Slug Stability in Flaring Geometries and Ramifications for Lava Lake Degassing. Issue 12 (21st December 2018)

• Record Type: Journal Article
• Authors: Qin, Zhipeng; Soldati, Arianna; Velazquez Santana, Liannie C.; Rust, Alison C.; Suckale, Jenny; Cashman, Katharine V.
• Is Part Of: Journal of geophysical research. Volume 123:Issue 12(2018)
• Page Start: 10, 431
• Page End: 10, 448
• Publication Date: 2018-12-21
• Subjects: lava lake -- gas slug -- stability -- geometry -- numerical simulation -- experiment; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1029/2018JB016113
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: Long‐lived, persistently active lava lakes are rare but have been studied extensively because they may provide a natural laboratory for studying magmatic convection in basaltic and other low‐viscosity volcanoes. However, lava lakes differ from other volcanic systems in various ways, particularly geometry: the presence of the lava lake requires a sudden and significant flaring of the conduit. The goal of this paper is to advance our understanding of the effect that a sudden increase in the conduit width has on the stability of large gas slugs and bubbles ascending from the plumbing system. We investigate this question by linking analog laboratory experiments to direct numerical simulations in two dimensions. We find that the rapid change in the geometry associated with the transition from the conduit to the lava lake causes large gas slugs to break up. The nondimensional regime over which we observe the breakup depends sensitively on the flare angle of the lava lake and the importance of inertial effects in the flow, implying that degassing‐related eruptive activity at open‐system volcanoes is sensitive to the upper conduit and lake geometries. Applying this idea to the likely geometries and viscosities of actual lava lakes, our study suggests that all lava lakes except Erebus fall well within the regime where large gas slugs are prone to breakup. Key Points: The rapid change in the geometry associated with the transition from the conduit to the lava lake causes large gas slugs to break up Stability of the gas slug depends sensitively on the geometry and on the Reynolds number Most lava lakes fall well within the regime where large gas slugs are prone to breakup