/d are emitted. Therefore, it is demonstrated that
SO 2 monitoring, when complemented with other parameters, allows us to get a little closer
to the understanding of volcanic behavior.
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