Thermal, seismic and infrasonic evidences of variable degassing rates at Stromboli volcano

• Published in: Journal of volcanology and geothermal research Vol. 118; no. 3; pp. 285 - 297
• Main Authors: Ripepe, Maurizio, Harris, Andrew J.L., Carniel, Roberto
• Format: Journal Article
• Language: English
• Published: Lausanne Elsevier B.V 30-11-2002; Amsterdam Elsevier; New York, NY
• Subjects: conduit processes; convection; Crystalline rocks; degassing; Earth sciences; Earth, ocean, space; Exact sciences and technology; Igneous and metamorphic rocks petrology, volcanic processes, magmas; infrasound; Stromboli; thermal; Aeolian Islands; Tyrrhenian Sea; West Mediterranean; Stromboli; convection; thermal; degassing; infrasound; conduit processes; Stromboli; time series analysis; acoustical emissions; eruptive cycles; models; activity; strombolian-type eruptions; velocity; earthquakes; thermal emission; frequency; vents; amplitude; fluctuations; temperature; style; explosions; Mediterranean Sea
• ISSN: 0377-0273; 1872-6097
• DOI: 10.1016/S0377-0273(02)00298-6

During June 1999, we measured the amplitude and rate (number of events per second) at which gas exited the vent at Stromboli volcano as discrete gas bursts or puffs. This allowed us to identify two styles of gas burst (puffing) activity. The first is characterized by frequent, rapidly rising puffs, the second by less frequent, slowly rising puffs. Each style persisted over 5–40-min-long durations and was associated with a high and low number of strombolian explosions per hour, respectively. Each period was also associated with characteristic delay times between the arrival of the infrasonic and thermal signals during strombolian explosions; the delays were longer during vigorous puffing periods. To explain our observations, we propose a model in which the degassing process cycles between vigorous and weak degassing phases. During vigorous degassing phases, bubble layers ascend the conduit at a frequency of 0.5–1.0 s
−1. This high degassing level reflects a gas-rich magma column and leads to an increased rate in the formation of shallow foams and, hence, an increase in puffing and explosive activity, as well as a higher free surface level and/or gas jet velocity. During weak phases, bubble layers ascend the conduit at a reduced frequency of 0.2–0.3 s
−1. During such times the magma column is poor in gas. This leads to a decreased rate of foam layer formation and hence a reduction in puffing and explosive activity, as well as a lower free surface level and/or gas jet velocity. Variations in puffing activity can thus be used to track changes in the rate at which the shallow system is supplied by fresh, gas-rich magma. Our observations indicate that the two degassing styles last from 5 to 40 min and that the switch from one to the other occurs over a matter of minutes.