By Sylvia J.; Olson, Everett C. (editors) Czerkas
Dinosaurs: earlier and current 2 quantity Set
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Extra info for Dinosaurs Past and Present. Volume 2
D INGWELL , D. B. 1998. Recent experimental progress in the physical description of silicic magma relevant to explosive volcanism. In: G ILBERT , G. S. & S PARKS , R. S. G. (eds) The Physics of Explosive Volcanic Eruptions. Geological Society, London, Special Publication, 145, 9–26. H URWITZ , S. & N AVON , O. 1994. Bubble nucleation in rhyolitic melts — experiments at high-pressure, temperature, and water-content. Earth and Planetary Science Letters, 122, 267–280. I CHIHARA , M. & K AMEDA , M.
C OMMANDER , K. W. & P ROSPERETTI , A. 1989. Linear pressure waves in bubbly liquids — comparison between theory and experiments. Journal of the Acoustical Society of America, 85, 732– 746. D INGWELL , D. B. 1998. Recent experimental progress in the physical description of silicic magma relevant to explosive volcanism. In: G ILBERT , G. S. & S PARKS , R. S. G. (eds) The Physics of Explosive Volcanic Eruptions. Geological Society, London, Special Publication, 145, 9–26. H URWITZ , S. & N AVON , O.
The Q(f, depth) conduit profiles for NMF conditions. We present a comparison between an incompressible profile (following Collier et al. 2006) and a visco-elastic profile, accounting also for melt compressibility. The dashed area for f , 1 Hz indicates that both profiles are a close approximation to their corresponding numerical solution only from c. 1 Hz and higher. The addition of compressibility leads to very different profiles than the ones presented in Collier et al. (2006). Here, we present the lower section of the conduit where compressibility has a major role in the damping properties of the magma.