Titlebook: Topographic Waves in Channels and Lakes on the f-Plane; Thomas Stocker,Kolumban Hutter Textbook 1987 Springer-Verlag Berlin Heidelberg 198

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EWE

Thomas Stocker,Kolumban Hutterctures and applications‘. It appears somewhat later than is perhaps desirable for a volume resulting from a summer school. In return it contains a good many results which were not yet available at the time of the meeting. In particular it is now abundantly clear that the Deformation theory of algebr

landmark

Thomas Stocker,Kolumban Hutterlic loading under uniaxial tension-compression and standard temperature is used to identify some features and dissimilarities of isotropic and anisotropic hardening processes that occur during monotonic and cyclic loading. In order to describe these features in terms of the plasticity theory (the Bo

Abnormal

arabesque

Thomas Stocker,Kolumban Huttermaterial science.Describes structure-property relationships .This book describes the properties of single polymer molecules and polymeric materials and the methods how to characterize them. Molar masses, molar mass distributions and branching structure are discussed in detail. These properties are d

lobster

Entirety

Thomas Stocker,Kolumban Hutterntitative description of the toughness behaviour by means of fracture mechan- ics parameters and enables preventive failure analysis. In recent years this young scientific discipline has developed rapidly, and now the experimental results are looking for more applications in industrial practice. How

Nefarious

Thomas Stocker,Kolumban Hutterm polyethylene single crystals. The observations by transmission electron microscopy and electron diffraction indicate that substrate-free polyethylene crystals fail by brittle fracture at all temperatures between 77 K and 388 K and all strain rates between 10. and 10. sec.. The formation of fibers

出汗

following the last deglaciation. As a measure of this variation, sea-level indicators (SLIs) related to the RSL heights at specific past time epochs are used. For the inversion of the RSL-height change in terms of mantle viscosity, neighbouring SLIs may be grouped into an RSL diagram taken as repre

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