Unsteady high-pressure flow experiments with applications to explosive volcanic eruptions

• Published in: Journal of Geophysical Research: Solid Earth Vol. 115; no. B6
• Main Authors: Orescanin, M. M., Austin, J. M., Kieffer, S. W.
• Format: Journal Article
• Language: English
• Published: Washington, DC Blackwell Publishing Ltd 01-06-2010; American Geophysical Union
• Subjects: Blasts; Collapse; Disks; Earth sciences; Earth, ocean, space; Exact sciences and technology; experiments; Explosions; explosive volcanic eruptions; Geophysics; Mount St. Helens; Position (location); Unsteady flow; Vents; Volcanic eruptions; Volcanoes; Supersonic flow; experimental studies; Travel time; time scales; Volcanic eruption; vulcanian-type eruptions; Position; reservoirs; digital simulation; Unsteady flow; pressure; high pressure; vents; far-field; Jet; equilibrium; frame structure; Diameter; collapse
• ISSN: 0148-0227; 2169-9313; 2156-2202; 2169-9356
• DOI: 10.1029/2009JB006985

Motivated by the hypothesis that volcanic blasts can have supersonic regions, we investigate the role of unsteady flow in jets from a high‐pressure finite reservoir. We examine the processes for formation of far‐field features, such as Mach disk shocks, by using a shock tube facility and numerical experiments to investigate phenomena to previously unobtained pressure ratios of 250:1. The Mach disk shock initially forms at the edges of the vent and moves toward the centerline. The shock is established within a few vent diameters and propagates downstream toward the equilibrium location as the jet develops. The start‐up process is characterized by two different timescales: the duration of supersonic flow at the nozzle exit and the formation time of the Mach disk shock. The termination process also is characterized by two different timescales: the travel time required for the Mach disk shock to reach its equilibrium position and the time at which the Mach disk shock begins significantly to collapse away from its equilibrium position. The critical comparisons for the formation of steady state supersonic regions are between the two start‐up timescales and the termination timescales. We conclude that for typical vulcanian eruptions and the Mount St. Helens directed blast, the Mach disk shock could have formed near the vent, and that there was time for it to propagate a distance comparable to its equilibrium location. These experiments provide a framework for analysis of short‐lived volcanic eruptions and data for benchmarking simulations of jet structures in explosive volcanic blasts.