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Titlebook: Low Reynolds number hydrodynamics; with special applica John Happel,Howard Brenner Book 1983 Martinus Nijhoff Publishers, The Hague 1983 dy

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樓主: cerebral-cortex
31#
發(fā)表于 2025-3-26 22:58:50 | 只看該作者
32#
發(fā)表于 2025-3-27 04:04:19 | 只看該作者
The Motion of a Rigid Particle of Arbitrary Shape in an Unbounded Fluid, symmetry requires that the hydrodynamic force on the particle be parallel to its direction of motion. Before proceeding to other cases, where it is impossible to take advantage of such symmetry, it is appropriate to investigate the effect of particle orientation on resistance in a general way. This
33#
發(fā)表于 2025-3-27 07:00:32 | 只看該作者
Interaction between Two, or More Particles,nal forces, typically gravity. The particles are supposed sufficiently close to interact hydrodynamically. It is assumed that the particles are sufficiently distant from boundary walls for the surrounding fluid to be regarded as unbounded. Attention will be predominantly directed to situations where
34#
發(fā)表于 2025-3-27 11:01:12 | 只看該作者
35#
發(fā)表于 2025-3-27 15:01:50 | 只看該作者
36#
發(fā)表于 2025-3-27 21:22:00 | 只看該作者
d: over 100 illustrations, including about 15 maps in colour.The Landforms and Landscapes of France provides an informative and attractive overview of the most scenic landscapes of France. The geodiversity of France is emphasized, for example the glacial landscapes of the Mont-Blanc Massif, the volc
37#
發(fā)表于 2025-3-28 00:39:18 | 只看該作者
John Happel,Howard Brennerd: over 100 illustrations, including about 15 maps in colour.The Landforms and Landscapes of France provides an informative and attractive overview of the most scenic landscapes of France. The geodiversity of France is emphasized, for example the glacial landscapes of the Mont-Blanc Massif, the volc
38#
發(fā)表于 2025-3-28 03:27:43 | 只看該作者
39#
發(fā)表于 2025-3-28 08:03:04 | 只看該作者
40#
發(fā)表于 2025-3-28 13:15:29 | 只看該作者
John Happel,Howard Brennerraphy have taken shape from the Late Paleozoic to modern times. A uniform basement of the basin was amalgamated from terranes of different origin as late as in the Middle Miocene. Accordingly, older landforms had been created on either the European or the African plate, while since the Miocene geomo
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