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  • 1
    Online Resource
    Online Resource
    Burlington :Elsevier Science & Technology,
    Keywords: Physics -- Methodology. ; Vacuum. ; Vacuum technology. ; Electronic books.
    Description / Table of Contents: Vacuum Physics and Technology.
    Type of Medium: Online Resource
    Pages: 1 online resource (619 pages)
    Edition: 1st ed.
    ISBN: 9780080859958
    Series Statement: Issn Series ; v.Volume 14
    DDC: 533.5
    Language: English
    Note: Front Cover -- Vacuum Physics and Technology -- Copyright Page -- Contents -- Contributors -- Foreword -- Preface -- Chapter 1. Introduction -- 1.1. Survey -- 1.2. Basic Equations -- 1.3. Molecular Transport -- 1.4. Surface Physics -- Chapter 2. Measurement of Total Pressure in Vacuum Systems -- 2.1. Introduction -- 2.2. Manometers -- 2.3. Thermal Conductivity Gauges -- 2.4. Ionization Gauges -- 2.5. Placement and Calibration of Gauges -- Chapter 3. Partial Pressure Measurement -- 3.1. Mass Spectrometer -- Chapter 4. Production of High Vacua -- 4.1. Overview and Formulation of General Requirements -- 4.2. Fore-Vacuum Pumps -- 4.3. Diffusion Pumps -- 4.4. Other High Vacuum Pumps -- Chapter 5. Production of Ultrahigh Vacuum -- 5.1. Fundamental Concepts in the Production of Ultrahigh Vacuum -- 5.2. Getter Pumping -- 5.3. Ion Pumps -- 5.4. Cryogenic Pumping -- 5.5. Turbomolecular Vacuum Pumps -- Chapter 6. Metal Vacuum Systems and Components -- 6.1. A Diffusion Pumped Vacuum System and Its Schematic Representation -- 6.2. Vacuum Flanges -- 6.3. Vacuum, Water, and Gas Connectors: Function and Choices -- 6.4. Vacuum Valves -- 6.5. Traps, Baffles, and Valves in Combination -- 6.6. Flexible Connectors -- 6.7. Mechanical Motion Feedthroughs -- 6.8. Electrical Feedthroughs -- 6.9. Viewports -- Chapter 7. Glass Vacuum Systems -- 7.1. Use of Glass as the Vacuum Envelope -- 7.2. Systems and Components -- 7.3. Outgassing of Glass -- 7.4. Gas Permeation in Glass -- Chapter 8. Properties of Materials Used in Vacuum Technology -- 8.1. Introduction -- 8.2. Metals and Metal Alloys -- 8.3. Glasses -- 8.4. Ceramics -- 8.5. Elastomers and Plastomers -- 8.6. Sealants, Waxes, Greases, and Oils -- 8.7. Gases-Preparation, Properties, and Uses -- 8.8. Conclusion -- Chapter 9. Guidelines for the Fabrication of Vacuum Systems and Components -- 9.1. Soft Soldering. , 9.2. Hard Soldering -- 9.3. Welding -- 9.4. Bakeable and Coolable Vacuum Joints -- 9.5. Cleaning Techniques -- Chapter 10. Protective Devices for Vacuum Systems -- 10.1. Safety Considerations and Protective Devices -- 10.2. Interlocks and System Protective Devices -- Chapter 11. Design of High Vacuum Systems -- 11.1. General Considerations -- 11.2. Metal Systems -- Chapter 12. Operating and Maintaining High Vacuum Systems -- 12.1. General Considerations -- 12.2. High Vacuum Valve Control -- 12.3. Mechanical Pumps -- 12.4. Diffusion Pump Maintenance -- Chapter 13. Design and Performance of Bakeable Ultrahigh Vacuum Systems -- 13.1. Small Glass Uhv Systems -- 13.2. Small "All Metal" Uhv Systems -- 13.3. Intermediate Size Uhv Systems -- 13.4. Large Uhv Systems -- Chapter 14. Special Requirements in the Design, Operation, and Maintenance of Ultrahigh Vacuum Systems -- 14.1. Bakeout of Uhv Systems: Theory and Practice -- 14.2. Routine Maintenance and Cleaning -- Chapter 15. The Fine Art of Leak Detection and Repair -- 15.1. Basic Considerations -- 15.2. Types of Leak Detecting Equipment -- 15.3. Special Techniques and Problems -- 15.4. Repair Techniques -- Chapter 16. Vacuum Deposition Techniques -- 16.1 Introduction -- 16.2. Vacuum Evaporation Techniques -- 16.3. Vacuum Sputter Deposition -- 16.4. Comparison of Vacuum Evaporation and Sputtering Techniques -- Subject Index.
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Earth -- Core. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (609 pages)
    Edition: 1st ed.
    ISBN: 9780080549019
    Language: English
    Note: Front Cover -- The Mantle and Core -- Copyright Page -- Dedication -- Table of Contents -- Executive Editors' Foreword -- Contributors to Volume 2 -- Volume Editor's Introduction -- 1 INTRODUCTION -- 2 SOLAR INHERITANCE -- 3 WHOLE-MANTLE CHARACTERISTICS -- 4 THE IMPORTANCE OF RECYCLING -- 5 THE CHEMICAL CONSEQUENCES OF PARTIAL MELTING -- 6 IS WHAT WE SEE TODAY THE WAY IT HAS ALWAYS BEEN? -- 7 PROBING THE CORE -- 8 CLOSING THOUGHTS -- Chapter 2.01 Cosmochemical Estimates of Mantle Composition -- 2.01.1 INTRODUCTION AND HISTORICAL REMARKS -- 2.01.2 THE COMPOSITION OF THE EARTH'S MANTLE AS DERIVED FROM THE COMPOSITION OF THE SUN -- 2.01.3 THE CHEMICAL COMPOSITION OF CHONDRITIC METEORITES AND THE COSMOCHEMICAL CLASSIFICATION OF ELEMENTS -- 2.01.4 THE COMPOSITION OF THE PRIMITIVE MANTLE BASED ON THE ANALYSIS OF UPPER MANTLE ROCKS -- 2.01.5 COMPARISON OF THE PM COMPOSITION WITH METEORITES -- 2.01.6 THE ISOTOPIC COMPOSITION OF THE EARTH -- 2.01.7 SUMMARY -- REFERENCES -- Chapter 2.02 Seismological Constraints upon Mantle Composition -- 2.02.1 INTRODUCTION -- 2.02.2 UPPER-MANTLE BULK COMPOSITION -- 2.02.3 UPPER-MANTLE HETEROGENEITY -- 2.02.4 LOWER-MANTLE BULK COMPOSITION -- 2.02.5 LOWER-MANTLE HETEROGENEITY -- 2.02.6 SUMMARY -- REFERENCES -- Chapter 2.03 Sampling Mantle Heterogeneity through Oceanic Basalts: Isotopes and Trace Elements -- 2.03.1 INTRODUCTION -- 2.03.2 LOCAL AND REGIONAL EQUILIBRIUM REVISITED -- 2.03.3 CRUST-MANTLE DIFFERENTIATION -- 2.03.4 MID-OCEAN RIDGE BASALTS: SAMPLES OF THE DEPLETED MANTLE -- 2.03.5 OCEAN ISLAND, PLATEAU, AND SEAMOUNT BASALTS -- 2.03.6 THE LEAD PARADOX -- 2.03.7 GEOCHEMICAL MANTLE MODELS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.04 Orogenic, Ophiolitic, and Abyssal Peridotites -- 2.04.1 INTRODUCTION -- 2.04.2 TYPES, DISTRIBUTION, AND PROVENANCE -- 2.04.3 MAJOR- AND TRACE-ELEMENT GEOCHEMISTRY OF PERIDOTITES. , 2.04.4 MAJOR- AND TRACE-ELEMENT GEOCHEMISTRY OF PYROXENITES -- 2.04.5 Nd-Sr ISOTOPE GEOCHEMISTRY -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.05 Mantle Samples Included in Volcanic Rocks: Xenoliths and Diamonds -- 2.05.1 MANTLE XENOLITHS: THE NATURE OF THE SAMPLE -- 2.05.2 PERIDOTITE XENOLITHS -- 2.05.3 ECLOGITE XENOLITHS -- 2.05.4 DIAMONDS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.06 Noble Gases as Mantle Tracers -- 2.06.1 INTRODUCTION -- 2.06.2 NOBLE GASES AS GEOCHEMICAL TRACERS -- 2.06.3 MANTLE NOBLE GAS CHARACTERISTICS -- 2.06.4 NOBLE GASES AS MANTLE TRACERS -- 2.06.5 CONCLUDING REMARKS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.07 Mantle Volatiles-Distribution and Consequences -- 2.07.1 INTRODUCTION -- 2.07.2 EVIDENCE FROM MANTLE-DERIVED MAGMAS -- 2.07.3 EVIDENCE FROM MANTLE-DERIVED SAMPLES -- 2.07.4 SUMMARY AND CONCLUSIONS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.08 Melt Extraction and Compositional Variability in Mantle Lithosphere -- 2.08.1 INTRODUCTION -- 2.08.2 PHASE EQUILIBRIUM AND MELT EXTRACTION -- 2.08.3 THE NANTLE SAMPLE -- 2.08.4 THE ROLE OF MELT EXTRACTION -- 2.08.5 PERSPECTIVE ON MANTLE THERMAL EVOLUTION -- 2.08.6 SUMMARY -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.09 Trace Element Partitioning under Crustal and Uppermost Mantle Conditions: The Influences of Ionic Radius, Cation Charge, Pressure, and Temperature -- 2.09.1 INTRODUCTION -- 2.09.2 IONIC RADIUS AND LATTICE STRAIN THEORY -- 2.09.3 DETERMINATION OF Es AND ro -- 2.09.4 SIMULATIONS OF TRACE-ELEMENT SUBSTITUTION INTO GARNET -- 2.09.5 DEVIATIONS FROM SIMPLE BULK MODULUS SYSTEMATICS -- 2.09.6 TEMPERATURE AND PRESSURE DEPENDENCES OF Do AND PARTITIONING -- 2.09.7 GARNET-MELT PARTITIONING OF REE -- 2.09.8 DEPENDENCE OF Do ON IONIC CHARGE -- 2.09.9 MINERAL-MELT PARTITION COEFFICIENTS -- ACKNOWLEDGMENTS -- REFERENCES. , Chapter 2.10 Partition Coefficients at High Pressure and Temperature -- 2.10.1 PLANETARY DIFFERENTIATION -- 2.10.2 EXPERIMENTAL APPROACHES -- 2.10.3 METAL-SILICATE EQUILIBRIA -- 2.10.4 MINERAL-MELT EQUILIBRIA -- 2.10.5 MODELS -- 2.10.6 SUMMARY AND FUTURE -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.11 Subduction Zone Processes and Implications for Changing Composition of the Upper and Lower Mantle -- 2.11.1 INTRODUCTION -- 2.11.2 THERMAL STRUCTURE AND MINERALOGY OF THE SUBDUCTING PLATE -- 2.11.3 BERYLLIUM-10 SYSTEMATICS AND SEDIMENT SUBDUCTION -- 2.11.4 CROSS-ARC ELEMENT SYSTEMATICS -- 2.11.5 STORAGE OF SUBDUCTED ELEMENTS IN THE UPPER MANTLE -- 2.11.6 SUBDUCTION FLUXES AND MANTLE COMPOSITION -- 2.11.7 SUMMARY -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.12 Convective Mixing in the Earth's Mantle -- 2.12.1 INTRODUCTION -- 2.12.2 GEOCHEMICAL AND GEOPHYSICAL OBSERVATIONS OF MANTLE HETEROGENEITY -- 2.12.3 CHARACTERIZATION OF MIXING -- 2.12.4 OUTLOOK -- ACKNOWLEDGMENTS -- APPENDIX -- REFERENCES -- Chapter 2.13 Compositional Evolution of the Mantle -- 2.13.1 INTRODUCTION -- 2.13.2 RADIOGENIC ISOTOPIC COMPOSITIONS -- 2.13.3 TRACE-ELEMENT VARIATIONS: Nb/Th AND Nb/U IN THE MANTLE THROUGH TIME -- 2.13.4 ORIGIN OF CHEMICAL VARIATIONS IN THE EARTH'S MANTLE -- 2.13.5 NATURE OF CHEMICAL LAYERING IN THE MANTLE -- 2.13.6 FUTURE PROSPECTS -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.14 Experimental Constraints on Core Composition -- 2.14.1 INTRODUCTION -- 2.14.2 GENERAL APPROACHES -- 2.14.3 MAJOR ELEMENTS IN THE CORE -- 2.14.4 LIGHT ELEMENTS IN THE CORE -- 2.14.5 MINOR AND TRACE ELEMENTS IN THE CORE -- 2.14.6 CONCLUSIONS AND OUTLOOK -- ACKNOWLEDGMENTS -- REFERENCES -- Chapter 2.15 Compositional Model for the Earth's Core -- 2.15.1 INTRODUCTION -- 2.15.2 FIRST-ORDER GEOPHYSICS -- 2.15.3 CONSTRAINING THE COMPOSITION OF THE EARTH'S CORE. , 2.15.4 ACOMPOSITIONAL MODEL FOR THE CORE -- 2.15.5 RADIOACTIVE ELEMENTS IN THE CORE -- 2.15.6 TIMING OF CORE FORMATION -- 2.15.7 NATURE OF CORE FORMATION -- 2.15.8 THE INNER CORE, ITS CRYSTALLIZATION, AND CORE-MANTLE EXCHANGE -- 2.15.9 SUMMARY -- ACKNOWLEDGMENTS -- REFERENCES -- Subject Index.
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  • 3
    Publication Date: 2023-06-27
    Keywords: 61-462; 61-462A; 89-462A; Cerium; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Europium; Event label; Glomar Challenger; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Lanthanum; Leg61; Leg89; Lutetium; North Pacific; Samarium; Sample code/label; Terbium; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 117 data points
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  • 4
    Publication Date: 2023-06-27
    Keywords: 61-462A; 89-462A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Isotope dilution; Lead; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208/Lead-204 ratio; Leg61; Leg89; North Pacific; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 37 data points
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  • 5
    Publication Date: 2023-06-27
    Keywords: 61-462; 61-462A; 89-462A; Calculated; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Event label; Glomar Challenger; Isotope dilution; Leg61; Leg89; Neodymium; Neodymium-143/Neodymium-144 ratio; Neodymium-143/Neodymium-144 ratio, error; North Pacific; Rubidium; Samarium; Sample code/label; Sample comment; Strontium; Strontium-87/Strontium-86 ratio
    Type: Dataset
    Format: text/tab-separated-values, 231 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Castillo, Paterno R; Carlson, R W; Batiza, Rodey (1991): Origin of Nauru Basin igneous complex: Sr, Nd and Pb isotope and REE constraints. Earth and Planetary Science Letters, 103(1-4), 200-213, https://doi.org/10.1016/0012-821X(91)90161-A
    Publication Date: 2023-06-27
    Description: The tholeiitic basalts and microdolerites that comprise the Cretaceous igneous complex in the Nauru Basin in the western equatorial Pacific have moderate ranges in initial 87Sr/86Sr (0.70347 - 0.70356), initial 143Nd/144Nd (0.51278 - 0.51287), and measured 206Pb/204Pb (18.52 - 19.15), 207Pb/204Pb (15.48 - 15.66) and 208Pb/204Pb (38.28 - 38.81). These isotopic ratios overlap with those of both oceanic island basalts (OIB) and South Atlantic and Indian mid-ocean ridge basalts (MORB). However, the petrography, mineralogy, and bulk rock chemistry of the igneous complex are more similar to MORB than to OIB. Also, the rare earth element contents of Nauru Basin igneous rocks are uniformly depleted in light elements (La/Sm(ch) 〈 1) indicative of a mantle source compositionally similar to that of MORB. These results suggest that the igneous complex is the top of the original ocean crust in the Nauru Basin, and that the notion that the crust must be 15 to 35 m.y. older based on simple extrapolation and identification of the M-sequence magnetic lineations (Larson et al., 1981, doi:10.2973/dsdp.proc.61.1981; Moberly et al., 1985, doi:10.2973/dsdp.proc.81.1984) may be invalid because of a more complicated tectonic setting. The igneous complex most probably was extruded from an ocean ridge system located near the anomalously hot, volcanically active, and isotopically distinct region in the south central Pacific which has been in existence since c. 120 Ma.
    Keywords: 61-462; 61-462A; 89-462A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Leg61; Leg89; North Pacific
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 7
    Publication Date: 2024-01-09
    Keywords: 129-802A; Aluminium oxide; Caesium; Calcium oxide; Cerium; Cobalt; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Electron microprobe (EMP); Europium; Hafnium; Instrumental neutron activation analysis (INAA) (Reimann et al., 1998); Iron oxide, FeO; Joides Resolution; Lanthanum; Lead-206/Lead-204 ratio; Lead-207/Lead-204 ratio; Lead-208/Lead-204 ratio; Leg129; Lutetium; Magnesium oxide; Neodymium-143/Neodymium-144 ratio; North Pacific Ocean; Ocean Drilling Program; ODP; Phosphorus pentoxide; Potassium oxide; Samarium; Sample code/label; Sample comment; Scandium; Silicon dioxide; Sodium oxide; Strontium-87/Strontium-86 ratio; Tantalum; Terbium; Thorium; Titanium dioxide; Ytterbium
    Type: Dataset
    Format: text/tab-separated-values, 233 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 89-462A; Argon-40/Argon-39; Argon-40/Argon-39, standard deviation; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Leg89; North Pacific; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 9
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Castillo, Paterno R; Pringel, M S; Carlson, R W (1994): East Mariana Basin tholeiites: Cretaceous intraplate basalts or rift basalts related to the Ontong Java plume? Earth and Planetary Science Letters, 123(1-4), 139-154, https://doi.org/10.1016/0012-821X(94)90263-1
    Publication Date: 2024-01-09
    Description: Studies of seafloor magnetic anomaly patterns suggest the presence of Jurassic oceanic crust in a large area in the western Pacific that includes the East Mariana, Nauru and Pigafetta Basins. Sampling of the igneous crust in this area by the Deep Sea Drilling Program (DSDP) and the Ocean Drilling Program (ODP) allows direct evaluation of the age and petrogenesis of this crust. ODP Leg 129 drilled a 51 m sequence of basalt pillows and massive flows in the central East Mariana Basin. 40Ar/39Ar ages determined in this study for two Leg 129 basalts average 114.6 +/- 3.2 Ma. This age is in agreement with the Albian-late Aptian paleontologic age of the overlying sediments, but is distinctively younger than the Jurassic age predicted by magnetic anomaly patterns in the basin. Compositionally, the East Mariana Basin basalts are uniformly low-K tholeiites that are depleted in highly incompatible elements compared to moderately incompatible ones, which is typical of mid-ocean ridge basalts (MORB) erupted near hotspots. The Sr, Nd and Pb isotopic compositions of the tholeiites (87Sr/86Sr init = 0.70360-0.70374; 143Nd/144Nd init = 0.512769-0.512790; 206Pb/204Pb meas = 18.355-18.386) also overlap with some Indian Ocean Ridge MORB, although they are distinct from the isotopic compositions of Jurassic basalts drilled in the Pigafetta Basin, the oldest Pacific MORB. The isotopic compositions of the East Mariana Basin tholeiites are also similar to those of intraplate basalts, and in particular, to the isotopic signature of basalts from the nearby Ontong Java and Manihiki Plateaus. The East Mariana Basin tholeiites also share many petrologic and isotopic characteristics with the oceanic basement drilled in the Nauru Basin at DSDP Site 462. In addition, the new 110.8 +/- 1.0 Ma 40Ar/39Ar age for two flows from the bottom of Site 462 in the Nauru Basin is indistinguishable from the age of the East Mariana Basin flows. Thus, while magnetic anomaly patterns predict that the igneous basement in the Nauru and East Mariana Basins is Jurassic in age, the geochemical and chronological results discussed here suggest that the basement formed during a Cretaceous rifting event within the Jurassic crust. This magmatic and tectonic event was created by the widespread volcanism responsible for the genesis of the large oceanic plateaus of the western Pacific.
    Keywords: 129-802A; 89-462A; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; Glomar Challenger; Joides Resolution; Leg129; Leg89; North Pacific; North Pacific Ocean; Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 10
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Industrial & engineering chemistry 27 (1935), S. 638-640 
    ISSN: 1520-5045
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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