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  • 1
    Keywords: Dwellings -- Heating and ventilation -- Great Britain -- Congresses. ; Power resources -- Great Britain -- Congresses. ; Solar heating -- Great Britain -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (160 pages)
    Edition: 1st ed.
    ISBN: 9781483138541
    Language: English
    Note: Front Cover -- EDITOR'S INTRODUCTION -- The context of the problem -- Conclusions -- The technical issues -- Arrangement of papers -- Acknowledgements -- CHAPTER 1. FLUIDIC DIVERTER VALVES APPLIED TO INTERMITTENT DOMESTIC HEATING -- Summary -- Intermittent Control -- Sequence of Loads -- Fluidic Diverting Valves -- Energy Consumption of the Heating Circuits -- Conclusions -- References -- CHAPTER 2. SOME EFFECTS OF VENTILATION RATE, THERMAL INSULATION AND MASS ON THE THERMAL PERFORMANCE OF HOUSES IN SUMMER AND WINTER -- Summary -- Introduction -- Thermal Performance Calculations and Results -- Practical Aspects of Construction including the Moisture Problem -- Conclusions -- References -- CHAPTER 3. THERMAL COMFORT -- Summary -- The Thermal Environment People Prefer -- Conclusion -- References -- CHAPTER 4. THE ENERGY COST OF THE CONSTRUCTION AND HABITATION OF TIMBER FRAME HOUSING -- Summary -- Introduction -- Timber Frame Housing -- Energy Cost of Construction -- Energy Cost of Habitation -- References -- CHAPTER 5. ENERGY TO BUILD -- SUMMARY -- MATERIALS -- EXTERNAL SKIN OF BUILDINGS -- INTERNAL STRUCTURE -- CONCLUSIONS -- CHAPTER 6. HEATING BUILDINGS BY WINTER SUNSHINE -- Summary -- Introduction -- Solar Construction -- Economic Viability of a Solar Wall -- Solar Incidence and Sunshine Hours -- Estimates of Glasswall Temperature -- Is A Solar Wall Economic? -- Discussion -- Acknowledgement -- References -- CHAPTER 7. A THERMAL MODEL FOR A SOLAR HEATED BUILDING -- Summary -- Acknowledgement -- References -- CHAPTER 8. Solar Housing -- Summary -- Optimisation of monthly mean daily heat balance of a rectangular building -- Conclusion -- REFERENCES -- CHAPTER 9. THERMAL INSULATION STANDARDS -- Summary -- Current Standards -- Mean U-Values or Volumetric Heat Loss -- Relation with Thermal Capacity -- References. , CHAPTER 10. SOME PROBLEMS ASSOCIATED WITH THE DESIGN OF LOW ENERGY HOUSING -- PREDICTION OF ANNUAL ENERGY CONSUMPTION -- COSTS -- CONCLUSIONS -- REFERENCES -- CHAPTER 11. THE AUTONOMOUS HOUSING RESEARCH PROGRAMME -- Summary -- Introduction -- Justification -- Large Scale Systems -- Autonomous Systems Integration -- Power -- Water Supply and Food Production -- Design Guide -- Conclusion -- References -- CHAPTER 12. MINIMISING ENERGY COSTS IN BUILDINGS: THE SOCIOECONOMIC ENVIRONMENTAL AND POLITICAL IMPLICATIONS -- Summary -- The 'Energy Crisis' -- Energy Use and Conservation in Buildings -- Appropriate Technologies -- Decentralisation -- Implications -- References -- DISCUSSION SESSIONS -- Morning session -- Afternoon session -- List of Participants.
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  • 2
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (503 pages)
    Edition: 1st ed.
    ISBN: 9781119910572
    DDC: 612.1
    Language: English
    Note: Cover -- Title Page -- Copyright Page -- Contents -- Preface -- Acknowledgements -- Dedication -- Chapter 1 Fluid Physics in Circulatory Systems - Problems, Analogies and Methods -- Presentation philosophy -- 1.1 Basic Biological Notions and Fluid-Dynamical Ideas -- Conduit flow examples -- Basic continuous flow concepts -- Eulerian versus Lagrangian descriptions -- Steady versus transient models -- Newtonian versus non-Newtonian flows -- Porous media continuum flow models -- Darcy flows in human and animal tissue -- Objectives in conduit and Darcy flow modeling -- 1.2 Quantitative Modeling Perspectives -- 1.2.1 Rheology considerations in conduit flows -- Better arterial flow models needed -- 1.2.2 Darcy flow model in continuous media -- Temperature diffusion -- Darcy flow pressure diffusion -- Important porous media approach -- Relevance of Darcy flows to biofluids -- 1.3 Preview of Complicated but Simple Boundary Value Problem Solutions -- Closing remarks -- 1.4 References -- Chapter 2 Math Models, Differential Equations and Numerical Methods -- 2.1 Presentation Approach -- What we won't do -- Pursuing studies that uncover the physics -- Examples on presentation approach -- 2.2 Diffusion Processes, Partial Differential Equations and Formulation Development -- 2.2.1 Heat transfer applications -- 2.2.2 Heat equation derivation -- 2.2.3 Pressure diffusion in porous media -- 2.2.4 Dynamically coupled heat and pressure diffusion -- 2.3 Boundary-Conforming Curvilinear Grid Generation -- 2.3.1 Comments on classical coordinate transforms and conformal mapping -- 2.3.2 Curvilinear gridding method for irregular domains -- 2.3.2.1 Grid generation for eccentric annular flow -- Mapping formalism and key ideas -- Thompson's mapping -- Some reciprocity relations -- Relation to conformal mapping, finally -- Solutions to mesh generation equations. , Boundary conditions -- Fast iterative solutions -- On Laplacian transformations -- 2.3.2.2 Grid generation for singly-connected conduit flow -- 2.4 Finite Difference Solutions Made Easy - Iterative Methods, Programming and Source Code Details -- 2.4.1 Basic ideas in finite differences -- A simple differential equation -- Variable coefficients and grids -- 2.4.2 Formulating steady flow problems -- Direct versus iterative solutions -- Iterative methods -- Convergence acceleration -- Wells and internal boundaries -- Peaceman well corrections -- Derivative discontinuities -- Point relaxation methods -- Observations on relaxation methods -- Minimal computing resources -- Good numerical stability -- Fast convergence -- Why relaxation methods converge -- Over-relaxation -- Line and point relaxation -- Curvilinear grid generation and relaxation solutions -- Coupled equations on curvilinear meshes -- 2.5 References -- Chapter 3 Hagen-Poiseuille Extensions - Real Flow Effects and General Bifurcations -- 3.1 Blood Rheology and Overview -- 3.1.1 Hagen-Poiseuille - Misunderstandings and limitations -- 3.1.2 Ideal versus non-Newtonian rheology -- 3.1.3 Some conventional rheological models -- 3.1.4 Perfect concentric flow velocity, pressure and flow rate relations -- Newtonian flow solution -- Bingham Plastic pipe flow -- Power Law fluid pipe flow -- Herschel-Bulkley pipe flow -- Ellis fluid pipe flow -- 3.1.5 Example solutions for imperfect arteries with stenosis and book presentation outline -- Book presentation outline -- 3.2 Newtonian Flow in Simple Bifurcations -- 3.2.1 Theory - Two uneven bifurcated blood vessels with Q1 specified -- Case 1. Flow rate Q1 prescribed -- Case 2. Inlet pressure Pi prescribed -- Case 3. Identical outlet pressures Po,2 and Po,3 given -- 3.2.2 Software - Two uneven bifurcated arteries with Q1 specified (Reference, CODE-1). , An example computation -- An additional validation -- 3.2.3 Theory - Two uneven bifurcated arteries with Pi specified -- 3.2.4 Software - Two uneven bifurcated arteries with Pi specified (Reference, CODE-2) -- A practical example -- 3.3 Theory - Complicated Arteries with Chained Bifurcations -- 3.4 Network with Arbitrary Number of Bifurcations -- 3.5 Bifurcated Newtonian Flow in Noncircular Clogged Blood Vessels -- 3.6 References -- Chapter 4 Non-Newtonian Flow in Circular Conduits and Networks -- Bifurcation model and analytical approach -- Different rheological applications -- Validation procedures -- 4.1 Power Law Fluids with Inlet Flow Rate Prescribed -- Iterative "half-step" solution for Pa and Pi -- Shear stress -- Typical parameters -- Example calculations -- 4.2 Herschel-Bulkley Fluids and Yield Stress -- 4.2.1 Analytical and numerical approach -- Yield stress modeling -- 4.2.2 BIFURC-6 runs assuming ôy = 0 psi (Power Law limit) -- 4.2.3 BIFURC-6 runs assuming ôy = 0.00001 psi -- 4.3 Newtonian and Herschel-Bulkley Examples -- Power Law limitations -- 4.4 References -- Chapter 5 Flows in Clogged Arteries and Veins -- 5.1 Hagen-Poiseuille Revisited - Rectangular Coordinates -- Newtonian pipe flow recapitulation -- A physical description -- Detailed assessments -- Recapitulation -- 5.2 Non-Newtonian Power Law Circular Pipe Flow in Rectangular Coordinates -- 5.3 Clinical Implications for Pressure Gradient and Viscous Shear Stress -- 5.4 Evolutionary Approaches for Complicated Geometries -- Static versus evolutionary approaches -- 5.5 A Detailed Clog Flow Computation -- Simulation 1 - Newtonian flow in perfect circle -- Simulation 2 - Power Law flow in perfect circle -- Simulation 3 - Power Law flow in a clogged blood vessel -- 5.6 References -- Chapter 6 Square Stents, Centrifugal Effects, Pulsatile Flow, Clogged Bifurcations and Axial Variations. , 6.1 Stent Geometry Effects on Volume Flow Rate -- 6.1.1 Conventional stents, analytical flow model -- Stent detailed function -- Analytical modeling -- Exact analytical Hagen-Poiseuille solution -- 6.1.2 Finite difference method -- 6.1.3 Square stent designs, analytical and numerical models -- Exact analytical solution for rectangular stents -- Finite difference solution -- Example calculation -- 6.2 General Formulations and Solutions for Complicated Geometries and Arbitrary Fluids -- Recapitulation -- 6.3 Centrifugal Force Influence on Volume Flow Rate -- Straight, closed ducts -- Hagen-Poiseuille flow between planes -- Flow between concentric plates -- Typical calculations -- Flows in closed curved ducts -- 6.4 Unsteady Pulsatile Flow Model for Complicated Duct Cross-Sections -- 6.5 Bifurcated Conduits with Newtonian Flow in Clogged Geometric Cross-sections -- 6.6 Modeling Axial Variations with Pseudo-Three- Dimensional Method -- 6.7 Modeling Transient Wall Effects -- 6.8 Steady Bifurcated Newtonian Flows With Arbitrary Clogs, A Numerical Example -- 6.8.1 Motivating questions and examples -- 6.8.2 Detailed single-element pipe flow solutions -- 6.8.3 Method for bifurcated systems with clogged piping elements -- 6.8.4. Effective radius flow properties -- 6.8.5 Discussion and conclusions -- 6.9 References -- Chapter 7 Tissue Properties from Steady and Transient Syringe Pressure Analysis -- 7.1 Importance of Compressibility, Permeability, Anisotropy, Pressure and Porosity in Medical Applications -- Compressibility -- Permeability -- Anisotropy -- Local pressures -- Porosity -- Additional highlights -- 7.2 Geoscience Perspectives and Background -- 7.3 Formation Testing in Petroleum Well Logging -- 7.4 Operational Guidelines to Biofluids Pressure Testing -- Intelligent syringe concepts. , Multiprobe syringe assemblies for anisotropy and heterogeneity mapping -- 7.5 Intelligent Syringe Fundamentals -- 7.5.1 Background and Motivation -- 7.5.2 Clinical and Diagnostic Objectives -- 7.5.3 Syringe Flow Basics and Porous Media Pressure Conventions -- 7.5.4 Single Intelligent Syringe Basic Layout -- Figure 3A description -- Figure 3B description -- Figure 3C description -- Figure 3D description -- Figure 3E description -- General Comments -- 7.5.5 Syringe Arrays for Heterogeneity Mapping and Biopsy Sampler -- Array syringe and biopsy sampler -- Array syringe general concept -- 7.6 Mathematical Models for Porous Media Flow -- 7.6.1 Transient Isotropic Darcy Flow - Forward Solutions -- 7.6.2 Transient Transversely Isotropic Darcy Flow - Forward Solutions -- 7.6.3 Transient Isotropic and Transversely Isotropic Flow - Inverse Solutions -- 7.6.4 Steady Transversely Isotropic Flow - Inverse Solutions -- 7.6.5 Modeling Notes and Physical Consequences -- Geometric factor -- Flowline compressibility -- Flowline pressure drops -- Pressure effects on tissue -- 7.6.6 Anisotropic Permeabilities from Oscillatory Pressure Fields -- 7.6.7 Formulation for Supercharged Damage Zones -- 7.6.8 General Properties, Calculated Results and Validations -- Example 1. Forward and Inverse Simulations in Isotropic Media Using Drawdown Method -- Example 2. Forward and Inverse Simulations in Transversely Isotropic Media Using Pure Drawdown (or Pure Buildup) Methods -- Example 3. Forward and Inverse Simulations in Transversely Isotropic Media Using Drawdown-Buildup Method -- Example 4. Forward and Inverse Simulations in Transversely Isotropic Media Using Drawdown and Phase Delay Method -- Example 5. Forward and Inverse Simulations in Transversely Isotropic Media for Flows with Nonzero Dip Angle -- 7.6.9 Application to Subcutaneous Injection Yorkshire Swine Laboratory Data. , Experimental Details.
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  • 3
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Oil well drilling - Equipment and supplies - Design and construction. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (632 pages)
    Edition: 1st ed.
    ISBN: 9781118835265
    Language: English
    Note: Cover -- Title Page -- Copyright Page -- Contents -- Preface -- Acknowledgements -- 1 Motivating Ideas - General Formulation and Results -- 1.1 Overview -- 1.2 Introduction -- 1.3 Physical Model and Numerical Formulation -- 1.3.1 Design philosophy -- 1.3.2 New discretization approach -- 1.3.3 Analytical formulation -- 1.3.4 An alternative approach -- 1.3.5 Solution philosophy -- 1.3.6 Governing equations -- 1.3.7 Finite difference methodology -- 1.4 Validation Methodology -- 1.4.1 Fundamental physics -- 1.4.2 Biot-Savart finite coil validations -- 1.4.3 Analytical dipole validations -- 1.4.4 Fully three-dimensional solutions -- 1.5 Practical Applications -- 1.5.1 Example 1. Granularity transition to coil source -- 1.5.2 Example 2. Magnetic field, coil alone -- 1.5.3 Example 3. Steel mandrel at dip -- 1.5.4 Example 4. Conductive mud effects in wireline and MWD logging -- 1.5.5 Example 5. Longitudinal magnetic fields -- 1.5.6 Example 6. Elliptical coils -- 1.5.7 Example 7. Calculating electromotive force -- 1.5.8 Example 8. Detailed incremental readings -- 1.5.9 Example 9. Coil residing along bed interface -- 1.6 Closing Remarks -- 1.7 References -- 2 Detailed Theory and Numerical Analysis -- 2.1 Overview -- 2.2 Introduction -- 2.2.1 Physical and mathematical complications -- 2.2.2 Numerical challenges -- 2.2.3 Alternative approaches -- 2.2.4 Project summary -- 2.3 Preliminary Mathematical Considerations -- 2.3.1 General governing differential equations -- 2.3.2 Anisotropic model -- 2.3.3 Equivalent vector and scalar potential formulation -- 2.3.4 Recapitulation and mathematical observations -- 2.3.5 Matching conditions at bed interfaces -- 2.3.6 Exact surface charge modeling -- 2.3.7 Constant frequency analysis -- 2.4 Boundary Value Problem Formulation -- 2.4.1 Model for weak charge buildup -- 2.4.2 Distributed surface charge. , 2.4.3 Predictor-corrector model for strong polarization -- 2.4.4 Fully coupled model for strong polarization -- 2.5 Computational Issues and Strategies -- 2.5.1 Alternative computational approaches -- 2.5.2 Difference model at field points within layers -- 2.5.3 Discontinuous functions and normal derivatives -- 2.5.4 Scalar potential solution -- 2.5.5 No limiting assumptions -- 2.5.6 Logging tool mandrels -- 2.5.7 Matrix analysis -- 2.5.8 Programming notes -- 2.5.9 Validation procedures -- 2.6 Typical Simulation Results -- 2.6.1 Example 1. Vertical hole, 20 KHz -- 2.6.2 Example 2. Vertical hole, 2 MHz -- 2.6.3 Example 3. Vertical hole, 2 MHz, collar -- 2.6.4 Example 4. Tilted beds, 45° dip, 20 KHz -- 2.6.5 Example 5. Tilted beds, 45° dip, 2 MHz -- 2.6.6 Example 6. Tilted beds, 60° dip, 2 MHz -- 2.6.7 Example 7. Tilted beds, 75° dip, 2 MHz -- 2.6.8 Example 8. Tilted beds, 90° dip, 2 MHz -- 2.6.9 Example 9. 90° dip, 2 Hz, with collar -- 2.6.10 Example 10. Anisotropic effects -- 2.6.11 Example 11. More anisotropic effects -- 2.6.12 Example 12. Transmitter placement -- 2.6.13 Example 13. More, transmitter placement -- 2.6.14 Example 14. Double bed intersections -- 2.7 Post-Processing and Applications -- 2.7.1 Amplitude and phase -- 2.7.2 Effects of interfacial surface charge -- 2.7.3 Cylindrical radial coordinates -- 2.7.4 Coordinate system notes -- 2.7.5 Magnetic field modeling -- 2.8 Restrictions with Fast Multi-frequency Methods -- 2.8.1 Method 1 -- 2.8.2 Method 2 -- 2.9 Receiver Design Philosophy -- 2.10 Description of Output Files -- 2.10.1 Output 'Answer.Dat' files in rectangular coordinates -- 2.10.2 Output 'Quiklook.Dat' files in rectangular coordinates -- 2.10.3 Output functions in cylindrical coordinates -- 2.10.4 Typical "Point Summary" output -- 2.10.5 Additional simulation files. , 2.10.6 Creating color plots in planes perpendicular to z coordinate surfaces -- 2.11 Apparent Resistivity Using Classic Dipole Solution -- 2.12 Coordinate Conventions for Mud and Invasion Modeling -- 2.12.1 Modeling borehole mud and invaded zones -- 2.13 Generalized Fourier Integral for Transient Sounding -- 2.14 References -- 3 Validations - Qualitative Benchmarks -- 3.1 Overview -- 3.2 Introductory Problems -- 3.2.1 Example 1. Horizontal "coil alone," vertical well in homogeneous unlayered medium -- 3.2.1.1 Validation of results -- 3.2.1.2 Understanding electric fields -- 3.2.1.3 Understanding magnetic fields -- 3.2.1.4 Understanding point summaries -- 3.2.2 Example 2. Vertical "coil alone," horizontal well in homogeneous unlayered medium -- 3.2.3 Example 3. 45 degree "coil alone" problem in homogeneous unlayered medium -- 3.2.4 Example 4. Ninety degree dip, three-layer problem, "coil alone" -- 3.2.4.1 Understanding interfacial surface charge -- 3.2.5 Example 5. Ninety degree dip, three-layer problem, "steel mandrel" -- 3.2.6 Example 6. Forty-five degree dip, three-layer problem, "coil alone" -- 3.2.7 Example 7. Fully 3D, anisotropic, three-layer problem, with non-dipolar transmitter coil residing across three thin beds -- 3.3 Advanced Problems -- 3.3.1 Example 1. Vertical hole, 20 KHz -- 3.3.2 Example 2. Vertical hole, 2 MHz -- 3.3.3 Example 3. Vertical hole, 2 MHz, collar -- 3.3.4 Example 4. Titled beds, 45° dip, 20 KHz -- 3.3.5 Example 5. Tilted beds, 45° dip, 2 MHz -- 3.3.6 Example 6. Tilted beds, 60° dip, 2 MHz -- 3.3.7 Example 7. Tilted beds, 75° dip, 2 MHz -- 3.3.8 Example 8. Tilted beds, 90° dip, 2 MHz -- 3.3.9 Example 9. 90° dip, 2 MHz, with collar -- 3.3.10 Example 10. Anisotropic effects -- 3.3.11 Example 11. More anisotropic effects -- 3.3.12 Example 12. Transmitter placement -- 3.3.13 Example 13. More, transmitter placement. , 3.3.14 Example 14. Double bed intersections -- 3.4 Sign Conventions and Validation Methodology -- 3.5 References -- 4 Validations - Quantitative Benchmarks at 0° and 90° -- 4.1 Overview -- 4.2 Wireline Validations in Homogeneous Media -- 4.2.1 Simplified analytical models and comparison objectives -- 4.2.1.1 Classical dipole model -- 4.2.1.2 Nonconductive Biot-Savart model -- 4.2.1.3 Electromagnetic versus simulation parameters -- 4.2.1.4 Reiteration of basic ideas -- 4.2.2 Inverse dependence of magnetic field source strength on coil diameter -- 4.2.3 Calculating transmitter magnetic field source strength -- 4.2.4 Validating receiver Bimag/Breal ratio on a wide range of variable grids -- 4.2.4.1 Stretching Simulation Set No. 1 -- 4.2.4.2 Stretching Simulation Set No. 2 -- 4.2.4.3 Stretching Simulation Set No. 3 -- 4.2.4.4 Stretching Simulation Set No. 4 -- 4.2.5 Simulations holding resistivity fixed, with frequency varying -- 4.2.6 Simulations holding frequency fixed, with resistivity varying -- 4.3 Wireline Validations in Two-Layer Inhomogeneous Media -- 4.3.1 Remarks and observations -- 4.3.1.1 Detailed simulation results -- 4.3.1.2 Simulation differences explained -- 4.3.2 One inch diameter transmitter, vertical well -- 4.3.2.1 Run 22a highlights -- 4.3.2.2 Run 22b highlights -- 4.3.2.3 Run 22c highlights -- 4.3.3 Six inch diameter transmitter, vertical well -- 4.3.3.1 Run 23a highlights -- 4.3.3.2 Run 23b highlights -- 4.3.3.3 Run 23c highlights -- 4.3.4 One inch diameter transmitter, horizontal well -- 4.3.4.1 Run 25a highlights -- 4.3.4.2 Run 25b highlights -- 4.3.4.3 Run 25c highlights -- 4.3.5 Six inch diameter transmitter, horizontal well -- 4.3.5.1 Run 26a highlights -- 4.3.5.2 Run 26b highlights -- 4.3.5.3 Run 26c highlights -- 4.4 Electric and Magnetic Field Sensitive Volume Analysis for Resistivity and NMR Applications. , 4.4.1 Depth of electromagnetic investigation in layered media with dip -- 4.4.2 Typical layered media simulations (Cases 1-5) -- 4.5 MWD "Steel Collar" and Wireline Computations in Homogeneous and Nonuniform Layered Dipping Media -- 4.5.1 Wireline vs MWD logging scenarios -- 4.5.2 Wireline "coil alone" simulation in uniform media -- 4.5.3 MWD "steel drill collar" simulation in uniform media -- 4.5.4 Wireline "coil alone" simulation in layered media -- 4.5.5 MWD "steel drill collar" simulation in layered media -- 4.6 Exact Drill Collar Validation Using Shen Analytical Solution -- 4.7 Dipole Interpolation Formula Validation in Farfield -- 4.8 Magnetic Dipole Validation in Two-Layer Formation -- 4.9 References -- 5 Validations-Quantitative Benchmarks at Deviated Angles -- 5.1 Overview -- 5.2 Limit 1. No Collar, No Mud -- 5.2.1 Observations on variable mesh system -- 5.2.2 Review of results for 0° and 90° -- 5.2.3 Validation for general dip angles -- 5.3 Limit 2. Collar Only, No Mud -- 5.4 Limit 3. Mud Only, No Collar -- 5.5 Limit 4. Collar and Mud -- 6 Validations - Quantitative Benchmarks at Deviated Angles with Borehole Mud and Eccentricity -- 6.1 Overview -- 6.2 Repeat Validations -- 6.2.1 Simulation Set 1. Objective, validate steel drill collar logic for 6 inch transmitter coil in homogeneous medium, with borehole radius of "0" meaning "no mud" first. Later on, add mud effects -- 6.2.2 Simulation Set 2. Objective, borehole modeling at 0 deg dip, vertical well application. Here, 1 Ωm formation runs next, model the borehole with 0.01 Ωm if there is a hole, so we can "see" 0.02 its attenuative effects quickly -- 6.2.3 Simulation Set 3. Objective, repeat calculations immediately above, but for 90 deg dip, horizontal well application. Intention is to duplicate above results with differently oriented logic loop. , 6.2.4 Simulation Set 4. Objective, repeat work just above, but for 45° dip deviated well. Intention to duplicate prior results with differently oriented logic loop.
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  • 4
    Keywords: Konferenzschrift ; Anthropogene Klimaänderung
    Type of Medium: Book
    Pages: XXI, 308 S , Ill
    ISBN: 0262191016 , 0262690330
    DDC: 551.6/8
    RVK:
    RVK:
    Language: English
    Note: Sponsored by the Massachusetts Institute of Technology and hosted by the Royal Swedish Academy of Sciences and the Royal Swedish Academy of Engineering Sciences
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  • 5
    In: Marine geology, Amsterdam [u.a.] : Elsevier, 1964, 213(2004), 1, Seite 149-167, 0025-3227
    In: volume:213
    In: year:2004
    In: number:1
    In: pages:149-167
    Type of Medium: Article
    ISSN: 0025-3227
    Language: English
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  • 6
    Publication Date: 2016-12-13
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 7
    Publication Date: 2017-04-04
    Description: While the upper crustal structure of the Southern Apennines is known, lack of control on the deep structure allows competing thin-skinned and thick-skinned models of the orogen. In thin-skinned models, the detachment decouples a stack of rootless nappes from the basement. In thick-skinned models, basement is involved in the most recent phase of thrusting. To examine crustal structure, we use teleseismic data from the Calabria-Apennine-Tyrrhenian/Subduction- Accretion-Collision Network (CAT/SCAN) array in southern Italy. We use receiver functions (RF) processed into a common conversion point stack to generate images of the crust. Inter- pretation and correlation to geological structure are done using inversions of individual station RFs. We focus on a shallow discontinuity where P-to-S conversions occur. In the foreland, it corresponds to velocity jumps between carbonate and clastic strata with basement. A similar interpretation for the Apennines provides the most parsimonious explanation and supports a thick-skinned interpretation. In a thick-skinned reconstruction, the amount of shortening is much smaller than for a thin-skinned model. This implies considerably less Pliocene–Pleistocene shortening across the Apennines and suggests an east-southeast motion of the Calabrian arc subparallel to the southern Apennines rather than a radial expansion of the arc.
    Description: Published
    Description: 155-158
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: JCR Journal
    Description: reserved
    Keywords: thrust tectonics ; Apennines ; continental collision ; seismology ; receiver functions ; structural geology ; 01. Atmosphere::01.03. Magnetosphere::01.03.04. Structure and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2017-04-04
    Description: While the upper structure of the Southern Apennines is known, lack of control on the deep structure allows competing thin-skin and tick-skin models of the orogen. In thin-skin models the detachment decouples a stack of rootless nappes from the basement. In the tick-skin models, besement is involved in the most recent phase of thrusting. To examine crustal structure, we use teleseismic data from the CAT/SCAN array in southern Italy. We use receiver functions (RF) processed into a Common Conversion Point (CCP) stack to generate images of the crust. Interpretation and correlation to geological structure is done using inversions of individual station RFs. We focus on a shallow discontinuity where P-to-S conversions occur. In the foreland, it corresponds to velocity jumps between carbonate and clastic strata with basement. A similar interpretation for the Apennines provides the most parsimonious explanation and supports a tick-skin interpretation. In a thick-skin reconstruction, the amount of shortening is much smaller than for a thin-skin model. This implies considerably less Plio-Pleistocene shortening across the Apennines and suggests an E-SE motion of the Calabrian Arc subparallel to the southern Apennines rather than a radial expansion of the Arc.
    Description: In press
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: JCR Journal
    Description: open
    Keywords: receiver functions ; Apennines ; thrust tectonics ; structural geology ; 01. Atmosphere::01.03. Magnetosphere::01.03.04. Structure and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: manuscript
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  • 9
    Publication Date: 2017-04-04
    Description: Field geology, well data and seismic imaging have illuminated the upper crustal structure of the Southern Apennines. However, lack of control of the deep structure allows viable competing thin-skin and thick-skin models of the orogen. In thin-skin models the detachment decouples a stack of rootless nappes from the basement. In thick-skin models, basement is involved in the most recent phase of thrusting. To examine the deep crustal structure, we use the teleseismic recordings from the CAT/SCAN array, deployed in southern Italy from Dec. 2003-Oct. 2005. We use receiver functions processed into a Common Conversion Point stack to generate images of the crust. We image three main westward-dipping seismic-velocity discontinuities where P-to-S conversions occur. They correspond to velocity jumps at the Moho, the upper-lower crust boundary and sedimentary interfaces resulting from the contrast between clastic and carbonate strata with basement. The CCP image matches features from both thin-skin and thick skin model. The lateral continuity of the converters favors thin skin, but consistent interpretation across the image favors the thick skin. Overall, the results provide a better fit to the thick-skin interpretation. This suggests a change in structural style as the collision with Apulia halted motion. This model also implies considerably less Plio-Pleistocene shortening across the Apennines and a SE motion of the Calabrian Arc subparallel to the southern Apennines rather than a radial expansion of the Arc.
    Description: Published
    Description: AGU General Assembly, S. Francisco
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: open
    Keywords: Continental Crust ; Suduction zone processes ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 10
    Publication Date: 2017-04-04
    Description: Basaltic volcanism is most typically thought to produce effusion of lava, with the most explosive manifestations ranging from mild Strombolian activity to more energetic fire fountain eruptions. However, some basaltic eruptions are now recognized as extremely violent, i.e., generating widespread phreatomagmatic, subplinian and Plinian fall deposits. We focus here on the influence of conduit processes, especially partial open-system degassing, in triggering abrupt changes in style and intensity that occurred during two examples of basaltic Plinian volcanism. We use the 1886 eruption of Tarawera, New Zealand, the youngest known basaltic Plinian eruption and the only one for which there are detailed written eyewitness accounts, and the well-documented 122 BC eruption of Mount Etna, Italy, and present new grain size and vesicularity data from the proximal deposits. These data show that even during extremely powerful basaltic eruptions, conduit processes play a critical role in modifying the form of the eruptions. Even with very high discharge, and presumably ascent, rates, partial open-system behaviour of basaltic melts becomes a critical factor that leads to development of domains of largely stagnant and outgassed melt that restricts the effective radius of the conduit. The exact path taken in the waning stages of the eruptions varied, in response to factors which included conduit geometry, efficiency and extent of outgassing and availability of ground water, but a relatively abrupt cessation to sustained high-intensity discharge was an inevitable consequence of the degassing processes.
    Description: Published
    Description: 1-14
    Description: partially_open
    Keywords: basaltic Plinian eruption ; Etna ; Tarawera and explosive volcanism ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 520 bytes
    Format: 743033 bytes
    Format: text/html
    Format: application/pdf
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