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Chapter 11 - Magma–water interactions

Published online by Cambridge University Press:  05 March 2013

By
Ken Wohletz ,
Bernd Zimanowski  and
Ralf Büttner
Edited by
Sarah A. Fagents ,
Tracy K. P. Gregg  and
Rosaly M. C. Lopes
Sarah A. Fagents
Affiliation:
University of Hawaii, Manoa
Tracy K. P. Gregg
Affiliation:
State University of New York, Buffalo
Rosaly M. C. Lopes
Affiliation:
NASA-Jet Propulsion Laboratory, California
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Summary

Overview

Magma–water interaction is an unavoidable consequence of the hydrous nature of the Earth’s crust, and may take place in environments ranging from submarine to desert regions, producing volcanic features ranging from passively effused lava to highly explosive events. Hydrovolcanism is the term that describes this interaction at or near the Earth’s surface, and it encompasses the physical and chemical dynamics that determine the resulting intrusive or extrusive behavior, and the character of eruptive products and deposits. The development of physical theory describing the energetics and the hydrodynamics (dynamics of fluids and solids at high strain rates) of magma–water interaction relies on an understanding of the physics of water behavior in conditions of rapid heating, the physics of magma as a material of complex rheology, and the physics of the interaction between the two, as well as detailed field observations and interpretation of laboratory experiments. Of primary importance to address are the nature of heat exchange between the magma and water during interaction, the resulting fragmentation of the magma, and the constraints on system energetics predicted by equilibrium and non-equilibrium thermodynamics. Taken together, these approaches elucidate the relationships among aqueous environment, interaction physics, and eruptive phenomena and landforms.

Introduction: magma and the hydrosphere

The vast majority of volcanic eruptions take place under water because most volcanism concentrates at mid-oceanic ridges where new oceanic crust is produced. By definition, every kind of extrusive subaqueous volcanism on Earth is hydrovolcanic since some degree of water interaction must take place. The hydrosphere also exists in continental areas, as the consequence not only of lakes and rivers, but also of groundwater and hydrous fluids that circulate in joints and faults in the upper crust and fill pore space in sedimentary rocks. Such locations are typically referred to as geohydrological environments. As a consequence, subaerial volcanism is commonly influenced by magma–water interaction. Chapter 12 describes deep-sea eruptions in greater detail, whereas this chapter focuses on magma–water interaction in surface and near-surface environments.

Type
Chapter
Information
Modeling Volcanic Processes
The Physics and Mathematics of Volcanism
 , pp. 230 - 257
Publisher: Cambridge University Press
Print publication year: 2013

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References

Austin-Erickson, A., Büttner, R., Dellino, P., Ort, M. H., and Zimanowski, B. (2008). Phreatomagmatic explosions of rhyolitic magma: experimental and field evidence. Journal of Geophysical Research, 113, B11201, doi:.CrossRefGoogle Scholar
Baierlein, R. (1999). Thermal Physics. Cambridge University Press, 456 pp.CrossRefGoogle Scholar
Bejan, A. and Eden, M. (1999). Thermodynamic Optimization of Complex Energy Systems. Springer.CrossRefGoogle Scholar
Bischoff, J. L. and Rosenbauer, R. J. (1988). Liquid-vapor relations in the critical region of the system NaCl-H2O from 380 to 415°C: a refined determination of the critical point and two-phase boundary of seawater. Geochimica et Cosmochimica Acta, 52, 2121–2126.CrossRefGoogle Scholar
Board, S. J., Farmer, C. L. and Poole, D. H. (1975). Fragmentation in thermal explosions. Journal of Heat and Mass Transfer, 17, 331–339.CrossRefGoogle Scholar
Bonatti, E. (1976). Mechanisms of deep sea volcanism in the South Pacific. In Researches in Geochemistry 2, ed. Ableson, P. H.. New York: John Wiley & Sons, pp. 453–491.Google Scholar
Buchanan, D. J. (1974). A model for fuel-coolant interaction. Journal of Physics D: Applied Physics, 7, 1441–1457.CrossRefGoogle Scholar
Buchanan, D. J. and Dullforce, T. A. (1973). Mechanism for vapor explosions. Nature, 245, 32–34.CrossRefGoogle Scholar
Burnham, C. W., Holloway, J. R. and Davies, N. F. (1969). Thermodynamic properties of water to 1000˚C and 10 000 bars. Geological Society of America Special Paper, 132, 1–96.CrossRefGoogle Scholar
Büttner, R. and Zimanowski, B. (1998). Physics of thermohydraulic explosions. Physics Reviews E, 57(5), 5726–5729.CrossRefGoogle Scholar
Büttner, R., Zimanowski, B., Blumm, J. and Hagemann, L. (1998). Thermal conductivity of a volcanic rock material (olivine-melilitite) in the temperature range between 288 and 1470 K. Journal of Volcanology and Geothermal Research, 80, 293–302.CrossRefGoogle Scholar
Büttner, R., Dellino, P. and Zimanowski, B. (1999). Identifying modes of magma/water interaction from the surface features of ash particles. Nature, 401, 688–690.CrossRefGoogle Scholar
Büttner, R., Zimanowski, B., Lenk, C., Koopmann, A. and Lorenz, V. (2000). Determination of thermal conductivity of natural silicate melts. Applied Physics Letters, 77, 1810–1812.CrossRefGoogle Scholar
Büttner, R., Dellino, P., LaVolpe, L., Lorenz, V. and Zimanowski, B. (2002). Thermohydraulic explosions in phreatomagmatic eruptions as evidenced by the comparison between pyroclasts and products from Molten Fuel Coolant Interaction experiments. Journal of Geophysical Research, 107, doi: .CrossRefGoogle Scholar
Büttner, R., Zimanowski, B., Mohrholz, C.-O. and Kümmel, R. (2005). Analysis of thermohydraulic explosion energetics. Journal of Applied Physics, 98, 043524, doi:.CrossRefGoogle Scholar
Büttner, R., Dellino, P., Raue, H., Sonder, I., and Zimanowski, B. (2006). Stress induced brittle fragmentation of magmatic melts: Theory and experiments. Journal of Geophysical Research, 111, B08204, doi:.CrossRefGoogle Scholar
Carlisle, D. (1963). Pillow breccias and their aquagene tuffs: Quadra Island, British Columbia. American Journal of Science, 71, 48–71.Google Scholar
Corradini, M. L. (1981). Phenomenological modelling of the triggering phase of small-scale steam explosion experiments. Nuclear Science and Engineering, 78, 154–170.CrossRefGoogle Scholar
Courant, R. and Friedrichs, K. O. (1948). Supersonic Flow and Shock Waves. New York: Springer, 464 pp.Google Scholar
Cronenberg, A. W. (1980). Recent developments in the understanding of energetic molten fuel-coolant interactions. Nuclear Safety, 21, 319–337.Google Scholar
Delaney, P. T. (1982). Rapid intrusion of magma into wet rock: ground water flow due to pressure increases. Journal of Geophysical Research, 87, 7739–7756.CrossRefGoogle Scholar
Dellino, P., Isaia, R., La Volpe, L. and Orsi, G. (2001). Statistical analysis of textural data from complex pyroclastic sequences: Implications for fragmentation processes of the Agnano Monte Spina Tephra (4.1 ka), Phlegraean Fields, southern Italy. Bulletin of Volcanology, 63, 443–461.Google Scholar
Drumheller, D. S. (1979). The initiation of melt fragmentation in fuel-coolant interactions. Nuclear Science and Engineering, 72, 347–356.CrossRefGoogle Scholar
Ebert, H.-P., Hernberger, F., Fricke, J. et al. (2003). Thermophysical properties of a volcanic rock material. High Temperatures – High Pressures, 34, 561–668.CrossRefGoogle Scholar
Fisher, R. V. and Schmincke, H.-U. (1984). Pyroclastic Rocks. Berlin: Springer-Verlag, 472 pp.CrossRefGoogle Scholar
Fisher, R. V. and Waters, A. C. (1970). Base-surge bed forms in maar volcanoes. American Journal of Science, 268, 157–180.CrossRefGoogle Scholar
Frazzetta, G., La Volpe, L. and Sheridan, M. F. (1983). Evolution of the Fossa cone, Vulcano. Journal of Volcanology and Geothermal Research, 17, 329–360.CrossRefGoogle Scholar
Fuller, R. E. (1931). The aqueous chilling of basaltic lava on the Columbia River Plateau. American Journal of Science, 21, 281–300.CrossRefGoogle Scholar
Grady, D. E. (1982). Local inertial effects in dynamic fragmentation. Journal of Applied Physics, 53, 322–523.CrossRefGoogle Scholar
Grady, D. E. (1985). Fragmentation under impulsive stress loading. In Fragmentation by Blasting, ed. Fourney, W. L. and Boade, R. R.. Society for Experimental Mechanics, Brookfield Center, pp. 63–72.Google Scholar
Greer, S. C. and Moldover, M. R. (1981). Thermodynamic anomalies at critical points of fluids. Annual Reviews of Physical Chemistry, 32, 233–265.CrossRefGoogle Scholar
Heiken, G. (1971). Tuff rings: examples from the Fort Rock-Christmas Lake Valley, south-central Oregon. Journal of Geophysical Research, 76, 5615–5626.CrossRefGoogle Scholar
Heiken, G. and Wohletz, K. H. (1985). Ash, Volcanic. Berkeley, CA: University of California Press, 245 pp.
Heiken, G. and Wohletz, K. (1991). Fragmentation processes in explosive volcanic eruptions. In Sedimentation in Volcanic Settings, ed. Fisher, R. V. and Smith, G., Society of Sedimentary Geology Special Publication, 45, 19–26.Google Scholar
Henry, R. E. and Fauske, H. K. (1981). Required initial conditions for energetic steam explosions. In Fuel–Coolant Interactions. New York: American Society of Mechanical Engineers, Report HTD-V19.Google Scholar
Herrmann, H. J. and Roux, S. (1990). Statistical Models for the Fracture of Disordered Media, Amsterdam: North-Holland.Google Scholar
Holloway, J. R. (1977). Fugacity and activity of molecular species in supercritical fluids. In Thermodynamics in Geology, ed. Fraser, D. G.. Dordrecht, Holland: Reidel, pp. 161–181.Google Scholar
Honnorez, H. and Kirst, P. (1975). Submarine basaltic volcanism: morphometric parameters for discriminating hyaloclastites from hyalotuffs. Bulletin of Volcanology, 39, 441–465.CrossRefGoogle Scholar
Jaggar, T. A. (1949). Steam Blast Volcanic Eruptions; a Study of Mount Pelée in Martinique as a Type Volcano. Hawaii Volcano Observatory, 4th Special Report. Honolulu: The Hawaiian Volcano Research Association, 137.
Kieffer, S. W. and Delany, J. M. (1979). Isentropic decompression of fluids from crustal and mantle pressures. Journal of Geophysical Research, 84, 1611–1620.CrossRefGoogle Scholar
Kokelaar, P. (1986). Magma-water interactions in subaqueous and emergent basaltic volcanism. Bulletin of Volcanology, 48, 275–290.CrossRefGoogle Scholar
Krauskopf, K. B. (1967). Introduction to Geochemistry. New York: McGraw-Hill.Google Scholar
Landau, L. D. and Lifshitz, B. M. (1959). Fluid Mechanics: Volume 6, Course of Theoretical Physics. New York: Pergamon.Google Scholar
Mastin, L. G. (2007). Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds. Journal of Geophysical Research, 112, B02203, doi:.CrossRefGoogle Scholar
Moore, J. G., Nakamura, K. and Alcaraz, A. (1966). The 1965 eruption of Taal Volcano. Science, 151, 995–960.CrossRefGoogle ScholarPubMed
Morrissey, M., Zimanowski, B., Wohletz, K., and Büttner, R. (2000). Phreatomagmatic fragmentation. In Encyclopedia of Volcanism, ed. Sigurdsson, H.. London: Academic Press, pp. 431–445.Google Scholar
Muffler, L. J. P., White, D. E. and Truesdell, A. H. (1971). Hydrothermal explosion craters in Yellowstone National Park. Geological Society of America Bulletin, 82, 723–740.CrossRefGoogle Scholar
Nairn, I. A. and Solia, W. (1980). Late Quaternary hydrothermal explosion breccias at Kawerau geothermal field, New Zealand. Bulletin of Volcanology, 43, 1–13.CrossRefGoogle Scholar
Noe-Nygaard, A. (1940). Subglacial volcanic activity in ancient and recent times. Folia Geographica Danica, 1, no. 2.Google Scholar
Ollier, C. D. (1974). Phreatic eruptions and maars. In Physical Volcanology, ed. Civett, L., Gasparini, P., Luongo, G., and Rapolla, A.. New York: Elsevier, pp. 289–310.Google Scholar
Ruggles, A E., Drew, D. A., Lahey, R. T., Jr. and Scarton, H. A. (1989). The relationship between standing waves, pressure pulse propagation and the critical flow rate in two-phase mixtures. Journal of Heat Transfer, 111, 467–473.CrossRefGoogle Scholar
Ruggles, A. E., Vasiliev, A. D., Brown, N. W. and Wendel, M. W. (1997). Role of heater thermal response in reactor thermal limits during oscillatory two-phase flows. Nuclear Science and Engineering, 125, 75–83.CrossRefGoogle Scholar
Schmid, A., Sonder, I., Seegelken, R. et al. (2010). Experiments on the heat discharge at the dynamic magma-water-interface. Geophysical Research Letters, 37, L20311, doi: CrossRefGoogle Scholar
Self, S., Kienle, J. and Huot, J.-P. (1980). Ukinrek maars, Alaska, II. Deposits and formation of the 1977 craters. Journal of Volcanology and Geothermal Research, 7, 39–65.CrossRefGoogle Scholar
Servicos Geologicos de Portugal (1959). Le volcanisme de l’isle de Faial et l’éruption de volcan de Capelinhos. Memorandum 4, 100 pp.Google Scholar
Sheridan, M. F. and Wohletz, K. H. (1983). Hydrovolcanism: basic considerations and review. Journal of Volcanology and Geothermal Research, 17, 1–29.CrossRefGoogle Scholar
Sigvaldason, G. (1968). Structure and products of subaquatic volcanoes in Iceland. Contributions to Mineralogy and Petrology, 18, 1–16.CrossRefGoogle Scholar
Sonder, I., Büttner, R. and Zimanowski, B. (2006). Non-Newtonian viscosity of basaltic magma. Geophysical Research Letters, 33, L02303, doi:.CrossRefGoogle Scholar
Sonder, I., Schmid, A., Seegelken, R., Zimanowski, B. and Büttner, R. (2011). Heat source or heat sink: What dominates behavior of non-explosive magma-water interaction?Journal of Geophysical Research, 116, B09203, doi:.CrossRefGoogle Scholar
Sourirajan, S. and Kennedy, G. C. (1962). The system H2O-NaCl at elevated temperatures and pressures. American Journal of Science, 260, 115–141.CrossRefGoogle Scholar
Tazieff, H. K. (1958). L’éruption 1957–1958 et la tectonique de Faial (Azores). Annales de la Sociéte Géologique de Belgique, 67, 14–49.Google Scholar
Theofanous, T. G. (1995). The study of steam explosion in nuclear systems. Nuclear Engineering Design, 155, 1–26.CrossRefGoogle Scholar
Thorarinsson, S. (1964). Surtsey, the New Island in the North Atlantic. Reykjavik: Almenna Bokofelagid.Google Scholar
Turekian, K. K. (1968). Oceans. New Jersey: Prentice-Hall, 150 pp.Google Scholar
Varotsos, P. A. and Alexopoulos, K. D. (1986). Thermodynamics of Point Defects and Their Relation with Bulk Properties. Amsterdam: North-Holland.Google Scholar
Waters, A. C. and Fisher, R. V. (1971). Base surges and their deposits: Capelinhos and Taal Volcanoes. Journal of Geophysical Research, 76, 5596–5614.CrossRefGoogle Scholar
Wentworth, C. K. (1938). Ash Formations of the Island of Hawaii. Hawaii Volcano Observatory, 3rd Special Report. Honolulu: Hawaiian Volcano Research Association, 183 pp.Google Scholar
White, J. D. L. (1996). Impure coolants and interaction dynamics of phreatomagmatic eruptions. Journal of Volcanology and Geothermal Research, 74, 155–170.CrossRefGoogle Scholar
Wohletz, K. H. (1983). Mechanisms of hydrovolcanic pyroclast formation: grain-size, scanning electron microscopy, and experimental results. Journal of Volcanology and Geothermal Research, 17, 31–63.CrossRefGoogle Scholar
Wohletz, K. H. (1986). Explosive magma-water interactions: thermodynamics, explosion mechanisms, and field studies. Bulletin of Volcanology, 48, 245–264.CrossRefGoogle Scholar
Wohletz, K. H. (1987). Chemical and textural surface features of pyroclasts from hydrovolcanic eruption sequences. In Clastic Particles, ed. Marshall, J. R.. New York: Van Nostrand Reinhold, pp. 79–97.Google Scholar
Wohletz, K. H. (1993). Hidrovolcanismo. In Nuevas Tendencias: La Volcanologia Actual, ed. Martí, J. and Araña, V.. Madrid: Consejo Superior de Investigaciones Cientificas, pp. 99–196.Google Scholar
Wohletz, K. H. (2003). Water/magma interaction: physical considerations for the deep submarine environment. In Submarine Explosive Volcanism, American Geophysical Union Monograph, 140, 25–49.CrossRef
Wohletz, K. H. and Heiken, G. (1992). Volcanology and Geothermal Energy. Berkeley, CA: University of California Press.Google Scholar
Wohletz, K. H. and McQueen, R. G. (1984). Experimental studies of hydromagmatic volcanism. In Explosive Volcanism: Inception, Evolution, and Hazards. Washington: National Academy Press, pp. 158–169.Google Scholar
Wohletz, K. H. and Sheridan, M. F. (1983). Hydrovolcanic explosions II. Evolution of basaltic tuff rings and tuff cones. American Journal of Science 283, 385–413.CrossRefGoogle Scholar
Wohletz, K. H., McQueen, R. G. and Morrissey, M. (1995a). Analysis of fuel-coolant interaction experimental analogs of hydrovolcanism. In Intense Multiphase Interactions, ed. Theofanous, T. G. and Akiyama, M.. Proceedings of US (NSF) Japan (JSPS) Joint Seminar, Santa Barbara, CA, pp. 287–317.Google Scholar
Wohletz, K. H., Orsi, G. and de Vita, S. (1995b). Eruptive mechanisms of the Neapolitan Yellow Tuff interpreted from stratigraphy, chemistry, and granulometry. Journal of Volcanology and Geothermal Research, 67, 263–290.CrossRefGoogle Scholar
Yew, C. H. and Taylor, P. A. (1994). A thermodynamic theory of dynamic fragmentation. International Journal of Impact Engineering, 15, 385–394.CrossRefGoogle Scholar
Yuen, W. W. and Theofanous, T. G. (1994). The prediction of 2D thermal detonations and resulting damage potential. Nuclear Engineering Design, 155, 289–309.CrossRefGoogle Scholar
Zel’dovich, Ya. B. and Kompaneets, A. S. (1960). Theory of Detonation. London: Academic Press.Google Scholar
Zel’dovich, Ya. B. and Raizer, Yu. P. (1966). Physics of Shock Waves and High-Temperature Hydrodynamic Phenomena, Volumes I and II. New York: Academic Press.Google Scholar
Zimanowski, B. (1998). Phreatomagmatic explosions. In From Magma to Tephra, ed. Freundt, A. and Rosi, M.. Developments in Volcanology, 4. Amsterdam: Elsevier, pp. 25–54.Google Scholar
Zimanowski, B. and Büttner, R. (2002). Dynamic mingling of magma and liquefied sediments. In Peperite, ed. Skilling, I., White, J. D. L. and McPhie, J.. Amsterdam: Elsevier, pp. 37–44.Google Scholar
Zimanowski, B. and Büttner, R. (2003). Phreatomagmatic explosions in subaqueous eruptions. In Explosive Subaqueous Volcanism, ed. White, J. D. L., Smellie, J. L. and Clague, D.. American Geophysical Union Monograph, 140. Washington, pp. 51–60.Google Scholar
Zimanowski, B., Fröhlich, G. and Lorenz, V. (1991). Quantitative experiments on phreatomagmatic explosions. Journal of Volcanology and Geothermal Research, 48, 341–358.CrossRefGoogle Scholar
Zimanowski, B., Büttner, R., Lorenz, V. and Häfele, H.-G. (1997a). Fragmentation of basaltic melt in the course of explosive volcanism. Journal of Geophysical Research, 107, 803–814.CrossRefGoogle Scholar
Zimanowski, B., Büttner, R. and Nestler, J. (1997b). Brittle reaction of a high temperature ion melt. Europhysics Letters, 38, 285–289.CrossRefGoogle Scholar
Zimanowski, B., Wohletz, K. H., Büttner, R. and Dellino, P. (2003). The volcanic ash problem. Journal of Volcanology and Geothermal Research, 122, 1–5.CrossRefGoogle Scholar

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