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  • 1
    Online Resource
    Online Resource
    Singapore : Springer Singapore | Singapore : Imprint: Springer
    Keywords: Mineralogy. ; Geochemistry. ; Geology. ; Natural disasters. ; Eruption ; Kristallisation ; Ausdehnung ; Blasenbildung ; Phasenumwandlung ; Thermodynamik ; Phreatomagmatische Eruption ; Magma ; Ergussgestein ; Gasblase ; Explosive Kristallisation ; Viskosität ; Vulkan ; Vulkanismus ; Bimsstein ; Gefüge ; Kohlendioxid ; Tephra ; Gesteinsbildung ; Gasphase ; Entmischung ; Phasengleichgewicht ; Wasserdampf
    Description / Table of Contents: - Inspired by nature -- Conditions for magma vesiculation -- Mechanism of bubble formation -- Growth and expansion of bubbles -- Temporal development of vesiculation -- Other bubble-related processes -- Cooling crystallization of magma -- Crystallization induced by vesiculation -- CSD (Crystal Size Distribution) -- Application -- Appendix.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXXII, 427 p. 220 illus.)
    Edition: 1st ed. 2022.
    ISBN: 9789811642098
    Series Statement: Advances in Volcanology, An Official Book Series of the International Association of Volcanology and Chemistry of the Earth’s Interior
    Language: English
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  • 2
    Online Resource
    Online Resource
    Singapore :Springer Singapore Pte. Limited,
    Keywords: Magmas-Laboratory manuals. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (449 pages)
    Edition: 1st ed.
    ISBN: 9789811642098
    Series Statement: Advances in Volcanology Series
    Language: English
    Note: Intro -- Preface for English Version -- Preface -- Contents -- Notations -- 1 Inspired by Nature -- 1.1 1986 Izu-Oshima Eruption -- 1.1.1 Changes in Eruption Styles -- 1.1.2 Bubbles and Crystals -- 1.2 Pumice and Plinian Eruption -- 1.2.1 Eruption Emitting Pumice or Scoria -- 1.2.2 Towada Volcano -- 1.2.3 Widespread Volcanic Ash -- 1.2.4 Reticulite: The Ultimate Pumice -- 1.2.5 Volcanic Eruptions as Global Phenomena -- 1.2.6 Variety and Unified Classification of Explosive Eruptions -- 1.3 Lava Dome and Pyroclastic Flow -- 1.3.1 Eruptions that Do Not Produce Pumice or Scoria: Non-explosive Eruptions -- 1.3.2 Heisei Eruption of Unzen Volcano -- 1.3.3 Temporal Change of Discharge Rate -- 1.3.4 Block-and-Ash Flow -- 1.3.5 Interior of Pyroclastic Particles -- 1.3.6 Microlite -- 1.4 Crystallization and Vesiculation of Magma that Cooled down and Solidified -- 1.4.1 Dike as a Place for Cooling Crystallization Experiment in Nature -- 1.4.2 Vesiculation in Dikes -- 1.4.3 Magma Vesiculation as a Driving Force for Volcanic Explosions -- References -- 2 Conditions for Magma Vesiculation -- 2.1 Significance of Equilibrium Theory -- 2.2 Solubility of Gas Components in Liquid and Henry's Law -- 2.3 Dissolution Reaction of Water in Silicate Melt -- 2.4 Change of Solubility with Pressure: Burnham's Model -- 2.5 Solubility When Bubbles and Liquid Have Different Pressure -- 2.5.1 General Case Where Bubbles and Liquid Are Not in Mechanical Equilibrium -- 2.5.2 Case Where Bubbles and Liquid Are in Dynamic Equilibrium -- 2.6 Pressure Dependence of Solubility of Water in the Case of Incomplete Dissociation -- 2.7 Change in Solubility by Temperature -- 2.8 The Influence of Water on Melting Points of Crystals and Decompression-Vesiculation Induced Crystallization -- 2.9 Concentration of Volatiles and Vesiculation Caused by Cooling Crystallization. , 2.10 A System Containing Carbon Dioxide -- 2.10.1 Solubility of Carbon Dioxide -- 2.10.2 Solubility in a System Containing Water and Carbon Dioxide -- 2.10.3 Gas Composition Change with Progress of Vesiculation Relationship Among Total Pressure, Partial Pressure, and Solubility -- 2.10.4 Gas Composition and Change of Pressure with Addition of Carbon Dioxide-Rich Fluid -- References -- 3 Mechanism of Bubble Formation -- 3.1 Energetics of Bubble Nucleation -- 3.1.1 Thermodynamics of Fluctuations -- 3.1.2 Energy of Bubble Generation -- 3.2 Homogeneous Nucleation -- 3.3 Kinetics of Bubble Nucleation -- 3.3.1 Master Equation -- 3.3.2 Fokker-Planck Equation for Bubble (Cluster) Size Distribution -- 3.3.3 Equilibrium Distribution -- 3.3.4 Derivation of the Steady State Nucleation Rate -- 3.3.5 Steady State Size Distribution -- 3.4 Heterogeneous Nucleation -- 3.5 Non-steady State Nucleation Rate -- 3.6 Various Kinds of Correction for Classical Nucleation Theory -- 3.6.1 Tolman Correction -- 3.6.2 Poynting Correction -- 3.6.3 Viscosity Correction -- References -- 4 Growth and Expansion of Bubbles -- 4.1 Outline of Calculation of Bubble Growth and Expansion -- 4.2 Equilibrium Concentration at the Bubble Surface -- 4.2.1 General Expression -- 4.2.2 Equilibrium Concentration in the Mechanical Equilibrium -- 4.2.3 Expression Using the Critical Radius -- 4.3 Steady-State Diffusion-Limited Growth -- 4.3.1 Case Not Including the Advection Term -- 4.3.2 Case Including the Advection Term -- 4.4 Non-steady State Diffusion Growth -- 4.5 Bubble Expansion Under Mechanical Equilibrium -- 4.5.1 Adiabatic Expansion Versus Isothermal Expansion and the Influence of Latent Heat -- 4.5.2 Expansion Rate of Bubbles as a Function of the Bubble Radius -- 4.6 An Equation Describing Change in the Bubble Radius in a Viscous Fluid: The Rayleigh-Plesset Equation. , 4.7 Time Change of Bubble Expansion: Inertial Expansion -- 4.7.1 Bubble Expansion in Inviscid Liquid -- 4.7.2 The Case Where the Pressure in Bubbles is Constant: Simple Inertial Expansion -- 4.8 The Influence of Viscosity on Bubble Expansion: Viscosity-Limited Expansion -- 4.8.1 The Case Where Pressure in Bubbles and Overpressure in Bubbles are Constant -- 4.8.2 Expansion Under Constant Amount of Decompression -- 4.8.3 The Case of Decompression at a Constant Rate -- 4.8.4 Bubble Growth Calculation with a Combination of Diffusion and Viscosity -- 4.9 Outline of Bubble Growth and Experimental Results -- 4.9.1 Characteristic Timescale in Bubble Growth -- 4.9.2 Dimensionless Parameters Controlling Bubble Growth -- 4.9.3 Comparison with Experiments -- 4.10 Extension of the Rayleigh-Plesset Equation -- 4.10.1 Extension to Viscoelastic Liquid -- 4.10.2 Extension to Multi-bubbles: A Cell Model -- References -- 5 Temporal Development of Vesiculation -- 5.1 Overall Scheme -- 5.2 Temporal Development of Vesiculation Using the Eulerian Approach -- 5.2.1 Partial Differential Equation Representing the Conservation of the Number of Bubbles -- 5.2.2 Derivation of a Moment Equation -- 5.3 Temporal Development of Vesiculation Using the Lagrangian Approach -- 5.4 Controlling Parameters in Decompression-Induced Vesiculation -- 5.5 Temporal Development of Vesiculation Under the Condition of Constant Decompression Rate -- 5.5.1 Decompression Rate -- 5.5.2 Solution by Moment Equations Based on Eulerian Description -- 5.5.3 Solution by Lagrangian Description -- 5.5.4 Bubble Growth as a Factor Determining BND -- 5.6 Temporal Development of Vesiculation Process Under the Condition of a Constant Amount of Decompression -- 5.6.1 Outline of Nucleation and Growth -- 5.6.2 Maximum Nucleation Rate -- 5.6.3 Bubble Number Density. , 5.6.4 The Rate of Decrease in Water Concentration in Melt -- 5.7 Vesiculation Experiments -- 5.7.1 Experiment Under Constant Decompression Rates -- 5.7.2 Experiment Under Constant Amount of Decompression -- 5.8 The Limits of Homogeneous Nucleation -- 5.9 Second Nucleation -- References -- 6 Other Bubble-Related Processes -- 6.1 Secondary Growth of Bubbles: Ostwald Ripening -- 6.1.1 Mechanism of Secondary Growth -- 6.1.2 Solution of the Size Distribution by Lifshitz and Slyozov (The LS Theory) -- 6.1.3 Qualitative Understanding of the Growth Law -- 6.1.4 Comparison with Experiments -- 6.2 Deformation of Bubbles -- 6.2.1 Theoretical Study -- 6.2.2 Experimental Study -- 6.3 Coalescence of Bubbles -- 6.3.1 Coalescence Frequency -- 6.3.2 Shortening Process of Interbubble Distance: An Elemental Process of Coalescence -- 6.3.3 Shape Relaxation of Bubbles -- 6.3.4 Temporal Development of Size Distribution in the Case Where the Initial Size Distribution Is Monodisperse -- 6.3.5 Analysis by Continuous Size Distribution -- 6.3.6 Comparison with Experiments -- 6.4 Development of Gas Permeability -- 6.4.1 Importance of Gas Permeability -- 6.4.2 Bubble Connection in an Isotropic Field Without Flow -- 6.4.3 Bubble Connection in Shear Flow -- 6.5 Detachment and Ascending of Bubbles -- 6.5.1 Detachment of Bubbles -- 6.5.2 Bubble Ascent -- 6.5.3 Bubble Ascent and Advective Overpressure -- 6.6 Bubble Shrinkage -- 6.6.1 Rayleigh Collapse -- 6.6.2 The Influence of Gas in Bubbles on Bubble Shrinkage -- 6.7 Bubble Oscillation -- 6.7.1 The Case Where the Amount of Gas in a Bubble Is Constant -- 6.7.2 Linear Analysis of the Rayleigh-Plesset Equation -- 6.8 Influence of Viscoelasticity of Liquid on Collapse and Oscillation of Bubbles -- References -- 7 Cooling Crystallization of Magma -- 7.1 Thermodynamics of Cooling Crystallization. , 7.1.1 Melting Points of Crystals and Equilibrium Phase Diagrams -- 7.1.2 Thermodynamic Discussion of Crystal Nuclei and Gibbs-Thomson Relation -- 7.2 Classical Understanding of Igneous Rock Texture Using Nucleation Rate and Growth Rate -- 7.3 Nucleation of Crystals -- 7.3.1 Basic Characteristics of Homogeneous Nucleation -- 7.3.2 Comparison with Nucleation Experiments -- 7.4 Diffusion-Limited Growth -- 7.4.1 Steady-State Diffusion Growth of Spherical Crystals -- 7.4.2 Non-steady State Diffusion Growth on the Plane Crystal Face -- 7.5 Reaction-Limited Growth -- 7.5.1 Theoretical Consideration -- 7.5.2 Comparison with Experiments -- 7.5.3 Balanced Growth Between Diffusion and Reaction -- 7.6 Temporal Development of the Crystallization Process: Crystallization of a Binary Eutectic System -- 7.6.1 Scaling and Controlling Parameters -- 7.6.2 Basic Behavior of the Crystallization Process Under Constant Heat Loss -- 7.6.3 Crystallization Parameters Characterizing Crystallization Process -- 7.6.4 Relationship Between the Cooling Rate Dependence of the Crystal Number Density and the Crystal Growth Law -- 7.6.5 Comparison with Laboratory Experiments -- 7.6.6 Experiments in Nature -- 7.6.7 Summary of Factors Controlling the Crystal Number Density -- 7.7 Chemical Composition of Crystals -- 7.7.1 The Solid-Liquid Equilibrium and Disequilibrium in Binary Solid Solution and Chemical Composition of Crystals -- 7.7.2 Relationship Between the Growth Law and Zoning Structure -- 7.7.3 Diffusion Profile Taking the Moving Interface into Consideration and Chemical Composition of Crystals -- References -- 8 Crystallization Induced by Vesiculation -- 8.1 Similarity and Difference Between Decompression-Induced Crystallization and Cooling Crystallization -- 8.1.1 Phase Equilibrium Relation -- 8.1.2 The Degree of Supercooling in Decompression-Induced Crystallization. , 8.2 Crystallization in the Equilibrium Vesiculation Regime.
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  • 3
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Bulletin of volcanology 61 (1999), S. 345-346 
    ISSN: 1432-0819
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Type of Medium: Electronic Resource
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  • 5
    ISSN: 1432-0819
    Keywords: Key words Vesicle layering ; Liesegang ring ; Igneous layering ; Bubble nucleation ; Diffusion
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  We report a novel type of layering structure in igneous rocks. The layering structure in the Ogi picrite sill in Sado Island, Japan, is spatially periodic, and appears to be caused by the variation in vesicle volume fraction. The gas phase forming the vesicles apparently exsolved from the interstitial melt at the final stage of solidification of the magma body. We call this type of layering caused by periodic vesiculation in the solidifying magma body "vesicle layering." The presence of vesicle layering in other basic igneous bodies (pillow lava at Ogi and dolerite sill at Atsumi, Japan) implies that it may be a fairly common igneous feature. The width of individual layers slightly, but regularly, increases with distance from the upper contact. The layering plane is perpendicular to the long axes of columnar joints, regardless of gravitational direction, suggesting that the formation of vesicles is mainly controlled by the temperature distribution in the cooling magma body. We propose a model of formation of vesicle layering which is basically the same as that for Liesegang rings. The interplay between the diffusion of heat and magmatic volatiles in melt, and the sudden vesiculation upon supersaturation, both play important roles.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 108 (1991), S. 106-117 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The nucleation and growth of liquidus phases in cooling magmas at constant rates are modeled taking into account homogeneous nucleation, diffusion-limited growth, and depletion of crystallizing component from melt, and the temperature-dependent diffusivity. The formulation of governing equations shows that four dimensionless parameters, whose physical meanings are the nucleation difficulty, the fusion enthalpy, the ratio of the growth rate to the cooling rate, and the activation energy of diffusion, control the crystallization phenomena. The nucleation behavior with time (or temperature) is determined primarily by the competition between increasing nucleation rate with cooling and the reduced supersaturation with depletion by progressive growth of crystals previously nucleated. The maximum nucleation rate and the number density of crystals increase with decreasing interfacial tension and diffusivity, and with increasing fusion enthalpy and cooling rate. Quantitative expressions of the time or temperature interval for which the nucleation remains appreciable, the peak nucleation rate, the number density of crystals and the mean crystal radius are derived as functions of controlling parameters, and can be used to estimate the cooling rate or other unknown parameters from the number density of crystals of a rock.
    Type of Medium: Electronic Resource
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  • 7
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    Unknown
    Volcanological Society of Japan
    In:  Bulletin of the Volcanological Society Japan, 2. Ser. 35 (4). pp. 395-398.
    Publication Date: 2020-07-21
    Type: Article , PeerReviewed
    Format: text
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