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Knowing something of the gestation of these papers, I for one will be
very interested to see the ensuing debate.

Roger Musson

British Geological Survey
West Mains Road
Edinburgh EH9 3LA

tel: +44 (0)131-650-0205
fax: +44 (0)131-667-1877 

> -----Original Message-----
> From: Tectonics & structural geology discussion list 
> [mailto:[log in to unmask]] On Behalf Of Falk H. Koenemann
> Sent: 26 May 2008 18:24
> To: [log in to unmask]
> Subject: stress news
> 
> Hi folks, 
> 
> today I have been informed by the chief editor of the 
> 'International Journal of Modern Physics B' that three papers 
> have been accepted for publication at once: 
> 
> ON THE SYSTEMATICS OF ENERGETIC TERMS IN CONTINUUM MECHANICS, 
> AND A NOTE ON GIBBS (1877) (date of acceptance May 24)
> 
> POTENTIAL THEORY AND ELASTICITY: A COMMENT ON GURTIN (1972) (May 24)
> 
> AN APPROACH TO DEFORMATION THEORY BASED ON THERMODYNAMIC 
> PRINCIPLES (May 6)
> 
> 
> Abstract of 'Systematics & Gibbs': 
> The systematics of energetic terms as they are taught in 
> continuum mechanics deviate seriously from standard views in 
> physics, resulting in a profound misconception. It is 
> demonstrated that the First Law of Thermodynamics has been 
> routinely re-interpreted in a sense that would make it 
> subordinate to Bernoulli's energy conservation law.
> Furthermore, it is shown that the attempt by Gibbs to find a 
> thermodynamic understanding for elastic deformation does not 
> sufficiently account for all the energetic properties of such 
> a process. 
> 
> 
> Abstract of 'Gurtin': 
> In an exhaustive presentation of the linear theory of 
> elasticity by Gurtin (1972) the author included a chapter on 
> the relation of the theory of elasticity to the theory of 
> potentials. Potential theory distinguishes two fundamental 
> physical categories: divergence-free and divergence-involving 
> problems. From the criteria given in the source quoted by the 
> author it is evident that elastic deformation of solids falls 
> into the latter category. It is documented in this short note 
> that the author presented volume-constant elastic deformation 
> as a divergence-free physical process, systematically 
> ignoring all the information that was available to him that 
> this is not so. 
> 
> In plain English: the guy cheated. He misled an entire 
> generation of scientists. 
> 
> 
> Abstract of 'Approach':
> The Cauchy stress theory has been shown to be profoundly at 
> variance with the principles of the theory of potentials. 
> Thus, a new physical approach to deformation theory is 
> presented which is based on the balance of externally applied 
> forces and material forces. The equation of state is 
> generalized to apply to solids, and transformed into vector 
> form. By taking the derivatives of an external potential and 
> the material internal energy with respect to the coordinates, 
> two vector fields are defined for the forces exerted by 
> surrounding at the system, subject to the boundary 
> conditions, and vice versa, subject to the material 
> properties. These vector fields are then merged into a third 
> one that represents the properties of the loaded state. 
> Through the work function the force field is then directly 
> transformed into the displacement field. The approach permits 
> fully satisfactory prediction of all geometric and energetic 
> properties of elastic and plastic simple shear. It predicts 
> the existence of a bifurcation at the transition from 
> reversible to irreversible behavior whose properties permit 
> correct prediction of cracks in solids. It also offers a 
> mechanism for the generation of sheath folds in plastic shear 
> zones and for turbulence in viscous flow. Finally, an example 
> is given how to apply the new approach to deformation of a 
> discrete sample as a function of loading configuration and 
> sample shape.
> 
> 
> Phenomena for which my approach delivers fully satisfactory 
> predictions are: 
> - S-C fabrics in mylonites,
> - elastic-reversible dilatancy,
> - orientation of joints in rocks,
> - properties of microfabric diagrams for minerals with
>   simple geometric properties,
> - the energetics of elastic and plastic pure shear and
>   simple shear
>   deformation, as they are known from experiments,
> - the observed orientation of the regional stress field
>   in California around the San Andreas Fault,
> - turbulence in viscous flow,
> - generation of sheath folds in plastic shear zones,
> - generation of cracks in brittle deformation. 
> 
> 
> 
> Delivery of the three papers in paper print is scheduled for 
> July. The PDF files can be downloaded from my website, 
> 
> www.elastic-plastic.de
> 
> 
> Concerning the work done so far, based on Hooke, Euler, 
> Cauchy, Navier-Stokes, Prandtl-Reuss, Taylor-Bishop-Hill - It 
> is going to be a spectacle like the Hindenburg at Lakehurst. 
> No regrets. 
> 
> 
> Falk Koenemann
> Aachen, Germany
> 
> -- 
> 
> .___________________________________________________________________
> |  Dr. Falk H. Koenemann                           Aachen, Germany  |
> |                                                                   |
> |  Email: [log in to unmask]               Phone: *49-241-75885  |
> |-------------------------------------------------------------------|
> |                     www.elastic-plastic.de                        |
> |___________________________________________________________________|
> 
> 

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