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Engineering Physics of High-Temperature Materials


Engineering Physics of High-Temperature Materials

Metals, Ice, Rocks, and Ceramics
1. Aufl.

von: Nirmal K. Sinha, Shoma Sinha

169,99 €

Verlag: Wiley
Format: PDF
Veröffentl.: 15.02.2022
ISBN/EAN: 9781119420453
Sprache: englisch
Anzahl Seiten: 432

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Beschreibungen

<b>ENGINEERING PHYSICS OF HIGH-TEMPERATURE MATERIALS</b> <p><b>Discover a comprehensive exploration of high temperature materials written by leading materials scientists </b> <p>In <i>Engineering Physics of High-Temperature Materials: Metals, Ice, Rocks, and Ceramics</i> distinguished researchers and authors Nirmal K. Sinha and Shoma Sinha deliver a rigorous and wide-ranging discussion of the behavior of different materials at high temperatures. The book discusses a variety of physical phenomena, from plate tectonics and polar sea ice to ice-age and intraglacial depression and the postglacial rebound of Earth’s crust, stress relaxation at high temperatures, and microstructure and crack-enhanced Elasto Delayed Elastic Viscous (EDEV) models. At a very high level, <i>Engineering Physics of High-Temperature Materials (EPHTM)</i> takes a multidisciplinary view of the behavior of materials at temperatures close to their melting point. The volume particularly focuses on a powerful model called the Elasto-Delayed-Elastic-Viscous (EDEV) model that can be used to study a variety of inorganic materials ranging from snow and ice, metals, including complex gas-turbine engine materials, as well as natural rocks and earth formations (tectonic processes). It demonstrates how knowledge gained in one field of study can have a strong impact on other fields. <p><i>Engineering Physics of High-Temperature Materials</i> will be of interest to a broad range of specialists, including earth scientists, volcanologists, cryospheric and interdisciplinary climate scientists, and solid-earth geophysicists. The book demonstrates that apparently dissimilar polycrystalline materials, including metals, alloys, ice, rocks, ceramics, and glassy materials, all behave in a surprisingly similar way at high temperatures. This similarity makes the information contained in the book valuable to all manner of physical scientists. <p>Readers will also benefit from the inclusion of: <ul><li>A thorough introduction to the importance of a unified model of high temperature material behavior, including high temperature deformation and the strength of materials</li> <li>An exploration of the nature of crystalline substances for engineering applications, including basic materials classification, solid state materials, and general physical principles</li> <li>Discussions of forensic physical materialogy and test techniques and test systems</li> <li>Examinations of creep fundamentals, including rheology and rheological terminology, and phenomenological creep failure models</li></ul> <p>Perfect for materials scientists, metallurgists, and glaciologists, <i>Engineering Physics of High-Temperature Materials: Metals, Ice, Rocks, and Ceramics</i> will also earn a place in the libraries of specialists in the nuclear, chemical, and aerospace industries with an interest in the physics and engineering of high-temperature materials.
<p>Acknowledgments xiii</p> <p>Engineering Physics of High-Temperature Materials xv</p> <p><b>1 Importance of a Unified Model of High-Temperature Material Behavior </b><b>1</b></p> <p>1.1 The World’s Kitchens – The Innovation Centers for Materials Development 1</p> <p>1.1.1 Defining High Temperature Based on Cracking Characteristics 4</p> <p>1.2 Trinities of Earth’s Structure and Cryosphere 7</p> <p>1.2.1 Trinity of Earth’s Structure 7</p> <p>1.2.2 Trinity of Earth’s Cryospheric Regions 7</p> <p>1.3 Earth’s Natural Materials (Rocks and Ice) 8</p> <p>1.3.1 Ice: A High-Temperature Material 9</p> <p>1.3.2 Ice: An Analog to Understand High-Temperature Properties of Solids 10</p> <p>1.4 Rationalization of Temperature: Low and High 12</p> <p>1.5 Deglaciation and Earth’s Response 12</p> <p>1.6 High-Temperature Deformation: Time Dependency 13</p> <p>1.6.1 Issues with Terminology: Elastic, Plastic, and Viscous Deformation 13</p> <p>1.6.2 Elastic, Delayed Elastic, and Viscous Deformation 13</p> <p>1.7 Strength of Materials 16</p> <p>1.8 Paradigm Shifts 18</p> <p>1.8.1 Paradigm Shift in Experimental Approach 18</p> <p>1.8.2 Breaking Tradition for Creep Testing 19</p> <p>1.8.3 Exemplification the Novel Approach 19</p> <p>1.8.4 Romanticism for a Constant-Structure Creep Test 23</p> <p>References 25</p> <p><b>2 Nature of Crystalline Substances for Engineering Applications </b><b>29</b></p> <p>2.1 Basic Materials Classification 30</p> <p>2.2 Solid-state Materials 31</p> <p>2.2.1 Structure of Crystalline Solids 31</p> <p>2.2.2 Structure of Amorphous Solids 33</p> <p>2.3 General Physical Principles 34</p> <p>2.3.1 Solidification of Materials 34</p> <p>2.3.2 Phase Diagrams 35</p> <p>2.3.3 Crystal Imperfections 37</p> <p>2.4 Glass and Glassy Phase 40</p> <p>2.4.1 Glass Transition 40</p> <p>2.4.2 Structure of Real Glass 41</p> <p>2.4.3 Composition of Standard Glass 41</p> <p>2.4.4 Thermal Tempering 42</p> <p>2.4.5 Material Characteristics 43</p> <p>2.5 Rocks: The Most Abundant Natural Polycrystalline Material 44</p> <p>2.5.1 Sedimentary Rocks 44</p> <p>2.5.2 Metamorphic Rocks 45</p> <p>2.5.3 Igneous Rocks 45</p> <p>2.6 Ice: The Second Most Abundant Natural Polycrystalline Material 45</p> <p>2.7 Ceramics 47</p> <p>2.8 Metals and Alloys 48</p> <p>2.8.1 Iron-base Alloys 48</p> <p>2.8.2 Nickel-base Alloys 50</p> <p>2.8.3 Titanium-base Alloys 53</p> <p>2.8.4 Mechanical Metallurgy 54</p> <p>2.9 Classification of Solids Based on Mechanical Response at High Temperatures 55</p> <p>References 56</p> <p><b>3 Forensic Physical Materialogy </b><b>59</b></p> <p>3.1 Introduction 59</p> <p>3.1.1 Material Characterization 60</p> <p>3.2 Polycrystalline Solids and Crystal Defects 61</p> <p>3.2.1 Etch-Pitting Technique – A Powerful Tool 63</p> <p>3.3 Structure and Texture of Natural Hexagonal Ice, <i>I</i><sub>h</sub> 67</p> <p>3.4 Section Preparation for Microstructural Analysis 69</p> <p>3.4.1 Thin Sectioning of Ice 69</p> <p>3.4.2 Large 300mm Diameter Polariscope 69</p> <p>3.4.3 Sectioning for Forensic Analysis of Compression Failure 70</p> <p>3.5 Etching of Prepared Section Surfaces 71</p> <p>3.5.1 Surface Etching 72</p> <p>3.6 Sublimation Etch Pits in Ice, <i>I</i><sub>h</sub> 72</p> <p>3.7 Etch-Pitting Technique for Dislocations 75</p> <p>3.7.1 Simultaneous Etching and Replicating 76</p> <p>3.7.2 Etching Processes and Their Applications 77</p> <p>3.8 Chemical Etching and Replicating of Ice Surfaces 79</p> <p>3.9 Displaying Dislocation Climb by Etching 81</p> <p>3.10 Thermal Etching: An Unexploited Materialogy Tool 82</p> <p>References 88</p> <p><b>4 Test Techniques and Test Systems </b><b>91</b></p> <p>4.1 On the Strength of Materials and Test Techniques 91</p> <p>4.1.1 Issues with Stress–Strain (<i>σ</i>–<i>ε</i>) Diagrams at High Temperatures 93</p> <p>4.1.2 Fundamentals of Displacement Rate, Strain Rate, and Stress Rate Tests 95</p> <p>4.1.3 Time – An Important Parameter at High Temperatures 96</p> <p>4.2 Static Modulus and Dynamic Elastic Modulus 97</p> <p>4.3 Thermal Expansion Over a Wide Range of Temperature 97</p> <p>4.4 Creep and Fracture Strength 98</p> <p>4.5 Bending Tests 99</p> <p>4.5.1 Three-Point Bending 99</p> <p>4.5.2 Four-Point Bending 99</p> <p>4.5.3 Cantilever Beam Bending 102</p> <p>4.6 Compression Tests – Uniaxial, Biaxial, and Triaxial 103</p> <p>4.6.1 Uniaxial Compression Tests 103</p> <p>4.6.2 Biaxial or Confined Compression Tests 103</p> <p>4.6.3 Triaxial or Multiaxial Compression and Tension Tests 103</p> <p>4.7 Tensile and/or Compression Test System 104</p> <p>4.7.1 Tests with Single Top-Lever Loading Frame 104</p> <p>4.7.2 Universal Testing Machine and Systems: Introduction to SRRT Methodology 105</p> <p>4.8 Stress Relaxation Tests (SRTs) 107</p> <p>4.8.1 Necessity for Stress Relaxation Properties 108</p> <p>4.8.2 Basic Principle of SRTs 109</p> <p>4.9 Cyclic Fatigue 110</p> <p>4.9.1 Low-Cycle Fatigue (LCF) and High-Cycle Fatigue (HCF Tests) 110</p> <p>4.9.2 Uncharted Characteristics of Delayed Elasticity in Cyclic Loading 112</p> <p>4.9.3 Cyclic Loading of Snow and Thermal Cycling on Asphalt Concrete 113</p> <p>4.10 Acoustic Emission (AE) and/or Microseismic Activity (MA) 114</p> <p>4.11 Tempering of Structural and Automotive Glasses 116</p> <p>4.12 Specimen Size and Geometry: Depending on Material Grain Structure 119</p> <p>4.13 In Situ Borehole Tests: Inspirations from Rock Mechanics 119</p> <p>References 123</p> <p><b>5 Creep Fundamentals </b><b>129</b></p> <p>5.1 Overview 130</p> <p>5.2 On Rheology and Rheological Terminology 132</p> <p>5.3 Forms of Creep and Deformation Maps 132</p> <p>5.3.1 Generalization for Polycrystalline Materials 132</p> <p>5.3.2 Nabarro–Herring Creep 133</p> <p>5.3.3 Coble Creep 133</p> <p>5.3.4 Harper–Dorn Creep 133</p> <p>5.3.5 Ashby–Verrall Creep 133</p> <p>5.3.6 Deformation Mechanism Maps 134</p> <p>5.4 Grain-Boundary Shearing or Sliding 134</p> <p>5.5 Creep Curves – Classical Primary, Secondary, and Tertiary Descriptions 135</p> <p>5.5.1 Elasticity and Annealing of Glass 136</p> <p>5.5.2 Phenomenological Rheology of Glass 137</p> <p>5.5.3 Normalized Creep – Another Presentation of Rheology of Glass 140</p> <p>5.6 Phenomenology of Primary Creep in Metals, Ceramics, and Rocks 144</p> <p>5.7 Primary Creep in Ice: Launching SRRT Technique and EDEV Model 148</p> <p>5.8 Grain-Boundary Shearing (gbs) and Grain-Size Dependent Delayed Elasticity 151</p> <p>5.9 Generalization of EDEV Model: Introduction of Grain-Size Effect 153</p> <p>5.10 Logarithmic Primary Creep: An Alternative Form of the EDEV Model 157</p> <p>5.11 Shifting Paradigms: Emphasizing Primary Creep of Polycrystalline Materials 158</p> <p>5.12 SRRT for Primary Creep and EDEV Model of a Titanium-Base Superalloy (Ti-6246) 158</p> <p>5.13 SRRT for Primary Creep and EDEV Model for a Nickel-Base Superalloy (Waspaloy) 162</p> <p>5.14 SRRT for Primary Creep of a Nickel-Rich Iron-Base Alloy (Discaloy) 169</p> <p>5.15 SRRTs for Primary Creep and EDEV Model of a Nickel-Base Superalloy (IN-738LC) 170</p> <p>5.16 EDEV-Based Strain-Rate Sensitivity of High-Temperature Yield Strength 175</p> <p>5.16.1 Constant Strain-Rate Yield 176</p> <p>5.16.2 Yield Strength of Ti-6246 at 873 K (0.45 <i>T</i><sub>m</sub>) 178</p> <p>5.16.3 Yield Strength of Waspaloy at 1005 K (0.62 <i>T</i><sub>m</sub>) 178</p> <p>5.17 Single-Crystal (SX) Superalloy Delayed Elasticity and <i>γ</i>/<i>γ </i>Interface Shearing 185</p> <p>5.18 Creep, Steady-State Tertiary Stage, and Elasto–Viscous (EV) Model for Single Crystals 191</p> <p>5.19 Creep Fracture and EV Model for CMSX-10 SXs 194</p> <p>5.20 Fracture and Inhomogeneous Deformation 198</p> <p>5.21 Dynamic Steady-State Tertiary Creep of Several Nickel-Base SXs 200</p> <p>5.21.1 MAR-M-247 Single Crystal 200</p> <p>5.21.2 CMSX-3 Single Crystal 201</p> <p>5.21.3 CMSX-4 Single Crystal with Rhenium 202</p> <p>5.21.4 CMSX-4 Single Crystal 202</p> <p>5.21.5 TMS-75 Single Crystal 203</p> <p>5.21.6 SRR99 Single Crystal 205</p> <p>References 205</p> <p><b>6 Phenomenological Creep Failure Models </b><b>215</b></p> <p>6.1 Creep and Creep Failure 215</p> <p>6.2 Steady-State Creep 216</p> <p>6.3 Commonly Used Creep Experiments and Strength Tests 217</p> <p>6.3.1 Constant Stress and Constant Deformation (CD) Rate Tests 217</p> <p>6.3.2 A Short Glimpse of Creep Tests 220</p> <p>6.3.3 Power Law for Creep 220</p> <p>6.3.4 Larsen and Miller Concept 223</p> <p>6.3.5 Monkman and Grant (M-G) Relationship 223</p> <p>6.3.6 Rabotnov–Kachanov Concept for Creep Fracture 224</p> <p>6.3.7 Breaking Tradition – <i>θ</i>-Projection Concept 224</p> <p>6.4 Modeling Very Long-Term Creep Rupture from Short-Term Tests 225</p> <p>6.4.1 Traditional Approaches for Power-Generation Operations 225</p> <p>6.4.2 Captivating and Entrenched Focus on Minimum Creep Rate 226</p> <p>6.5 High-Temperature Low-Cycle Fatigue (HT-LCF) and Dwell Fatigue 226</p> <p>6.6 Crucial Tests on Rate Sensitivity of High-Temperature Strength 227</p> <p>6.7 Rational Approach Inspired by the Principle of “Hindsight 20/20” 232</p> <p>References 233</p> <p><b>7 High-Temperature Grain-Boundary Embrittlement and Creep </b><b>237</b></p> <p>7.1 Fracture and Material Failure 237</p> <p>7.1.1 Griffith’s Model for Crack Propagation 239</p> <p>7.1.2 Crack Nucleation Mechanisms at Low Homologous Temperatures 240</p> <p>7.1.3 Acoustic Emissions and Cracks 241</p> <p>7.1.4 A Novel Treatment of AE and Cracks in Ice Engineering 242</p> <p>7.2 Grain Size Effects on Strength 245</p> <p>7.2.1 Popular Low-Temperature Concept of Strength 245</p> <p>7.2.2 Problems with Estimating Grain Size 245</p> <p>7.2.3 Inapplicability of the Hall–Petch Relation at High Temperatures 246</p> <p>7.3 Grain-Boundary Shearing (gbs) Induced Crack Initiation 246</p> <p>7.3.1 Groundwork for a High-Temperature Crack-Initiation Hypothesis 248</p> <p>7.3.2 Gold’s Classic Studies on Creep Cracking by Visual Observations 249</p> <p>7.3.3 Forensic Microstructural Examinations of First Creep Cracks 251</p> <p>7.3.4 First Grain-Facet-Sized Cracks and Critical Delayed Elastic Criterion 252</p> <p>7.3.5 Critical Time and Stress for Onset of Creep Fracture 254</p> <p>7.3.6 Critical Strain for First Cracks (or Fracture Failure) 255</p> <p>7.3.7 Apparent Activation Energy for First Cracks and Fracture 257</p> <p>7.3.8 Kinetics of Creep Cracking 258</p> <p>References 260</p> <p><b>8 Microstructure and Crack-Enhanced Elasto – Delayed-Elastic – Viscous Models </b><b>265</b></p> <p>8.1 Physics-Based Holistic Model Approach 265</p> <p>8.1.1 On Transient Creep and the Shape of Creep Curves 266</p> <p>8.1.2 On “Limiting Transient Creep Strain” (<i>ε</i><sub>T</sub>) 267</p> <p>8.1.3 On the Traditions of Creep Testing and Shifting Paradigms 268</p> <p>8.2 Kinetics of Microcracking and Structural Damage 271</p> <p>8.3 Microcrack-Enhanced EDEV Model 271</p> <p>8.4 EDEV-Based Algorithm for Constant Strain Rate, Encompassing Cracking 273</p> <p>8.4.1 EDEV-Based Stress–Strain Diagrams 275</p> <p>8.5 Constant Stress, Crack-Enhanced Creep: EDEV Predictions 279</p> <p>8.5.1 Apparent Brittle–Ductile Transition in Constant Stress Creep 281</p> <p>8.5.2 Power-Law Breakdown for Minimum Creep Rate 283</p> <p>8.5.3 Grain-Size Effects on Creep with Crack Formation 284</p> <p>8.5.4 Creep Dilatation in Polycrystalline Columnar-Grained and Equiaxed Solids 287</p> <p>8.5.5 Crack Damage at Minimum Creep Rate and Upper Yield 291</p> <p>8.5.6 Strain-Rate Sensitivity of Initial Deformation, Dilatancy, and Residual Strength 293</p> <p>8.6 Cyclic Fatigue 293</p> <p>8.6.1 Low-Cycle Constant Strain Rate Loading 294</p> <p>8.6.2 Low-Cycle, High-Strain Fatigue: Repeated Constant Load 295</p> <p>8.7 Crack Healing or Closure of w-Type Voids Generating r-Type Cavities 295</p> <p>References 298</p> <p><b>9 Stress Relaxation at High Temperatures </b><b>303</b></p> <p>9.1 The Role of Stress Relaxation Tests at High Temperatures 303</p> <p>9.1.1 Traditional SRTs 304</p> <p>9.1.2 Phenomenology of Stress Relaxation 306</p> <p>9.1.3 Capabilities and Inadequacies of SRT for Creep Estimation 308</p> <p>9.1.4 Rationalization of SRT Processes 309</p> <p>9.1.5 SRT on Coarse-Grained Materials 310</p> <p>9.1.6 New Approaches for Examining Applicability of SRT for Fine-Grained Materials 313</p> <p>9.1.7 Grain-Size-Based Optimization of Initial Strain, <i>ε</i><sub>0</sub>, for SRT 317</p> <p>9.2 Constitutive Equations without Effect of Grain Size 318</p> <p>9.2.1 Constitutive Equation for Uniaxial Creep at High Temperatures 318</p> <p>9.2.2 SR Based on Constitutive Equation 321</p> <p>9.2.3 Type-A Engineering Prediction for SRT 321</p> <p>9.3 Temperature and Grain-Size Effects on SR 327</p> <p>9.3.1 EDEV Constitutive Equation Incorporating Grain Size and Temperature 327</p> <p>9.3.2 EDEV-Based SRT Algorithm for Grain-Size and Temperature Dependency 328</p> <p>9.3.3 Lack of Grain-Size-Dependent Data on Primary Creep of Engineering Materials 328</p> <p>9.4 Forecasting Grain-Size Effects on SR in Pure Ice Based on EDEV Equation 328</p> <p>9.4.1 Basis of Calculation for Ice 329</p> <p>9.4.2 Effect of Strain, <i>ε</i><sub>0</sub> (Constant Temperature and Grain Size) 329</p> <p>9.4.3 Effect of Temperature (Constant Strain and Grain Size) 331</p> <p>9.4.4 Effect of Grain Size (Constant Strain and Temperature) 331</p> <p>9.4.5 Strain (<i>ε</i><sub>0</sub>) Dependence of Strain Components (Constant Temperature and Grain Size) 332</p> <p>9.4.6 Grain-Size Effect on Strain Components During SRT (Constant Strain and Temperature) 332</p> <p>9.4.7 Comments on SRTs Related to Ice and Field Experience 332</p> <p>9.5 High-Temperature Forming, Delayed Spring-Back, and Grain-Size Effects on SR in Metals 335</p> <p>References 339</p> <p><b>10 Ice Age and Intraglacial Depression and Postglacial Rebound of Earth’s Crust </b><b>343</b></p> <p>10.1 Tectonic Plates, Lake Ice, and High-Temperature Materials: What Is the Connection? 343</p> <p>10.2 On Glaciers and Oceanic Ice Cover: Past and Present 345</p> <p>10.2.1 Rise of Canada – Postglacial Uplift 346</p> <p>10.2.2 Postglacial Adjustments of North America’s Landscape 346</p> <p>10.3 Dow’s Lake Studies 347</p> <p>10.3.1 Dow’s Lake Ice Sheet: Crowd Load/Unload During Winter of 1985 347</p> <p>10.3.2 Swimming Pool Loading Experiment on Dow’s Lake Ice in 1986 351</p> <p>10.4 Elasto – Delayed-Elastic (EDE) Theory for Plates 356</p> <p>References 362</p> <p><b>11 Plate Tectonics and Polar Sea Ice </b><b>365</b></p> <p>11.1 Retrospective Introduction 365</p> <p>11.2 Earth and Plate Tectonics 368</p> <p>11.2.1 On Sea Ice: Analog for Tectonic Plates 369</p> <p>11.2.2 Trinity of Tectonic Plates 371</p> <p>11.2.3 Trinity of Tectonic Plate Boundaries 371</p> <p>11.3 Scale of Observations 372</p> <p>11.3.1 Messengers of Earth Below and Sky Above 376</p> <p>11.4 Vertical Temperature Profiles of Earth and Ice Sheet 378</p> <p>11.5 Time–Temperature Shift Function 381</p> <p>11.6 Nonlinear, Grain-Size-Dependent Delayed Elasticity (Anelasticity) of Mantle 382</p> <p>11.7 Stress Field of Earth’s Crust 385</p> <p>11.8 Koyna and Warna Dams in India and Reservoir-Triggered Seismicity (RTS) 386</p> <p>11.9 Movement of Tectonic Plates, Indentation, and Fracture 391</p> <p>11.10 Looking Forward 394</p> <p>References 395</p> <p>Index 401</p>
<p><b>Nirmal K. Sinha,</b> Retired, Institute for Aerospace Research, National Research Council of Canada, Ottawa, Ontario, Canada.</p> <p><b>Shoma Sinha,</b> Queen's Partnerships and Innovation, Queen's University, Kingston, Ontario, Canada.</p>
<p><b>Discover a comprehensive exploration of high temperature materials written by leading materials scientists </b></p> <p>In <i>Engineering Physics of High-Temperature Materials: Metals, Ice, Rocks, and Ceramics</i> distinguished researchers and authors Nirmal K. Sinha and Shoma Sinha deliver a rigorous and wide-ranging discussion of the behavior of different materials at high temperatures. The book discusses a variety of physical phenomena, from plate tectonics and polar sea ice to ice-age and intraglacial depression and the postglacial rebound of Earth’s crust, stress relaxation at high temperatures, and microstructure and crack-enhanced Elasto Delayed Elastic Viscous (EDEV) models. At a very high level, <i>Engineering Physics of High-Temperature Materials (EPHTM)</i> takes a multidisciplinary view of the behavior of materials at temperatures close to their melting point. The volume particularly focuses on a powerful model called the Elasto-Delayed-Elastic-Viscous (EDEV) model that can be used to study a variety of inorganic materials ranging from snow and ice, metals, including complex gas-turbine engine materials, as well as natural rocks and earth formations (tectonic processes). It demonstrates how knowledge gained in one field of study can have a strong impact on other fields. <p><i>Engineering Physics of High-Temperature Materials</i> will be of interest to a broad range of specialists, including earth scientists, volcanologists, cryospheric and interdisciplinary climate scientists, and solid-earth geophysicists. The book demonstrates that apparently dissimilar polycrystalline materials, including metals, alloys, ice, rocks, ceramics, and glassy materials, all behave in a surprisingly similar way at high temperatures. This similarity makes the information contained in the book valuable to all manner of physical scientists. <p>Readers will also benefit from the inclusion of: <ul><li>A thorough introduction to the importance of a unified model of high temperature material behavior, including high temperature deformation and the strength of materials</li> <li>An exploration of the nature of crystalline substances for engineering applications, including basic materials classification, solid state materials, and general physical principles</li> <li>Discussions of forensic physical materialogy and test techniques and test systems</li> <li>Examinations of creep fundamentals, including rheology and rheological terminology, and phenomenological creep failure models</li></ul> <p>Perfect for materials scientists, metallurgists, and glaciologists, <i>Engineering Physics of High-Temperature Materials: Metals, Ice, Rocks, and Ceramics</i> will also earn a place in the libraries of specialists in the nuclear, chemical, and aerospace industries with an interest in the physics and engineering of high-temperature materials.

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