標(biāo)題: Titlebook: Continuum Micromechanics; Theory and Applicati Dazhi Jiang Book 2023 The Editor(s) (if applicable) and The Author(s), under exclusive licen [打印本頁] 作者: TEMPO 時間: 2025-3-21 18:17
書目名稱Continuum Micromechanics影響因子(影響力)
作者: Climate 時間: 2025-3-21 21:42
Dazhi JiangContains numerous step-by-step tutorials.Provides a special chapter on next generation Flash.Includes a large number of MATLAB and MathCad codes作者: 許可 時間: 2025-3-22 01:47
Springer Geophysicshttp://image.papertrans.cn/c/image/237078.jpg作者: 去才蔑視 時間: 2025-3-22 05:25
https://doi.org/10.1007/978-3-031-23313-5Multiscale analysis; MathCad; Microstructures; Lithospheric deformation; Continental rheology; Continenta作者: BUOY 時間: 2025-3-22 09:25 作者: ALB 時間: 2025-3-22 13:59 作者: ALB 時間: 2025-3-22 19:27 作者: 陶器 時間: 2025-3-23 00:29 作者: defeatist 時間: 2025-3-23 01:44
Der Vermittler, die Vermittlung,ccur in the strain tensor definitions. This Chapter is concerned with the mathematical description of finite strain deformations. We will consider two configurations of a continuous body: the reference configuration and the deformed configuration. The reference configuration may be the undeformed st作者: 撫慰 時間: 2025-3-23 08:52 作者: 演講 時間: 2025-3-23 12:03 作者: duplicate 時間: 2025-3-23 14:09 作者: nitric-oxide 時間: 2025-3-23 19:14 作者: Inculcate 時間: 2025-3-23 23:09 作者: 相信 時間: 2025-3-24 04:31 作者: Paradox 時間: 2025-3-24 06:52 作者: 親屬 時間: 2025-3-24 10:56
https://doi.org/10.1007/978-3-531-90106-0sing the Green function and integral formalism as Chap. . for 3D problems..In Chaps. . and ., we have developed formal and, where possible, explicit solutions for a 3D elastic (or viscous) ellipsoid in an infinite elastic (or viscous) medium. Two-dimensional (2D) inclusion problems may be regarded a作者: ECG769 時間: 2025-3-24 17:58
Vergleichende Sozialkapitalforschung and strain. We introduced the Voigt and Reuss averages, which are, respectively, based on the uniform strain and uniform stress assumptions. These two averages are upper and lower bounds for the properties of the “average” material. In Earth Sciences, phenomenological approaches have been proposed 作者: lipoatrophy 時間: 2025-3-24 22:03 作者: 分期付款 時間: 2025-3-25 01:24
Neue Methoden der Familienarbeithosphere, they undoubtedly affect the rheology of the lithosphere. Shear zones also serve as conduits for the movement of fluids and melt and are often sites of economically significant minerals. In this chapter, we use Eshelby’s equivalent-inclusion approach to investigate the stress field and prog作者: 乳白光 時間: 2025-3-25 04:01
https://doi.org/10.1007/978-3-531-90211-1lanking structures as an example to use Eshelby’s exterior solutions..Flanking structures [Fig. .; Passchier (J Struct Geol 23(6–7):951–962, 2001)] are deflections of linear and planar fabric elements around a cross-cutting element such as a fault, vein, dyke, or any other heterogeneity. Many author作者: TIA742 時間: 2025-3-25 09:23 作者: Fraudulent 時間: 2025-3-25 14:10 作者: gait-cycle 時間: 2025-3-25 19:10
Verhandlung und Verhandlungstheorie,thematical description of deformation. Strain rate and vorticity in the rate-of-deformation description in this Chapter correspond, respectively, to strain and rotation in the two-state description in Chap. ..作者: BARB 時間: 2025-3-25 22:22 作者: laxative 時間: 2025-3-26 01:41 作者: justify 時間: 2025-3-26 04:44 作者: 盟軍 時間: 2025-3-26 10:15
Book 2023the theory, understand the approach, and to further develop and apply the methods to geological problems. Multiscale and multi-physics investigations of Earth and planetary processes have been an active trend of research in Earth Sciences, thanks to the development of scientific computation and comp作者: 折磨 時間: 2025-3-26 14:08
2364-9119 odes.The book integrates theory, numerical methods, and practical applications seamlessly. MATLAB and MathCad programs are provided for readers to master the theory, understand the approach, and to further develop and apply the methods to geological problems. Multiscale and multi-physics investigati作者: prolate 時間: 2025-3-26 20:15 作者: Corporeal 時間: 2025-3-26 22:01 作者: RAG 時間: 2025-3-27 01:33
Hans-Joachim Lauth,Jürgen R. Winklerer simple shearing. Simple shearing flows are the most studied flow type in materials science and geology literature. The results of this Chapter will be used later to verify a more general investigation of an elastic prolate object in a Newtonian viscous flow.作者: formula 時間: 2025-3-27 05:59 作者: 鈍劍 時間: 2025-3-27 13:18
https://doi.org/10.1007/978-3-531-90211-1w viscous rheology, by the linearization method. We then formulate a self-consistent multiscale model based on extended formalism. Finally, we summarize how the self-consistent model may be applied to the modelling of multiscale structures in Earth’s lithosphere.作者: Absenteeism 時間: 2025-3-27 16:03
Orientation of Fabric Elements,nes the preferred orientation of feldspars in that sample. During progressive deformation, . is a function of time. We mathematically characterize the orientation and rotation of line elements and 3D fabric elements. We also explore how to generate linear or 3D orientation sets to follow a certain given distribution in 3D space in this Chapter.作者: DEVIL 時間: 2025-3-27 21:24 作者: companion 時間: 2025-3-27 22:00 作者: overreach 時間: 2025-3-28 03:56 作者: 毀壞 時間: 2025-3-28 09:54
Constitutive Equations,, the constitutive equations, rheological equations, or flow laws. In addition to the elastic behavior, other rheological behaviors such as viscous, plastic, viscoelastic, and viscoplastic behaviors are important in the deformation of Earth’s lithosphere. They are briefly reviewed in this Chapter.作者: Tempor 時間: 2025-3-28 14:29 作者: 不近人情 時間: 2025-3-28 18:08 作者: Costume 時間: 2025-3-28 19:19 作者: Limerick 時間: 2025-3-28 23:41 作者: 激怒某人 時間: 2025-3-29 03:47
Stress, Strain, and Elasticity,initesimal strain tensor, more general strain tensors are introduced from displacement field gradients in preparation for finite deformation study. Anisotropic elasticity is discussed with elastic stiffness and elastic compliance expressed both in the standard Vogit matrix notation and in terms of f作者: 前奏曲 時間: 2025-3-29 10:28 作者: 北京人起源 時間: 2025-3-29 15:08 作者: 埋葬 時間: 2025-3-29 19:15
Flow and Finite Deformation in Tabular Zones,n discuss the finite strain geometry in homogeneous zones with parallel boundaries (tabular zones). There is a rich literature on the kinematic modeling of high-strain zones since Ramsay and Graham (.). We review and summarize the work in a unified approach in this Chapter. Geologists commonly regar作者: 可忽略 時間: 2025-3-29 23:17
Constitutive Equations,responses in this Chapter. The mathematical relations between the strain or strain rate tensor and the stress tensor for material are called, variably, the constitutive equations, rheological equations, or flow laws. In addition to the elastic behavior, other rheological behaviors such as viscous, p作者: Range-Of-Motion 時間: 2025-3-30 00:34 作者: CRATE 時間: 2025-3-30 06:06 作者: 異端 時間: 2025-3-30 10:41
,Eshelby’s Inclusion and Inhomogeneity Problem,nd orientation during deformation. We discuss the powerful method of John Douglas Eshelby (1916–1981) in this Chapter which solves the problem of a deformable ellipsoid. The point force and equivalent inclusion method of Eshelby’s can be applied to many other problems, such as deformation in and aro作者: breadth 時間: 2025-3-30 13:44
Viscous Inclusions in Anisotropic Materials,ials. In Chap. ., we presented the solutions for the classic inclusion/inhomogeneity problem (Eshelby, Proc R Soc Lond Ser A- 241(1226):376–396, 1957; Eshelby, Proc R Soc Lond Ser A- 252(1271):561–569, 1959) of an elastic inclusion/inhomogeneity in an isotropic elastic medium. The solutions have bee作者: 無意 時間: 2025-3-30 18:11
Two-Dimensional Inclusion Problems,sing the Green function and integral formalism as Chap. . for 3D problems..In Chaps. . and ., we have developed formal and, where possible, explicit solutions for a 3D elastic (or viscous) ellipsoid in an infinite elastic (or viscous) medium. Two-dimensional (2D) inclusion problems may be regarded a作者: 驚呼 時間: 2025-3-30 21:32
Effective Stiffnesses of Heterogeneous Materials, and strain. We introduced the Voigt and Reuss averages, which are, respectively, based on the uniform strain and uniform stress assumptions. These two averages are upper and lower bounds for the properties of the “average” material. In Earth Sciences, phenomenological approaches have been proposed 作者: 揉雜 時間: 2025-3-31 03:43
Application Example 1: An Elastic Prolate Object in a Viscous Matrix,ased on Jeffery’s (Proc R Soc Lond Ser A-Containing Papers of a Mathematical and Physical Character 102(715):161–179, 1922) original equations on the traction forces the viscous fluid exerts on the object’s surface [Forgacs and Mason (J Colloid Sci 14(5):457–472, 1959); Goldsmith and Mason (The micr作者: 谷物 時間: 2025-3-31 05:58 作者: Panacea 時間: 2025-3-31 12:54 作者: Aspiration 時間: 2025-3-31 16:04
,Generalization of Eshelby’s Formalism and a Self-Consistent Model for Multiscale Rock Deformation,linear rheology (either elastic or Newtonian viscous). We have also presented methods to evaluate the formal solutions numerically. In Chaps. .–., we applied the theory to some geology problems, assuming that the rheology is linear and the problems can be approximated by “a single ellipsoid in an in作者: 闖入 時間: 2025-3-31 17:59 作者: 不連貫 時間: 2025-3-31 21:59
Rotation of Rigid Objects in Homogeneous Flows,a rigid ellipsoid in slow viscous flows is combined with the rotation equation to form an initial value problem for the motion of a rigid ellipsoid in viscous flow. The problem is solved analytically for a spheroid in monoclinic flows. The problem is solved numerically for more general situations. M作者: cavity 時間: 2025-4-1 02:32 作者: Fluctuate 時間: 2025-4-1 08:47
