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  • 1
    Online-Ressource
    Online-Ressource
    Newark :American Geophysical Union,
    Schlagwort(e): Oxidation-reduction reaction. ; Electronic books.
    Materialart: Online-Ressource
    Seiten: 1 online resource (429 pages)
    Ausgabe: 1st ed.
    ISBN: 9781119473299
    Serie: Geophysical Monograph Series
    DDC: 551.13
    Sprache: Englisch
    Anmerkung: Cover -- Title Page -- Copyright Page -- Contents -- List of Contributors -- Preface -- Chapter 1 Redox Equilibria: From Basic Concepts to the Magmatic Realm -- 1.1 General Aspects and Rationale -- 1.2 Oxygen Fugacity: The Centrality of an Elusive Parameter -- 1.3 Concluding Remarks and Perspectives -- Acknowledgments -- References -- Part I Redox from the Earth's Accretion to Global Geodynamics -- Chapter 2 Redox Processes Before, During, and After Earth´s Accretion Affecting the Deep Carbon Cycle -- 2.1 The Redox State of Planetary Interiors and the Speciation of Carbon in the Earth -- 2.2 Oxidation State of Earth´s Building Blocks and Early Differentiation -- 2.3 Mantle Oxidation State Over Time and Its Effect on the C-O-H Volatile Speciation -- 2.4 The Mantle Great Oxidation Event: Fact or Artefact? -- Acknowledgments -- References -- Chapter 3 Oxygen Fugacity Across Tectonic Settings -- 3.1 Introduction -- 3.2 Sample Selection, Methodology, and Design of this Study -- 3.3 Results -- 3.4 Discussion -- 3.5 Conclusions and Future Directions -- Acknowledgments -- Oxygen Fugacity Calculations -- References -- Chapter 4 Redox Variables and Mechanisms in Subduction Magmatism and Volcanism -- 4.1 Introduction -- 4.2 Redox Variables -- 4.3 Mechanisms -- 4.4 Discussion -- Acknowledgments -- References -- Chapter 5 Redox Melting in the Mantle -- 5.1 Introduction -- 5.2 Mantle Melting with Volatile Components -- 5.3 Redox Melting -- 5.4 Compositions of Melts Formed by Redox Melting -- 5.5 The Oxidation State in the Mantle Lithosphere, Asthenosphere, and Subduction Zones -- 5.6 Discussion -- 5.7 Closing Comments -- Acknowledgments -- References -- Part II Redox at Work: From Magma Sources to Volcanic Phenomena -- Chapter 6 Ionic Syntax and Equilibrium Approach to Redox Exchanges in Melts: Basic Concepts and the Case of Iron and Sulfur in Degassing Magmas. , 6.1 Introduction -- 6.2 Ionic Syntax, Speciation State and the Melt/Glass Network: State of the Art and Conceptual Framework -- 6.3 Redox Evolution and Magmatic Degassing -- 6.4 Discussion -- 6.5 Conclusions -- Acknowledgments -- References -- Chapter 7 The Petrological Consequences of the Estimated Oxidation State of Primitive MORB Glass -- 7.1 Introduction -- 7.2 Modeling Methods and Sample Selection -- 7.3 Results -- 7.4 Summary and Prospects -- Acknowledgments -- References -- Chapter 8 Oxygen Content, Oxygen Fugacity, the Oxidation State of Iron, and Mid-Ocean Ridge Basalts -- 8.1 Oxygen Content, Oxygen Fugacity, and the Oxidation State of Iron -- 8.2 Mid-Ocean Ridge Basalts -- Acknowledgments -- References -- Chapter 9 Chromium Redox Systematics in Basaltic Liquids and Olivine -- 9.1 Introduction -- 9.2 Measuring Cr Valence in Geologic Materials with Cr-K edge XANES Spectroscopy -- 9.3 Cr-Redox Systematics in Silicate Liquids: What We Know and Don´t Know -- 9.4 Cr-Valence Systematics in Equilibrium Liquid-Olivine Pairs -- 9.5 Concluding Remarks -- Acknowledgments -- References -- Chapter 10 The Thermodynamic Controls on Sulfide Saturation in Silicate Melts with Application to Ocean Floor Basalts -- 10.1 Introduction -- 10.2 Sulfide Capacity -- 10.3 The Thermodynamic Meaning of the Sulfide Capacity -- 10.4 A New Parameterization of Sulfide Capacity for Basaltic Melts -- 10.5 Sulfide Content at Sulfide Saturation (SCSS) -- 10.6 Application to Mid-Ocean Ridge and Similar Basalts -- 10.7 The Sulfur Fugacity (fS2) of Ocean Floor Basalts -- 10.8 Conclusions -- Acknowledgments -- References -- Chapter 11 Redox State of Volatiles and Their Relationships with Iron in Silicate Melts -- 11.1 Introduction -- 11.2 Water Concentration in Melt and its Effect on Redox -- 11.3 The Sulfur Species and the Redox (Fe3+/SigmaFe Ratio) of Silicate Melts. , 11.4 Natural Systems: Magma Degassing and Redox -- 11.5 Concluding Remarks -- Acknowledgments -- References -- Chapter 12 Iron in Silicate Glasses and Melts -- 12.1 Introduction -- 12.2 Iron Distribution in the Different Terrestrial Envelopes -- 12.3 Redox Equilibrium in Melts -- 12.4 Physical Properties: Highlights on Density and Viscosity -- 12.5 Influences on Crystallization and Degassing in Magmatic Systems -- 12.6 Concluding Remarks -- Acknowledgments -- References -- Part III Tools and Techniques to Characterize the Redox and its Effect on Isotope Partitioning -- Chapter 13 How to Measure the Oxidation State of Multivalent Elements in Minerals, Glasses, and Melts? -- 13.1 Introduction -- 13.2 Wet-Chemical Analyses -- 13.3 Electronic Microprobe -- 13.4 Mössbauer Spectroscopy -- 13.5 Optical Absorption Spectroscopy -- 13.6 X-ray Absorption Spectroscopy -- 13.7 Raman Spectroscopy -- 13.8 In situ Redox Determination at High Temperature or at High Pressure -- 13.9 Conclusion -- Acknowledgments -- References -- Chapter 14 Oxidation State, Coordination, and Covalency Controls on Iron Isotopic Fractionation in Earth´s Mantle and Crust -- 14.1 Introduction -- 14.2 Theory: Equilibrium Isotopic Fractionation from Vibrational Properties -- 14.3 Calculation of Vibrational Properties -- 14.4 Iron Isotope Studies Based on NRIXS or DFT -- 14.5 Comparison of Equilibrium Fractionation Factors Derived from Various Techniques -- 14.6 Parameters Controlling Equilibrium Fractionation Factors -- 14.7 Selected Applications to the Interpretation of Iron Isotopic Variations in Igneous Rocks -- 14.8 Conclusions and Perspectives -- Acknowledgments -- References -- Chapter 15 The Role of Redox Processes in Determining the Iron Isotope Compositions of Minerals, Melts, and Fluids -- 15.1 Introduction -- 15.2 Principles and Nomenclature. , 15.3 Methods for the Calibration of Iron Isotope Fractionation Factors -- 15.4 Fundamental Controls on Isotopic Fractionation Between Minerals, Melts, and Fluids -- 15.5 Effect of Redox Processes in Influencing Iron Isotope Fractionation in Natural Systems -- 15.6 Conclusion -- Acknowledgments -- References -- Chapter 16 Zinc and Copper Isotopes as Tracers of Redox Processes -- 16.1 Introduction -- 16.2 The Determination of Cu and Zn Isotope Ratios -- 16.3 Theoretical and Experimental Constraints on Cu and Zn Isotope Behavior in Relation to Redox Processes -- 16.4 Application of Cu and Zn to Trace Redox Processes in Natural Systems -- 16.5 Summary and Conclusions -- Acknowledgments -- References -- Chapter 17 Mineral-Melt Partitioning of Redox-Sensitive Elements -- 17.1 Introduction -- 17.2 Theoretical Background -- 17.3 Transition Metals (Fe, Cr, Ti, V) -- 17.4 Rare Earths (Ce, Eu) -- 17.5 Uranium (U) -- 17.6 Siderophile Elements (MO, W, Re, Pt GROUP ELEMENTS) -- 17.7 Concluding Remarks -- Acknowledgments -- References -- Chapter 18 Titanomagnetite - Silicate Melt Oxybarometry -- 18.1 Introduction -- 18.2 Oxybarometers Related to Titanomagnetite -- 18.3 Oxybarometers Based on Mineral Equilibria Involving Titanomagnetite -- 18.4 Oxybarometers Based on Element Partitioning Between Titanomagnetite and Silicate Melt -- 18.5 Application of Titanomagnetite-Based Oxybarometers to Natural Silicic Rocks -- 18.6 Conclusions -- Acknowledgments -- References -- Supplementary references -- Chapter 19 The Redox Behavior of Rare Earth Elements -- 19.1 Introduction -- 19.2 Geochemistry of Rare Earth Elements -- 19.3 Multivalent Rare Earth Elements -- 19.4 Conclusions and Perspectives -- Acknowledgments -- References -- Index -- EULA.
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  • 2
    Schlagwort(e): Konferenzschrift
    Materialart: Buch
    Seiten: 226 S. , Ill., graph. Darst.
    Serie: Chemical geology 229.2006,1/3
    Sprache: Englisch
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  • 3
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Community dentistry and oral epidemiology 25 (1997), S. 0 
    ISSN: 1600-0528
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Medizin
    Notizen: Abstract The study presents the results of a preventive program based on a children's book and carried out in the elementary schools of Bergamo, Italy. The book was published to improve 8-year-old schoolchildren's knowledge of primary dentition, dental plaque, nutrition, oral hygiene, fluoride and regular dental visits. The study was experimental. A total of 440 schoolchildren were selected to test the effectiveness of the book. They were divided into four groups: two groups underwent the training program and the other two were control groups. Measurements were made using the Quigley-Hein index before and after the program. A significant difference reduction of the plaque index of –0.6 was observed (P〈0.005).
    Materialart: Digitale Medien
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  • 4
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Journal of food science 45 (1980), S. 0 
    ISSN: 1750-3841
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft , Werkstoffwissenschaften, Fertigungsverfahren, Fertigung
    Notizen: The characteristics of mango (Mangifera indica var. Haden) polyphenol oxidase (PPO) extract were investigated in order to use it in mango processing. The optimum pH of the enzyme was 5.6–6.0, which is unusual as compared to other fruits. For heat inactivation, half-activity of the enzyme was lost after 2.1 and 4.0 mm of treatment at 85 and 80°C, respectively. Regarding the effect of inhibitors on the enzyme, sodium metabisulfite was the most effective, while ascorbic acid was the least. Polyacrylamide gel electrophoresis revealed two isoenzymes which moved toward the anode at pH 8.6 as detected with catechol as substrate; no bands were observed when L-tyrosine was used as substrate. It was found that electrophoretic patterns of mango PPO were quite different, compared to other plant PPO systems.
    Materialart: Digitale Medien
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  • 5
    Publikationsdatum: 2019-09-23
    Beschreibung: Eruptive activity at Turrialba volcano (Costa Rica) has escalated significantly since 2014, causing airport and school closures in the capital city of San José. Whether or not new magma is involved in the current unrest seems probable but remains a matter of debate as ash deposits are dominated by hydrothermal material. Here, we use high frequency gas monitoring to track the behavior of the volcano between 2014 and 2015, and to decipher magmatic vs. hydrothermal contributions to the eruptions. Pulses of deeply-derived CO2-rich gas (CO2/Stotal 〉 4.5) precede explosive activity, providing a clear precursor to eruptive periods that occurs up to two weeks before eruptions, which are accompanied by shallowly derived sulfur-rich magmatic gas emissions. Degassing modeling suggests that the deep magmatic reservoir is ~8-10 km deep, whereas the shallow magmatic gas source is at ~3-5 km. Two cycles of degassing and eruption are observed, each attributed to pulses of magma ascending through the deep reservoir to shallow crustal levels. The magmatic degassing signals were overprinted by a fluid contribution from the shallow hydrothermal system, modifying the gas compositions, contributing volatiles to the emissions, and reflecting complex processes of scrubbing, displacement, and volatilization. H2S/SO2 varies over two orders of magnitude through the monitoring period and demonstrates that the first eruptive episode involved hydrothermal gases whereas the second did not. Massive degassing ( 〉3000 T/day SO2 and H2S/SO2 〉 1) followed, suggesting boiling off of the hydrothermal system. The gas emissions show a remarkable shift to purely magmatic composition (H2S/SO2 〈 0.05) during the second eruptive period, reflecting the depletion of the hydrothermal system or the establishment of high temperature conduits bypassing remnant hydrothermal reservoirs, and the transition from phreatic to phreatomagmatic eruptive activity.
    Materialart: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 6
    Publikationsdatum: 2012-05-01
    Beschreibung: Raman spectroscopy can measure water concentrations of hydrous silicate glasses with several advantages such as: (1) high-spatial resolution of 1–2 μm2; (2) non-destructive character; and (3) easy access, without any specific sample preparation or mounting techniques. The latter reasons render Raman highly suitable for studying natural products, such as volcanic pumice and scoriae fragments. Two spectral regions can be distinguished in Raman spectra of hydrated silicate glasses: a low-wavenumber region (15–1500 cm−1), which corresponds to vibrations of the silicate network, and a high-wavenumber region (3100–3750 cm−1), corresponding to the OH stretching vibrations of H2O molecules and OH groups. Behrens et al. (2006) have published empirical equations relating the area ratio between these two regions and the water content. However, the proposed internal calibrations depend on chemical composition of the glasses. In this paper, we reinvestigated the previous procedures to improve the background subtraction. Our results allow us to present a more general and linear calibration. Water concentrations up to 13 wt% can be measured for a broad range of natural silicate melts, from basalts to rhyolite (40 up to 80 wt% SiO2), using a single calibration curve with an absolute error of 0.2 wt%.
    Print ISSN: 0003-004X
    Digitale ISSN: 1945-3027
    Thema: Geologie und Paläontologie
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  • 7
    Publikationsdatum: 2016-11-04
    Beschreibung: Steam-driven eruptions, both phreatic and hydrothermal, expel exclusively fragments of non-juvenile rocks disintegrated by the expansion of water as liquid or gas phase. As their violence is related to the magnitude of the decompression work that can be performed by fluid expansion, these eruptions may occur with variable degrees of explosivity. In this study we investigate the influence of liquid fraction and rock petrophysical properties on the steam-driven explosive energy. A series of fine-grained heterogeneous tuffs from the Campi Flegrei caldera were investigated for their petrophysical properties. The rapid depressurization of various amounts of liquid water within the rock pore space can yield highly variable fragmentation and ejection behaviors for the investigated tuffs. Our results suggest that the pore liquid fraction controls the stored explosive energy with an increasing liquid fraction within the pore space increasing the explosive energy. Overall, the energy released by steam flashing can be estimated to be one order of magnitude higher than for simple (Argon) gas expansion, and may produce a higher amount of fine material even under partially-saturated conditions. The energy surplus in the presence of steam flashing leads to a faster fragmentation with respect to gas-expansion, and in to higher ejection velocities imparted to the fragmented particles. Moreover, weak and low permeability rocks yield a maximum fine fraction. Using experiments to unravel the energetics of steam-driven eruptions has yielded estimates for several parameters controlling their explosivity. These findings should be considered for both modeling and evaluation of the hazards associated with steam-driven eruptions.
    Print ISSN: 0148-0227
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley-Blackwell im Namen von American Geophysical Union (AGU).
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  • 8
    Publikationsdatum: 2020-11-25
    Beschreibung: Over the past two decades, La Soufrière volcano in Guadeloupe has displayed a growing degassing unrest whose actual source mechanism still remains unclear. Based on new measurements of the chemistry and mass flux of fumarolic gas emissions from the volcano, here we reveal spatio-temporal variations in the degassing features that closely relate to the 3D underground circulation of fumarolic fluids, as imaged by electrical resistivity tomography, and to geodetic-seismic signals recorded over the past two decades. Discrete monthly surveys of gas plumes from the various vents on La Soufrière lava dome, performed with portable MultiGAS analyzers, reveal important differences in the chemical proportions and fluxes of H2O, CO2, H2S, SO2 and H2, which depend on the vent location with respect to the underground circulation of fluids. In particular, the main central vents, though directly connected to the volcano conduit and preferentially surveyed in past decades, display much higher CO2/SO2 and H2S/SO2 ratios than peripheral gas emissions, reflecting greater SO2 scrubbing in the boiling hydrothermal water at 80–100 m depth. Gas fluxes demonstrate an increased bulk degassing of the volcano over the past 10 years, but also a recent spatial shift in fumarolic degassing intensity from the center of the lava dome towards its SE–NE sector and the Breislack fracture. Such a spatial shift is in agreement with both extensometric and seismic evidence of fault widening in this sector due to slow gravitational sliding of the southern dome sector. Our study thus provides an improved framework to monitor and interpret the evolution of gas emissions from La Soufrière in the future and to better forecast hazards from this dangerous andesitic volcano.
    Beschreibung: Published
    Beschreibung: id 480
    Beschreibung: 4V. Processi pre-eruttivi
    Beschreibung: JCR Journal
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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  • 9
    Publikationsdatum: 2021-01-05
    Beschreibung: Induced seismicity can be associated to the activity of fluid withdrawal and injection from/into the shallow crust (fracking, wastewater disposal into the deep crust, Enhanced Geothermal Systems technology, fluid extraction in oil fields and geothermal power plants). Long-term injection of large volumes of fluids is normally associated with induced seismicity, but the effect of withdrawal-reinjection in the same reservoir is less known, at least regarding its relation to simple injection. However, it is common experience worldwide that small (i.e. 10 MW or less) geothermal plants with withdrawal and re-injection of fluids in the same reservoir are mostly not associated with significant induced/triggered seismicity. This paper aims at understanding how to discriminate, on a numerical modelling basis, the seismogenic potential of withdrawal-reinjection with respect to injection only. With this aim, we analysed the induced pressure changes, the perturbed volumes of rocks and the potential for induced seismicity due to these operations. A set of simulations of injection or withdrawal-reinjection cycles, obtained by using the numerical code TOUGH2®, is applied to simple models of geothermal reservoirs, with varying permeability and lateral boundary constraints. For each permeability model, we then compare the time growth of perturbed volumes obtained with withdrawal-reinjection cycles to those obtained during simple injection, using the same flow rates. The size of perturbed volumes is then related to the maximum magnitude of induced/triggered seismicity, using models accredited in recent literature. Our results show that, for all models, withdrawal-reinjection is by far less critical than simple injection, because the perturbed volumes are remarkably smaller and remain constant over the simulated time, so minimizing the likelihood of interference with seismogenic faults. These results have significant implications for geothermal projects, and in the assessment of the potential risk related to fluid stimulation and induced seismicity.
    Beschreibung: Published
    Beschreibung: 101770
    Beschreibung: 1TR. Georisorse
    Beschreibung: JCR Journal
    Schlagwort(e): geothermal energy ; geothermal energy
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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  • 10
    Publikationsdatum: 2021-02-10
    Beschreibung: Ischia, one active volcano of the Phlegraean Volcanic District, prone to very high risk, is dominated by a caldera formed 55 ka BP, followed by resurgence of the collapsed area. Over the past 3 ka, the activity extruded evolved potassic magmas; only a few low-energy explosive events were fed by less evolved magmas. A geochemical and Sr–Nd–O isotope investigation has been performed on minerals and glass from products of three of such eruptions, Molara, Vateliero, and Cava Nocelle (\2.6 ka BP). Data document strong mineralogical, geochemical, and isotopic heterogeneities likely resulting from mingling/ mixing processes among mafic and felsic magmas that already fed the Ischia volcanism in the past. Detailed study on the most mafic magma has permitted to investigate its origin. The mantle sector below Ischia underwent subduction processes that modified its pristine chemical, isotopic, and redox conditions by addition of B1 % of sediment fluids/melts. Similar processes occurred from Southeast to Northwest along the Apennine compressive margin, with addition of up to 2.5 % of sediment-derived material. This is shown by volcanics with poorly variable, typical d18O mantle values, and 87Sr/86Sr progressively increasing toward typical continental crust values. Multiple partial melting of this modified mantle generated distinct primary magmas that occasionally assimilated continental crust, acquiring more 18O than 87Sr. At Ischia, 7 % of Hercynian granodiorite assimilation produced isotopically distinct, K-basaltic to latitic magmas. A SW–NE regional tectonic structure gave these magmas coming from large depth the opportunity to mingle/mix with felsic magmas stagnating in shallower reservoirs, eventually triggering explosive eruptions.
    Beschreibung: Published
    Beschreibung: 1173 - 1194
    Beschreibung: 2V. Struttura e sistema di alimentazione dei vulcani
    Beschreibung: 3V. Proprietà chimico-fisiche dei magmi e dei prodotti vulcanici
    Beschreibung: 4V. Processi pre-eruttivi
    Beschreibung: 6A. Geochimica per l'ambiente e geologia medica
    Beschreibung: JCR Journal
    Schlagwort(e): Ischia ; Mineral chemistry ; Mingling/mixing ; Mantle enrichment/ ; crustal contamination ; Oxidizing fluids
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
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