Titlebook: IUTAM Symposium on Scaling in Solid Mechanics; Proceedings of the I F.M. Borodich (borodichfm@cardiff.ac.uk) Conference proceedings 2009 Sp

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書目名稱IUTAM Symposium on Scaling in Solid Mechanics影響因子(影響力)




書目名稱IUTAM Symposium on Scaling in Solid Mechanics影響因子(影響力)學(xué)科排名




書目名稱IUTAM Symposium on Scaling in Solid Mechanics網(wǎng)絡(luò)公開(kāi)度




書目名稱IUTAM Symposium on Scaling in Solid Mechanics網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書目名稱IUTAM Symposium on Scaling in Solid Mechanics被引頻次




書目名稱IUTAM Symposium on Scaling in Solid Mechanics被引頻次學(xué)科排名




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書目名稱IUTAM Symposium on Scaling in Solid Mechanics年度引用學(xué)科排名




書目名稱IUTAM Symposium on Scaling in Solid Mechanics讀者反饋




書目名稱IUTAM Symposium on Scaling in Solid Mechanics讀者反饋學(xué)科排名

Recess

Scaling Transformations in Solid Mechanics,ricted to just the equivalence of dimensionless parameters characterising the problem under consideration. A wealth of scaling approaches to solid mechanics is demonstrated on problems of contact and fracture mechanics. It is considered dimensional analysis and classic self-similarity, solutions des

malapropism

Expurgate

Mumble

打擊

nonchalance

Internal Variables and Scale Separation in Dynamics of Microstructured Solids,omomentum cannot be separated by means of the scale separation because these equations should concern all fields together and, therefore, all scales together. However, the intrinsic interaction force requires a kinetic relation for internal variables. This kinetic relation depends on representation

prosperity

On Rational Boundary Conditions for Higher-Order Long-Wave Models,ed by underlying micro-structure. Since such models feature higher spatial derivatives, one needs to formulate additional boundary conditions when confined to bounded domains. There is a certain controversy associated with these boundary conditions, because it does not seem possible to justify their

Atrium

vibrant

Space and Time Scaling Laws Induced by the Multiscale Fracturing of The Arctic Sea Ice Cover,amics characterized by temporal and spatial scaling laws, a vision at odds with the classical smooth, fluid-like modelling framework of the sea ice cover. We propose here a simple multiscale fracturing model that explains the observed scaling properties of the deformation fields from the fractal pro