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Titlebook: Very Slow Flows of Solids; Basics of Modeling i Louis A. Lliboutry Book 1987 Martinus Nijhoff Publishers, Dordrecht 1987 Deformation.contin

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書目名稱Very Slow Flows of Solids
副標(biāo)題Basics of Modeling i
編輯Louis A. Lliboutry
視頻videohttp://file.papertrans.cn/983/982616/982616.mp4
叢書名稱Mechanics of Fluids and Transport Processes
圖書封面Titlebook: Very Slow Flows of Solids; Basics of Modeling i Louis A. Lliboutry Book 1987 Martinus Nijhoff Publishers, Dordrecht 1987 Deformation.contin
描述This book is written primarily for Earth scientists faced with problems in thermo- mechanics such as the flow and evolution of ice-sheets, convection currents in the mantle, isostatic rebound, folding of strata or collapse of cavities in salt domes. Failure, faults, seismic waves and all processes involving inertial terms will not be dealt with. In general such scientists (graduate students beginning a Ph. D. for instance) have too small a background‘in continuum mechanics and in numerical computation to model conveniently these problems, which are not elementary at all. Most of them are not linear, and therefore seldom dealt with in treatises. If the study of reality were clearly cut into two successive steps: first to make a physical model, setting up a well-posed problem in thermo-mechanics, and second to solve it, the obvious solution would be to find a specialist in computational mechanics who could spend enough time on a problem which, although maybe crucial for on-going fundamental research, has little practical interest in general, and cannot be considered properly as a noteworthy progress in Mechanics. But this is not the way Science develops. There is a continuous dialect
出版日期Book 1987
關(guān)鍵詞Deformation; continuum mechanics; dynamics; elasticity; finite element method; geodynamics; matrix; mechani
版次1
doihttps://doi.org/10.1007/978-94-009-3563-1
isbn_softcover978-94-010-8094-1
isbn_ebook978-94-009-3563-1Series ISSN 0921-3805
issn_series 0921-3805
copyrightMartinus Nijhoff Publishers, Dordrecht 1987
The information of publication is updating

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Diffusion and advection of heat with a single space variable,emperature and pressure. The thermal conductivity is assumed to be isotropic, an assumption which, even in the case of very anisotropic rocks, is not too bad. The temperature at a point with fixed coordinates is .(., ., ., .). The heat transfered by conductivity per unit time (in Js.m., in S.I. unit
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Microscopic processes of creep,ope, with simple crystallographic nets: close-packed hexagonal as Mg, Zn, Ti; face-centered cubic (which is another close-packed structure for a set of spherical atoms), as Al, Cu, Ni; or body-centered cubic as Fe (below 911oC), Cr, W. The macroscopic behavior of metals will allow us to define some
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Viscoelasticity and transient creep,troduced. The principle of local action (Section 5.1) will always be assumed. Therefore, the constitutive relationship involves the values at some material point of the diverse variables and of their space derivatives of low order only. Nevertheless, it may include not only the actual values, but th
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