標(biāo)題: Titlebook: A First Course in Boundary Element Methods; Steven L. Crouch,Sofia G. Mogilevskaya Book 2024 The Editor(s) (if applicable) and The Author( [打印本頁] 作者: Taylor 時(shí)間: 2025-3-21 16:25
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作者: Cognizance 時(shí)間: 2025-3-21 21:34 作者: 溫和女人 時(shí)間: 2025-3-22 00:50 作者: mosque 時(shí)間: 2025-3-22 06:15
An Illustration of the Boundary Element Approach,several examples are worked to demonstrate the accuracy of the methods. The two boundary element methods in this chapter are called ., because the sources . and . are generally not physically meaningful. It is shown that the methods can also be viewed as numerical representations of integral expressions for single and double layer potentials.作者: 隱士 時(shí)間: 2025-3-22 10:48 作者: glowing 時(shí)間: 2025-3-22 13:24 作者: ensemble 時(shí)間: 2025-3-22 17:16
Elasticity,, as well as limit values for the displacement formula for two dimensions for the case that .. When the boundary . represents a crack, comparable formulas are developed for the displacements, stresses, and tractions at a point . inside . in terms of the displacement discontinuities along the crack. These formulas are attributed to Volterra.作者: 出汗 時(shí)間: 2025-3-22 23:33 作者: 規(guī)章 時(shí)間: 2025-3-23 02:59 作者: Lipoma 時(shí)間: 2025-3-23 08:58
Potential Theory, terms of single and double layer potentials with density functions equal to (a) the normal derivative of the potential on . and (b) the potential on the same boundary. Expressions are also given for the gradient and normal derivative of the potential . at points . inside region ., as well as limit values of all expressions for the case that ..作者: 雄辯 時(shí)間: 2025-3-23 10:28 作者: 激勵(lì) 時(shí)間: 2025-3-23 14:25
Growing Calcite and Other Carbonatesespecially important result is Green’s representation formula, which gives the potential at a point . inside a region ., but not on its boundary ., in terms of single and double layer potentials with density functions equal to (a) the normal derivative of the potential on . and (b) the potential on 作者: FLUSH 時(shí)間: 2025-3-23 20:44
https://doi.org/10.1007/978-1-4757-0471-6at a point inside a region ., but not on its boundary ., in terms of single and double layer potentials with density functions equal to (a) the normal derivative of the potential on . and (b) the potential on the same boundary. For two dimensions, this formula can be discretized by dividing the boun作者: 隱士 時(shí)間: 2025-3-24 01:43 作者: 分開 時(shí)間: 2025-3-24 04:26
G. D. Ilyushin,L. N. Dem’yanetsngth simple source . along a straight line segment in an infinite homogeneous region. Now, however, the source is a stress discontinuity . with components . and ., and superposition of . such sources along a boundary .?leads to a system of 2. algebraic equations in 2. unknowns. Details are provided 作者: medium 時(shí)間: 2025-3-24 06:40
https://doi.org/10.1007/978-1-4613-1141-6t strength dipole source . along a straight?line segment in an infinite homogeneous region. Now, however, the source is a displacement discontinuity . with components . and ., and superposition of . such sources along a boundary . leads to a system of 2. algebraic equations in 2. unknowns. Details a作者: 縱火 時(shí)間: 2025-3-24 11:17
G. D. Ilyushin,L. N. Dem’yanetsgion ., but not on its boundary ., in terms of the counterparts in elasticity for the single and double layer potentials in potential theory with density functions equal to (a) the tractions on .?and (b) the displacements on the same boundary. For two dimensions,?this formula can be discretized by d作者: 卷發(fā) 時(shí)間: 2025-3-24 14:50
Yu. I. Gorina,G. A. Kalyuzhnayastic half-planes. These solutions can be used to generalize?the boundary element methods developed previously for an infinite region to the case of a semi-infinite region with a traction-free boundary. It is also shown how the solution for a concentrated force in an isotropic half-plane can be exten作者: 門閂 時(shí)間: 2025-3-24 19:55 作者: 叫喊 時(shí)間: 2025-3-25 01:51
Mathematical Engineeringhttp://image.papertrans.cn/b/image/167020.jpg作者: thwart 時(shí)間: 2025-3-25 05:47
https://doi.org/10.1007/978-3-031-63341-6Boundary element method textbooks; Single layer potential; Double layer potential; Green’s representati作者: 手術(shù)刀 時(shí)間: 2025-3-25 08:44 作者: FAR 時(shí)間: 2025-3-25 13:25
A First Course in Boundary Element Methods978-3-031-63341-6Series ISSN 2192-4732 Series E-ISSN 2192-4740 作者: 阻塞 時(shí)間: 2025-3-25 18:00
2192-4732 ytical and numerical derivations for isotropic and anisotropic materials, prioritizing simplicity in presentation while progressively advancing towards more intricate mathematical concepts978-3-031-63343-0978-3-031-63341-6Series ISSN 2192-4732 Series E-ISSN 2192-4740 作者: 嘲笑 時(shí)間: 2025-3-25 22:09 作者: Lime石灰 時(shí)間: 2025-3-26 00:16
The Stress Discontinuity Method,the boundary integral representation?of the analogue of the single layer potential for elasticity. Because the stress discontinuities . and . are not in general physically meaningful the stress discontinuity method is an . method.作者: 壓迫 時(shí)間: 2025-3-26 05:09 作者: 情感 時(shí)間: 2025-3-26 08:59
,Extensions and?Refinements,crack tips; and crack growth simulation. Finally, a simplified Galerkin formulation of the displacement discontinuity method is provided?to show how the system of algebraic equations can be written in?terms of the displacement discontinuities at the element endpoints rather than at collocation point作者: 財(cái)產(chǎn) 時(shí)間: 2025-3-26 14:08
Book 2024ary value problems.??Tailored for beginning graduate students, this self-contained textbook offers detailed analytical and numerical derivations for isotropic and anisotropic materials, prioritizing simplicity in presentation while progressively advancing towards more intricate mathematical concepts作者: Euthyroid 時(shí)間: 2025-3-26 18:29 作者: inconceivable 時(shí)間: 2025-3-27 00:50
G. D. Ilyushin,L. N. Dem’yanetsthe boundary integral representation?of the analogue of the single layer potential for elasticity. Because the stress discontinuities . and . are not in general physically meaningful the stress discontinuity method is an . method.作者: faultfinder 時(shí)間: 2025-3-27 04:02
G. D. Ilyushin,L. N. Dem’yanetss are provided for both constant strength elements and straight line elements with piecewise linear approximations?of the boundary parameters, and several examples are worked to demonstrate the accuracy of the approach. The chapter concludes with a discussion of curvilinear isoparametric elements wi作者: jungle 時(shí)間: 2025-3-27 06:06
Yu. I. Gorina,G. A. Kalyuzhnayacrack tips; and crack growth simulation. Finally, a simplified Galerkin formulation of the displacement discontinuity method is provided?to show how the system of algebraic equations can be written in?terms of the displacement discontinuities at the element endpoints rather than at collocation point作者: overhaul 時(shí)間: 2025-3-27 12:47
An Illustration of the Boundary Element Approach,he solution for a constant strength simple source . along a straight line segment in an infinite homogeneous region, and the second on the solution for a constant strength dipole source . along the segment. In both cases, it is assumed that the boundary of the region of interest can be approximated 作者: organism 時(shí)間: 2025-3-27 15:30
Potential Theory,especially important result is Green’s representation formula, which gives the potential at a point . inside a region ., but not on its boundary ., in terms of single and double layer potentials with density functions equal to (a) the normal derivative of the potential on . and (b) the potential on 作者: 商品 時(shí)間: 2025-3-27 21:00 作者: Modicum 時(shí)間: 2025-3-28 01:44
Elasticity,ory. An especially important result is Somigliana’s displacement formula, which gives the displacements at a point . inside a region ., but not on its boundary ., in terms of the counterparts in elasticity for the single and double layer potentials in potential theory with density functions equal to作者: BAIT 時(shí)間: 2025-3-28 02:55 作者: delegate 時(shí)間: 2025-3-28 07:06 作者: albuminuria 時(shí)間: 2025-3-28 12:53
,The Direct Boundary Integral Method for?Elasticity,gion ., but not on its boundary ., in terms of the counterparts in elasticity for the single and double layer potentials in potential theory with density functions equal to (a) the tractions on .?and (b) the displacements on the same boundary. For two dimensions,?this formula can be discretized by d作者: 梯田 時(shí)間: 2025-3-28 16:14
,Extensions and?Refinements,stic half-planes. These solutions can be used to generalize?the boundary element methods developed previously for an infinite region to the case of a semi-infinite region with a traction-free boundary. It is also shown how the solution for a concentrated force in an isotropic half-plane can be exten作者: conjunctiva 時(shí)間: 2025-3-28 21:07
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